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Journal of Applied Science Studies - Ozean Publications

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Volume 3, Issue 1<br />

March 2010<br />

Spectra out <strong>of</strong> Oxygen and Ozone in Dielectric Barrier<br />

Discharge.<br />

M. A. HASSOUBA and N. DAWOOD<br />

Extension Mechanisms Influencing The Adoption Of Sprinkler<br />

Irrigation System In Iran<br />

SEYED JAMAL F.HOSSEINI, YOSRA KHORSAND and SHABALDEEN<br />

SHOKRI<br />

Geoelectric Assessment Of Groundwater Prospect And<br />

Vulnerability Of Overburden Aquifers At Idanre, Southwestern<br />

Nigeria<br />

OMOSUYI, G.O.<br />

Comparative vegetative and foliar epidermal features <strong>of</strong> three<br />

Paspalum L. species in Edostate, Nigeria.<br />

E.A OGIE-ODIA, A.I MOKWENYE, O. KEKERE and O. TIMOTHY<br />

Digital Moulding <strong>of</strong> the Solicitations within the Dielectric <strong>of</strong><br />

the Transformers and the Evaluation <strong>of</strong> Life Cycle <strong>of</strong> the<br />

Insulation Systems<br />

MARIUS-CONSTANTIN POPESCU and CRISTINEL POPESCU<br />

A disconnect congestion detection from TCP to improve the<br />

robustness<br />

ISSA KAMAR and SEIFEDDINE KADRY<br />

Analysis Of Microwave Signal Reception Using Finite<br />

Difference Implementation. (A Case Study Of Akure – Owo<br />

Digital Microwave Link In South Western Nigeria)<br />

OTASOWIE P.O and UBEKU E.U.<br />

Estimation <strong>of</strong> C factor for soil erosion modeling using NDVI in<br />

Buyukcekmece watershed<br />

AHMET KARABURUN<br />

<strong>Journal</strong> <strong>of</strong><br />

<strong>Applied</strong> <strong>Science</strong><br />

Physiological properties studies on essential oil <strong>of</strong> Jasminum<br />

grandiflorum L. as affected by some vitamins<br />

RAWIA.A.EID, LOBNA, S. TAHA and SOAD , M.M. IBRAHIM<br />

Effect <strong>of</strong> zinc and / or iron foliar application on growth and<br />

essential oil <strong>of</strong> sweet basil (Ocimum basilicum L.) under salt<br />

stress<br />

H.A.H. SAID-AL AHL and ABEER A. MAHMOUD<br />

Growth and yield <strong>of</strong> Foeniculum vulgare var.azoricum as<br />

influenced by some vitamins and amino acids<br />

S.F. HENDAWY and AZZA A.EZZ EL-DIN<br />

Effect <strong>of</strong> water stress and potassium humate on the<br />

productivity <strong>of</strong> oregano plant using saline and fresh water<br />

irrigation<br />

H.A.H. SAID-AL AHL and M.S. HUSSEIN<br />

Influence <strong>of</strong> Foliar Application <strong>of</strong> Pepton on Growth, Flowering<br />

and Chemical Composition <strong>of</strong> Helichrysum bracteatum Plants<br />

under Different Irrigation Intervals.<br />

SOAD , M.M. IBRAHIM, LOBNA, S. TAHA and M.M. FARAHAT<br />

Permeability and Porosity Prediction from Wireline logs Using<br />

Neuro-Fuzzy Technique<br />

WAFAA EL-SHAHAT AFIFY and ALAA H. IBRAHIM HASSAN<br />

Response <strong>of</strong> vegetative growth and chemical constituents <strong>of</strong><br />

Schefflera arboricola L. plant to foliar application <strong>of</strong> inorganic<br />

fertilizer (grow-more) and ammonium nitrate at Nubaria.<br />

MONA, H. MAHGOUB, EL-QUESNI, FATMA E.M. and MAGDA,M.<br />

KANDIL<br />

Statistical Modelling For Outlier Factors<br />

Ahmet KAYA


OZEAN JOURNAL <strong>of</strong><br />

APPLIED SCIENCE<br />

A PEER REVIEVED INTERNATIONAL JOURNAL<br />

----------------------------------------------------------------------------------------------------------------------------------------------<br />

Volume 3, Issue 1, March 2010<br />

ONLINE ISSN 1943-2542 PRINTED ISSN: 1943-2429<br />

----------------------------------------------------------------------------------------------------------------------------------------------<br />

Gerald S. Greenberg, Ohio State University, USA<br />

Hakki Yazici, Afyon Kocatepe University, Turkey<br />

Hayati Akyol, Gazi University, Turkey<br />

Hayati Doganay, Ataturk University, Turkey<br />

Laurie Katz, Ohio State University, USA<br />

Lisandra Pedraza, University <strong>of</strong> Puerto Rico in<br />

Rio Piedras, Puerto Rico<br />

Lutfi Ozav, Usak University, Turkey<br />

Managing Editor<br />

Ali Ozel, Dumlupinar University<br />

Publication Coordinator<br />

Taskin Inan, Dumlupinar University<br />

Editorial Board<br />

Mihai Maxim, Bucharest University, Romania<br />

Ibrahim Atalay, Dokuz Eylul University, Turkey<br />

Ibrahim S. Rahim, National Research Center, Egypt<br />

Janet Rivera, NOVA University, USA<br />

Ramazan Ozey, Marmara University, Turkey<br />

Samara Madrid, Northern Illinois University, USA<br />

Samia Abdel Aziz-Ahmed Sayed, National Research<br />

Center, Egypt<br />

Web: http://www.ozelacademy.com E-mail: editorejes@gmail.com<br />

Copyright © 2008 <strong>Ozean</strong> Publication, 2141 Baneberry Ct. 43235, Columbus, Ohio, USA


<strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

OZEAN JOURNAL <strong>of</strong><br />

APPLIED SCIENCE<br />

A PEER REVIEVED INTERNATIONAL JOURNAL<br />

---------------------------------------------------------------------------------------------------------------------------------<br />

Volume 3, Issue 1, March 2010<br />

ONLINE ISSN 1943-2542 PRINTED ISSN: 1943-2429<br />

---------------------------------------------------------------------------------------------------------------------------------<br />

Spectra out <strong>of</strong> Oxygen and Ozone in Dielectric Barrier Discharge.<br />

M. A. HASSOUBA and N. DAWOOD<br />

Extension Mechanisms Influencing The Adoption Of Sprinkler Irrigation System In Iran<br />

SEYED JAMAL F.HOSSEINI, YOSRA KHORSAND and SHABALDEEN SHOKRI<br />

Geoelectric Assessment Of Groundwater Prospect And Vulnerability Of Overburden Aquifers At<br />

Idanre, Southwestern Nigeria<br />

OMOSUYI, G.O.<br />

Comparative vegetative and foliar epidermal features <strong>of</strong> three Paspalum L. species in Edostate,<br />

Nigeria.<br />

E.A OGIE-ODIA, A.I MOKWENYE, O. KEKERE and O. TIMOTHY<br />

Digital Moulding <strong>of</strong> the Solicitations within the Dielectric <strong>of</strong> the Transformers and the Evaluation <strong>of</strong><br />

Life Cycle <strong>of</strong> the Insulation Systems<br />

MARIUS-CONSTANTIN POPESCU and CRISTINEL POPESCU<br />

A disconnect congestion detection from TCP to improve the robustness<br />

ISSA KAMAR and SEIFEDDINE KADRY<br />

Analysis Of Microwave Signal Reception Using Finite Difference Implementation. (A Case Study Of<br />

Akure – Owo Digital Microwave Link In South Western Nigeria)<br />

OTASOWIE P.O and UBEKU E.U.<br />

Estimation <strong>of</strong> C factor for soil erosion modeling using NDVI in Buyukcekmece watershed<br />

AHMET KARABURUN<br />

Physiological properties studies on essential oil <strong>of</strong> Jasminum grandiflorum L. as affected by some<br />

vitamins<br />

RAWIA.A.EID, LOBNA, S. TAHA and SOAD , M.M. IBRAHIM<br />

Effect <strong>of</strong> zinc and / or iron foliar application on growth and essential oil <strong>of</strong> sweet basil (Ocimum<br />

basilicum L.) under salt stress<br />

H.A.H. SAID-AL AHL and ABEER A. MAHMOUD<br />

Growth and yield <strong>of</strong> Foeniculum vulgare var.azoricum as influenced by some vitamins and amino<br />

acids<br />

S.F. HENDAWY and AZZA A.EZZ EL-DIN


<strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Effect <strong>of</strong> water stress and potassium humate on the productivity <strong>of</strong> oregano plant using saline and<br />

fresh water irrigation<br />

H.A.H. SAID-AL AHL and M.S. HUSSEIN<br />

Influence <strong>of</strong> Foliar Application <strong>of</strong> Pepton on Growth, Flowering and Chemical Composition <strong>of</strong><br />

Helichrysum bracteatum Plants under Different Irrigation Intervals.<br />

SOAD , M.M. IBRAHIM, LOBNA, S. TAHA and M.M. FARAHAT<br />

Permeability and Porosity Prediction from Wireline logs Using Neuro-Fuzzy Technique<br />

WAFAA EL-SHAHAT AFIFY and ALAA H. IBRAHIM HASSAN<br />

Response <strong>of</strong> vegetative growth and chemical constituents <strong>of</strong> Schefflera arboricola L. plant to foliar<br />

application <strong>of</strong> inorganic fertilizer (grow-more) and ammonium nitrate at Nubaria.<br />

MONA, H. MAHGOUB, EL-QUESNI, FATMA E.M. and MAGDA,M. KANDIL<br />

Statistical Modelling For Outlier Factors<br />

Ahmet Kaya<br />

Web: http://www.ozelacademy.com E-mail: editorejes@gmail.com<br />

Copyright © 2008 <strong>Ozean</strong> Publication, 2141 Baneberry Ct. 43235, Columbus, Ohio, USA<br />

A peer revieved international journal<br />

ONLINE ISSN 1943-2542 PRINTED ISSN: 1943-2429<br />

http://ozelacademy.com/ojas.htm


<strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

Spectra out <strong>of</strong> Oxygen and Ozone<br />

in Dielectric Barrier Discharge.<br />

M. A. Hassouba* and N. Dawood<br />

<strong>Applied</strong> Physics Dept., Faculty <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s, Taibah Univ., KSA.<br />

*E-mail address for correspondence: hassouba@yahoo.com<br />

________________________________________________________________________________________<br />

Abstract: Dielectric-barrier discharges (DBD) are very attractive for industrial applications because they can<br />

provide nonequilibrium plasma conditions at about atmospheric pressure. DBD is an excellent source <strong>of</strong> ideal<br />

energetic electrons with 1–10 eV and high density. Its unique advantageous is to generate low excited atomic<br />

and molecular species, free radicals and excimers with several electron volt energy.Spectra out <strong>of</strong> ozone<br />

synthesis system, in dielectric barrier discharge (DBD) using oxygen gas, have been detected in the range <strong>of</strong> 300<br />

to 400 nm. The dependence <strong>of</strong> spectral intensity on the discharge voltage and the oxygen pressure has been<br />

studied. The half-width <strong>of</strong> the detected lines was found to be within 20 A o approximately. Spectroscopic<br />

technique is a well-known technique for the measurement <strong>of</strong> the mean electron temperature in the gas discharge.<br />

The electron temperature within the microdischarge has been estimated by using the relative intensity <strong>of</strong> the line<br />

to line ratio technique <strong>of</strong> the identified spectral lines. An average mean electron temperature <strong>of</strong> 3.6 eV was<br />

obtained and it has been found to be insensitive to the gas pressure variation.<br />

Key Words:- Dielectric Barrier Discharge, Ozone Spectra, Electron Temperature<br />

measurements ,Plasma Spectroscopic Models.<br />

__________________________________________________________________________________________<br />

INTRODUCTION<br />

Dielectric-barrier discharges (silent discharges) combine the ease <strong>of</strong> atmospheric pressure operation with<br />

nonequilibrium plasma conditions suited for many plasma chemical processes. In most gases at this pressure the<br />

discharge consists <strong>of</strong> a large number <strong>of</strong> randomly distributed short-lived microdischarges.. Traditionally mainly<br />

used for industrial ozone production, dielectric-barrier discharges have found additional large volume<br />

applications in surface treatment, high-power CO2 lasers, excimer ultraviolet lamps, pollution control and, most<br />

recently, also in large-area flat plasma display panels. Future applications may include their use in greenhouse<br />

gas control technologies [1].<br />

Many articles [1-7] have been published about the optical emission from DBDs by using other gases such as Xe,<br />

Cl, Ar, He. The dielectric barrier discharges (silent discharge) <strong>of</strong>fer the possibility <strong>of</strong> building large area and<br />

high intensity UV-sources, for industrial processing.<br />

Burm [8] investigate two plasma sources, an air plasma torch and a nitrogen dielectric barrier discharge. Optical<br />

emission spectroscopy is used to determine the heavy particles and the vibration (electron) temperatures for the<br />

two plasma sources. The two temperatures are measured to obtain an estimation <strong>of</strong> the deviation from local<br />

thermal equilibrium and to compare the two source configurations which are used for surface treatment.<br />

The present work is originally directed toward the design <strong>of</strong> a cheap and simple DBD ozonizer [9]. The spectra<br />

out from this system have been detected and the electron temperature <strong>of</strong> the discharge is determined using the<br />

spectroscopic method.<br />

1


The experiment setup consists <strong>of</strong> two parts<br />

1- Discharge Cell<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

EXPERIMENTAL SETUP<br />

In the present work, the cell <strong>of</strong> the discharge consists <strong>of</strong> coaxial electrodes. The inner electrode has been made <strong>of</strong><br />

brass rod with radii 0.5 cm. The outer electrode is made <strong>of</strong> graphite coated on the outer wall <strong>of</strong> a Silica glass<br />

tube, which has been used as a dielectric material and as a window for the study output radiation <strong>of</strong> the system.<br />

The gap space between the inner electrode and the inner wall <strong>of</strong> glass tube was 0.175 cm. The length <strong>of</strong> the<br />

reactor region was 30 cm and the pressure <strong>of</strong> gas could be controlled by the needle valves, which enable<br />

controlling the flow rate in the system. The pressure inside the discharge tube was measured by using manometer<br />

and gauge model P200-H (RS-497-606) which enables the pressure to be measured in the range from 1 to 2.25<br />

bars within 1 mbar experimental error. The flow rate <strong>of</strong> oxygen (98.7% purity) has been measured by using a<br />

flow meter (Cole Parmer). Figure (1) shows the present DBD system.<br />

The electric circuit <strong>of</strong> the discharge is also shown in Fig. (1) which consists <strong>of</strong> AC power supply (0�220 V , 50<br />

Hz) connected to a high voltage transformer with a variable output, 0�20 kV. In order to measure the applied<br />

potential across the discharge cell, a potential divider has been built, which consists <strong>of</strong> two resistors in the ratio<br />

<strong>of</strong> (1/450) connected in parallel with the discharge cell. Only the potential difference across the lower part <strong>of</strong> the<br />

divider is measured, and then the actual applied potential across the cell can be estimated.<br />

2- The Spectroscopic Setup<br />

Figure (2) shows the present spectroscopic setup, which is controlled by PC computer. The spectroscopic<br />

devices <strong>of</strong> type Oriel, consists <strong>of</strong> mono-chromator 25 cm path length and has a diffraction grating <strong>of</strong> 1200<br />

mm. The relative intensity <strong>of</strong> lines has been measured by using photo-multiplier (PMT) capable <strong>of</strong> measuring the<br />

spectra in the range <strong>of</strong> 185–650 nm. PMT connect to readout system for reading the intensity <strong>of</strong> light, the readout<br />

capable <strong>of</strong> current amplification up to 10 9 A. PC computer with interface and stepper motor driver has been used<br />

to control in the motion <strong>of</strong> the grating, so that it enables to variation <strong>of</strong> the wavelength one angstrom by step.<br />

1- Spectra <strong>of</strong> Oxygen in Silent Discharge<br />

RESULTS AND DISCUSSION<br />

The only detectable spectra have been found in the region from 300 to 400 nm. The absorption cross section <strong>of</strong><br />

ozone is known to be high in two ranges; Hartly band; 160 - 320 nm and Chappuis band; 420-730 nm [10].<br />

Therefore, no spectra emission could be seen or measured in these two ranges.<br />

Typical spectrums <strong>of</strong> DBD at different pressure and discharge voltages are shown in Figs. (3-a, b and c).<br />

It is noticed that, the emitted lines could not be detected until the applied potential reached the onset potential<br />

where the ozone starts to build up, which depends on the working gas pressure p, inner electrode distance d and<br />

the type <strong>of</strong> the dielectric material and its thickness T.<br />

e= e/d =<br />

constant * V/p), where q is the electron charge, V is the applied voltage, d is the gap space distance between the<br />

e is the mean free path <strong>of</strong> the electrons.<br />

Figure (4) shows a typical graph for the present relation between (VB) and (p*d) in oxygen (right hand side <strong>of</strong> the<br />

Paschen Curve) under the given conditions where VB is increasing linearly with (p*d). Also as a ozone<br />

composition is a chemical reaction it is therefore the current is the main parameter which controls the number <strong>of</strong><br />

ozone reactions that take place in this system. Figure (5) shows the relation between the voltage and the current<br />

flowing in the system at different gas pressures.<br />

2


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

When the pressure is kept constant the mean free path is constant but if the applied voltage is increased, the<br />

number <strong>of</strong> electrons capable on excitation and ionization increases. Therefore, it is expected in this case that the<br />

intensity <strong>of</strong> the emitted lines will increase with the applied potential, [at p=1.25 bar]. Also, when the pressure<br />

increases the collision frequency increases, therefore the intensity <strong>of</strong> the emitted lines increases.<br />

It can be noticed that the half width <strong>of</strong> any <strong>of</strong> these lines is less than 2 nm, which could be, used more or less as a<br />

monochromatic radiation [10]. Such radiation could be easily generated on a large scale for the purpose <strong>of</strong><br />

industrial applications [11].<br />

2- Mean Electron Temperature.<br />

Spectroscopic technique is a well-known technique for the measurement <strong>of</strong> the mean electron temperature in the<br />

gas discharge.<br />

In the present work not all the radiation lines has been identified, although pure oxygen <strong>of</strong> 98.7% purity has<br />

been used and unfortunately only few lines <strong>of</strong> them has been identified and were therefore used for the deriving<br />

<strong>of</strong> the electron temperature.<br />

The line to line relative intensity ratio technique (for the same ionization stage) is used to determine the<br />

mean electron temperature, Te, in silent discharge, according to the following equation [11]:-<br />

Where: -<br />

K is the Boltzmann`s constant, Te is the mean electron temperature, I, I’ are the relative intensity <strong>of</strong> the two<br />

given lines, �, � ` are the wavelengths <strong>of</strong> two lines, g, g ` are the statistical weight <strong>of</strong> two lines, f, f ` are the<br />

oscillator strength <strong>of</strong> two lines, E` is the excitation energy for the higher ionization stage and E is the excitation<br />

energy for the lower ionization stage. The lines identified are <strong>of</strong> the wavelengths tabulated in Table (1), together<br />

with their values <strong>of</strong> the above parameters [11]. The intensities <strong>of</strong> the identified lines were taken from the<br />

measured discharge spectra in Fig. (3).<br />

Wavelength (�)<br />

A o<br />

'<br />

(E � E)<br />

KTe<br />

�<br />

3 ' '<br />

I�<br />

g f<br />

ln( )<br />

' 3<br />

I � gf<br />

Table (1) The parameters <strong>of</strong> the selected lines used in the calculation.<br />

Excitation<br />

Energy (E)<br />

Oscillator<br />

Strength (f)<br />

3<br />

Statistical<br />

Weight (g)<br />

Product <strong>of</strong><br />

(f) x (g)<br />

3709.5 45.07 eV 0.0747 1 0.0747<br />

3754.7 36.29 eV 0.277 5 1.385<br />

3911.96 28.71 eV 0.0326 4 0.130<br />

3945 26.45 eV 0.113 4 0.452<br />

In order to derive the mean electron temperature from the above equation two couples <strong>of</strong> lines have to be chosen<br />

so that their wavelengths are very near to each other, and from the same stage <strong>of</strong> ionization.<br />

The parameters <strong>of</strong> these couples <strong>of</strong> lines were substituted in the equation and hence the mean electron<br />

temperature was calculated and has been tabulated below.<br />

The results for the couple <strong>of</strong> lines <strong>of</strong> wavelengths 391.19 nm and 394.5 nm emitted from O + are shown in Table<br />

(2). Also, the results <strong>of</strong> the couple <strong>of</strong> lines <strong>of</strong> wavelengths 370.95 nm and 375.47 nm, which emitted from O ++<br />

are shown in Table (2).


Pressure<br />

(bar)<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table (2) Shows the results for the couple <strong>of</strong> lines <strong>of</strong> wavelengths 391.19 nm<br />

and 394.5 nm emitted from O + at different conditions.<br />

Lines 391.19 nm and 394.5 nm Lines 370.9 nm and 375.47 nm<br />

V (dis.)<br />

18 kV<br />

Electron<br />

Temp.(Te)<br />

V(dis.)<br />

13.5 kV<br />

Electron<br />

Temp.(Te)<br />

4<br />

V (dis.)<br />

18 kV<br />

Electron<br />

Temp. (Te)<br />

V(dis.)<br />

13.5 kV<br />

Electron<br />

Temp. (Te)<br />

1.005 3.77 eV 3.6 eV 3.8 eV 3.4 eV<br />

1.25 3.6 eV 3.7 eV 3.6 eV 3.2 eV<br />

1.5 3.7 eV 3.7 eV 3.8 eV 3.4 eV<br />

1.75 3.77 eV 3.8 eV 3.85 eV 3.4 eV<br />

The mean electron temperature has been drawn as a function <strong>of</strong> gas pressure and applied voltage and is shown in<br />

Fig. (6-a, b).<br />

It can be noticed from Fig. (6-a, b) that the mean electron temperature in the dielectric barrier discharge is nearly<br />

constant at a mean electron temperature is 3.6 eV and does not depend on the gas pressure.<br />

CONCLUSION<br />

The silent discharge is a non-equilibrium discharge which can be operated up to pressures <strong>of</strong> several bars. It is<br />

industrially used on a large scale for the generation <strong>of</strong> ozone from air or oxygen. Ozone generators have a typical<br />

power consumption ranging from some kilowatts to several megawatts. The main characteristic <strong>of</strong> the silent<br />

discharge is that narrow discharge gaps <strong>of</strong> a few millimeter spacing are used and that at least one <strong>of</strong> the<br />

electrodes is covered by an insulating layer. For this reason the silent discharge is also referred to as the<br />

"dielectric-barrier discharge" (DBD).<br />

The present work is originally directed toward the design <strong>of</strong> a cheap and simple DBD ozonizer.<br />

It is noticed that, the emitted lines could not be detected until the applied potential reached the onset potential<br />

where the ozone starts to build up, which depends on the working gas pressure p, inner electrode distance d and<br />

the type <strong>of</strong> the dielectric material and its thickness T<br />

Spectroscopic technique is a well-known technique for the measurement <strong>of</strong> the mean electron temperature in the<br />

gas discharge.<br />

It is concluded that, that the mean electron temperature in the dielectric barrier discharge is nearly constant at a<br />

mean electron temperature is 3.6 eV and does not depend on the gas pressure.


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

FIGURES<br />

Figure (1) shows the discharge Cell.<br />

PC Computer Steeper Motor<br />

P.S. for PMT<br />

A/D Converter Readout Amp.<br />

Figure (2) shows the spectroscopic setup.<br />

5<br />

PMT<br />

Mono- Plasma<br />

chromator Source


Intensity (Arb. Unit)<br />

Silica<br />

p=1.25 bar<br />

V(dis.)=13.5 KV<br />

300 320 340 360 380 400<br />

Wavelength (nm)<br />

Intensity (Arb. Unit)<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

3<br />

2<br />

2<br />

1<br />

1<br />

CB<br />

BA<br />

0<br />

300 320 340 360 380<br />

Wavelength (nm)<br />

400<br />

6<br />

B<br />

Silica<br />

p.=1.75 bar<br />

V(dis)=18 kV<br />

Figure (3-A, B and C) show the spectra <strong>of</strong> the discharge at different conditions and at T =0.15 cm, d<br />

= 0.175 cm and L = 30 cm.


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Figure (4) shows the relation between V (breakdown) and (pressure*gap space).<br />

Figure (5) shows the relation between I(dis.) and V(dis.) at d=0.175 cm, L=30 cm and<br />

T=0.15 cm<br />

7


Ele.Temp.(eV)<br />

Ele.Temp.(eV)<br />

5<br />

4<br />

3<br />

2<br />

1<br />

0<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

O(++)<br />

3709.5 A<br />

& 3754.7 A<br />

0.75 1.00 1.25 1.50 1.75 2.00<br />

Pressure (bar)<br />

5<br />

4<br />

3<br />

2<br />

1 O(+)<br />

3911.96<br />

0<br />

& 3954.7 A<br />

0.75 1.00 1.25 1.50 1.75 2.00<br />

Pressure (bar)<br />

Figure-(6-A, B) show the Figure relation between (7-a, the b) electron show the temperature relation and between the pressure the at + electron 13.5 and temperature 18.0 KV an<br />

at 13.5 and 18.0 KV<br />

8<br />

BA<br />

AB


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

REFERENCES<br />

A.A.Garamoon, F.F.Elakshar and A.M.Nossair, (1999), GEC 52 nd , Virginia, USA, 324.<br />

A.Baulch, (1980), J. Phys. Chem. Ref. Data, 9, 296.<br />

H.R.Griem, (1964), Plasma Spectroscopy , McGraw-Hill, New York., p.382..<br />

Haile Lei, Yongjian Tang, Jun Li, and Jiangshan Luo, (2007), Appl. Phys. Lett. 91, 113119.<br />

K.G. Kostov; R. Y. Honda; L.M.S. Alves and M.E. Kayama Braz, (2009), J. Phys., 39, 2.<br />

K.T.A. Burm, (2005), Contrib. Plasma Phys., 45, 54.<br />

M.P.Milden, (2001), J. <strong>of</strong> Phys. D: Appl. Phys. 34, L1.<br />

Takaaki Tomai, Tsuyohito Ito and Kazuo Terashima, (2006), Thin Solid Films, 507 , 409.<br />

U.Kogelschatz, (1997), J. de Physique IV, 7, C4-47 to C4-66.<br />

U.Kogelschatz, (1997), ICPIG XXIII, Toulouse, France, 1.<br />

Ulrich Kogelschatz², Baldur Eliasson and Walter Egli, (1999), Pure Appl. Chem., 71, 1819.<br />

Young Sun Mok, (2005), XXVIIth ICPIG, Eindhoven, the Netherlands, 18-22 July, PP. 18.<br />

9


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

Extension mechanisms influencing the adoption <strong>of</strong> sprinkler irrigation system in Iran<br />

Seyed Jamal F.Hosseini*, Yosra Khorsand** and Shabaldeen Shokri***<br />

*Islamic Azad University, <strong>Science</strong> and Research Branch Tehran, Iran<br />

**Islamic Azad University, Birjand branch Birjand, Iran<br />

***Department <strong>of</strong> Agricultural development Islamic Azad University, <strong>Science</strong> and Research Branch<br />

Tehran, Iran<br />

*Email address for correspondence: jamalfhosseini@yahoo.com<br />

__________________________________________________________________________________________<br />

Abstract: Horticultural producers were surveyed in order to explore their perception about the role <strong>of</strong> extension<br />

mechanisms in adopting the sprinkler irrigation system in Iran. The methodology used in this study involved a<br />

combination <strong>of</strong> descriptive and quantitative research. The total population for this study was 150 gardeners who<br />

adopted the sprinkler irrigation system in Chenaran Township in Khorasan Razavi Province. Based on the<br />

results <strong>of</strong> the mean score, respondents indicated that visiting extension agents in the service centers was the<br />

most effective individual extension method main in helping them to adopt the sprinkler irrigation systems. It was<br />

also reported from the findings <strong>of</strong> the study 45% <strong>of</strong> the variance in the perception <strong>of</strong> gardeners about the role <strong>of</strong><br />

extension mechanisms in adopting the sprinkler irrigation systems could be explained by visiting extension<br />

agents in service centers, extension classes, visiting extension agents in the field and visiting sample farm.<br />

Kewords: Extension Mechanisms, Sprinkler Irrigation System, Iran, Gardener.<br />

__________________________________________________________________________________________<br />

INTRODUCTION<br />

World Bank predicted that by the year 2035, three billion people will live in the tough conditions because <strong>of</strong><br />

water shortage (World Bank, 2009). According to the Human Development Report, by the year 2080 climate<br />

change would affect the life <strong>of</strong> many people throughout the world and more than 1.8 billion people would face<br />

water shortages (UNDP, 2007, p.30).<br />

Today, there are several major issues in connection with the water sector in developing and developed countries<br />

which include: water cycle, quality <strong>of</strong> life, equality <strong>of</strong> water, sustainability and human rights (Sohail and Cavill,<br />

2006). In Iran, the policy <strong>of</strong> government has been to increase agricultural production for various reasons, such as<br />

price stability, improved per capita income and increased need for non-oil foreign exchange resources and this<br />

trend has become an unavoidable reality for agricultural sector. Increasing agricultural production has resulted<br />

in consumption <strong>of</strong> more water and there is no other way to change the amount <strong>of</strong> water used which is the<br />

equivalent <strong>of</strong> 130 billion cubic meters a year unless to use water more efficiently and to adopt new methods <strong>of</strong><br />

irrigation.<br />

Consumption <strong>of</strong> water by agriculture sector in Iran has always been an issue <strong>of</strong> concerns which caused by high<br />

water losses in farm fields, farms inappropriate shape and size, lack <strong>of</strong> knowledge <strong>of</strong> farmers about making<br />

optimum use <strong>of</strong> water, rapid destruction <strong>of</strong> water infrastructure, loss in quality <strong>of</strong> irrigation networks,<br />

inappropriate methods <strong>of</strong> irrigation, irrigation efficiency and loss <strong>of</strong> water in irrigation systems (Keshavarz,<br />

2000).<br />

Omani et al (2009) citing Keshavarz, Heydari, and Ashrafi (2003) pointed out that the overall irrigation<br />

efficiency in Iran ranges from 33 to 37%, which is lower than the average for both developing countries (45%)<br />

and developed countries (60%).<br />

11


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Unfortunately, inefficient use <strong>of</strong> water in the past decades has nearly reduced more than 40 meter in<br />

underground water level (Unit, 2005). Currently, the total water consumption is approximately 88.5 bm3, out <strong>of</strong><br />

which more than 93% is used in agriculture, while less than 7% is allocated to urban and industrial<br />

consumption. Under the present situation 82.5 bm3 <strong>of</strong> water is utilized for irrigation on 7.5 million hectares <strong>of</strong><br />

land under irrigated agriculture (Ommani & Noorivandi, 2003).<br />

In order to combat this problem, there is need for new technologies and methods to manage water more<br />

efficiently especially in agricultural sector (Karami, Rezaei-Moghaddam, and Ebrahimi., 2006). On one hand a<br />

more comprehensive water management is needed to achieve sustainable development and participatory<br />

mechanism could accelerate this process (Guterstan, 2008). On the other hand the principle <strong>of</strong> sustainable<br />

development is an essential imperative for the water industry which should be seen as an opportunity not a<br />

limitation (Asheley et al. 2003).<br />

Khorasan Razavi province is among regions in Iran with low rainfall. The amount <strong>of</strong> evaporation and<br />

transpiration <strong>of</strong> rainfall in this province is very significant which is 2 to 3 times higher than the average in<br />

country. According to the latest statistics, total volume <strong>of</strong> water consumption from surface water and<br />

groundwater is 9261.8 million cubic meters and more than 8445 million cubic meters <strong>of</strong> this amount used in<br />

agricultural sector.<br />

The traditional methods <strong>of</strong> water management have many problems and the best option currently to use for<br />

irrigating farms is sprinkler irrigation systems. The results <strong>of</strong> Study show that implementation <strong>of</strong> this irrigation<br />

method resulted in decreasing rate <strong>of</strong> water consumption from 12,000 cubic meters in hectare to 6,200 cubic<br />

meters (Vojdani, 2006). Despite, financial facilities which are allocated each year for farmers, the participation<br />

<strong>of</strong> farmers has not reached to a satisfactory level.<br />

Agricultural extension by its nature has an important role in promoting the adoption <strong>of</strong> new technologies and<br />

innovations. Extension organizations have a key role in brokering between providers <strong>of</strong> technologies and<br />

farmers. However, adopting is rarely instantaneous; the technology has to be taught and learned, adapted to<br />

experience, and integrated into production. As is <strong>of</strong>ten the case with technological innovation, potential and<br />

expectations can outpace reality (Bonati and Gelb, 2005).<br />

Omani et al (2009) citing Evenson (1997) pointed out to this fact that agricultural extension and education as<br />

achieving its highest economic impact and sustainability in agriculture by providing information to increase<br />

farmers awareness, knowledge, adoption and productivity.<br />

Therefore, understanding the extension mechanisms which would speed up the development and adoption <strong>of</strong> the<br />

sprinkler irrigation system in the township <strong>of</strong> Chenaran in Khorasan Razavi Province was investigated in this<br />

research.<br />

MATERIAL AND METHODS<br />

The methodology used in this study involved a combination <strong>of</strong> descriptive and quantitative research and<br />

included the use <strong>of</strong> correlation, regression and descriptive analysis as data processing methods. The total<br />

population for this study was 150 gardeners who adopted the sprinkler irrigation system. Data were collected by<br />

using questionnaire and through interview schedules.<br />

A series <strong>of</strong> in-depth interviews were conducted with some senior experts in the Department <strong>of</strong> Agriculture and<br />

Power in the Khorasan Razavi Province to develop the questionnaire. The questionnaire included both openended<br />

and fixed-choice questions. The open-ended questions were used to gather information not covered by the<br />

fixed-choice questions and to encourage participants to provide feedback.<br />

Content and face validity were established by a panel <strong>of</strong> experts consisting <strong>of</strong> faculty members at Islamic Azad<br />

University, <strong>Science</strong> and Research Branch and some experts in the Departments <strong>of</strong> Agriculture and Power. A<br />

pilot study was conducted with 25 specialists who had not been interviewed before the earlier exercise <strong>of</strong><br />

determining the reliability <strong>of</strong> the questionnaire for the study. Computed Cronbach’s Alpha score was 85.0%,<br />

which indicated reliability <strong>of</strong> the questionnaire.<br />

Independent variables in the study included extension mechanisms and personal characteristics <strong>of</strong> respondents.<br />

The dependent variable in this research study were the adoption <strong>of</strong> the sprinkler irrigation system by gardeners...<br />

For measurement <strong>of</strong> correlation between the independent variables and the dependent variable correlation<br />

coefficients have been utilized and include spearman test <strong>of</strong> independence.<br />

12


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

RESULTS<br />

Table 1 summarizes the demographic pr<strong>of</strong>ile and descriptive statistics <strong>of</strong> respondents. The results <strong>of</strong> descriptive<br />

statistics indicated that average age <strong>of</strong> respondents was 46 years old and majority <strong>of</strong> respondents did not have<br />

high school diploma. The study shows that average work experience was 19 years and the main occupation <strong>of</strong><br />

respondents was farming and gardening. Approximately 43 percent <strong>of</strong> respondents owned their lands and the<br />

remainder either had a collective ownership or rented the land.<br />

Respondents were asked to respond the question about role <strong>of</strong> water shortages in implementing sprinkler<br />

irrigation system. As a result, 71 percent <strong>of</strong> respondents indicated that agricultural water shortage was the main<br />

factor in the implementation <strong>of</strong> the irrigation system.<br />

The perception <strong>of</strong> respondents about the sources which help them to acquire information about sprinkler<br />

irrigation systems was displayed in Table 2. The highest mean refers to extension agents (mean=3.58) and the<br />

lowest mean refers to experiment stations (mean=1.59).<br />

The results <strong>of</strong> perception <strong>of</strong> respondents about the role <strong>of</strong> communication channels which would influence the<br />

adoption <strong>of</strong> sprinkler irrigation systems by gardeners were displayed in Table 2. The results indicated that the<br />

highest mean number refers to extension agents (mean=4.11) and the lowest mean number refers to relatives<br />

(mean=1.67).<br />

The respondents’ perception about the role <strong>of</strong> extension mechanisms in adopting the sprinkler irrigation systems<br />

was displayed in Table 4. As can be seen from this table, the highest mean refers to visit by extension agents in<br />

agricultural service centers (mean=3.18) and the lowest mean refers to extension workshops (mean=2.57).<br />

Spearman coefficient was employed for measurement <strong>of</strong> relationships between perceptions <strong>of</strong> gardeners about<br />

the role <strong>of</strong> extension mechanisms in adopting the sprinkler irrigation system as dependent variable. Table 5<br />

displays the results which show that there was relationship between perception <strong>of</strong> respondents about the age,<br />

visiting extension agents in the service centers, extension classes, visiting the sample farm and visiting extension<br />

agents in the field and adopting the sprinkler irrigation system.<br />

Table 6 shows the result for regression analysis by stepwise method. Independent variables that were<br />

significantly related to perception <strong>of</strong> respondents about role <strong>of</strong> extension mechanisms in adopting the sprinkler<br />

irrigation system were entered. The result indicates that 45% <strong>of</strong> the variance in the perception <strong>of</strong> gardeners<br />

about the role <strong>of</strong> extension mechanisms in adopting the sprinkler irrigation systems could be explained by<br />

visiting extension agents in service centers, extension classes, visiting extension agents in the field and visiting<br />

sample farm.<br />

CONCLUSION<br />

The perception <strong>of</strong> gardeners about the role <strong>of</strong> extension mechanisms in adopting sprinkler irrigation system was<br />

discussed in this article. As the regression analysis showed visiting sample farms, visiting extension agents in<br />

the service centers and field and extension classes caused 45% <strong>of</strong> variance on the perception <strong>of</strong> respondents<br />

regarding the role <strong>of</strong> extension mechanisms in adopting sprinkler irrigation systems. This result is consistent<br />

with Okunade (2007) conclusion in which skill is better acquired through group contact methods. These<br />

methods have the nature <strong>of</strong> practical demonstration which will help the clientele from desire stage through<br />

conviction and probably into taking action. The individual contact method is considered to be important tool to<br />

help farmers to adopt a new technology. This may be as a result <strong>of</strong> the nature <strong>of</strong> the methods <strong>of</strong> giving<br />

information and deeper understanding <strong>of</strong> the innovation concerned.<br />

Based on the results <strong>of</strong> the study by Chizari, etal. (1998) the majority <strong>of</strong> extension agents believed the result<br />

demonstration were the most effective method for teaching their clientele. Result demonstrations are the<br />

processes <strong>of</strong> showing farmers the impact <strong>of</strong> using a particular practice. The second most effective method<br />

identified by extension agents was method demonstration. Method demonstrations typically occur after result<br />

demonstrations.<br />

Based on the results <strong>of</strong> the mean score, respondents indicated that visiting extension agents in the service centers<br />

was the most effective individual extension method main in helping them to adopt the sprinkler irrigation<br />

systems. The results demonstrated that respondents preferred individual teaching methods compared with group<br />

13


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

and mass methods. Although all agents use a variety <strong>of</strong> teaching methods, agricultural agents generally tend to<br />

use more individual methods than the other agents. Farm visits and on-farm demonstrations model the early<br />

farm demonstration method <strong>of</strong> providing research-based recommendations to the local producer.<br />

IMPLICATIONS<br />

The perception <strong>of</strong> gardeners about the extension mechanisms in adopting the sprinkler irrigation system was<br />

discussed in this article. The results demonstrated that visiting sample farms and face to face meetings with<br />

extension agents in service center and farms are the most important mechanisms in helping gardeners in<br />

adopting sprinkler irrigation systems. Successful adoption <strong>of</strong> this technology in Iran will depend on the<br />

appropriate government support and the authorities should develop policies that would overcome the challenges<br />

in adopting this method <strong>of</strong> irrigation.<br />

In Iran like some <strong>of</strong> the developing countries, there is not a clear understanding about role <strong>of</strong> the new methods<br />

<strong>of</strong> irrigation in sustainable water management in agriculture sector and policy makers have difficulty in<br />

prioritizing the policies and strategies. In this regard, public involvement will enhance and accelerate the<br />

adoption process.<br />

REFERENCES<br />

Ashley, R., Blackwood, D., Butler, D., Davies, J., Jowitt, P., & Smith, H. (2003). Sustainable decision making<br />

for UK water industry. Engineering Sustainability, 1, 41-49.<br />

Bonati, G., and Gelb, E. (2005) 'Evaluating internet for extension in agriculture.' In: gelb, B. And Offer, A.<br />

(ed.), ICT in Agriculture: Perspectives <strong>of</strong> Technological Innovation, Paris: European Federation for<br />

Information Technologies in Agriculture, Food and the Environment.<br />

Chizari, M., Karbasioun, M., and Lindner, J.R. (1998). Obstacles facing extension agents in the development<br />

and delivery <strong>of</strong> extension educational programs for adult farmers in the Province <strong>of</strong> Esfahan, Iran.<br />

<strong>Journal</strong> <strong>of</strong> Agricultural Education, 1, 48-54.<br />

Evenson, R. (1997). The economic contributions <strong>of</strong> agricultural extension to agricultural and rural development.<br />

In Food and Agriculture Organization <strong>of</strong> the United Nations (eds.) Improving agricultural extension.<br />

FAO. Rom. pp. 27–36.<br />

Guterstam, B. (2008). Toward Sustainable Water Resource Management in Central Asia. [on-line]<br />

Available:www.water.tkk.fi/English/wr/research/global/material/CA_chapters/02-CA_Waters-<br />

Guterstam.pdf<br />

Karami, E., Rezaei-Moghaddam, K., & Ebrahimi, H. (2006). Predicting sprinkler irrigation adoption:<br />

Comparison <strong>of</strong> models. <strong>Journal</strong> <strong>of</strong> <strong>Science</strong> and Technology <strong>of</strong> Agricultural and Natural Resources, 1,<br />

90–104.<br />

Keshavarz, A. (2000). Recommendation on policies and programs about water and irrigation in Iran. Tehran:<br />

Agricultural Extension Organization.<br />

Keshavarz, A., Heydari, N., and Ashrafi, S. (2003). Management <strong>of</strong> agricultural water consumption, drought,<br />

and supply <strong>of</strong> water for future demands. pp. 42–48. In: Proceedings <strong>of</strong> the Seventh International<br />

Conference on the Development <strong>of</strong> Dryland, September 14–17, 2003, Tehran, Iran.<br />

Okunade, E.O. (2007). Effectiveness <strong>of</strong> extension teaching methods in acquiring knowledge, skills and attitude<br />

by women farmers in Osun State. <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong> Research, 4, 282-286.<br />

Ommani, A. R., Chizari, M., Salmanzadeh, C., & Hosaini, J. (2009). Predicting Adoption Behavior <strong>of</strong> Farmers<br />

Regarding On-Farm Sustainable Water Resources Management (SWRM): Comparison <strong>of</strong> Models.<br />

<strong>Journal</strong> <strong>of</strong> Sustainable Agriculture, 5, 595- 616.<br />

Ommani, A.R., & Noorivandi, A. (2003). Water as food security resource (Crises and Strategies). Jihad Monthly<br />

Scientific, Social and Economic Magazine, 255, 58–66.<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Sohail, M., and Cavill, S. (2006). Ethics: making it the heart <strong>of</strong> water supply. Civil Engineering, 5, 11-15.<br />

UNDP. (2007). Human Development Report 2007/2008. [on-line] Available: Http://hrd.undp.org<br />

Vojdani, M. (2006). Assessing factors influencing the adoption <strong>of</strong> irrigation technologies by farmers in<br />

Township <strong>of</strong> Bahar. Master Thesis in Agricultural Extension and Education, Tehran, Iran.<br />

World Bank. (2009). Water Resource Management. [on-line] Available :<br />

http://web.worldbank.org/WBSITE/EXTERNAL/TOPICS/EXTWAT/0,,contentMDK:21630583~men<br />

uPK:4602445~pagePK:148956~piPK:216618~theSitePK:4602123,00.html<br />

Main Occupation Farming and Gardening (44%) Gardening (24.0%)<br />

Age (year) Mean=46<br />

Work Experience (Year) Mean=19<br />

Educational level Secondary School (75%) Diploma (25%)<br />

Amount <strong>of</strong> land owned (Hectares) Mean= 10.5<br />

Table 1. Personal Characteristics <strong>of</strong> Respondents.<br />

Sources Mean and Standard Deviation<br />

15<br />

Mean SD<br />

Extension Agents 3.58 0.959<br />

Rural Cooperatives 2.77 0.886<br />

Agricultural Magazines 2.55 1.347<br />

Agricultural Input suppliers 2.43 0.890<br />

Local Leaders 2.31 1.056<br />

Neighbors 2.13 0.824<br />

Rural Service Centers 2.09 0.928<br />

Relatives 1.67 0.864<br />

Experiment Stations 1.59 1.783<br />

Table 2. Means <strong>of</strong> respondents’ views about the sources which help them to acquire information about sprinkler<br />

irrigation system (1=Too little; 5=Too much).


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Communication Channels Mean and Standard Deviation<br />

Extension Agents 3.80<br />

Television 3.58<br />

Visit the sample farm 3.09<br />

16<br />

Mean SD<br />

1.069<br />

0.959<br />

0.963<br />

Rural organizations 2.77 0.886<br />

Printing Materials 2.63 1.178<br />

Private Sector 2.41 0.881<br />

Local Leaders 2.31 1.563<br />

Radio 2.18 1.063<br />

Neighbors 2.13 0.824<br />

Researchers 2.08 0.900<br />

Relatives 1.67<br />

0.864<br />

Table 3. Means <strong>of</strong> respondents’ views about the role communication channels which influence the adoption <strong>of</strong><br />

sprinkler irrigation systems by gardeners (1=strongly disagree; 5=strongly agree).<br />

ٍ Extension Mechanisms Mean and Standard Deviation<br />

Visiting extension agents in service centers 3.18<br />

Extension Classes 3.17<br />

Visit the sample farm 2.96<br />

Mean SD<br />

1.032<br />

1.042<br />

1.021<br />

Extension films 2.81 1.024<br />

Visiting extension agents in the field 2.78 1.041<br />

Workshops 2.57 1.057<br />

Table 4. Means <strong>of</strong> respondents’ views about the role <strong>of</strong> extension mechanisms in adopting sprinkler irrigation<br />

systems by gardeners (1=strongly disagree; 5=strongly agree).<br />

Independent variables Dependent variable Gardeners<br />

r Sig.<br />

Age Adoption <strong>of</strong> Sprinkler Irrigation System 0.535 0.000**<br />

Workshop Adoption <strong>of</strong> Sprinkler Irrigation System 0.050 0.550<br />

Visiting Extension Agents in service centers Adoption <strong>of</strong> Sprinkler Irrigation System 0.329 0.021*<br />

Working Experience Adoption <strong>of</strong> Sprinkler Irrigation System 0.519 0.000**<br />

Extension Classes Adoption <strong>of</strong> Sprinkler Irrigation System 0.315 0.025*<br />

Visiting the Sample Farm Adoption <strong>of</strong> Sprinkler Irrigation System 0.327 0.020*<br />

Extension films Adoption <strong>of</strong> Sprinkler Irrigation System 0.094 0.562<br />

Visiting extension agents in the field Adoption <strong>of</strong> Sprinkler Irrigation System 0.306 0.031*<br />

**p


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

B Beta T Sig.<br />

Constant 0.402 ------- 0.792 0.434<br />

Visiting extension agents in service<br />

centers<br />

0.414 0.386 4.327 0.000<br />

Extension classes 0.226 0.284 3.086 0.004<br />

Visiting extension agents in field 0.197 0.240 2.963 0.005<br />

Visiting the sample farm 0.210 0.292 2.750 0.010<br />

R 2 =0.45<br />

Table 6. Multivariate Regression Analysis (adopting the sprinkler irrigation system as dependent variable).<br />

17


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

GEOELECTRIC ASSESSMENT OF GROUNDWATER PROSPECT AND<br />

VULNERABILITY OF OVERBURDEN AQUIFERS AT IDANRE, SOUTHWESTERN<br />

NIGERIA<br />

OMOSUYI, G.O.<br />

Department <strong>of</strong> <strong>Applied</strong> Geophysics, Federal University <strong>of</strong> Technology,<br />

P.M.B. 704, Akure, Nigeria<br />

E-mail address for correspondence : droluomosuyi@yahoo.com<br />

___________________________________________________________________________________________<br />

Abstract: Idanre and environs, southwestern Nigeria, is characterized by extensive outcrops <strong>of</strong> crystalline<br />

basement rocks, largely <strong>of</strong> granite gneiss petrology. Inadequate municipal water supply, coupled with<br />

hydrogeologically difficult nature <strong>of</strong> the terrain, individuals and corporate bodies indiscriminately sink tube wells<br />

and boreholes within the unconsolidated overburden materials, with glaring lack <strong>of</strong> concerns for the vulnerability<br />

status <strong>of</strong> aquifers, and possible environmental risk. Sixty five (65) Schlumberger depth sounding data from the<br />

area were interpreted in order to assess the groundwater prospect, focused on the thickness <strong>of</strong> the unconsolidated<br />

materials overlying the crystalline bedrock. The resistivity parameter <strong>of</strong> the geoelectric topmost layer across the<br />

area was also used to assess the vulnerability <strong>of</strong> the underlying aquifers to near-surface contaminants. The<br />

thickness <strong>of</strong> the unconsolidated overburden varies from 0.5m to 15.8m, where about 81.5% falls within the 1-5.9m<br />

brackets. This shows that unconsolidated materials are generally not significantly thick and hence <strong>of</strong> apparently<br />

low groundwater prospect. The topmost geoelectric layer has resistivity mostly within the range <strong>of</strong> 1-100 Ohm-m<br />

(77%) across the area. Resistivity values within these brackets tend to indicate silt or clay sequence, which can<br />

constitute effective protective geologic barriers for the underlying aquifers. This suggests that aquifers within the<br />

unconsolidated overburden at Idanre are mostly capped by impervious/semi-pervious materials, geologically<br />

protecting the underlying aquifers from near-surface contaminants.<br />

___________________________________________________________________________________________<br />

INTRODUCTION<br />

Groundwater has become immensely important for human water supply in urban and rural areas in developed and<br />

developing nations alike. Despite its importance, there is gross inadequate supply <strong>of</strong> water at Idanre, the study<br />

area.<br />

Idanre lies within the Precambrian basement complex terrain <strong>of</strong> southwestern Nigeria (Rahaman, 1988).The<br />

crystalline basement rocks are extensively exposed in the area (Ocan, 1991). In basement terrains, groundwater is<br />

generally believed to occur within the overlying unconsolidated material derived from the in-situ weathering <strong>of</strong><br />

rocks, and the fractured/faulted bedrock (Clark, 1985; Jones, 1985; Acworth, 1987; Bala and Ike, 2001). Since the<br />

intrinsic resistivity <strong>of</strong> the unconsolidated overburden and that <strong>of</strong> the crystalline basement differs by orders <strong>of</strong><br />

magnitude, geoelectric methods are suitable to map the thickness and extent <strong>of</strong> the overburden (1975; Koefoed,<br />

19


1989; Parasnis, 1997). The electrical resistivity depth sounding is useful in locating areas <strong>of</strong> maximum aquifer<br />

thickness and serves as a good predictive tool for estimation <strong>of</strong> borehole depth.<br />

Aquifers in basement complex terrains <strong>of</strong>ten occur at shallow depths, thus exposing the water within to<br />

environmental risks, that is, vulnerable to surface or near-surface contaminants. A recent study (Omosehin, 2009)<br />

reveals that the people around Idanre abstracts water from the unconsolidated materials overlying the crystalline<br />

basement through uncontrolled sinking <strong>of</strong> tube wells, with glaring lack <strong>of</strong> concern for aquifer vulnerability to<br />

near-surface contaminants and quality status <strong>of</strong> the groundwater.<br />

This work, in addition to assessing the groundwater prospect <strong>of</strong> the unconsolidated materials in the area, the<br />

geoelecrtic parameters <strong>of</strong> the near-surface materials overlying the aquifers were also used to assess the<br />

vulnerability <strong>of</strong> the near-surface aquifers to near-surface contaminants. The work is anticipated to upgrade our<br />

knowledge on groundwater potential <strong>of</strong> the unconsolidated material in the area, and the vulnerability <strong>of</strong> the<br />

aquifers within.<br />

Geologic setting<br />

Idanre area is underlain by the Precambrian basement complex <strong>of</strong> southwestern Nigeria (Ajibade and Fitches,<br />

1988), where six major petrologic units has been identified and described by Rahaman (1988). The study area is<br />

underlain by three <strong>of</strong> these six major petrologic units: the migmatite gneisses, members <strong>of</strong> the older granite suite<br />

and charnockitic rocks (Ocan, 1991). Most <strong>of</strong> the outcrops observed in Idanre are melanocratics, therefore<br />

possibly rich in biotite and/or hornblende. Field observation shows that granite rocks constitute extensive outcrops<br />

in the entire area (Fig 1). Granite gneisses outcrops either occur alone or in association with other components.<br />

Minerallogically, the granite gneiss around Idanre are composed <strong>of</strong> alkaline feldspar, quartz, plagioclase and<br />

biotite (Ocan, 1991).<br />

Materials and Methods <strong>of</strong> study<br />

The vertical electrical soundings (VES) were conducted using the Schlumberger electrode array (Zhody et al.,<br />

1974). The Ohmega Resistivity Meter was used for resistance measurement. The geoelectric survey comprised <strong>of</strong><br />

sixty five (65) depth soundings (Fig 2), with maximum current electrode spacing (AB) ranging from 130m to<br />

200m (AB/2 = 65 - 100). The field curves were interpreted through partial curve matching (Koefoed, 1979),<br />

engaging master curves and auxiliary point charts (Orellana and Mooney, 1966).<br />

20


5 00' E<br />

7 15' N<br />

7 15' N<br />

River Osun<br />

River Apurare<br />

River Owena<br />

5 00' E<br />

Owena<br />

60<br />

50<br />

Ago - M<strong>of</strong>erere<br />

Gberiwojo<br />

Ago - Ireti<br />

Aponmu Akore<br />

Odoko Bekun Odoji<br />

ALADE<br />

IDANRE<br />

Odo - Isa<br />

Odo - Isa<br />

21<br />

Apefon<br />

Igbo - Olokun<br />

Igbo - Epo - Aiyem<strong>of</strong>ewa<br />

Omiwonja<br />

Ajegunle - Arun<br />

Iwanja - M<strong>of</strong>erere<br />

Igbo - Epo<br />

Igbo - Epo - Owom<strong>of</strong>ewa<br />

300 m<br />

0<br />

River Aponmu<br />

River Esun<br />

A<br />

50<br />

40<br />

River Iwari<br />

River Imoja<br />

Porphyritic Granites<br />

Massive charnockite<br />

Granitic charnockite<br />

Migmatite<br />

Strike and dip <strong>of</strong> Foliation<br />

Major fault<br />

Idanrore<br />

Tejugbala<br />

Ajegunle - Iwonja<br />

B<br />

1 0 1 2 3 4 5 Km<br />

0 2000 4000 6000 8000 10000 12000<br />

LEGEND<br />

ALADE River Arun<br />

20<br />

A<br />

Cross Section Across Direction A - B<br />

River Ogburugburu<br />

Opa - Idanre<br />

Kajola - Asoko<br />

River Owena<br />

Oposinle<br />

River Otan<br />

AKURE<br />

Orientation Of feldspar in granite<br />

Roads<br />

Footpaths<br />

Village<br />

Fig. 1: Simplified Geological Map around Idanre (Ocan, 1991).<br />

50<br />

60<br />

River<br />

40<br />

20<br />

40<br />

Italepo - Odo<br />

Ododin Ipinlerere<br />

B<br />

30<br />

30<br />

Oda<br />

Oke - Alafia<br />

5 15' E<br />

5 15' E<br />

7 15' N<br />

7 00' N


The manually derived geoelectric parameters were subjected to an inversion (Vander Velpen, 1988), which<br />

successfully reduced the interpretation error to acceptable levels (Barker, 1989).<br />

The electrical resistivity contrasts existing between lithological sequences in the subsurface (Dodds and Ivic, 1998;<br />

Lashkaripour, 2003) were used in the delineation <strong>of</strong> geoelectric layers, identification <strong>of</strong> aquiferous materials<br />

(Deming, 2002) and assessment <strong>of</strong> groundwater prospect <strong>of</strong> the area. Also, the resistivity parameter <strong>of</strong> the<br />

uppermost geoelectric layer (topsoil) was used to evaluate, in quantitative terms, its permeability to surface/nearsurface<br />

contaminants, and hence the vulnerability <strong>of</strong> the underlying aquifers, as demonstrated in Draskovits et al.<br />

(1995).<br />

7 06' 27.4''<br />

7 06' 22.3'' 5 06' 15.0''<br />

v54<br />

o<br />

T<br />

A<br />

e<br />

r u<br />

k<br />

v53<br />

v51<br />

v52<br />

v1<br />

v3<br />

v2<br />

v7<br />

v4<br />

o<br />

r v6 v5<br />

l v8<br />

v11 v12<br />

a<br />

d<br />

v9<br />

v10<br />

v13<br />

v37<br />

v14<br />

v33 v36 v19 v18<br />

v15<br />

v35<br />

v32<br />

v17<br />

v16<br />

v27<br />

v26 v31 v34<br />

v25 v30<br />

v20<br />

v23 v21<br />

v28 v24<br />

v29<br />

v22<br />

v38<br />

v42<br />

v41<br />

v39<br />

v40<br />

v43 v44 v45 v46 v47<br />

m<br />

m<br />

o<br />

C<br />

v49 v48<br />

v50<br />

e r c i a<br />

T o A p e f o n<br />

T o A b a B a b u b u<br />

Scale<br />

0 1000 2000<br />

Fig. 2: Layout Map <strong>of</strong> Idanre showing VES positions (Inset: Map <strong>of</strong> Nigeria).<br />

m<br />

v59<br />

22<br />

v57<br />

v58<br />

v56<br />

v60 v61 v62 v63<br />

v65<br />

v64<br />

v55<br />

T o<br />

l<br />

S c<br />

h<br />

l a<br />

i c<br />

n<br />

T e c<br />

h .<br />

T o A p e t a n<br />

5 08' 22.3''<br />

Study Area<br />

N<br />

NIGERIA<br />

v<br />

LEGEND<br />

Road / Major Street<br />

Minor Street<br />

VES Location<br />

River<br />

Scale<br />

0 300 Km


RESULTS AND DISCUSSIONS<br />

The Schlumberger depth soundings produced a short range <strong>of</strong> sounding curves: three-layer case <strong>of</strong> type A (41.5%),<br />

H type (24.6%), and four-layer curves <strong>of</strong> type KH (15.4%) were mostly recorded. Typical curves are shown in Fig<br />

3. Field curves <strong>of</strong>ten mirror-image (geoelectrically) the nature <strong>of</strong> the successive lithologic sequence in a place and<br />

hence can be used, in qualitative sense, to assess the groundwater prospect <strong>of</strong> an area (Worthington, 1977). Type<br />

H and KH curves are <strong>of</strong>ten associated with groundwater possibilities while type A may typify a rapid resistivity<br />

progression, indicative <strong>of</strong> shallow, resistive bedrock.<br />

Aquifer Delineation: Electrical resistivity contrasts exists across interfaces <strong>of</strong> lithologic units in the subsurface.<br />

These contrasts are <strong>of</strong>ten adequate to delineate discrete geoelectric layers and identify aquiferous or nonaquiferous<br />

layers (Schwarz, 1988). The geoelectric parameters <strong>of</strong> the aquifer units were determined from the<br />

interpretation <strong>of</strong> the sounding curves. Resistivity <strong>of</strong> earth materials is strongly affected by water saturation and<br />

water quality (Lucius et al., 2001). The resistivity parameter <strong>of</strong> a geoelectric layer is an important factor to<br />

adjudge an aquifer or otherwise.<br />

Cross sections <strong>of</strong> interpreted resistivity data from the area (Fig 4) show three to four geoelectric layers: the topsoil,<br />

the lateritic or weathered layer, and the fractured/fresh bedrock. In the topsoil, resistivity values range from 20 to<br />

260 Ohm-m, with layer thickness varying between 0.5 and 2.1m. The lateritic or weathered layer has resistivity in<br />

the range <strong>of</strong> 35 to 600 Ohm-m, with most <strong>of</strong> the values (67%) less than 150 Ohm-m. Layer thickness ranges from<br />

0.8 to 7.8m. In few areas however, the thickness gets up to over 20m, but about 85% <strong>of</strong> layer thickness obtained is<br />

less than 6m. The presumed decomposed portion <strong>of</strong> the bedrock has resistivity in the range <strong>of</strong> 69 to 874 Ohm-m,<br />

while the thickness ranges from 3.2 to 24m.<br />

NORTH<br />

DEPTH (m)<br />

-1<br />

-3<br />

-5<br />

-7<br />

-9<br />

-11<br />

-13<br />

-15<br />

-17<br />

(a)<br />

VES 54<br />

61<br />

150Ohm-m<br />

8121<br />

Depth (m)<br />

4<br />

2<br />

33<br />

Scale<br />

0<br />

0 400<br />

Distance (m)<br />

VES 3<br />

VES 11 VES 38<br />

VES 8 VES 42<br />

99<br />

31<br />

54694<br />

22<br />

197<br />

2522<br />

114<br />

23<br />

299<br />

103<br />

5683<br />

59<br />

27<br />

599<br />

73<br />

54 Ohm-m<br />

1199<br />

LEGEND<br />

VES 25 VES 29<br />

79<br />

26<br />

9233<br />

Topsoil<br />

67<br />

109<br />

24<br />

1175 Ohm-m<br />

590<br />

7251<br />

Weathered layer<br />

Fractured basement<br />

Fresh basement<br />

SOUTH


DEPTH (m)<br />

WEST<br />

0<br />

-2<br />

-4<br />

-6<br />

-8<br />

-10<br />

-12<br />

-14<br />

VES 43<br />

88<br />

VES 44<br />

83 Ohm-m<br />

8868<br />

(b)<br />

66<br />

159<br />

26840<br />

Depth (m)<br />

VES 45 VES 27 VES 26 VES 31<br />

4<br />

2<br />

64<br />

79<br />

8284<br />

Scale<br />

0<br />

0 300 600<br />

Distance (m)<br />

22<br />

119<br />

23<br />

12742<br />

24<br />

60<br />

38<br />

351<br />

1206<br />

13<br />

891<br />

Fig 4(a) & (b): Cross Sections <strong>of</strong> Interpreted Resistivity data from Idanre.<br />

Assessment <strong>of</strong> Groundwater Prospect<br />

VES 34<br />

26<br />

3172 Ohm-m<br />

221<br />

1553<br />

LEGEND<br />

Topsoil<br />

Weathered layer<br />

Fractured basement<br />

Fresh basement<br />

VES 17<br />

No acceptable framework has yet emerged, as to where exactly is the major focus for groundwater resources in a<br />

typical crystalline basement terrain. Acworth (1987) reported successful completion <strong>of</strong> boreholes in shallow<br />

weathered zones in a typical basement terrain. Fracture-zone aquifers in crystalline rocks are also believed to be<br />

important sources <strong>of</strong> water for rural communities (Meju et al., 1999). Lenkey et al (2005) however believes that<br />

the thickest layer above the basement constitute the main water-bearing layer.<br />

The approach <strong>of</strong> Lenkey et al (2005) has been adapted for this study. Fig 5 is a contour map while figure 6 is the<br />

numerical value distribution, showing the thickness <strong>of</strong> unconsolidated materials overlying the crystalline<br />

basement in Idanre; the thickness ranges from 0.5m to 15.8m, with an average <strong>of</strong> 4.5m. Fig 5 shows that<br />

overburden thickness <strong>of</strong> 1-5.9m in the area constitutes about 81.5%, thus suggesting that the water-bearing<br />

horizon (Lenkey et al., 2005) across the area is generally not significantly thick.<br />

Assessment <strong>of</strong> Aquifer Vulnerability<br />

Due to shallow depth <strong>of</strong> occurrence, aquifers in crystalline basement terrains are <strong>of</strong>ten exposed to environmental<br />

risks. An effective groundwater protection is given by protective geologic barriers with sufficient thickness<br />

(Mundel et al., 2003) and low hydraulic conductivity. Laterite, silt or clay <strong>of</strong>ten constitutes protective geologic<br />

barriers. When found above an aquifer they constitute its cover (Lenkey et al., 2005).<br />

The resistivity parameters <strong>of</strong> the uppermost geoelectric layer in the study area have been used to assess the<br />

vulnerability <strong>of</strong> the underlying aquifers. Fig 7 is a contour map <strong>of</strong> resistivity <strong>of</strong> the first layer while figure 8 shows<br />

the numerical resistivity distribution across the first layer in the area.<br />

35<br />

56<br />

12480<br />

EAST


7 06' 27.4''<br />

7 06' 22.3''<br />

Frequency<br />

v53<br />

v54<br />

v51<br />

v52<br />

v1<br />

v3<br />

v2<br />

v7<br />

v4<br />

v8 v6 v5<br />

v11v12 v9<br />

v42<br />

v10<br />

v37<br />

v13<br />

v14<br />

v15<br />

v33 v36<br />

v19v18<br />

v35<br />

v32<br />

v17<br />

v16<br />

v27<br />

v26 v31<br />

v34<br />

v25 v30<br />

v20<br />

v23 v21<br />

v28 v24<br />

v29<br />

v22<br />

v38<br />

v49 v48<br />

v50<br />

v41<br />

v39<br />

v43 v46<br />

v44v45<br />

v47<br />

v40<br />

To Aba Babubu<br />

5 06' 15.0''<br />

To Akure<br />

Commercial road<br />

Scale<br />

To Apefon<br />

0 1000 2000 m<br />

25<br />

v65<br />

v59<br />

v58<br />

v57<br />

v64<br />

v60v61v63<br />

v62<br />

v56<br />

v55<br />

To Technical Schl.<br />

To Apetan<br />

N<br />

5 08' 22.3''<br />

Fig. 5: Map <strong>of</strong> thickness <strong>of</strong> unconsolidated material overlying the Basement at Idanre.<br />

30<br />

25<br />

20<br />

15<br />

10<br />

5<br />

0<br />

1 - 2.9 3 - 5.9 6 - 8.9 9 - 11.9 12 - 14.9 15 -17.9<br />

Overburden Thickness (m)<br />

Fig 6: Distribution <strong>of</strong> thickness <strong>of</strong> unconsolidated material at Idanre.<br />

v<br />

Series1<br />

22 m<br />

19<br />

16<br />

13<br />

10<br />

7<br />

4<br />

1<br />

LEGEND<br />

Road / Major Street<br />

Minor Street<br />

VES Location


7 06' 27.4''<br />

7 06' 22.3''<br />

Frequency<br />

v53<br />

v54<br />

v51<br />

v52<br />

v1<br />

v3<br />

v2<br />

v7<br />

v4<br />

v8 v6 v5<br />

v11v12 v9<br />

v42<br />

v10<br />

v37<br />

v13<br />

v14<br />

v15<br />

v33 v36<br />

v19v18<br />

v35<br />

v32<br />

v17<br />

v16<br />

v27<br />

v26 v31<br />

v34<br />

v25 v30<br />

v20<br />

v23 v21<br />

v28 v24<br />

v29<br />

v22<br />

v38<br />

v49 v48<br />

v50<br />

v41<br />

v39<br />

v43 v46<br />

v44v45<br />

v47<br />

v40<br />

To Aba Babubu<br />

5 06' 15.0''<br />

60<br />

50<br />

40<br />

30<br />

20<br />

10<br />

0<br />

To Akure<br />

Commercial road<br />

Scale<br />

To Apefon<br />

0 1000 2000<br />

26<br />

m<br />

v65<br />

v59<br />

v58<br />

v57<br />

v64<br />

v60v61v63<br />

v62<br />

v56<br />

v55<br />

To Technical Schl.<br />

To Apetan<br />

N<br />

5 08' 22.3''<br />

Fig. 7: Contour Map <strong>of</strong> Resistivity Distribution in the First Layer at Idanre.<br />

1-100 101-200 201-300 301-400 401-500 501-600 601-700 701-800 801-900 901-<br />

1000<br />

Resistivity (Ohm-m)<br />

Fig 8: Distribution <strong>of</strong> resistivity in the topmost geoelectric layer at Idanre<br />

Series1<br />

v<br />

800 Ohm-m<br />

750<br />

700<br />

650<br />

600<br />

550<br />

500<br />

450<br />

400<br />

350<br />

300<br />

250<br />

200<br />

150<br />

100<br />

50<br />

0<br />

LEGEND<br />

Road / Major Street<br />

Minor Street<br />

VES Location


About 77% <strong>of</strong> the resistivity values <strong>of</strong> the topmost geoelectric layer fall within 1-100 Ohm-m range. In Nigerian<br />

geological circumstances, this suggests considerable clayey or silt sequences (aquitard), with effective capacity to<br />

constitute impervious/semi-impervious barriers.<br />

CONCLUSIONS AND RECOMMENDATIONS<br />

Due to rugged geologic terrain, the unconsolidated materials overlying the crystalline basement rocks around<br />

Idanre constitute the major water-bearing horizon from which the inhabitants abstract water for domestic needs.<br />

Geoelectric depth sounding around the area reveals that the thickness <strong>of</strong> the unconsolidated materials varies from<br />

0.5m to 15.8m, where values within 1-5.9m brackets constitute about 81.5%. This indicates that the<br />

unconsolidated material in the area is not significantly thick, thus suggesting that the groundwater potential is<br />

apparently low.<br />

About 77% <strong>of</strong> the resistivity values <strong>of</strong> the topmost geoelectric layer in the area fall within the range <strong>of</strong> 1-100<br />

Ohm-m. Values <strong>of</strong> resistivity within this brackets suggest aquitard (silt or clay), which constitute effective,<br />

impervious geologic barriers to infiltrating near-surface contaminants. Aquifers within the unconsolidated<br />

materials at Idanre are therefore mostly capped by impervious/semi-pervious geologic materials, suggesting that<br />

they are mostly non-vulnerable to near-surface contaminants.<br />

Since decomposed bedrock in the crystalline basement terrain can house significant quantity <strong>of</strong> groundwater,<br />

groundwater developers in the area may explore the bedrock for bedrock aquifers, to complement the aquifers<br />

within the unconsolidated overburden.<br />

ACKNOWLEDGEMENT<br />

Messrs T. Omosehin, E. Faleye and M. Bawallah assisted in the data acquisition while Messrs O.Adegoke and A.<br />

I. Adeyemo helped in preparing the figures. The author gratefully acknowledged these assistances.<br />

REFERENCES<br />

Acworth, R.I. (1987). The development <strong>of</strong> crystalline basement aquifers in a tropical environment. Q. J. Eng. Geol.<br />

London. Vol. 20, pp. 265-272<br />

Ajibade, A.C. and Fitches, W.R. (1988). The Nigerian Precambrian and the Pan- African Orogeny. In:<br />

Precambrian Geology <strong>of</strong> Nigeria. A publication <strong>of</strong> the Geological Survey <strong>of</strong> Nigeria. Pp 329.<br />

Barker, R.D. (1989). Depth <strong>of</strong> investigation <strong>of</strong> collinear symmentrical four-electrode arrays. Geophysics 54, 1031-<br />

1037<br />

Bala, A. E. and Ike, E. C. (2001). The Aquifer <strong>of</strong> the Crystalline Basement Rocks in Gusau Area, North-Western<br />

Nigeria. <strong>Journal</strong> <strong>of</strong> Mining and Geology, Vol. 37, No. 2, pp. 177 – 184.<br />

Clark, L. (1985). Groundwater abstraction from Basement Complex areas <strong>of</strong> Africa. Q. J. Eng. Geol. London. Vol.<br />

18, pp 25-32.<br />

Deming, D. (2002). Intrduction to Hydrogeology. McGraw Hill Company. Pp 468.<br />

Dodds, A.R. and Ivic, D. (1988). Integrated geophysical methods used for groundwater studies in the Murray<br />

Basin, South Australia. In Geotechnical and Environmental <strong>Studies</strong> Geophysics, Vol II: Soc. Explor<br />

Geophys.,Tulsa, pp 303-310.<br />

27


Draskovits, P, Maayar, B and Pattantyus-A, M. (1995). Geophysical methods in groundwater prospecting and<br />

environmental protection. Fisica de la Tierra, no 7, 53-86.<br />

Lones, M.J. (1985). The weathered zone aquifers <strong>of</strong> the basement complex areas <strong>of</strong> Africa. Q. J. Eng. Geol.<br />

London. Vol. 18, pp 35-46.<br />

Koefeod, O. (1979). Geosounding Principles, 1. Resistivity sounding measurements. Elsevier Scientific<br />

Publishing Comp., Amsterdam, pp 275.<br />

Lenkey, L., Hamori, Z and Mihalffy, P. (2005). Investigating the hydrogeology <strong>of</strong> a water-supply area using<br />

direct-current vertical electrical soundings. Geophy, Vol.70. no. 4, H1-H19<br />

Lashkarripour, G.R. (2003). An investigation <strong>of</strong> groundwater condition by geoelectrical resistivity method: A case<br />

study in Korin aquifer, southeast Iran. <strong>Journal</strong> <strong>of</strong> Spatial Hydrology, Vol.3, No. 1, pp1-5.<br />

Lucius, J.E., Bisdort, R. J. and Abraham, J. (2001). Results <strong>of</strong> electrical survey near Red River, New Mexico.<br />

USGS Open-File Report 01-331, pp24.<br />

Meju, M.A., Fontes, S.L., Oliveira, M.F.B., Lima, J.P.R., Ulugerger, E.U. and Carrasquilla, A.A. (1999). Regional<br />

aquifer mapping using combined VES-TEM-AMT?EMAP methods in the semiarid eastern margin <strong>of</strong><br />

Parnaiba Basin, Brazil. Geophysics, Vol. 64, No. 2. P. 337-356.<br />

Mundel, J.A., Lother, L., Oliver, E.M. and Allen-Long, S. (2003). Aquifer vulnerability analysis for Water<br />

Resources Protection. Indiana Department <strong>of</strong> Environmental Management (IDEM), ‘Source Water<br />

Assessment Plan’, pp 25.<br />

Ocan, T. (1990). Petrogenesis <strong>of</strong> the rock units <strong>of</strong> Idanre, southwestern Nigeria. Unpublished Ph.D thesis,<br />

Obafemi Awolowo University, Ile Ife, Nigeria, pp 194.<br />

Omosehin, T.B. (2008). Geoelectric delineation <strong>of</strong> aquifers and assessment <strong>of</strong> their vulnerability in Idanre,<br />

Southwestern Nigeria. Unpublished M. Tech. thesis, Federal University <strong>of</strong> Tech., Akure, Nigeria. Pp 83.<br />

Orellana, E. and Mooney, H.M. (1966). Master tables and curves for vertical electrical<br />

sounding over layered structures. Inteciencis, Madrib, 34pp.<br />

Parasnis, D.S. (1979). Principles <strong>of</strong> <strong>Applied</strong> Geophysics. Chapman and Hill, London. Pp 98 130.<br />

Rahaman, M.A. (1988). Recent advances in the study <strong>of</strong> the Basement complex <strong>of</strong> Nigeria. Precambrian Geology<br />

<strong>of</strong> Nigeria. A Publication <strong>of</strong> Geological Survey <strong>of</strong> Nigeria. Pp. 11-41.<br />

Schwarz, S.D. (1988). Application <strong>of</strong> Geophysical Methods to Groundwater Exploration in the Tolt River Basin,<br />

Washington State. In Geotechnical and Environmental Geophysics. Vol 1. Soc. Explor. Geophs, Tulsa,<br />

pp 213-217.<br />

Vander Velpen, B. P. A. (1988). Resist Version 1.0, M.Sc. Research Project, ITC. Delft, Netherlands.<br />

Worthington, P. R. (1977). Geophysical investigations <strong>of</strong> groundwater resources in the Kalahari Basin.<br />

Geophysics, Vol. 42, No 4, pp.838-849.<br />

Zohdy, A. A. R., Eaton, G. P., and Mabey, D. R. (1974). Application <strong>of</strong> surface geophysics to groundwater<br />

investigations: Techniques <strong>of</strong> water resources investigations <strong>of</strong> U.S. Geol. Survey: Book 2, Chapter DI,<br />

U.S. Government Printing Office, Washington, pp.66.<br />

28


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Comparative vegetative and foliar epidermal features <strong>of</strong> three Paspalum L. species in<br />

Edostate, Nigeria.<br />

E.A Ogie-Odia*, A.I Mokwenye*, O. Kekere ** and O. Timothy ***<br />

*Department <strong>of</strong> Botany, Ambrose Alli University, Ekpoma , Edo State.<br />

** Department <strong>of</strong> Plant <strong>Science</strong> and Biotechnology, Adekunle Ajasin University, Akungba Akoko, Ondo State.<br />

*** Department <strong>of</strong> Environmental <strong>Science</strong>, Western Delta University, Oghara, Delta State.<br />

*Email address for correspondence: effexing@yahoo.com<br />

___________________________________________________________________________________________<br />

Abstract: Investigations into the vegetative morphology and epidermal features <strong>of</strong> three species <strong>of</strong> the genus<br />

Paspalum L. (P. conjugatum Berg, P. scrobiculatum L. and P. vaginatum Sw.) was carried out. Pictorial<br />

illustrations are presented. For the vegetative features, it was observed that there is variability <strong>of</strong> hairs on both the<br />

margins <strong>of</strong> the lamina and leaf sheath <strong>of</strong> P. scrobiculatum. In the epidermal studies, macro-hairs were observed on<br />

the margins <strong>of</strong> the lamina <strong>of</strong> two out <strong>of</strong> the three taxa; prickles were observed on the intercoastal zone <strong>of</strong> two out <strong>of</strong><br />

the three taxa; papillae was observed in the intercoastal zone <strong>of</strong> one <strong>of</strong> the three taxa; micro-hairs were observed in<br />

two out <strong>of</strong> the three taxa. It was observed that the shape <strong>of</strong> the subsidiary cells <strong>of</strong> P. conjugatum varied from low<br />

dome to triangular in the adaxial surface and mainly triangular shaped in the abaxial surface. P.scrobiculatum had<br />

mainly triangular shaped subsidiary cells, while that <strong>of</strong> was low dome shaped in the adaxial surface and triangular<br />

shaped in the abaxial surface. On the basis <strong>of</strong> the variations that exist in its morphological and epidermal features, a<br />

taxonomic key has been produced for identification and separation <strong>of</strong> the various taxa.<br />

Keywords: Vegetative, leaf epidermal, genus, Paspalum, Poaceae, systematic.<br />

___________________________________________________________________________________________<br />

INTRODUCTION<br />

Poaceae which is the grass family includes approximately 10,000 species classified into 600 to 700 genera (Clayton<br />

and Renvoize, 1986). The grasses are included with lilies, Orchids, Pineapples and Palms in the group known as<br />

monocotyledons which includes all flowering plants with a single seed leaf (Kellogg, 2001). The members <strong>of</strong> this<br />

group are present in all the conceivable habitats, suitable for growth <strong>of</strong> plant communities (Mitra and Mukherjee,<br />

2005). The grass family Poaceae, is noted for its wide diversity and complexity and so has posed many problems to<br />

the taxonomists using the traditional methods based on gross morphology (Strivastava, 1978).<br />

Before the later part <strong>of</strong> the 19 th century, taxonomists were confined to the use <strong>of</strong> the features <strong>of</strong> reproductive organs<br />

as floral characters were considered to provide the most valuable characters to taxonomic affinities (Nwokeocha,<br />

1996). Of all the non-reproductive organs, the leaf is the most widely used in plant taxonomy (Stace, 1984).<br />

Strivastava (1978) described the leaf epidermis as the second most important character after cytology for solving<br />

taxonomic problems.<br />

29


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Paspalum L. is a member <strong>of</strong> the tribe Paniceae R. Br. Within the Paniceae, Paspalum is one <strong>of</strong> the most complex<br />

genera containing over 400 species that are largely endemic to the tropics and subtropics <strong>of</strong> the world (Clayton and<br />

Renvoize, 1986). The centre <strong>of</strong> diversity <strong>of</strong> this genus is South America (Fernandes et al, 1968). In Nigeria, Lowe<br />

(1989) reported that the genus is represented by five species which are mostly straggling plants grown in damp open<br />

places. The reported species are P. vaginatum, P. conjugatum, P. notatum, P. scrobiculatum and P. auriculatum.<br />

The economic values <strong>of</strong> these species are many. For example, P. vaginatum provides for dune stabilization and<br />

waterflow fodder under saline and fresh water environments respectively and can also be cultivated as a turfgrass for<br />

soil stabilization. On the other hand, P. scrobiculatum has been domesticated as a cereal grain in Asia (Jarret et al.,<br />

1998). The use <strong>of</strong> morphological and leaf epidermal features has been found to be <strong>of</strong> immense interest in taxonomy.<br />

An excellent review <strong>of</strong> the application <strong>of</strong> morphological features in systematic studies is shown in the works <strong>of</strong><br />

Olowokudejo 1990, Mensah and Gill (1997), Edeoga and Ikem 2001, Gill and Mensah (2001) and Kharazian<br />

(2007).The use <strong>of</strong> leaf epidermal features in systematics has become popular and distinctive and has been used as a<br />

great taxonomic tool at the levels <strong>of</strong> family, genus and species.<br />

This study is to give the morphological description <strong>of</strong> the three Paspalum species and also to compare/determine the<br />

intraspecific relationship and patterns <strong>of</strong> variation associated with the epidermal features/characteristics among the<br />

taxa studied.<br />

METHODOLOGY<br />

Fresh and matured leaves <strong>of</strong> Paspalum scrobiculum L. and Paspalum conjugatum Berg. were collected from<br />

Beverly-Hills area, <strong>of</strong>f Benin-Auchi express road, Ekpoma, while Paspalum vaginatum Sw. was collected close to<br />

the bank <strong>of</strong> the Ikpoba river in Benin-city, Edo State. They were first boiled in water to restore to their normal<br />

shape. The tissue above the epidermis was gradually scraped away with a safety razor blade and during this<br />

operation the leaf was continuously irrigated with commercial Jik. The epidermal peels were then washed in water,<br />

stained with 1% safranin solution in 50% alcohol and temporary mounts (under low and high power) viewed under<br />

the microscope. Photo micrographs <strong>of</strong> the epidermal features were taken from the slides using a Light microscope<br />

fitted with a Cannon digital camera (5.0 mega pixels). The terminologies for the epidermal morphology are that <strong>of</strong><br />

Metcalfe (1960) and Van Cottem (1973).<br />

RESULTS<br />

The morphological (vegetative) features <strong>of</strong> the three Paspalum species investigated are summarized in Table 1. The<br />

descriptions <strong>of</strong> the leaf epidermal studies are presented in Tables 2; the epidermal and morphological Keys are also<br />

presented while the epidermal slides are illustrated in Plates 1, 2 and 3. The vegetative results <strong>of</strong> the three taxa<br />

studied showed that the habit <strong>of</strong> the three Paspalum species are perrenial herbs with P. scrobiculatum being a turfed<br />

perennial herb. The heights are about the same (60cm) with P. scrobiculatum growing up to 100cm and while <strong>of</strong> the<br />

habit and height <strong>of</strong> is perennial herb and respectively. Similarly the leaf shapes shows that they are all linear<br />

although P. conjugatum is linear lanceolate while the the inflorescence is raceme for P. conjugatum and P.<br />

vaginatum (terminal) and P. scobiculatum is digitate. The stem types varies with P. conjugatum having prostrate<br />

stoloniferous stems, P. scrobiculatum with erect or decumbent stem and P. vaginatum with creeping stoloniferous<br />

stem . Equally, all the spikelets in the three species have two rows with P. scrobiculatum and P. vaginatum being<br />

hairless while P. conjugatum has hairs.<br />

30


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 1: Vegetative characters <strong>of</strong> the three Paspalum species studied<br />

Characters Paspalum conjugatum Paspalum scrobiculatum Paspalum vaginatum<br />

Habit Perennial herb Turfed perennial herb Perennial herb<br />

Height 60cm 60-100cm 60cm<br />

Stem type Prostrate stolon Erect or decumbent Creeping stolon<br />

Leaf shape Linear or lanceolate Linear Linear<br />

Leaf texture Smooth with hairy margins S<strong>of</strong>t with rough margins and<br />

sometimes hairy<br />

31<br />

Smooth and hairless<br />

Inflorescence Raceme Digitate Terminal raceme<br />

Spikelet Two rows and hairy Two rows and hairless Two rows and hairless<br />

Ligules Toothed Distinct and short Dense<br />

Table 2: Summary <strong>of</strong> leaf epidermal features<br />

Species Surface MIC MAH PRK PAP SSc OPB Distribution<br />

<strong>of</strong> stomata<br />

Paspalum conjugatum<br />

Berg.<br />

Paspalum<br />

scrobiculatum L.<br />

Paspalum vaginatum<br />

Sw.<br />

AD C<br />

IC<br />

AB C<br />

IC<br />

AD C<br />

IC<br />

AB C<br />

IC<br />

AD C<br />

IC<br />

AB C<br />

IC<br />

-<br />

b<br />

-<br />

B<br />

-<br />

b<br />

-<br />

B<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

+<br />

-<br />

+<br />

-<br />

+<br />

-<br />

+<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

-<br />

+<br />

-<br />

-<br />

LD, T<br />

T<br />

T<br />

T<br />

LD<br />

T<br />

Db, S<br />

-<br />

S, Cr<br />

-<br />

Db, Cr<br />

-<br />

Db, Cr<br />

-<br />

HES<br />

-<br />

Db, Cr<br />

-<br />

AMP<br />

AMP<br />

AMP


Legends for Plates and Table 2<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

AB = Abaxial surface SHC = Short cell<br />

AD = Adaxial surface C = Coastal zone<br />

OPB = Opaline body LD = Low dome shaped<br />

IC = Intercoastal zone S = Saddle shaped<br />

MIC = Micro-hair Cr = Cross shaped<br />

b = Bi-cellular Db = Dumb bell shaped<br />

MAH = Macro-hair Amp = Amphistomatic<br />

PRK = Prickle HES = Horizontally elongated surface<br />

PAP = Papillae SSc = Subsidiary cell<br />

LNC = Long cell T = Triangular<br />

+ = Present - = Absent<br />

Paspalum conjugatum Berg.<br />

Leaf blade up to 9.5cm long and 6.1mm broad, with prickles and macro-hairs present on leaf margins.<br />

a. Adaxial surface: Clearly separated into coastal and intercoastal zone.<br />

Solitary short cells are present in the intercoastal zone. Long cell vary from slightly to straight anticlinal walls.<br />

Prickles present in the intercoastal zone. Bi-cellular micro-hairs with distal cell having tapering apices present in the<br />

intercoastal zone. Papillae and micro-hair were absent in the coastal and intercoastal zones. Subsidiary cells <strong>of</strong> the<br />

stomata vary from low-dome to triangular shape. Opaline bodies <strong>of</strong> the coastal zone vary from dumbbell to rounded<br />

or saddle shaped<br />

b. Abaxial surface: Clearly separated into coastal and intercoastal zone<br />

Long cells rectangular shaped with some tending to be square shaped with sinuous anticlinal walls. Long cells<br />

observed in the coastal zone. Bi-cellular micro-hairs present in the coastal zone, distal cells with tapering apices.<br />

Prickles present in the intercoastal zone. Macro-hairs and papillae absent, subsidiary cells <strong>of</strong> stomata are triangular<br />

shaped. Opaline bodies mostly saddle shaped, occasionally cross shaped in the coastal zone<br />

32


Plate 1a Adaxial surface <strong>of</strong> P. conjugatum<br />

Plate 1b Abaxial surface <strong>of</strong> P. conjugatum<br />

Paspalum scrobiculatum L.<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Leaf blade up to 16cm long and 0.9mm broad with prickles and macro-hairs present on margins.<br />

a. Adaxial surface: Clearly distinguished into coastal and intercoastal zone.<br />

Long cell are rectangular shaped with some tending to be square with sinuous walls. Solitary short cells present in<br />

the intercoastal zone. Long cells present in the coastal regions. Bi-cellular micro-hairs present in the intercoastal<br />

zone, with distal cells having tapering apices. Prickles with hook shape present in the intercoastal zone. Papillae and<br />

33<br />

C<br />

C<br />

IC<br />

PRK<br />

IC<br />

MIC<br />

SSc<br />

LNC<br />

LNC<br />

MIC<br />

SSc


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

micro-hairs absent and stomata present with triangular shaped subsidiary cells. Opaline bodies <strong>of</strong> the coastal zone<br />

are mainly cross and dumb bell shaped.<br />

b. Abaxial surface: Coastal and intercoastal zone clearly distinct.<br />

Long cells rectangular shaped with sinuous anticlinal walls. Long cells present in the coastal zone. Solitary short<br />

cells present in the intercoastal zone. Hook shaped prickles present in the intercoastal zone. Papillae and macro-hair<br />

absent, bi-cellular micro-hairs present in the intercoastal region and stomata with triangular shaped subsidiary cells.<br />

Opaline bodies vary from cross to dumb bell shaped in the coastal zone.<br />

Plate 2a Adaxial surface <strong>of</strong> P. scrobiculatum<br />

Plate 2b Abaxial surface <strong>of</strong> P. scrobiculatum<br />

Paspalum vaginatum Sw.<br />

34<br />

C<br />

C<br />

SSc<br />

IC<br />

MIC<br />

IC<br />

SSc<br />

LNC<br />

LNC<br />

MIC


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Leaf blade up to 6cm long and 2.5mm broad with prickles and macro-hairs present on margins.<br />

a. Adaxial surface: Clearly seperated into coastal and intercoastal zone.<br />

Long cell are rectangular shaped with some tending to be square with slightly sinuous to straight anticlinal walls.<br />

Short cells is absent in the intercoastal zone. Macro-hairs and micro-hairs absent, papillae tend to overarch with<br />

stomata in the intercoastal zone. Subsidiary cells <strong>of</strong> the stomata were low-dome shaped. Opaline bodies in the<br />

coastal regions are horizontally elongated.<br />

b. Abaxial surface: Clearly distinguished into coastal and intercoastal zone.<br />

Long cells are rectangular shaped with sinuous anticlinal walls in the intercoastal zone. Long cells present in the<br />

coastal zone. Short cells are paired, occasionally solitary in the intercoastal zone. Prickles, micro-hairs and macrohairs<br />

are absent. Subsidiary cells <strong>of</strong> stomata are triangular shaped.<br />

Opaline bodies vary from dumb bell to cross shaped in the coastal zone.<br />

Plate 3a Adaxial surface <strong>of</strong> P. vaginatum<br />

35<br />

C<br />

IC<br />

PAP<br />

SSc<br />

LNC


Plate 3b Abaxial surface <strong>of</strong> P. vaginatum<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Key to the three species <strong>of</strong> Paspalum studies based on their epidermal features<br />

1. Prickles present on both surfaces………………………………………………2<br />

1. Prickles absent on both surfaces……………………………………………….4<br />

2. Macro-hairs variable on the leaf margins………………………..scrobiculatum<br />

2. Macro-hairs constant on the leaf margins…………………….........conjugatum<br />

3. Papillae present on adaxial surfaces…………………………………………...4<br />

3. Papillae absent on both surfaces……………………………………………….2<br />

4. Micro-hairs present on both surfaces…………………………………………..2<br />

4. Micro-hairs absent on both surfaces………………………………....vaginatum<br />

Key to the three species studies based on their morphological features<br />

Inflorescence: Consisting <strong>of</strong> 2 long slender raceme between 8-15cm that has greenish yellow<br />

spikelets which are almost circular lying flat with hairy fringe on their margin……..P. conjugatum<br />

Inflorescence: Consisting <strong>of</strong> 2-10 racemes, each with two rows <strong>of</strong> overlapping swollen circular<br />

spikelets…...................................................................................................................P. scrobiculatum<br />

Leaves: Borne in two distinct ranks on either side <strong>of</strong> the culm<br />

Inflorescence: Consisting <strong>of</strong> 1-3 racemes, sometimes a pair <strong>of</strong> terminal racemes with 2 rows <strong>of</strong> overlapping ovate<br />

spikelets …………………………………………………..……..P. vaginatum<br />

DISCUSSION<br />

36<br />

C<br />

IC<br />

SSc<br />

OPB<br />

SHC<br />

LNC


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

The morphological (vegetative) features observed showed that there were little or slight differences in the features <strong>of</strong><br />

the three species <strong>of</strong> Paspalum studied and this suggests their differences in species level as they exhibited different<br />

characters though some <strong>of</strong> the characters were quite identical.<br />

Some differences in type <strong>of</strong> stem and the inflorescence and spikelets (Table 1) were observed, although the heights<br />

were almost the same in the three species except for P.scrobiculatum which grows up to 100cm. The analysis <strong>of</strong> the<br />

morphological structure <strong>of</strong> the three studied species has revealed characteristics, which correspond to those<br />

mentioned by Lowe (1989) and Akobundu and Agwayaka (1998). The epidermal cells are arranged in horizontal<br />

files. Leaf epidermis <strong>of</strong> the genus Paspalum is clearly distinguished into coastal and intercoastal zones. The coastal<br />

zones are generally narrower while the intercoastal zones are broader. <strong>Studies</strong> carried out by Sharma and Salam<br />

(1984); Sharma and Mittal (1986) have reported similar observations in other genera and tribes <strong>of</strong> Poaceae. The<br />

epidermal cells possess sinuous, slightly to straight anticlinal walls. Metcalfe (1960) reported similar undulations in<br />

various genera and tribes <strong>of</strong> Poaceae. Explanations have been given for the wavy nature <strong>of</strong> the anticlinal walls <strong>of</strong> the<br />

epidermal cells. One <strong>of</strong> the explanations for this phenomenon relates the undulations to the development <strong>of</strong> stress<br />

during the differentiation <strong>of</strong> the leaf (Avery, 1933). Another concept is that the waviness is caused by the method <strong>of</strong><br />

hardening <strong>of</strong> the differentiating cuticle (Watson, 1942). Furthermore, Linsbauer (1930) and Watson (1942) stated<br />

that the waviness is also affected by environmental conditions prevailing during leaf development. Prickles with<br />

hook shape have been observed in the adaxial and abaxial surfaces <strong>of</strong> P. conjugatum and P. scrobiculatum. Prickles<br />

with angular spines were restricted to the margins <strong>of</strong> leaf lamina <strong>of</strong> the three species., various shapes <strong>of</strong> prickles in<br />

tribes <strong>of</strong> Poaceae have been described by Sharma and Mittal (1986) Sharma and Salam (1984). Font Quer (1975)<br />

defines papillae as the simplest <strong>of</strong> trichomes, characterized by wall projection followed by the protoplast <strong>of</strong><br />

epidermal cells. According to Ellis (1979), Poaceae papillae occur in long and short cells, especially in intercostal<br />

zones, in numbers that may vary from one to many per cell. Papillae are absent in most <strong>of</strong> the three species studied<br />

except on the adaxial surface <strong>of</strong> P. vaginatum where it was found to be present. Thus, the absence <strong>of</strong> papillae in this<br />

last mentioned species can be interpreted as a taxonomic indicator. Micro-hairs observed are mainly bi-cellular with<br />

tapering apices in the intercoastal zones <strong>of</strong> both the adaxial and abaxial surfaces <strong>of</strong> P. conjugatum and P.<br />

scrobiculatum. Metcalfe (1960) have described bi-cellular hairs in a number <strong>of</strong> grass species. Macro-hairs were<br />

absent in the coastal and intercoastal zones <strong>of</strong> the three species but were present on the margins <strong>of</strong> P. conjugatum. In<br />

P. scrobiculatum, it varied (i.e it was present in some and absent in the others). The reason for this could be<br />

probably due to the presence or absence <strong>of</strong> hairs on the leaf margins <strong>of</strong> the grass or other factors could be<br />

responsible. The stomata are restricted to the intercoastal zones on both adaxial and abaxial surfaces. According to<br />

Ellis (1979), the Poaceae stomata generally occur in well-defined bands in intercostal zones, and they may be<br />

classified according to the shape <strong>of</strong> subsidiary cells. Subsidiary cells <strong>of</strong> the stomata varied from triangular to low<br />

dome shape in the adaxial surface <strong>of</strong> P. conjugatum while it was the same in the abaxial surfaces <strong>of</strong> the remaining<br />

two species. Mensah and Gill (1997) have reported similar observations in other genera and tribes <strong>of</strong> Poaceae like<br />

Sporoboleae. Opaline bodies which are depositions <strong>of</strong> silica materials were mainly dumbbell, cross, saddle and<br />

horizontally elongated in shape. The importance <strong>of</strong> opaline bodies as a systematic tool in grasses has been<br />

overemphasized by many researchers including Metcalfe (1960).<br />

Grasses are currently identified based on their floral characters, but a problem encountered with the system <strong>of</strong><br />

identification is that grasses do not flower for a greater part <strong>of</strong> their life cycle. Hence, a biosystematic approach<br />

could be used in tackling this problem through gathering <strong>of</strong> data from various studies such as cytology, palynology,<br />

epidemiology etc. The study <strong>of</strong> different epidermal characters such as macro-hairs, prickles, papillae, micro-hairs,<br />

distribution <strong>of</strong> stomata, nature <strong>of</strong> long cells, subsidiary cells, opaline bodies and surface views <strong>of</strong> the leaf helps us<br />

classify and identify grasses into their various tribes and genus and thus adds to our knowledge on the<br />

biosystematics <strong>of</strong> grass species. It will also be beneficial as a research tool to cytologist, weed scientist and research<br />

workers.<br />

REFERENCES<br />

Akonbondu O.I and Agwaraka W. C (1998) A handbook <strong>of</strong> West African weeds, IITA, Ibadan 564p<br />

Avery G. S Jr (1933). Structure and development <strong>of</strong> the Tobacco leaf. Amer. Jour. Bot. 20: 565-592<br />

37


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Clayton W. D and Renvoize, S. A (1986). Genera Graminae: grasses <strong>of</strong> the world. Royal Bot. Gard. Kew, London.<br />

Kew Bulletin. Additional series XIII<br />

Edeoga H.O and Ikem C.L (2001). Comparative Morphology <strong>of</strong> the leaf epidermis in three species <strong>of</strong> Boehavia L.<br />

Nyctagininaceae. J.Pl. Anat Morph. 1:14-21.<br />

Ellis R. P. (1979). A procedure for standardizing comparative leaf anatomy in the Poaceae II: the epidermis as seen<br />

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Font Quer P. (1975). Diccionario de Botanica. Labor., 1244p.<br />

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Euphytica 104: 119-125<br />

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in Iran Turk J. Bot. 31: 1 – 9.<br />

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Lowe J. (1989). The Flora <strong>of</strong> Nigeria grasses. Ibadan University Press, Ibadan. 326p.<br />

Mensah J.K. and Gill L. S (1997).Cuticular and leaf blade anatomical studies <strong>of</strong> the tribe Sporoboleae (Poaceae)<br />

from West Africa. J.Plant.Anat.Morph.7: 72-81.<br />

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Bengal. Indian J. Tradit. Knowledge 4(4): 396-402.<br />

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in Punjab plains II Leaf epidermis Res. Bull. Pangab Univ. 35: 7 – 11.<br />

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38


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

Digital Moulding <strong>of</strong> the Solicitations within the Dielectric <strong>of</strong><br />

the Transformers and the Evaluation <strong>of</strong><br />

Life Cycle <strong>of</strong> the Insulation Systems<br />

MARIUS-CONSTANTIN POPESCU* and CRISTINEL POPESCU<br />

Faculty <strong>of</strong> Electromechanical and Environmental Engineering, University <strong>of</strong> Craiova,<br />

B-dul Decebal, nr.107, 200440-Craiova, Dolj, ROMÂNIA<br />

*E-mail address for correspondence: mrpopescu@em.ucv.ro<br />

_________________________________________________________________________________________<br />

Abstract: This papers analyses the evaluation methods <strong>of</strong> the wear <strong>of</strong> transformers that occurs on their charging<br />

with alternating load, taking into consideration mainly the thermal ageing <strong>of</strong> electroinsulation material,<br />

especially <strong>of</strong> those <strong>of</strong> A class.<br />

Key-Words: wear <strong>of</strong> transformer, thermal parameters.<br />

_________________________________________________________________________________________<br />

INTRODUCTION<br />

In regular service conditions, the transformer is subject to added solicitations which influence the long-term<br />

response <strong>of</strong> the transformer. Among the elements <strong>of</strong> the transformer, the insulation, which this chapter deals<br />

with, is stressed in different conditions in use from those <strong>of</strong> the lab. In regular service conditions the insulation <strong>of</strong><br />

the transformers is under nominal voltage <strong>of</strong> the electric network, reaching the crest working voltage at the most.<br />

In lab conditions, the insulation <strong>of</strong> the transformers is subject to the action <strong>of</strong> pro<strong>of</strong> stress which has the value,<br />

form and time period appropriate for the concepts and actual conditions <strong>of</strong> coordination <strong>of</strong> the insulation, applied<br />

in transformer plants and distribution stations. As a result, the testing <strong>of</strong> the insulation <strong>of</strong> the transformers in lab<br />

must guarantee the safe running <strong>of</strong> the transformers under most unfavorable conditions. The insulation <strong>of</strong> the<br />

electrical power transformers is subject to different kinds <strong>of</strong> stress, both in real and in lab conditions. In standard<br />

conditions, electrical (<strong>of</strong> nominal voltage and <strong>of</strong> overvoltage), mechanical (due to the short-circuit stresses),<br />

chemical (due to deposits or chemical agents) and thermal (due to changes in temperature and in the atmosphere)<br />

stresses are applied on the insulation. Due to these stresses, in the course <strong>of</strong> utilization, the properties <strong>of</strong> the<br />

electroinsulation materials deteriorate, bringing about the ageing <strong>of</strong> these materials. On the whole, the ageing<br />

process <strong>of</strong> the insulating materials is a complex process because <strong>of</strong> the multitude <strong>of</strong> different kinds <strong>of</strong> factors<br />

which influence it. Among these stresses, those which influence the most the insulation are those due to internal<br />

overvoltage, caused by the changes in the parameters <strong>of</strong> the electroenergetic system, and to external overvoltage<br />

(atmospherical), caused by lightning, the temperature <strong>of</strong> the oil/paper insulation complex from the transformer<br />

respectively. After the changes in the physical properties <strong>of</strong> the electroinsulation materials, changes occurred in<br />

use, the marking <strong>of</strong> the state <strong>of</strong> an insulation can not be carried out taking into consideration a single property<br />

due to the fact that the changes are the result <strong>of</strong> the action <strong>of</strong> a large number <strong>of</strong> external actions, the<br />

combinations <strong>of</strong> which are random, their accurate reproduction being impossible. It is difficult to study the<br />

transformers while they are working, because it would take a long time, namely decades. Shortening the length<br />

<strong>of</strong> the trials could be carried out by introducing accelerated ageing procedures, but these methods do not<br />

guarantee results that can be applied in real conditions. Therefore, the trial conditions must be created in a way<br />

that they are as similar as possible to the real ones and in accordance to the purpose for which the results are<br />

used later on. For this reason, the functional trials carried out on mock-ups are <strong>of</strong> great scientific value.<br />

39


1.External stresses <strong>of</strong> the insulation <strong>of</strong> the electrical power transformers<br />

In the case <strong>of</strong> the external stresses, the potential pulse that applies stresses on the insulation can be:<br />

- full-wave impulse - <strong>of</strong> long standing, after which high voltage oscillations develop in the windings hence<br />

resulting stresses both among the spires and between the winding and the earth point.<br />

- chopped-wave impulse – the amplitude <strong>of</strong> which is not so great, but due to scarp cutting, it can bring about<br />

voltage gradients that are dangerous to the insulation on entrance or at the neutral point <strong>of</strong> the transformer.<br />

- steep-wave impulse – has great amplitude but it lasts little and as a consequence it produces the most stresses.<br />

These can apply stress on the insulation at the table and the insulation among the entrance spires <strong>of</strong> the winding.<br />

In lab conditions, the transformer is subject to a minute sinusoidal pro<strong>of</strong> voltage, namely a pro<strong>of</strong> voltage <strong>of</strong><br />

impulse. Each <strong>of</strong> the pro<strong>of</strong> voltages is referred to maximum overvoltage in use, equating the overvoltage in use<br />

to lab conditions.<br />

The pro<strong>of</strong> voltage <strong>of</strong> the internal insulation with full-wave is stated by the relation:<br />

[Uinc]up=Kt[Ugp]up+0,5UN (1)<br />

where: Kt is coefficient with the value 1.15 for the 6 -35 kV transformers and 1.10 for the 110 and 220 kV<br />

transformers; UN is nominal voltage <strong>of</strong> the winding <strong>of</strong> the transformer.<br />

The pro<strong>of</strong> voltage <strong>of</strong> the internal insulation with the chopped-wave impulse is stated by the relation:<br />

[Uinc]ut=1.15*1.25[Ugp]up (2)<br />

where 1.15 takes into account the cumulative effect, and 1.25 takes into account the increase <strong>of</strong> voltage at the lug<br />

<strong>of</strong> the transformer in relation with the lightning arrester.<br />

The minute sinusoidal pro<strong>of</strong> voltage is stated by the relation:<br />

�U �<br />

inc �<br />

Ua�<br />

�<br />

� � K<br />

si<br />

c<br />

where: βsi is equation coefficient <strong>of</strong> the Usi internal overvoltages in use with the Uα minute pro<strong>of</strong> voltages in lab;<br />

Kc ≈0.9 is the coefficient that takes into account the cumulative effect <strong>of</strong> repeated stresses in exploitation.<br />

2. Factors that determine the state <strong>of</strong> the insulation<br />

The insulation <strong>of</strong> the transformers is influenced by the following factors [1, 2, 4, 5]:<br />

The alien substances in the internal insulation are: moisture left in the insulation after an inappropriate drying<br />

procedure; residues <strong>of</strong> the coating varnish solvent that have not been removed when the windings were dried;<br />

blisters or gaseous inclusions left in the insulation after the filling <strong>of</strong> the transformer with oil; dirt resulted from<br />

an inappropriate operating process. The contamination <strong>of</strong> the external insulation, the thermal operating<br />

conditions and the altitude at which the transformer works. Damping the insulation causes: an increase in<br />

dielectric losses and a decrease in dielectric rigidity. The presence in oil <strong>of</strong> water in the form <strong>of</strong> emulsion (in<br />

dispersed state) leads to a rapid decrease <strong>of</strong> rupturing voltage <strong>of</strong> the oil. The water molecularly dissolved in oil<br />

does not influence the dielectric rigidity and losses. But in the presence <strong>of</strong> alien fields in the oil-water<br />

molecularly dissolved changes into dispersed state leading to the decrease <strong>of</strong> dielectric rigidity. Variations in<br />

temperature also cause changes in rupturing voltage. Thus, when the temperature increases from 20�C to 60�C,<br />

at a frequency <strong>of</strong> 50 Hz, an important increase in rupturing voltage takes place. The electrical insulating oil,<br />

commercially pure, contains an amount <strong>of</strong> moisture, dissolved gases and solid impurities (waste and grains).<br />

When the temperature increases the dilution <strong>of</strong> water increases and the waters turns from the state <strong>of</strong> emulsion<br />

into the state <strong>of</strong> dilution leading to the decrease <strong>of</strong> dielectric rigidity. The effect that the temperature variations<br />

40<br />

(3)


have on the insulation <strong>of</strong> the transformers in a long time cause an ageing <strong>of</strong> the insulation, which loses its<br />

mechanical properties (it becomes fragile). The impurities and the dirt from the atmosphere reduce the value <strong>of</strong><br />

the rupturing voltage <strong>of</strong> the external insulation <strong>of</strong> the transformers, even under working stress. Gaseous<br />

inclusions or blisters lead to partial discharges and thus to the decomposition <strong>of</strong> the structural insulation, having<br />

negative effects on the dielectric rigidity as it decreases. Low atmospheric pressure in mountainous regions cause<br />

the decrease <strong>of</strong> the voltage <strong>of</strong> the external insulation because <strong>of</strong> the decrease <strong>of</strong> the relative density <strong>of</strong> the air.<br />

The quality <strong>of</strong> the impregnation process and especially the polymerization degree <strong>of</strong> the varnish highly influence<br />

the condition <strong>of</strong> the insulation <strong>of</strong> the transformers, incomplete polymerization causing an increase in dielectric<br />

losses, the decrease <strong>of</strong> the dielectric rigidity, the oxidation and ageing <strong>of</strong> the electrical insulating oil.<br />

3. The testing <strong>of</strong> the insulation <strong>of</strong> transformers<br />

The testing with direct voltage have as purpose the finding out <strong>of</strong> the dampness <strong>of</strong> the insulation <strong>of</strong> transformers,<br />

if there are or not deficiencies able to cause partial discharges (gaseous inclusions, deficient junctions), if<br />

changes in the response <strong>of</strong> the dielectric occur by applying stress for a long period <strong>of</strong> time. Based on the<br />

variations from the initial state <strong>of</strong> the insulation, variations caused by the influence <strong>of</strong> dampness, <strong>of</strong> the ageing <strong>of</strong><br />

the insulation <strong>of</strong> the transformers or <strong>of</strong> an overcharge, it can be decided if the occurring deficiencies can be<br />

remedied or if the transformer must be submitted to a general overhaul. Furthermore, the main tests on the<br />

electrical power transformers are presented [4], [7], [10], [12], [14], [15], [16].<br />

The measurement <strong>of</strong> the insulation resistance. The insulation resistance, through the absorption coefficient<br />

R60/R15 allows the estimation <strong>of</strong> the degree <strong>of</strong> moistness <strong>of</strong> the insulation <strong>of</strong> transformers. For a dry enough<br />

transformer the absorption coefficient must relate to the following: R60/R15≥1,5. When applying direct voltage,<br />

in time, an alternative current is established through the dielectric which decreases and then settles at a value.<br />

Initially the current has a high value and thus the insulation resistance has a high value due to the polarization<br />

current and to the charging current. Compared to a dry dielectric, at a damp dielectric, to the polarization current,<br />

displacement current, an orientation component is added and as a consequence the line current rises. The<br />

insulation resistance <strong>of</strong> a dielectric is given by the relation between the applied direct voltage and the resulted<br />

full current. The value <strong>of</strong> the insulation resistance is influenced by the following factors: the value <strong>of</strong> the direct<br />

voltage which is applied, the length <strong>of</strong> applying the voltage, the electrostatic charge, the temperature <strong>of</strong> the<br />

insulation and the dampness degree <strong>of</strong> the insulation. The state <strong>of</strong> the insulation <strong>of</strong> the transformer is determined<br />

through the diagram I=f(U) by means <strong>of</strong> the position <strong>of</strong> the break which appears in the curve at a certain value <strong>of</strong><br />

the voltage. The higher the voltage at which the break appears and the gentler the transfer from a slope to another<br />

is, the better the state <strong>of</strong> the insulation is. If the break appears below the value 2 * U max,<br />

the insulation is<br />

considered to be weakened and the transformer must be overhauled. If the current suddenly increases the<br />

insulation is disrupted and the tests must be stopped. The state <strong>of</strong> the insulation <strong>of</strong> the transformer can also be<br />

determined through the variation <strong>of</strong> the insulation resistance and <strong>of</strong> the current depending on the applied voltage.<br />

After a while the insulation resistance, namely the through the insulation reach a set value. If the stabilization<br />

takes place in a short period <strong>of</strong> time and also at a low value, it means that the conductance component IS is high<br />

compared to the polarization component Ip and consequently the insulation is damp. On the other hand, the low<br />

values <strong>of</strong> the insulation resistance due to the high content <strong>of</strong> water in the insulation do not mean that the<br />

transformer is aged or permanently deteriorated. The insulation resistance is not standardized. It is to be<br />

compared with the values <strong>of</strong> the measurements at the same temperature. If the previous measurements have been<br />

carried out at different temperatures then their values are reduced to the temperature <strong>of</strong> the latest measurement.<br />

The insulation resistance varies in inverse ratio to the temperature. As the measurements can not be carried out<br />

all the time at the same temperature, recomputed values are used, recomputed through recomputation values <strong>of</strong><br />

the insulation resistance depending on the temperature. For each transformer two measurements are carried out<br />

at temperatures between 20�C and 75�C. The relation to the same temperature is performed by the multiplication<br />

or the division <strong>of</strong> the values <strong>of</strong> the insulation resistance with its variation coefficient by the temperature<br />

difference K1 following the values presented in Table 1.<br />

Δt<br />

( 0 C)<br />

Table 1. The values <strong>of</strong> the coefficient <strong>of</strong> variation K1<br />

1 2 3 4 5 10 15 20 25 30 35 40 45 50<br />

Val K1 1.05 1.07 1.12 1.16 1.23 1.4 1.74 2.23 2.65 3.35 4.05 5.15 6,1 7.5<br />

41


The insulation resistance must not drop below 70% <strong>of</strong> the initial value <strong>of</strong> the insulation resistance. When<br />

measuring, the following are taken into consideration:<br />

- For the new transformers, when putting it to service, the R60 value must not be below 70% <strong>of</strong> the its value set in<br />

the factory;<br />

- For the transformers in use, R60 must not drop below the values shown in Table 2.<br />

Un (kV)<br />

Table 2. R60 values for different values <strong>of</strong> the nominal voltage.<br />

R60<br />

20 0 C 50 0 C<br />

≤ 60 300 90<br />

110 – 220 600 180<br />

400 1000 300<br />

In time, the insulation resistance <strong>of</strong> the transformer rises up to practically a set value. The variation <strong>of</strong> the<br />

insulation resistance in relation with the time represents the absorption curve. The measurement <strong>of</strong> the insulation<br />

resistance is carried out after 15, 60s respectively. The absorption coefficient R60/R15 tends to the value 1if the<br />

insulation has a great content <strong>of</strong> dampness. The absorption coefficient provides information on the variation <strong>of</strong><br />

the insulation resistance in time, which is why the state <strong>of</strong> the insulation resistance is judged by absorption<br />

curves and polarization curves. The absorption coefficient is used as one <strong>of</strong> the criteria to establish the dampness<br />

<strong>of</strong> the curves, the shape <strong>of</strong> the absorption curve depending on the degree <strong>of</strong> dampness <strong>of</strong> the dielectric and its<br />

build. The absorption curve shows the variation <strong>of</strong> the insulation resistance in time and <strong>of</strong> the current through the<br />

insulation. The measurements are carried out in the specified thermal and dampness conditions, in fair weather,<br />

at a relative dampness <strong>of</strong> the environment, <strong>of</strong> 80% at the most, taking into consideration the following<br />

observations:<br />

- When it starts working the Kabs value must not be over 5% below the value set in the factory;<br />

- For the transformers in use the Kabs value is not standardized;<br />

- The value <strong>of</strong> the absorption coefficient at 20�C is considered normal if: Kabs≥1,2 for power transformers with<br />

U≤110kV; Kabs≥1,3 for power transformers with U≤110kV.<br />

The dissipation factor. The tgδ dissipation factor is also a criterion for evaluating the state <strong>of</strong> the insulation. The<br />

increase <strong>of</strong> the tgδ value is determined by the chemical degradation <strong>of</strong> the oil, its getting wet, the ageing <strong>of</strong> the<br />

solid insulation affected by dampness, oxigen or by temperature. The measuring <strong>of</strong> tgδ is compulsory for all<br />

transformers <strong>of</strong> over 110kV voltage and powers <strong>of</strong> over 10 MVA inclusive, respecting the following<br />

observations:<br />

- When putting into service tgδ the measuring must be carried out at the temperature recommended in the manual<br />

provided by the factory (±5 0 C), not below 10 0 C .<br />

- The values measured at the putting into function are compared to the values measured in the factory. The<br />

values in use must be kept between the limits provided in the Table 3.<br />

Table 3. Normal values for tgδ.<br />

Un (kV) 20 0 C 50 0 C<br />


In use, the values obtained for tgδ at one <strong>of</strong> the two reference temperatures is compared to the values measured<br />

previously (in the factory, at putting into service). In the case <strong>of</strong> new transformers, the tgδ value must not<br />

increase over the value set in factory with over 30%. If the previous measurement has been carried out at a<br />

different temperature from the one <strong>of</strong> the latest measurement, it will relate to the temperature <strong>of</strong> the latest<br />

measurement by division or multiplication by the coefficient <strong>of</strong> variation K2, depending on the difference <strong>of</strong><br />

temperature Δt ( 0 C).<br />

Δt<br />

( 0 C)<br />

Table 4. The values <strong>of</strong> the coefficient K2<br />

1 2 3 4 5 10 15 20 25 30 35 40 45 50 55 60<br />

Val K2 1.04 1.07 1.10 1.11 1.16 1.26 1.52 1.65 2 2.4 2.55 3 3.4 4 4.5 5.4<br />

For all transformers, the real values <strong>of</strong> the reporting coefficient is determined from the diagram obtained from<br />

measuring the tgδ at the temperature <strong>of</strong> 50±5 0 C, after which the tgδ=f(t) line is used when the temperature has<br />

dropped to 20±5 0 C. For measuring we employ a measuring bridge for MD – 16 capacity assembled after a<br />

Scherine assemblage.<br />

The measuring <strong>of</strong> the ohmic resistance <strong>of</strong> the curves. The purpose <strong>of</strong> the measuring <strong>of</strong> the ohmic resistance <strong>of</strong><br />

the curves is: to determine the real resistance <strong>of</strong> the curves; to check the welds or junctions from the conductors<br />

<strong>of</strong> the windings; to track down the possible interruptions; to make evident the dead short circuits among the<br />

spires or other deficiencies which are reflected in the value <strong>of</strong> the resistance. The measuring is carried out in<br />

direct current at a value that exceeds with 20% the value <strong>of</strong> the non-load current, but it is not to exceed 0,1In.<br />

While the ohmic measurements are carried out, the winding temperature is put down. The measured resistance is<br />

related to another temperature by means <strong>of</strong> the relation:<br />

T � t<br />

R * 2<br />

t � R<br />

2 t1<br />

T � t1<br />

T = 235 both for the copper windings and for the aluminum windings.<br />

Taking these into consideration, some special measurements have been carried out on some electrical power<br />

transformers from Romania. The gathered data, recorded in the task report, have been synthesized in a tabular<br />

and graphic form. Analyzing the result <strong>of</strong> the measurements, conclusions regarding the behaviour <strong>of</strong> the<br />

transformers in use could be drawn. Fig’s 1 and 2 show the results <strong>of</strong> the measurements carried out on electrical<br />

power transformers considered to be matters <strong>of</strong> study. The study has been completed for the main sizes that<br />

characterize the behavior <strong>of</strong> the transformers, from 1998 to 2008. For each size the measured value has been<br />

compared to the normalized value and to the value EPC set in the factory. From the obtained data and the<br />

graphical representations it can be determined that only in the case <strong>of</strong> the transformer T11 (from a Station in<br />

Romania) a negative variation can be observed both <strong>of</strong> the insulation resistance and <strong>of</strong> the tangent delta,<br />

especially between 2004 and 2005. As a consequence, the increase <strong>of</strong> the insulation over the EPC values calls for<br />

a further close surveillance <strong>of</strong> the insulation. The rest <strong>of</strong> the transformers can be considered suitable to be in<br />

service.<br />

Table 5. The result <strong>of</strong> the measurements TS – earth point performed on the T9 power transformer.<br />

EPC<br />

Tg la EPC 38 C<br />

Tg EPC trans la 20C<br />

R 15 EPC la 38 1200 TS-TI Trafo 11<br />

R 15 EPCla 20 2472<br />

R 60 EPCla 38 2400 Vn 20 C= 600 Mohm Vn 50 C=180 Mohm<br />

R 60 EPCla 20 4944 Vn 20 C= 2,5% Vn 50 C= 7 %<br />

R1-rez EPCla 38 1,373 An EPC-1986<br />

t1-EPC 38 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005<br />

Tg mas trans la 20 C 0,23 0,25 0,29 0,28 0,32 0,24 0,28 0,25 0,25 0,23 0,30<br />

Tg masurata 0,35 0,38 0,4 0,42 0,45 0,4 0,42 0,4 0,38 0,4 0,42<br />

%R60mas din R60EPC la 20gr 60 65 51 49 54 60 49 50 41 56 54<br />

R60 transpus la 20 2980 3220 2527 2429 2652 2966 2429 2448 2024 2768 2652<br />

R 60 masurata 1560 1750 1560 1320 1560 1440 1320 1230 1100 1230 1560<br />

Roh plot 1-mas 1,332 1,326 1,312 1,325 1,313 1,345 1,326 1,338 1,325 1,353 1,316<br />

t2-calc la mas 38,0 36,5 35,4 32,9 35,3 33,1 38,9 35,4 37,6 35,3 40,4 33,6<br />

Delta t<br />

kiz<br />

18,0<br />

2,06<br />

16,5<br />

1,91<br />

15,4<br />

1,84<br />

12,9<br />

1,62<br />

15,3<br />

43 1,84<br />

13,1<br />

1,7<br />

18,9<br />

2,06<br />

15,4<br />

1,84<br />

17,6<br />

1,99<br />

15,3<br />

1,84<br />

20,4<br />

2,25<br />

13,6<br />

1,7<br />

k tg 1,65 1,55 1,51 1,38 1,51 1,42 1,65 1,51 1,6 1,51 1,75 1,42<br />

R15 transpus la 20 2197 1748 1426 1838 1105 1813 1041 1325 1593 1766 1586<br />

R15 masurat 1150 950 880 999 650 880 566 666 866 785 933<br />

Kabs 1,36 1,84 1,77 1,32 2,40 1,64 2,33 1,85 1,27 1,57 1,67<br />

(4)


Fig. 1. The variation <strong>of</strong> the insulation resistance <strong>of</strong> the T9 power transformer.<br />

Table 6. The TS – TI measurement results performed on the T 11 power transformer.<br />

EPC<br />

Tg la EPC 38 C 0,49<br />

Tg EPC trans la 20C 0,30<br />

R 15 EPC la 38 2680 TS-masa Trafo 9 st Mare - 199999<br />

R 15 EPCla 20 5521<br />

R 60 EPCla 38 4930 Vn 20 C= 600 Mohm Vn 50 C=180 Mohm<br />

R 60 EPCla 20 10156 Vn 20 C= 2,5% Vn 50 C= 7 %<br />

R1-rez EPCla 38 1,353 An EPC-1986<br />

t1-EPC 38 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006<br />

Tg mas trans la 20 C 0,29 0,25 0,25 0,26 0,30 0,30 0,32 0,28 0,32 0,29 0,32 0,31<br />

Tg masurata 0,45 0,38 0,35 0,4 0,43 0,5 0,48 0,45 0,48 0,5 0,45 0,45<br />

%R60mas din R60EPC la 20gr 33 31 27 27 26 27 26 29 29 32 32 31<br />

R60 transpus la 20 3343 3110 2722 2760 2635 2719 2668 2985 2944 3263 3230 3186<br />

R 60 masurata 1750 1690 1680 1500 1550 1320 1450 1500 1600 1450 1900 1800<br />

Roh plot 1-mas 1,332 1,326 1,312 1,325 1,313 1,345 1,326 1,338 1,325 1,353 1,316 1,322<br />

t2-calc la mas 38,0 36,5 35,4 32,9 35,3 33,1 38,9 35,4 37,6 35,3 40,4 33,6 34,7<br />

Delta t 18,0 16,5 15,4 12,9 15,3 13,1 18,9 15,4 17,6 15,3 20,4 13,6 14,71377<br />

kiz 2,06 1,91 1,84 1,62 1,84 1,7 2,06 1,84 1,99 1,84 2,25 1,7 1,77<br />

k tg 1,65 1,55 1,51 1,38 1,51 1,42 1,65 1,51 1,6 1,51 1,75 1,42 1,46<br />

R15 transpus la 20 3362 3533 1944 2429 1870 3296 3165 3343 2263 2768 2584 2620<br />

R15 masurat 1760 1920 1200 1320 1100 1600 1720 1680 1230 1230 1520 1480<br />

Kabs 0,99 0,88 1,40 1,14 1,41 0,83 0,84 0,89 1,30 1,18 1,25 0,00<br />

Fig. 2. The variation <strong>of</strong> the dissipation factor <strong>of</strong> the T9 power transformer.<br />

Fig. 3. The variation <strong>of</strong> the insulation resistance <strong>of</strong> the T 11 power transformer.<br />

44


Fig. 4. The variation <strong>of</strong> tangent delta <strong>of</strong> the T11 power transformer.<br />

Table 7. The results <strong>of</strong> the TI – earth point measurements performed on the T11 power transformer.<br />

EPC<br />

Tg la EPC 38 C 0,25<br />

Trafo 11<br />

Tg EPC trans la 20C 0,15<br />

R 15 EPC la 38 1000 TI-masa<br />

R 15 EPCla 20 2060<br />

R 60 EPCla 38 2200<br />

Vn 20 C= 600 Mohm Vn 50 C=180 Mohm<br />

R 60 EPCla 20 4532<br />

Vn 20 C= 2,5% Vn 50 C= 7 %<br />

R1-rez EPCla 38 1,373 An EPC-1986<br />

t1-EPC 44 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005<br />

Tg mas trans la 20 C 0,21 0,24 0,30 0,34 0,44 0,44 0,33 0,21 0,29 0,31 0,37<br />

Tg masurata 0,33 0,36 0,42 0,52 0,62 0,72 0,5 0,33 0,44 0,55 0,52<br />

%R60mas din R60EPC la 20gr 70 63 58 67 64 78 71 76 69 79 65<br />

R60 transpus la 20 3171 2852 2608 3036 2890 3543 3220 3423 3128 3600 2924<br />

R 60 masurata 1660 1550 1610 1650 1700 1720 1750 1720 1700 1600 1720<br />

Roh plot 1-mas 1,332 1,326 1,312 1,325 1,313 1,345 1,326 1,338 1,325 1,353 1,316<br />

t2-calc la mas 38,0 36,5 35,4 32,9 35,3 33,1 38,9 35,4 37,6 35,3 40,4 33,6<br />

Delta t 18,0 16,5 15,4 12,9 15,3 13,1 18,9 15,4 17,6 15,3 20,4 13,6<br />

kiz 2,06 1,91 1,84 1,62 1,84 1,7 2,06 1,84 1,99 1,84 2,25 1,7<br />

k tg 1,65 1,55 1,51 1,38 1,51 1,42 1,65 1,51 1,6 1,51 1,75 1,42<br />

R15 transpus la 20 1815 1693 2138 1582 1105 3193 2453 3483 1380 1575 1326<br />

R15 masurat 950 920 1320 860 650 1550 1333 1750 750 700 780<br />

Kabs 1,75 1,68 1,22 1,92 2,62 1,11 1,31 0,98 2,27 2,29 2,21<br />

Fig. 5. The variation <strong>of</strong> the insulation resistance <strong>of</strong> the T11 power transformer.<br />

45


Fig. 6. The variation <strong>of</strong> the dissipation factor <strong>of</strong> the T11 power transformer.<br />

4.Thermal ageing <strong>of</strong> the electroinsulation materials<br />

The lifetime <strong>of</strong> a transformer is influenced by a series <strong>of</strong> factors which determine the changes in physical<br />

properties, properties <strong>of</strong> a mechanical, electrical, thermal or chemical nature.<br />

- Alien substances in the internal insulation: moisture left in the insulation after an inappropriate drying<br />

procedure; residues <strong>of</strong> the coating varnish solvent that have not been removed when the windings were dried;<br />

blisters or gaseous inclusions left in the insulation after the filling <strong>of</strong> the transformer with oil; dirt resulted from<br />

an inappropriate operating process. The damping <strong>of</strong> the insulation brings about an increase <strong>of</strong> the dielectric<br />

losses as well as a decrease <strong>of</strong> the dielectric rigidity.<br />

- The contamination <strong>of</strong> the external insulation, the thermal operating conditions and the altitude at which the<br />

transformer works.<br />

The ageing <strong>of</strong> the transformers occurs due to the alterations <strong>of</strong> the physical properties, ageing that brings about<br />

the reduction <strong>of</strong> their lifetime. The way in which the external factors influence the transformers' lifetime is hard<br />

to study as such a study includes some pro<strong>of</strong> tests that take a great deal <strong>of</strong> time, that is decades. This is why the<br />

study time must be reduced by reducing the period <strong>of</strong> testing and by settling the conditions <strong>of</strong> the testings. For<br />

this purpose functional testings on models are employed. Consequently, mathematical laws have been<br />

established to mirror as much as possible the ageing process <strong>of</strong> the transformers.<br />

Concerning the electrical equipment, the most sensitive component is the insulation, the lifetime <strong>of</strong> which<br />

actually determines the lifetime <strong>of</strong> the equipment. Concerning electrical transformers and static devices<br />

generally, the ageing <strong>of</strong> the insulation is essential. For the lifetime, laws have been defined experimentally to<br />

state the lifetime <strong>of</strong> the insulation. For example the Montsinger’s law in which the lifetime is expressed in<br />

degrees Celsius, while in Bűssing’s law the lifetime is expressed in degrees Kelvin.<br />

���<br />

D � �*<br />

e , (5)<br />

V. M. Montsinger’s relation, valid for temperatures between 90� C and 110� C, namely<br />

B<br />

T<br />

D � A*<br />

e , (6)<br />

W. Bűssing’s relation, valid for a large range <strong>of</strong> temperatures and for a great number <strong>of</strong> materials <strong>of</strong> different<br />

classes, here: D - the lifetime <strong>of</strong> electroinsulant materials; θ, T – the temperature <strong>of</strong> the electroinsulant material<br />

expressed in degrees Celsius, in degrees Kelvin respectively; α, β, A, B – constant specific to the electroinsulant<br />

material.<br />

The ageing method is based on Arhhenius’s equation, which expresses the degradation rate <strong>of</strong> an electroinsulant<br />

material:<br />

46


�E<br />

�<br />

� � A*<br />

e KT<br />

, (7)<br />

Arhhenius’s relation, where: A is constant specific to the material; ΔE is activation energy; K is Boltzman’s<br />

constant; T is the temperature <strong>of</strong> the electroinsulant material expressed in degrees Kelvin.<br />

The law expressed by the relation (5) was established by V.M. Montsinger and it was proved to be valid for A<br />

class electroinsulant materials, but for a relatively limited range <strong>of</strong> temperature, 90�C...110�C. The law given by<br />

the relation (6) was demonstrated for the first time by W. Bűssing through the kinetic theory <strong>of</strong> chemical<br />

reactions and it proved to be valid for a great deal <strong>of</strong> electroinsulant materials <strong>of</strong> different classes and for a wide<br />

range <strong>of</strong> temperatures. The lifetime laws <strong>of</strong> electroinsulant materials take into account not only the temperature<br />

as decisive factor, but also the other factors. The other factors are taken into account when choosing the<br />

constants A and B, and α and β. The values <strong>of</strong> these constants are chosen in keeping with functional trials <strong>of</strong><br />

accelerated ageing. The factors which determine the ageing <strong>of</strong> the transformers determine their lifetime, deriving<br />

from the lifetime equation <strong>of</strong> transformers. Thus, the ageing <strong>of</strong> transformers is marked by:<br />

- The relative factor <strong>of</strong> thermal ageing, also named relative factor <strong>of</strong> thermal wear<br />

- Relative thermal ageing, also named relative thermal wear.<br />

The relative factor <strong>of</strong> thermal ageing is defined by:<br />

� B B �<br />

� � �<br />

�TN<br />

T � � � e<br />

(8)<br />

where: T is the absolute temperature expressed in degrees Kelvin; TN is the absolute temperature at which a<br />

normal lifetime if obtained; B is a constant characteristic to the material.<br />

Considering that the temperature varies in relation to time, the relative ageing factor will be, too, time function as<br />

follows:<br />

�(<br />

t) � e<br />

� B B<br />

� �<br />

�TN<br />

T<br />

The relative ageing factor p(t) marks the degradation rate <strong>of</strong> the insulating material and, thus, the extent <strong>of</strong> heat<br />

density <strong>of</strong> the electroinsulant material. Relative thermal ageing is given by the average value <strong>of</strong> the relative<br />

ageing factor in a certain period <strong>of</strong> time, namely:<br />

Replacing the expression for p(t), we obtain:<br />

1 �t<br />

u(<br />

t)<br />

�<br />

�t<br />

0<br />

47<br />

�<br />

� � � t �<br />

��(<br />

t)<br />

dt<br />

1<br />

u(<br />

t)<br />

� � e<br />

�t<br />

� B B �<br />

�t � � �<br />

�TN<br />

T ( t)<br />

�<br />

The two obtained expressions mark the thermal ageing <strong>of</strong> the electroinsulant material for a single time interval<br />

taken into consideration. If there are several time intervals taken into consideration, the expression <strong>of</strong> relative<br />

thermal ageing becomes:<br />

0<br />

(9)<br />

(10)<br />

(11)


n<br />

�ui�ti<br />

u(<br />

t)<br />

� i�1<br />

n<br />

(12)<br />

� �ti<br />

i�1<br />

Considering the same range <strong>of</strong> validity for the relations (5) and (6) written for the temperatures θ şi θN, and T şi<br />

TN, by equaling the following results:<br />

where the following can be written:<br />

and:<br />

e<br />

��<br />

( � ��<br />

)<br />

� �<br />

e<br />

N � e<br />

��(<br />

�N<br />

��)<br />

48<br />

B B<br />

�<br />

TN<br />

T<br />

1 �t<br />

����<br />

��<br />

�<br />

N ( t)<br />

u<br />

�<br />

� e dt<br />

�t<br />

0<br />

The two relations allow the evaluation <strong>of</strong> the ageing and wear degree <strong>of</strong> the insulation <strong>of</strong> electrical transformer.<br />

Where transformers are concerned, temperature is the main factor that influences their behavior, affecting<br />

especially the oil/paper insulation. In this case, dampness is another influencing factor, besides temperature. The<br />

ageing state marked by the thermal ageing factor p, the relative thermal ageing u, respectively, does not allow a<br />

different marking <strong>of</strong> the insulation considering temperature as main influencing factor. And that is because the<br />

degradation rate <strong>of</strong> the insulation is influenced by dampness at any temperature, and the ageing p factor may be<br />

considered as a ratio between two degradation rates, one <strong>of</strong> which the working temperature θ is expressed in<br />

degrees Celsius, namely T expressed in degrees Kelvin, the other at standard temperature θN, TN respectively, the<br />

relative ageing u being the average value <strong>of</strong> the ageing factor p in a certain period <strong>of</strong> time. thus, it may be<br />

considered that, if the change in the dampness degree influences in the same way the degradation rate <strong>of</strong> the<br />

oil/paper insulation, the ageing factor p can be regarded non dependent on dampness. The main component <strong>of</strong><br />

the ageing factor p is temperature, but at the same time, through the material constants α and β (actually θ şi β),<br />

A and B respectively (actually TN and B), it depends on the other chemical, mechanical or electrical factors that<br />

influence the ageing process <strong>of</strong> the oil/paper insulation from <strong>of</strong> the transformers.<br />

5.Thermal wear <strong>of</strong> the transformers<br />

In most cases the thermal wear <strong>of</strong> transformers in oil is determined by the wear <strong>of</strong> the paper impregnated with oil<br />

insulation. It is usually exposed to the highest <strong>of</strong> temperatures <strong>of</strong> the transformer close to the curves. The starting<br />

points <strong>of</strong> analyzing the wear <strong>of</strong> the transformer are two distinct cases: the temperature <strong>of</strong> the transformer varies<br />

distortionless with time and the temperature varies exponentially with time. Each <strong>of</strong> the cases can be treated as<br />

having as basis either Molntsinger’s law (5) or Bűssing’s law (6) [6], [9], [11], [14].<br />

6.1. The case <strong>of</strong> distortionless variation <strong>of</strong> temperature in relation with time<br />

The case in which the ageing <strong>of</strong> the transformer is reflected by Montsinger’s law (5). Taking into consideration<br />

at the initial moment t=0, θ=θi, after a time t=tf the temperature θ=θf respectively, the distortion less variation <strong>of</strong><br />

the temperature can be written in relation with time, in degrees Celsius, after an expression as follows:<br />

t<br />

� ( t) � �i<br />

� ��<br />

�t<br />

,<br />

��<br />

� �<br />

f � �i<br />

(13)<br />

(14)<br />

(15)<br />

(16)


where: θi is the temperature at the beginning <strong>of</strong> the time period taken into consideration, expressed in degrees<br />

Celsius; θf is the temperature at the end <strong>of</strong> the time period taken into consideration, expressed in degrees Celsius;<br />

Δt is the period <strong>of</strong> time during which the temperature increases from θi to θf.; t is time as current variable.<br />

The case in which the lifetime law <strong>of</strong> the transformer is expressed by the relation (6) given by Bűssing. In this<br />

case, the temperature variation in relation with time is expressed in degrees Kelvin after an expression as the<br />

following:<br />

T( t)<br />

� Ti<br />

� �T<br />

t<br />

�t<br />

There are the following relations between the two temperatures:<br />

,<br />

49<br />

T T � � �<br />

f i T<br />

(17)<br />

Ti=273+ θi; Tf=273+ θf, (18)<br />

namely ΔT=Δθ (19)<br />

The thermal ageing factor p as well as the relative thermal ageing u by means <strong>of</strong> their parameters link the relative<br />

sizes that lead to the ageing <strong>of</strong> the materials and based on the variation <strong>of</strong> these factors in time the curves that<br />

will characterise the ageing <strong>of</strong> the electroinsulant materials will be able to be marked <strong>of</strong>f. This paper deals with<br />

the evaluation <strong>of</strong> the relative thermal wear based on the Montsinger’s law employing the relation (5).<br />

Thus, considering the distortionless variation <strong>of</strong> temperature the relation becomes:<br />

By integrating the expression u(t), we bwill obtain:<br />

� � t ��<br />

�t ����N<br />

���i<br />

���*<br />

�<br />

1<br />

�<br />

t<br />

u t � e � � � �<br />

( ) � *<br />

�dt<br />

�t<br />

0<br />

1 � ��<br />

u � * e<br />

���<br />

��<br />

��N ��<br />

f � ��<br />

�<br />

�� ��<br />

e N i �� ��<br />

The expression (21) allows us to determine by computing the relative thermal wear, applicable both for a cooling<br />

process and in the case <strong>of</strong> one cooling process.<br />

6.2 The case <strong>of</strong> exponential variation <strong>of</strong> temperature in relation with time<br />

The exponential variation <strong>of</strong> temperature is deducted using the heating equation considering the parameter<br />

constant Tt only in input condition with P=constant. When I= constant, Tt depends on I, and when U=constant it<br />

depends on U and t. In these conditions we will continue to consider the hypothesis that P=constant and/or<br />

I=constant.<br />

In the case <strong>of</strong> exponential variation <strong>of</strong> temperature, temperatures θ and T become:<br />

respectively:<br />

t<br />

�<br />

T<br />

� �t� � �<br />

t<br />

r � ��*<br />

e<br />

(20)<br />

(21)<br />

(22)


T<br />

�t� � T � �T<br />

* e<br />

r<br />

where: θr, Tr – stand for stationary regime temperatures expressed in degrees Celsius, and degrees Kelvin<br />

respectively; Δθ, ΔT – stand for the difference between the stationary regime temperature and the temperature at<br />

the beginning <strong>of</strong> the thermal process expressed in degrees Celsius, and degrees Kelvin respectively; Tt is time<br />

constant with wich the temperature variation process takes place[s], having the following relation between the<br />

temperatures:<br />

50<br />

t T<br />

t<br />

�<br />

(23)<br />

Tr=273+ θr; Δθ=ΔT (24)<br />

The temperature differences Δθ, ΔT are <strong>of</strong> different symbols, according to the process, whether it is <strong>of</strong> cooling or<br />

<strong>of</strong> heating. If we take into consideration the thermal wear based on Montsinger’s relation, the following results:<br />

�t<br />

1<br />

u � � e<br />

�t<br />

0<br />

� � t ��<br />

� � � ��<br />

����<br />

���<br />

���<br />

T<br />

N<br />

��<br />

� �<br />

r * e t<br />

��<br />

� �<br />

�<br />

� �<br />

��<br />

�<br />

Placing the independent <strong>of</strong> time factors before the integral, the following results:<br />

��<br />

u �<br />

�� � � � �t<br />

N r<br />

�<br />

�t<br />

0<br />

e<br />

t<br />

�<br />

����*<br />

e<br />

Tt<br />

Consequently, the wear variation u can be figured for different values <strong>of</strong> the material constat β and certain values<br />

<strong>of</strong> the time value Tt.<br />

In order to simplify the display, relative values can be thus used:<br />

� � ��<br />

*<br />

;<br />

With the above, the expression <strong>of</strong> thermal wear becomes:<br />

e<br />

u �<br />

* t<br />

t �<br />

Tt<br />

�<br />

�� *<br />

��<br />

*<br />

�<br />

�<br />

�<br />

r N<br />

� �t *<br />

���<br />

* �<br />

*<br />

e<br />

t<br />

* � e<br />

�t<br />

0<br />

;<br />

dt<br />

dt<br />

* dt<br />

dt �<br />

Tt<br />

The value <strong>of</strong> the integral in the expression <strong>of</strong> the thermal wear depends on the parameters Δθ * and Δt * which<br />

have a symbol for a cooling process and a different one for a heating process. Thus, in the case <strong>of</strong> the heating<br />

process Δθ * is positive, and in the case <strong>of</strong> the cooling process Δθ * is negative. Consequently, the evaluation <strong>of</strong><br />

the thermal wear must be dealt with differently.<br />

dt<br />

*<br />

(25)<br />

(26)<br />

(27)<br />

(28)


6.2.1 The case <strong>of</strong> thermal heating process<br />

In the case <strong>of</strong> the thermal heating process, Δθ * being positive, the following form <strong>of</strong> expressing the heating<br />

integral Ii appears to be more convenient, employing the relation (28):<br />

�t *<br />

�e�<br />

�ln ��<br />

*<br />

�t<br />

*<br />

�<br />

�<br />

� � � *<br />

Ii<br />

� e<br />

dt<br />

0<br />

If lnΔθ * -t * is noted with x, dx=-dt * results, the expression <strong>of</strong> the integral Ii becoming:<br />

The function<br />

I<br />

51<br />

(29)<br />

ln ��<br />

*<br />

�e<br />

x<br />

i � � e dx<br />

ln ��<br />

*<br />

��t<br />

*<br />

(30)<br />

y � e<br />

is shown in the Fig. 7a the shaded area represents the value <strong>of</strong> the integral in the relation (10).<br />

�e<br />

a) b)<br />

Fig. 7. The variation <strong>of</strong> function: a) y=f(x); b) f(x).<br />

The value <strong>of</strong> the integral can be expressed as a difference between two values <strong>of</strong> the function f(x):<br />

Considering the limits <strong>of</strong> integration:<br />

x<br />

� 0 x<br />

f ( x)<br />

x<br />

* *<br />

x ln�� � �t<br />

the integral Ii can be expressed at heating as it follows:<br />

� ,<br />

� e<br />

�e<br />

x<br />

dx<br />

*<br />

0 � ln�<br />

x<br />

(31)<br />

(32)<br />

(33)


� � � � *<br />

* *<br />

ln�� � �t<br />

� ln��<br />

Ii � f<br />

f<br />

(34)<br />

The graphical representation <strong>of</strong> f(x) in relation to x is shown in Fig. 7b where the way <strong>of</strong> obtaining the integral Ii<br />

is also explained. The graphical representation requires the setting <strong>of</strong> the limits <strong>of</strong> integration x0 and xi <strong>of</strong> the<br />

heating integral Ii. The limit <strong>of</strong> integration x0 is chosen in a way that it accomplishes the condition lnΔθ *


where:<br />

Ir � g<br />

x<br />

x<br />

e �e 1�<br />

�(<br />

x)<br />

� � �<br />

x<br />

0<br />

53<br />

dx<br />

*<br />

* * * *<br />

�ln�� ��<br />

���<br />

g�ln��<br />

��<br />

��<br />

t � � �t<br />

� �t<br />

a) b)<br />

Fig. 8. The variation <strong>of</strong> the function y= e .<br />

The graphical representation <strong>of</strong> the function � (x)<br />

is shown in the Fig. 8b, illustration followed by the<br />

explanation <strong>of</strong> how the integral Ir is obtained. The random limit <strong>of</strong> integration x0, similar to the case <strong>of</strong> the<br />

heating process, depends on the sought accuracy in obtaining the value <strong>of</strong> the integral Ir. If a 1% error is<br />

accepted, it can be considered that at cooling the curve y is identical with an asymptote to which it tends<br />

(ordinate asymptote 1) when y reaches the value 1.01. The corresponding abscissa is a result <strong>of</strong> e �1,<br />

01 as<br />

being x0= - 4.6. Thus, for x


values <strong>of</strong> the constants β şi B. Fig. 9 [9] shows: curve 1 with dotted line – relation (14), corresponding to the “8<br />

degree Celsius rule”, with β=0.08664 0 C -1 ; curve 2 with dotted line - relation (14), corresponding to the “6<br />

degree rule”, with β=0.11552 0 C -1 ; curve 1 with solid line – relation (8), with B=11500 0 K; curve 2 with solid<br />

line – relation (8), with B=14573 0 K; curve 3 with solid line – relation (8), with B=17184 0 K.<br />

For all the cases the following were considered : θN=95 0 C, and TN=368 0 K, resulting ρ=1.<br />

θN and TN represent the temperature at which the degradation rate <strong>of</strong> the electroinsulant material is considered to<br />

be normal. These constants have been set starting from the hypothesis that the highest temperature admisible<br />

must allow a 25000 hour working time <strong>of</strong> the transformer, that is at a temperature <strong>of</strong> 95�C about 30 years <strong>of</strong><br />

working time. Thus, taking into consideration the lifetime laws and all the above mentioned, θN is considered to<br />

be ranging between 95 0 şi până la 98 0 C. Even 110�C is acceptable. The highest temperature admisible<br />

determines the aspect <strong>of</strong> the curves that characterise the thermal wear <strong>of</strong> the transformers [11], [13]. Regarding<br />

the transformers with oil its limit is 115�C<br />

Fig. 9. The variation curves <strong>of</strong> the thermal ageing relative factor ρ in relation to the temperature.<br />

Sometimes in cases <strong>of</strong> overvoltage conditions, this peak temperature can increase, without having negative<br />

effects on the way the transformer works though. Experiments have revealed that in cases <strong>of</strong> overvoltage the oil<br />

can reach 115�C, while the curves can reach even 200�C. This does not break the transformer if it lasts between<br />

one and four hours, but it influences its ageing process. In case <strong>of</strong> shortcircuits the temperature limit <strong>of</strong> 250�C is<br />

considered, in the hottest spot <strong>of</strong> the transformer.<br />

6.2.3 The heating process case<br />

The numerical computation <strong>of</strong> the function f(x) defined by the relation (31) allows the evaluation <strong>of</strong> the thermal<br />

ageing <strong>of</strong> the transformer in case <strong>of</strong> a heating process, the limits <strong>of</strong> integration x0 and xi being set according to<br />

the above.<br />

Thus, the limit <strong>of</strong> integration x0 is obtained from the condition:<br />

where lnΔθ*max is the peak value <strong>of</strong> Δθ* that can appear in use.<br />

X0>lnΔθ*max (42)<br />

The starting point is the hypothesis that the peak temperature <strong>of</strong> stationary regime that can appear in use is<br />

Δrlim=200 0 C. In this case, the initial temperature can be lower than that which determines a minimum thermal<br />

wear relative factor ρmin which must be taken into account. Therefore, when computing the function f(x) that<br />

minimum value <strong>of</strong> Δθ is taken into account, value which at θr=200 0 C determines a temperature <strong>of</strong> which a<br />

relative wear factor ρmin complies with. For higher values <strong>of</strong> Δθ, we will consider ρ=0 and so f(x), too. Taking all<br />

these into consideration Δθ*max will be obtained from the condition:<br />

54


� �� ���<br />

���<br />

��<br />

� N r<br />

then considering ρmin=0.1 and θr=200 0 C the following results:<br />

e<br />

55<br />

max � �<br />

min<br />

(43)<br />

Δθ*max=β(200-θN)+2.3 (44)<br />

Taking into account the relation (43) in order to obtain the highest value <strong>of</strong> Δθ*max the lowest value possible<br />

must be considered for θN and the highest for β. On the observations carried out previously we can consider the<br />

extreme values θN=95 0 C, and β=0.126 0 C -1 . We thus obtain:<br />

From the relations (41) and (44) the following results:<br />

Δθ*max=0.126*(200-95)+2.3=15.53 (45)<br />

X0=ln 15.53=2.75 (46)<br />

When x has values over 2.75, we consider f(x)=0. The lower value <strong>of</strong> the variable x that is taken into<br />

consideration is the one defined by the relation (31), namely xi= - 4.6. Fig. 10 [8] presents the variation curves<br />

for f(x), and Δθ respectively, for different values <strong>of</strong> the constant β.<br />

Fig. 10. The variation <strong>of</strong> the function f(x) and <strong>of</strong> temperature for different values <strong>of</strong> the material constant β.<br />

When using the curve f(x) the wear corresponding to the wear factors below 0.1 is neglected only in the critical<br />

case θr=θrlim. At other values <strong>of</strong> θr by using the curve f(x) the neglect <strong>of</strong> the wear appears in the case <strong>of</strong> wear<br />

factors below a critical case <strong>of</strong> ρ than 0.1. This critical case can be determined with the relation:


considering x0=2.75.<br />

56<br />

x<br />

�� ���<br />

�e<br />

0 ��<br />

��<br />

N r<br />

� lim � e<br />

(47)<br />

As established, the constant ρlim depends on the parameters β, θr, θN, but it must always be ρlim≤0,1.<br />

6.2.4 The cooling process case<br />

The numerical computation <strong>of</strong> the function φ(x) defined by the relation (39) allows the evaluation <strong>of</strong> the thermal<br />

ageing <strong>of</strong> the transformer in case <strong>of</strong> a cooling process, the limits <strong>of</strong> integration x0 and xi being set according to<br />

the above. Thus, the value <strong>of</strong> the minimum limit is x0= - 4.6. The upper limit <strong>of</strong> integration results from the<br />

condition:<br />

xS<br />

�� � �<br />

� ln �<br />

* max<br />

considering –Δθ*max as the peak value for -Δθ* that can appear in use.<br />

As shown previously, we take the hypothesis that the cooling temperature can not be higher than 140�C as<br />

starting point. Exaggeratedly considering that the cooling takes place towards 0�C, the following results –<br />

Δθ*max=140 0 C. The peak value <strong>of</strong> -Δθ* complies with the peak value <strong>of</strong> β=0.126 0 C -1 . Consequently we obtain:<br />

(48)<br />

xS=ln(0.126*140)=2.87 (49)<br />

With the limits x0 şi xs thus delimited in the Fig. 11 the variation <strong>of</strong> the function φ(x) has been featured together<br />

with that <strong>of</strong> Δθ with the help <strong>of</strong> which the evaluation <strong>of</strong> the ageing factor <strong>of</strong> the insulation <strong>of</strong> the transformer can<br />

be carried out. The function φ(x) becomes equal with zero when x=-4.6. Because when x=-4.5, φ(x)=0.001<br />

results, employing the curve in Fig. 11 [9] we will consider φ(x)=0 la x≤-4.5.<br />

Fig. 11. The variation <strong>of</strong> the function φ(x) and <strong>of</strong> size Δθ for different material constants β.


6.3. Computing examples<br />

As stated previously, the lifetime as well as the wear factor determines the state <strong>of</strong> ageing <strong>of</strong> the transformers.<br />

For example, by using the Mathcad medium, the cases <strong>of</strong> some transformers from a transformer station from<br />

Romania has been taken into consideration.<br />

1) In the case <strong>of</strong> the first transformer, to compute the wear the following initial data have been used: the initial<br />

temperature θi=78 0 C, the temperature is considered to vary exponentially with time, the stationary regime value<br />

is θr=110 0 C, the time period <strong>of</strong> the thermal process is considered to be 2.25 hours, the time constant <strong>of</strong> the<br />

thermal process is considered to be 1.5 hours. θN=95 0 C şi β=0.086643 0 C -1 are accepted, considering the “8<br />

degree Celsius rule”. The stationary regime temperature being higher than the initial temperature, and so a<br />

heating process takes place for which Δθ=110-78=32 0 C and as a consequence the f(x) curve will be used to<br />

determine the values x1 and f(x1). Therefore, on the basis <strong>of</strong> the diagram in Fig. 10 for β=0.086643 0 C -1 , the<br />

following values will be obtained: x1=1.02, f(1.02)=0.01745. Using relative values we obtain:<br />

For the limit x2 the following is obtained x2=x1-Δt * =1.02-1.5=-0.48 with which f(-0.48)=0.4376 complies.<br />

Consequently, considering the relations 28 and 33, the thermal wear will be:<br />

e<br />

u �<br />

0.<br />

086643<br />

1.<br />

5<br />

�110�95� �0. 4376 � 0.<br />

01745�<br />

�1.<br />

03<br />

As the wear u is over unity, the thermal wear for the considered time period is lower than the normal wear. From<br />

the Fig. 10, it can be established that, at the end <strong>of</strong> the time period, as x2=-0,48 complies with Δθ=7 0 C, the final<br />

temperature will be θf=110-7=103 0 C.<br />

2) In the case <strong>of</strong> the second transformer, the initial data are the following: the initial temperature θi=120 0 C, the<br />

temperature varies exponentially with the time, the stationary regime temperature is θr=85 0 C, the period <strong>of</strong> time<br />

for the thermal process is 4 hours, the time constant <strong>of</strong> the thermal process is 2 hours. θN=98 0 C şi β=0.11552 0 C -<br />

1 0<br />

are accepted, taking into consideration the six degrees rule. From the initial data, Δθ=85-120=-35 C, resulting<br />

that we are dealing with a cooling process, the function φ(x) will be employed. From the diagram φ(x), for the<br />

value β=0.11552 0 C -1 , the following results: –Δθ=35 0 * 4<br />

C, x1=1.40, φ(1,40)=18.42; in relative values: �t � � 2 .<br />

At x2=x1-Δt * =1.40-2=-0.60, in Fig. 11, we can establish φ (-0.60)=0.62. The thermal wear, computed on the<br />

basis <strong>of</strong> the relations (28) and (41), will be:<br />

0,<br />

11552<br />

e<br />

u �<br />

�85�98� 18,<br />

42 � 0,<br />

62 � 2<br />

2<br />

� � � 2,<br />

21<br />

Furthermore, with the help <strong>of</strong> the graphical representations in Fig. 11 the temperature at the end <strong>of</strong> the 4 hour<br />

period can be established. Thus, from the diagram <strong>of</strong> the function φ (x), for x2=-0.6 –Δθ=5 0 C will result and so<br />

the final temperature will be: θf=85+5=90 0 C.<br />

3) The general case in which the variation range <strong>of</strong> the constant β can be considered with the following initial<br />

data: the initial temperature θi=75 0 C, the temperature varies exponentially with time, the stationary regime<br />

temperature is θr=110 0 C and θN=95 0 C. The graphical representation <strong>of</strong> the function f(x) by reproducing the<br />

coordinates, is presented in Fig. 12.<br />

57<br />

.<br />

�t<br />

*<br />

�<br />

2,<br />

25<br />

1,<br />

5<br />

2<br />

�<br />

1,<br />

5<br />

.


Fig. 12. The variation <strong>of</strong> the function f(x).<br />

The variation <strong>of</strong> the thermal wear with the variable parameter with the help <strong>of</strong> the Mathcad program is shown in<br />

Fig. 13.<br />

Fig. 13. The variation <strong>of</strong> the thermal wear with the material constant β.<br />

Considering the same initial data we can observe the variation <strong>of</strong> the thermal wear with the temperature in Fig.<br />

14.<br />

58


Fig. 14. The variation <strong>of</strong> thermal wear with temperature.<br />

CONCLUSIONS<br />

As a result <strong>of</strong> the studies carried out, it can be stated that a number <strong>of</strong> the transformers from different transformer<br />

stations are improperly employed, that is under their real potential. An estimation <strong>of</strong> the wear <strong>of</strong> the transformers<br />

and <strong>of</strong> their ageing degree can be carried out considering the lifetime law by taking into consideration certain<br />

grounds and specific particularities:<br />

- the transformers are subject to different stresses, among which the thermal stress can be considered to be the<br />

most significant;<br />

- transformers can be considered to have a certain typical thermal behaviour;<br />

- the evaluation <strong>of</strong> the behaviour is carried out by applying the lifetime law with certain values <strong>of</strong> the constants<br />

that interfere with the law, most <strong>of</strong>ten making use <strong>of</strong> the rule <strong>of</strong> ”n” degrees. The most eloquent results have<br />

been obtained by using the “8 degree Celsius rule”;<br />

- certain load curves, <strong>of</strong> special shapes, are allowable.<br />

The thermal behaviour <strong>of</strong> transformers can be understood by means <strong>of</strong> mathematical relations, simulated through<br />

mathematical computation programme, such as the Mathcad programme. The results <strong>of</strong> the mathematical<br />

simulation can be visualised using curves and tables in which a particularization <strong>of</strong> the calculus is needed having<br />

in view: the behaviour <strong>of</strong> the transformers from a thermal point <strong>of</strong> view, the charging conditions <strong>of</strong> the<br />

transformer, the characteristics <strong>of</strong> the insulation and the evaluation method <strong>of</strong> the thermal ageing <strong>of</strong> the<br />

insulation.<br />

REFERENCES<br />

Ilie F., Bulucea C.A., Popescu M.C.,(2009), Simulations <strong>of</strong> Oil-filled Transformer Loss-<strong>of</strong>-Life Models,<br />

Proceedings <strong>of</strong> the 11 th International Conference on Mathematical Methods and Computational<br />

Techniques in Electrical Engineering (MMACTEE'09), Published by WSEAS Press, pp.195-202,<br />

Vouliagmeni Beach, Greece.<br />

Mastorakis N., Bulucea C.A., Manolea Gh., Popescu M.C., Perescu-Popescu L., (2009) Model for Predictive<br />

Control <strong>of</strong> Temperature in Oil-filled Transformers, Proceedings <strong>of</strong> the 11 th WSEAS International<br />

Conference on Automatic Control, Modelling and Simulation, pp.157-165, Istanbul, Turkey, May.<br />

Mastorakis N., Bulucea C.A., Popescu M.C., Manolea Gh., Perescu L., (2009) , Electromagnetic and Thermal<br />

Model Parameters <strong>of</strong> Oil-Filled Transformers, WSEAS Transactions on Circuits and Systems, Issue 6,<br />

Vol.8, pp.475-486, Available: http://www.worldses.org/journals/circuits/circuits-2009.htm<br />

59


Mastorakis, N.. Bulucea, C.A., Popescu M.C., (2009) Transformer Electromagnetic and Thermal Models,<br />

Proceedings <strong>of</strong> the 9 th WSEAS International Conference on Power Systems (PS`09): Advances in<br />

Power Systems, pp.108-117, Budapest, Hungary.<br />

Popescu M.C., Bulucea C.A., Perescu L., (2009) Improved Transformer Thermal Models, WSEAS Transactions<br />

on Heat and Mass Transfer, Issue 4, Vol.4, pp. 87-97, October.<br />

Available:http://www.worldses.org/journals/hmt/heat-2009.htm<br />

Popescu M.C., Manolea Gh., Bulucea C.A., Boteanu N., Perescu-Popescu L., Muntean I.O., (2009) Transformer<br />

Model Extension for Variation <strong>of</strong> Additional Losses with Frequency, Proceedings <strong>of</strong> the 11 th WSEAS<br />

International Conference on Automatic Control, Modelling and Simulation, pp.166-171, Istanbul,<br />

Turkey.<br />

Popescu M.C., Manolea Gh., Perescu L., (2009), Parameters Modelling <strong>of</strong> Transformer, WSEAS Transactions<br />

on Circuits and Systems, pp.661-675, Issue 8, Vol.8.<br />

Available:http://www.worldses.org/journals/circuits/circuits-2009.htm<br />

Popescu M.C., Mastorakis N., Bulucea C.A., Manolea Gh., Perescu L., (2009), Non-Linear Thermal Model for<br />

Transformers Study, WSEAS Transactions on Circuits and Systems, Issue 6, Vol.8, pp.487-497.<br />

Available: http://www.worldses.org/journals/circuits/circuits-2009.htm<br />

Popescu M.C., Mastorakis N., Bulucea C.A., Popescu-Perescu L., (2009) Modelling <strong>of</strong> Oil-filled Transformer,<br />

International <strong>Journal</strong> <strong>of</strong> Mathematical Models and Methods in <strong>Applied</strong> <strong>Science</strong>s, Issue 4, Vol.3, pp.346-<br />

355. Available: http://www.naun.org/journals/m3as/19-166.pdf<br />

Popescu M.C., Mastorakis N., Manolea Gh., (2009), Thermal Model Parameters Transformers, WSEAS<br />

Transactions on Power Systems, Issue 6, Vol.4, pp.199- 209,<br />

June.Available:http://www.worldses.org/journals/power/power-2009.htm<br />

Popescu M.C., Mastorakis N., Popescu-Perescu L., (2008) Electromagnetic and Thermal Model Parameters,<br />

International <strong>Journal</strong> <strong>of</strong> Energy, Issue 4, Vol.2, pp.51-65.<br />

Available: http://www.naun.org/journals/energy/19-141.pdf<br />

Popescu M.C., Mastorakis N.. Popescu-Perescu L., (2009), New Aspects Providing Transformer Models,<br />

International <strong>Journal</strong> <strong>of</strong> Systems Applications, Engineering & Development, Issue 2, Vol.3, pp.53- 63.<br />

Available: http://www.universitypress.org.uk/journals/saed/19-165.pdf<br />

Popescu M.C., Popescu C., (2009), Functional Parameters Modelling <strong>of</strong> Transformer, <strong>Journal</strong> <strong>of</strong> Mechanical<br />

Engieenering Research, pp.001-037.<br />

Available: http://www.academicjournals.org/JMER/contents/2009cont/Nov.htm.<br />

Popescu M.C., (2009), Transformer Thermal and Loss <strong>of</strong> Life Models, <strong>Journal</strong> Electrical and Electronics<br />

Engineering Research, pp.001-022.<br />

Available: http://www.academicjournals.org/JEEER/contents/2009cont/Nov.htm<br />

Popescu, M.C., Manolea, Gh., Bulucea, C.A., Perescu-Popescu, L., Drighiciu, M.A., (2009), Modelling <strong>of</strong><br />

Ambient Temperature Pr<strong>of</strong>iles in Transformer, Proceedings <strong>of</strong> the 13 th WSEAS International<br />

Conference on Circuits, (part <strong>of</strong> the 13 th WSEAS CSCC Multiconference), pp.128-137, Rodos, Greece.<br />

Stoenescu E., Popescu M.C., Bulucea C.A., Assessment <strong>of</strong> Improved Transformer Thermal Models, (2009),<br />

Proceedings <strong>of</strong> the <strong>Applied</strong> Computing Conference (ACC'09), Published by WSEAS Press, pp.189-195,<br />

Vouliagmeni Beach, Greece.<br />

60


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

A disconnect congestion detection from<br />

TCP to improve the robustness<br />

Issa Kamar and Seifeddine Kadry<br />

AUL university, Beirut, Lebanon<br />

Lebanese University - Faculty <strong>of</strong> <strong>Science</strong>, Lebanon<br />

E-mail: seifdine.kadry@aul.edu.lb, Issa.kamar@aul.edu.lb<br />

Abstract – The Transmission Control Protocol (TCP) is the most popular transport layer protocol for the internet.<br />

Congestion Control is used to increase the congestion window size if there is additional bandwidth on the network, and<br />

decrease the congestion window size when there is congestion.This paper uses a classic TCP which we called Robust<br />

TCP with an accurate algorithm <strong>of</strong> congestion detection in order to improve the performance <strong>of</strong> TCP. Our TCP Robust<br />

only reacts when it receives an ECN (Explicit Congestion Notification) mark. The evaluation result shows a good<br />

performance in the terms <strong>of</strong> drop ratio and throughput.<br />

Keywords: Congestion Control, TCP, ECN, Implicit Congestion Notification.<br />

________________________________________________________________________________________________<br />

I. INTRODUCTION<br />

TCP is a connection-oriented, end-to-end reliable protocol designed to fit into a layered hierarchy <strong>of</strong> protocols which<br />

support multi-network applications. Congestion events in communication networks cause packet losses, and it's well<br />

known that these losses occur in burst.TCP congestion control involves two tasks:<br />

1. Detect congestion<br />

2. Limit Transmission rate<br />

To achieve good performance and obtain a Robust TCP, it is necessary and important to control network congestion, by<br />

limiting the sending rate and regulating the size <strong>of</strong> congestion window (Cwnd) after the detection <strong>of</strong> congestion.TCP<br />

congestion control operates in a closed loop that infers network conditions and reacts accordingly by means <strong>of</strong> losses. A<br />

negative return is due to a loss <strong>of</strong> a segment which can be translated by decreasing the flow from the source through a<br />

reduction in the size <strong>of</strong> window control.<br />

TCP considers loss <strong>of</strong> a segment as a congestion in the network, the detection <strong>of</strong> this loss can be done in several ways:<br />

Timeout, Three Duplicate ACKs (Fast retransmit) and by receiving a partial ACK.<br />

The state is:<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

61


� If Packet Loss or congestion event =>TCP decreases Cwnd.<br />

� All is well and no congestion in the network, i.e., TCP increases Cwnd.<br />

At all cases, loss indication should be done with accuracy because it may lead to false indications like: Spurious<br />

retransmission.<br />

Spurious timeout occurs when a non lost packet is retransmitted due to a sudden RTT (Round Trip Time) increase (hand<br />

over, high delay, variability, rerouting . .) which implies to an expiration <strong>of</strong> the retransmission timer set with a previous<br />

and thus outdated RTT value.<br />

This effect is known to be the root cause <strong>of</strong> spurious retransmission.<br />

The function <strong>of</strong> the congestion control is an essential element to the stability <strong>of</strong> the internet.<br />

Indeed, TCP congestion control reduces the flow when it detects a loss in the network. Therefore, it is important to be<br />

accurate in the loss detection to improve the performance <strong>of</strong> TCP.<br />

A congestion event (or loss event) corresponds to one or several losses (or in the context <strong>of</strong> ECN: at least one<br />

acknowledgment path with an ECN-echo) occurring in one TCP window during one current RTT period, it means that a<br />

congestion event begins when the first loss occurs and finishes one RTT later.<br />

In this paper, we propose a congestion detection algorithm that is realized independently <strong>of</strong> the TCP code. To improve<br />

the TCP by reducing the Cwnd, we aim to illustrate the feasibility <strong>of</strong> the concept by demonstrating that we can both<br />

obtain similar performances and also improve the accuracy <strong>of</strong> the detection outside the TCP stack.<br />

We implement the Implicit Congestion Notification (ICN) algorithm to better understand and investigate the problem <strong>of</strong><br />

congestion events estimation.<br />

This paper is organized as follows: section 2 presents related works, section 3 shows the architecture <strong>of</strong> the congestion<br />

detection, section 4 presents the detailed discussion for the Robust TCP with ICN congestion detection algorithm, and<br />

section 5 presents an evaluation <strong>of</strong> the TCP Robust using simulations.<br />

Finally, section 6 concludes this article and presents some perspectives.<br />

II. RELATED WORKS:<br />

Over the past few years, several solutions have been proposed to improve the performance <strong>of</strong> TCP. In [5] proposed<br />

TCP-DCR modifications to TCP's congestion control mechanism to make it more robust to non-congestion events, this<br />

is implemented by using the delay "tau" based on a timer.<br />

Our mechanism is different; it relies on the accurate congestion detection algorithm (ICN) and uses the timestamp option<br />

to detect spurious timeout which can more improve the reliability <strong>of</strong> the algorithm and leads to a real Robust TCP.<br />

In Forward RTO-Recovery (F-RTO): the F-RTO algorithm <strong>of</strong> the TCP sender monitors the incoming<br />

acknowledgments to determine whether the timeout was spurious.<br />

TCP suffers from the inaccuracy <strong>of</strong> the congestion detection in the other TCP agents, for this reason we design an<br />

accurate mechanism <strong>of</strong> congestion detection (ICN) that interacts with TCP robust.<br />

Our study must prove the functionality <strong>of</strong> our TCP with ICN is better than other versions <strong>of</strong> TCP. For this point we have<br />

to show that the mechanism <strong>of</strong> congestion detection for some TCP variants (New-Reno, Sack) doesn’t detect well when<br />

there is congestion and doesn't not work well more than TCP Robust with ICN.<br />

In [5], the idea or the solution proposed for the detection <strong>of</strong> congestion is the delay <strong>of</strong> the time to infer congestion by T,<br />

and this value should be large to recover from non-congestion event, and should be small to avoid expensive RTO.<br />

Our approach is different by using a classic TCP that responds only to an accurate algorithm <strong>of</strong> congestion detection.<br />

62


III. STAND-ALONE TCP CONGESTION EVENTS ALGORITHMS<br />

In this section we present the architecture <strong>of</strong> decorrelating congestion Detection from the Transport Layer (figure 1).The<br />

main goal <strong>of</strong> this architecture is to simplify the task <strong>of</strong> kernel developers as well as improve TCP performances. This<br />

scheme opens the door to another way to react to congestion by enabling ECN emulation at end-host. In this case ICN<br />

emulates ECN marking to imply a congestion window reduction.<br />

Figure. 1. Decorrelating Congestion Detecting from the Transport Layer<br />

IV. ROBUST TCP ALGORITHM:<br />

Our proposed algorithm which we called Robust TCP is to make the congestion detection reliable and to distinguish the<br />

causes <strong>of</strong> losses in order to improve the flow control.<br />

The main idea is to determine CE (i.e. the congestion detection) which impact on the TCP flow performance by<br />

monitoring the TCP flow itself.<br />

The principle is to obtain a detection system at the edge <strong>of</strong> a network or at the sender side which analyses the TCP<br />

behavior through the observation <strong>of</strong> both data packets and acknowledgments paths.<br />

So, the scenario is to make a new version <strong>of</strong> TCP (Robust TCP) without detection <strong>of</strong> congestion. Robust TCP doesn't<br />

reacts (reducing <strong>of</strong> Cwnd) whenever it doesn't receive a notification ECN. Robust TCP must interact with ICN algorithm<br />

through ECN. Once we have congestion indication and the congestion event is validated, in this case it must notify the<br />

TCP we are exploring the functionality <strong>of</strong> Robust TCP and the ICN algorithm with the interaction between each other.<br />

Robust TCP maintains all the functions <strong>of</strong> TCP Reno (slow start, Congestion avoidance, Fast retransmit and Fast<br />

recovery) and modified by adding error control and limited transmit (like in New-Reno TCP) to avoid unnecessary<br />

timeouts.<br />

Robust TCP is a classic version <strong>of</strong> TCP but very sensitive to packet loss. It contains the major congestion control<br />

phases:<br />

1. Slow start and congestion avoidance (increase Window size).<br />

2. Fast retransmit (Detection <strong>of</strong> congestion).<br />

3. Fast recovery.<br />

1. Slow start:<br />

63


� When ACK received: cwnd++ which means for every ACK received, the sender sends two more segments.<br />

� Exponential increase in the window (Every RTT: cwnd = 2*cwnd)<br />

� Threshold (sstrhesh) controls the change to congestion avoidance.<br />

2. Congestion avoidance<br />

� When ACK received: cwnd+ = 1/cwnd.<br />

� Linear increment <strong>of</strong> cwnd (every RTT: cwnd++) slow start is exists until cwnd is smaller or equal to ssthresh.<br />

Later congestion avoidance takes over.<br />

3. Fast retransmit:<br />

TCP generates duplicate ACK when out-<strong>of</strong>-order segments are received. In this case Fast retransmit uses "duplicate<br />

ACK" to trigger retransmission packets, so the sender does not wait until timeout for retransmission, sender retransmits<br />

the missing packet after receiving 3<br />

DUPACK.<br />

4. Fast recovery:<br />

TCP retransmits the missing packet that was signaled by three duplicate ACKs and waits for an acknowledgment <strong>of</strong> the<br />

entire transmit window before returning to congestion avoidance. If there is no acknowledgment, TCP Robust<br />

experiences a timeout and enters the<br />

Slow-start state.<br />

TCP recovers much faster from fast retransmit than from timeout. When congestion window is small, the sender may not<br />

receive enough dupacks to trigger fast retransmit and has to wait for timer to expire but under<br />

Limited transmit, sender will transmit a new segment after receiving 1 or 2 DUPACKs if allowed by receivers advertised<br />

window to generate more dupacks.<br />

Robust TCP is poor in performance without detection <strong>of</strong> congestion and worse than other TCP like TCP New-Reno and<br />

Sack. It reacts only on the receiving <strong>of</strong> ECN notification.<br />

Once it doesn't receive a notification that means there is no congestion control on TCP and the window keep increasing,<br />

but in case <strong>of</strong> receiving ECN that will indicate the occurrence <strong>of</strong> congestion indication notified by ICN, than Robust TCP<br />

reacts by limiting its sending rate and takes the full meaning <strong>of</strong> its name.<br />

IV.1 ICN WITH TIMESTAMP<br />

ICN (implicit congestion notification) is an algorithm for congestion detection implemented outside the TCP stack to<br />

analyze TCP flow and to better understand the problem <strong>of</strong> congestion events and than to conclude if the congestion<br />

occurs in the network or no and it is also more accurate in congestion detection than TCP.<br />

The main goal <strong>of</strong> ICN is to determine the losses (i.e. the congestion detection) which impact on the TCP flow<br />

performance by observing the flow itself which mean by looking at the losses occurring over an RTT period given.<br />

ICN is a generic algorithm that doesn't depend on the TCP version used which implements a congestion control where a<br />

negative feedback means a loss. It is important to note that ICN doesn't manage the error control which remains under<br />

the responsibility <strong>of</strong> TCP<br />

Starting from the observation <strong>of</strong> the data segments and the acknowledgments, we identify each TCP connection with a<br />

state machine. This state machine indentifies the control congestion phase and classifies retransmission as spurious or<br />

not.TCP congestion control reacts following binary notification feedbacks allowing assessing whether the network is<br />

congested or not.<br />

ICN algorithm consists <strong>of</strong> two states:<br />

1. Normal state: which characterizes TCP connection without losses, in this state no congestion occurs and the sender<br />

receive the ACK normally.<br />

64


2. Congestion state: This state starts from the loss <strong>of</strong> the first window data segment. When a loss occurs ICN enters in<br />

this state and waits to the congestion event to be validated to notify Robust TCP about this loss. When the top <strong>of</strong> the<br />

window is acknowledged, ICN enters in the normal state.<br />

To improve the performance <strong>of</strong> the congestion detection algorithm and especially against spurious timeout we added the<br />

timestamp option, in order once the congestion happens ICN enter in this state and append a timestamp to let the sender<br />

to compute the RTT estimate based on returned timestamp in ACK.<br />

Time stamps used in this state to measure the round trip time (RTT) <strong>of</strong> a given TCP segment and including retransmitted<br />

segment, this option also can help to eliminate the retransmission ambiguity ( due to false indication) and identifies when<br />

retransmission is spurious or not.<br />

Spurious Timeout are inevitable and not rare in data networks, for this reason and once the congestion event occurs, ICN<br />

enter in the congestion event state, timestamp is added for each data segment. Timestamp can be considered as an<br />

acknowledging mechanism in the time domain.<br />

In the figure (2) shown below we will present the flowchart <strong>of</strong> TCP Robust with ICN mechanism:<br />

IV.2 Robust TCP and ICN interaction<br />

Figure 2: Robust TCP with ICN detection algorithm<br />

ICN is an accurate congestion detection algorithm where after detecting a loss event in the congestion state, the<br />

congestion event (CE) must be validated.<br />

The validation <strong>of</strong> CE should lead to a congestion indication which is the principle responsible to inform the Robust TCP<br />

about the congestion. The confirmation method due to a congestion indication is ECN (Explicit congestion notification),<br />

which is the main fag in the ACK to notify the loss to the source TCP. Once the source is signaled by ECN notification it<br />

reacts by reducing its window (Cwnd) and this time Robust TCP takes the full meaning <strong>of</strong> its name.<br />

After reducing its window, we can notice very well the decreasing <strong>of</strong> the number <strong>of</strong> dropped packets (d) in the network<br />

due to using <strong>of</strong> ICN congestion detector and our TCP becomes better in performance than others like<br />

TCP New-Reno and Sack.<br />

65


V. VALIDATIONS AND EVALUATIONS<br />

In this section we evaluate the performance <strong>of</strong> Robust TCP with ICN algorithm. The main idea is to build an algorithm <strong>of</strong><br />

congestion detection outside the TCP stack that is responsible to detect the loss and notify it to Robust TCP.<br />

The architecture <strong>of</strong> our tools is shown in the figure (3), which is mainly composed from the following components:<br />

1. Network topology.<br />

2. Traffic model.<br />

3. Performance evaluation metrics.<br />

After the simulation is done, a set <strong>of</strong> result statistics and graphs are generated.<br />

V .1 Network topology<br />

Figure 3: Architecture <strong>of</strong> our tools<br />

To study our TCP and ICN behavior we built our Network and application model shown in figure (4), in which source<br />

nodes and sink nodes connect to router 1 or router 2. The bandwidth between the two routers is much lower than the<br />

other links, which causes the link between the routers to be a bottleneck. (Traffic can be either uni-directional or<br />

bidirectional).<br />

V.2 Traffic Model<br />

Figure 4: Network topology<br />

The tool attempts to apply the typical traffic settings. In our application include the FTP traffic that uses infinite, nonstop<br />

file transmission, which begins at a random time and runs on the top <strong>of</strong> TCP. Implementation details and a<br />

comparative analysis <strong>of</strong> TCP Tahoe, Reno, New-Reno, SACK and Vegas choices <strong>of</strong> TCP variant are decided by users.<br />

V.3 Performance evaluation metrics<br />

The metrics used in our simulations are Throughput and Drop ratio. Throughput is the total elapsed flow since the<br />

beginning <strong>of</strong> simulation time. Throughput may also includes retransmitted traffic (repeated packets).Drop ratio is the<br />

total rate <strong>of</strong> packet loss during the simulation time. To obtain network statistics, we measure also the drop ratio metric<br />

that result in the failure <strong>of</strong> the receiver to decode the packet and simulation time is 100 seconds.<br />

66


Robust TCP is poor in performance as a standalone TCP but after adding the ICN it becomes much better (see figure 5)<br />

and accurate than TCP New-Reno as show in the figure (6). To evaluate our scenario, we compare TCP Robust with<br />

other TCP variants (TCP New-Reno) by using different metrics that will show us clearly the improvement <strong>of</strong> our TCP<br />

version compared to others. (Figure 6 and 7).<br />

Figure 5: Comparison between TCP Robust before and after adding ICN algorithm.<br />

The main difference between Robust and New-Reno TCP occurs in the reaction <strong>of</strong> each protocol. In the TCP New-Reno<br />

the reaction will be whenever an error or congestion occurs on the network by slowdown the transmission without being<br />

accurate if there is a congestion or not. In addition <strong>of</strong> that the main problem <strong>of</strong> New-Reno TCP that it suffers from the<br />

fact that it takes one RTT to detect each packet loss. When the ACK for the first retransmitted segment is received only<br />

then we can deduce which other segment was lost. This problem <strong>of</strong> inaccuracy in TCP New-Reno is solved by the ICN<br />

algorithm that the ICN receive the packet and check the presence <strong>of</strong> congestion by using the normal and congestion<br />

phase and by adding the timestamp option which can be make sure <strong>of</strong> the presence <strong>of</strong> congestion or no. The deduction <strong>of</strong><br />

congestion in TCP Robust is different from New-Reno, it will be deduced after signaling ECN from ICN to TCP robust,<br />

and then the TCP reacts by decreasing the transmission. This accuracy in detection <strong>of</strong> congestion can be up to 24 % as<br />

difference between the two protocols (Figure 6) before reaction <strong>of</strong> each one and starting slowdown retransmission.<br />

Due the fast reaction <strong>of</strong> TCP robust, the transmission <strong>of</strong> TCP become less than in TCP New-Reno which means that the<br />

throughput in the TCP robust must be less than in New-Reno, this is clear and deduced in the figure 7.<br />

Figure 6: Comparison between TCP Robust and TCP New-Reno<br />

67


In figure (6) represents that the drop ratio is less in Robust than in New-Reno due that TCP reacts only when receiving<br />

ECN which make its reaction faster.<br />

Figure 7: Comparison between TCP Robust and TCP New-Reno<br />

In figure (7) Robust TCP algorithm reaction is faster than the Reaction <strong>of</strong> New-Reno, thus Throughput in New-Reno is<br />

higher than when using Robust TCP. Congestion detection used by ICN algorithm is more accurate when using the<br />

timestamp option for detecting a spurious timeout which improve more the performance <strong>of</strong> TCP.<br />

The main difference between spurious timeout algorithms relies on the method how to detect spurious timeout by solving<br />

the retransmission ambiguity in many circumstances. After clarifying this ambiguity TCP can tell whether the data is there<br />

is spurious timeout has happened or not. DSACK, F-RTO and Robust TCP can see the problem <strong>of</strong> spurious timeout in<br />

different aspects.<br />

DSACK, an extension <strong>of</strong> TCP SACK, works it out in the sequence space. It requires the TCP receiver explicitly<br />

acknowledging duplicate segments with duplicate SACK options. F-RTO algorithm is used for detecting spurious<br />

retransmission timeouts with TCP. It is a TCP sender-only algorithm that does not require any TCP options to operate-<br />

RTO delays the decision <strong>of</strong> loss recovery and waits further two ACK. If the first arrived ACK forwards the sender's<br />

transmitting window, TCP concludes a spurious timeout and resume transmitting new data.<br />

Our approach is different than other TCP by using an algorithm <strong>of</strong> congestion detection outside the TCP code, where it<br />

can detect congestion and spurious timeout by using the timestamp option at the occurrence <strong>of</strong> loss or congestion event.<br />

The main advantage <strong>of</strong> ICN with timestamp algorithm is that it can work with spurious timeouts and the others loss<br />

events by detecting the congestion in the network immediately and then directly will be notified to Robust TCP in order<br />

that TCP after this action will reduce its window, which can improve very well the performance <strong>of</strong> our TCP.<br />

VI. CONCLUSION AND FUTURE WORK<br />

This paper has proposed a new algorithm, which is implemented as a stand alone component and not inside a TCP stack.<br />

This algorithm that interacts with a classic version <strong>of</strong> TCP is able to detect congestion and notify directly the loss to the<br />

Robust TCP through the congestion notification (ECN) in order to reduce its window which leads to a Robust TCP<br />

compared to other variants like New-Reno and SACK TCP. In our work we demonstrate that congestion event detection<br />

can be realized independently <strong>of</strong> the TCP code in sake <strong>of</strong> better detecting congestion occurring in the network.<br />

Following this work and the results obtained so far, we are currently planning to develop more the detection <strong>of</strong><br />

congestion by using the delay-based in the congestion detection algorithm (ICN) and the effect <strong>of</strong> fast reaction <strong>of</strong> TCP<br />

robust in the Network.<br />

68


REFERENCES<br />

A Comparative Analysis <strong>of</strong> TCP Tahoe, Reno, New- Reno, SACK and Vegas.<br />

Bhandarkar, S. and Reddy, A.L.N. (2004), Networking, May TCP-Dcr: Making TCP Robust to Non-Congestion Events.<br />

K. Ramakrishnan, S. Floyd, and D. Black, (2001), The addition to explicit congestion notification (ECN) to ip. Request<br />

for comments 3168,IETF.<br />

P. Anelli and F. Harivelo, E. lochin. On TCP congestion events detection.<br />

P.sarolahti and M. kojo. (2005), Forward rto-recovery (f-tro): An algorithm for detecting spurious retransmission<br />

timeouts with tcp and the stream control transmission protocol (sctp).rfc 4138,IETF.<br />

Reiner Ludwig and Randy H..Katz, (2000), The Eifel algorithm: making TCP robust against spurious retransmissions.<br />

SIGCOMM Comput. Common. Rev., 30(1):30-36.<br />

RFC 3649, (2003), High Speed TCP for Large Congestion Windows, S. Floyd.<br />

RFC 793, (1981), Transmission Control Protocol, September .<br />

S. Floyd, (2003), ICSI. RFC 3649 - High Speed TCP for Large Congestion Windows.<br />

69


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

ANALYSIS OF MICROWAVE SIGNAL RECEPTION USING FINITE DIFFERENCE<br />

IMPLEMENTATION. (A CASE STUDY OF AKURE – OWO DIGITAL MICROWAVE<br />

LINK IN SOUTH WESTERN NIGERIA)<br />

OTASOWIE P.O* and UBEKU E.U.<br />

Dept <strong>of</strong> Electrical /Electronic Engineering University <strong>of</strong> Benin, Benin City Nigeria.<br />

*E-mail address for correspondence : potasowie@yahoo.com<br />

______________________________________________________________________________________________<br />

Abstract: In this work, the finite difference method have been used to model microwave signal propagation. The data<br />

used for this analysis were gathered between January and December 2006 in Akure – Owo digital microwave line <strong>of</strong><br />

sight link in southwestern Nigeria.The data collected were analyzed using finite difference method and writing a<br />

program in MATLAB 7.0 s<strong>of</strong>tware program to obtain a model equation for the line <strong>of</strong> sight link. The results <strong>of</strong> the<br />

work shows that the months <strong>of</strong> August, September, July and January have the poorest signal reception while the<br />

months <strong>of</strong> February, march and April have the best signal reception in the link.The results <strong>of</strong> the predicted model<br />

were validated by measured data and the results obtained showed that the developed model can be used to accurately<br />

predict the link degradation parameters.<br />

Keywords: Microwave link, finite difference method, average signal level, signal reception.<br />

_____________________________________________________________________________________________<br />

Justification for the work<br />

INTRODUCTION<br />

Microwave signal transmission and reception in Nigeria especially for telephone services is very poor basically<br />

because <strong>of</strong> non-availability <strong>of</strong> data for planning and design <strong>of</strong> microwave links. There is a need for the build up <strong>of</strong><br />

such a database in Nigeria [1]<br />

Microwave signal propagation<br />

Microwave radio relay is a technology for transmitting digital and analog signals such as long – distance telephone<br />

calls and the relay <strong>of</strong> television programs between two locations on a line <strong>of</strong> sight radio path [ 2, 3 ]<br />

In a microwave radio relay, a line <strong>of</strong> sight link is required, therefore obstacles, the curvature <strong>of</strong> the earth, the<br />

geography <strong>of</strong> the area are important issues to consider when planning radio links.<br />

Microwave propagation hardly occur under ideal conditions, for most communication links, the analysis must be<br />

modified to account for the presence <strong>of</strong> the earth, the ionosphere and atmosphere precipitates such as fog, raindrops,<br />

snow and hail, for stations on the ground transmitting through the lower atmosphere is complicated by uncontrolled<br />

variables associated with climate weather and path terrain. Signals are said to undergo fading which refers to the fact<br />

71


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

that time – varying atmospheric processes influence the mechanisms <strong>of</strong> reflection, refraction and diffraction separately<br />

or in combination, so as to cause signal losses at a receiving antenna [3 ].<br />

Once a microwave signal is radiated by the antenna, it will propagate through space and will ultimately reach the<br />

receiving antenna. As would be expected the energy level <strong>of</strong> the signal decreases rapidly as the distance from the<br />

transmitting antenna is increased further.<br />

Mathematical Modeling<br />

The finite difference method is a full wave method <strong>of</strong> parabolic equation that directly solve a wave equation<br />

numerically subject to a number <strong>of</strong> assumptions and simplifications. The finite difference method is based on<br />

discretisation <strong>of</strong> the wave equation through the introduction <strong>of</strong> a rectangular gird and the evaluation <strong>of</strong> the various<br />

derivative terms using centered finite differences [ 4,5,6,7,8 ].<br />

The derivation <strong>of</strong> the parabolic equation normally start by reducing Maxwell’s equations to the Helmholtz equation.<br />

However in this instance if we assume the presence <strong>of</strong> an atmosphere described by a complex refractive index:<br />

n( r)<br />

� �( r)<br />

� �r<br />

( r)<br />

� j�<br />

( r)<br />

�� …………….(1.0)<br />

0<br />

which is a continuously varying function <strong>of</strong> position. Provided that � �ln n ��1,<br />

the scalar Helmholtz equation<br />

describes accurately each <strong>of</strong> the Cartesian components <strong>of</strong> the electric and magnetic fields.[,6,7]<br />

2 2 2<br />

� � � k n � � 0 ………………………(1.1)<br />

0<br />

The wave number in vacuo is now given by k 0 � 2� / �0<br />

. Considering a two dimensional propagation problem<br />

along the great circle path and making the approximation that the earth is flat over a short length for simplicity,<br />

Equation 1.1 can be expanded in Carteisian co-ordinates as:<br />

2 2<br />

� � � �<br />

� � k<br />

2 2<br />

�x<br />

�z<br />

2<br />

0<br />

2<br />

n � � 0<br />

……………….(1.2)<br />

We now introduce the assumption that an a priori preferred direction <strong>of</strong> propagation exists and identify this with the<br />

x axis. It is, therefore, reasonable that we can write the following form for the solution: [6,7]<br />

( , ) ( , ) exp( 0 ) x jk z x u z x �<br />

� � ………….(1.3)<br />

where the reduced wave amplitude u( x,<br />

z)<br />

can now be assumed to vary slowly along the x direction on the scale <strong>of</strong><br />

a free-space wavelength, � . Substituting Equation 1.3 into 1.2 and discarding the common factor exp( 0 ) x jk � after<br />

performing the differentiations yields the following equation for the reduced wave amplitude:<br />

2<br />

� u<br />

� 2 jk 2<br />

�x<br />

0<br />

2<br />

�u<br />

� u<br />

� � k 2<br />

�x<br />

�z<br />

2<br />

0<br />

( n<br />

2<br />

�1)<br />

u � 0<br />

……. (1.4)<br />

Equation 1.4 describes waves propagating both along the positive and negative x directions. By analogy with the<br />

one-dimensional wave equation<br />

2<br />

2<br />

� w 1.<br />

� w � � 1 � ��<br />

� 1 � �<br />

� � 0 �<br />

� 0<br />

2 2 2 � � ��<br />

� �w<br />

�x<br />

c �t<br />

� �x<br />

c �t<br />

��<br />

�x<br />

c �t<br />

�<br />

which has linearly independent solutions given as:<br />

w � f ( x � ct)<br />

and w � g(<br />

x � ct)<br />

……………………………. (1.5b)<br />

72<br />

0<br />

……………… (1.5a)


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

These can be identified as forward and backward traveling waves corresponding to the two<br />

differential operators in Equation 1.5a. If we factorise Equation 1.4 into forward and backward traveling wave<br />

operators; then we have<br />

…………………….(1.6)<br />

�<br />

�<br />

�<br />

�<br />

� jk<br />

� �x<br />

�<br />

� �<br />

� jk<br />

�<br />

�<br />

�x<br />

0<br />

0<br />

�<br />

�<br />

jk<br />

jk<br />

0<br />

0<br />

1�<br />

( n<br />

1�<br />

( n<br />

2<br />

2<br />

1 �<br />

�1)<br />

� 2<br />

k �z<br />

1 �<br />

�1)<br />

� 2<br />

k �z<br />

73<br />

0<br />

0<br />

2<br />

2<br />

2<br />

�<br />

�<br />

�<br />

�<br />

�<br />

�<br />

�u<br />

� 0<br />

�<br />

�<br />

If you discard the backward traveling wave for consistency with Equation 1.3, then finally, we have,<br />

�<br />

� �<br />

� jk<br />

�<br />

�<br />

�x<br />

0<br />

�<br />

jk<br />

0<br />

2<br />

2 1 �<br />

�n �1�<br />

� �u<br />

� 0<br />

1� 2 2<br />

k0<br />

�z<br />

�<br />

�<br />

�<br />

……(1.7)<br />

It is to be understood that the differential operator under the square root sign in Equation 1.7 can only be interpreted in<br />

a formal sense. Its numerical evaluation can only be achieved by replacing the square root by a power series, or<br />

rational fractions <strong>of</strong> operators.<br />

Thus, we rewrite Equation 1.4 as:<br />

�u<br />

�<br />

� jk �<br />

�x<br />

�<br />

�<br />

2<br />

2 1 � �<br />

1 � �n �1�<br />

� �u<br />

� jk �1 � 1�<br />

Q(<br />

x,<br />

z)<br />

�u ………….. (1.8)<br />

2 2<br />

k0<br />

�z<br />

�<br />

�<br />

0 1 �<br />

0<br />

The differential operator Q (x, z) must give a significantly smaller answer than the unity operator when operated on<br />

u (x,z), since by assumption, the oscillatory variation <strong>of</strong> i (x,z) is predominantly along the x direction, perpendicular to<br />

the z axis. Therefore, the z derivative on a scale <strong>of</strong> a wavelength (1/k0) is much smaller than the unity operator. For<br />

the atmosphere, we also know that n (x,z) � 1, giving: [7]<br />

Q( x,<br />

z)<br />

u(<br />

x,<br />

z)<br />

�� u(<br />

x,<br />

z)<br />

or formally ��1<br />

Q ………………………. (1.9)<br />

The simplest approximation for the square root term is given by the first two terms in its Taylor expansion, namely,<br />

1 Q( x,<br />

z)<br />

� 1�<br />

Q(<br />

x,<br />

z)<br />

/ 2<br />

� ……………….. (1.10)<br />

which finally yields the narrow-angle parabolic equation:<br />

�u<br />

�<br />

�x<br />

2 jk<br />

2 � � u<br />

�<br />

� � k 2<br />

� �z<br />

1 2<br />

0<br />

2<br />

0<br />

�<br />

�n �1�u<br />

�<br />

�<br />

�<br />

………………(1.11)<br />

Parabolic Equation – Finite difference Implementation<br />

This method is based on a more direct discretisaton <strong>of</strong> Equation 1.11, through the introduction <strong>of</strong> a rectangular grid<br />

and the evaluation <strong>of</strong> the various derivative terms using centered finite differences. The various terms appearing in<br />

Equation 1.11 are evaluated at the centre point through their finite difference discrete approximations to yield; [7,8]


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

n n<br />

u um<br />

um<br />

n<br />

x<br />

k<br />

�<br />

�1<br />

� 1<br />

( � ) �<br />

…..…………………..(1.12)<br />

� 2<br />

METHODOLOGY<br />

The line <strong>of</strong> sight microwave link used in this research work is situated between Akure located at latitude 071509.30N,<br />

longitude 0051142.60E (transmitting end) and Owo located at latitude 071220.00N longitude 0053402.00E (receiving<br />

end) over a path length <strong>of</strong> 41.42km. The Akure – Owo microwave link is owned and managed by NITEL – Nigeria<br />

Telecommunication Ltd. The microwave signal data were gathered between January and December 2006. The<br />

measurement was done with a data acquisition s<strong>of</strong>tware PROCOMM PLUS 3.0 s<strong>of</strong>tware program at the receiving<br />

end twice a week over a 24- hour period. This s<strong>of</strong>tware was installed in a computer system (laptop) type 3050 Acer<br />

Aspire. The Laptop computer system was then connected to the NITEL equipment at Owo. The PROCOMM PLUS<br />

3.0 s<strong>of</strong>tware detects and captures the received signal values in the link. The system characteristics <strong>of</strong> the Akure –<br />

Owo digital microwave link is given in Table 1.0.<br />

Table 1.0 System characteristics <strong>of</strong> the Akure – Owo digital microwave link[9]<br />

Characteristics Akure Owo<br />

Elevation (M) 348 320<br />

Latitude 071509.30N 071220.00N<br />

Longitude 0051142.60E 0053402.00E<br />

Antenna model VHP4 – VHP 4 –<br />

71W<br />

71W<br />

Antenna Height 90.00 90.00<br />

(M)<br />

Antenna Gain<br />

(dbi)<br />

Frequency (MHz) - 7500<br />

Polarization - Vertical<br />

Path length (km) - 41.42<br />

Radio Equipment model - MSM/H7 16E QPS<br />

Transmitted power (dBm) - 25.00 to 28.00<br />

Main received signal (dBm) - 45.03<br />

Received Threshold level (dBm) - 85.50<br />

36.60 36.60<br />

RESULTS AND DISCUSSION<br />

The recorded microwave signal data for the period (January to December 2006) were computed into monthly<br />

averages as shown in Table 2.0<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 2.0 Akure – Owo Digital Microwave link, Year 2006 Average monthly data<br />

Month Received Signal Level (dBm)<br />

January - 47.0<br />

February - 36.0<br />

March - 37.0<br />

April - 36.0<br />

May - 39.0<br />

June - 39.0<br />

July - 48.0<br />

August - 50.0<br />

September - 50.0<br />

October - 46.0<br />

November - 40.0<br />

December - 47.0<br />

(i) Variation <strong>of</strong> Average Signal level with months for Year 2006<br />

The analysis <strong>of</strong> the results shows that the months <strong>of</strong> February, March and April have the best signal reception while<br />

the months <strong>of</strong> August, September and July have the poorest signal reception.<br />

(ii) Analysis <strong>of</strong> Daily signal reception using the Finite difference model<br />

The figure 1.0 shows the plot <strong>of</strong> the finite difference implementation <strong>of</strong> daily received signal level with distance.<br />

Predicted Received Signal Level for Year 2006<br />

The model equation is<br />

Y = 9x10 -32 x 8 -1.4x10 -26 x 7 + 8.8 x 10 -22<br />

- 2.9 x 10 -17 x 5 + 5.4 x 10 -13<br />

Figure 1.0: Daily microwave received signal level with distance<br />

4<br />

x – 5.5 x10 19<br />

6<br />

x<br />

3<br />

x<br />

+ 2.8 x 10 -5 x 2 – 1.0x10 -5 x + 13 ………. (1.13)<br />

If x (dBm) = Received signal level measured in equation (1.13) then Y (dBm) = predicted values.<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

For example, on Mondays 15 th February 2006, the signal transmitted was 28dbm while the signal received was -<br />

35dBm. This corresponds to the model deduced as shown in equation 1.13 that if x = 28dbm then y = -35dBm.<br />

CONCLUSION<br />

In this work microwave signal received level were measured on a monthly basis and the finite difference method was<br />

used to develop a model that can predict microwave signal received level on a daily basis.<br />

The result <strong>of</strong> the research work shows that the months <strong>of</strong> August, September, July and January have poor signal<br />

reception while the months <strong>of</strong> February, march and April have good signal reception.<br />

The model equation developed using the finite difference method is reasonably accurate.<br />

REFERENCES<br />

Akleman, F; Sevgi, L (2008) “A novel finite difference time – Domain wave propagation IEE transaction on<br />

Antennas and propagation Vol 48 No 3.<br />

Barclay, L. (2003) “Propagation <strong>of</strong> Radio waves “IEE London 2 nd Edition pp 169-177.<br />

Bogucci, J; Wielowreyska, E. (2004) “Propagation reliability <strong>of</strong> line – <strong>of</strong> – sight radio systems” 17 th International<br />

Symposium and Exhibition on Electromagnetic Compatibility Wroclaw.<br />

Isaakidis, S.A; xenos, T.D. (2004) “Progress in Electromagnetic Research” Aristotle university <strong>of</strong> Thessaloniki<br />

Greece.<br />

Landstorfer, F.M. (1999) “wave propagation models for planning <strong>of</strong> mobile communication Networks” Proceedings<br />

<strong>of</strong> the 29 th European Microwave Conference (EUMC) Vol 1<br />

Matzler, C (2004) “Parabolic Equations for wave propagation and the advanced atmospheric effects prediction<br />

systems” (AREPS) Literar seminar<br />

Nigeria Telecommunication Ltd <strong>Journal</strong> (1992) Vol 2<br />

Otasowie, P.O; Edeko, F.O. (2008) “An investigation <strong>of</strong> microwave link degradation due to Atmospheric Conditions”<br />

(A case study <strong>of</strong> Akure – Owo Digital microwave link) <strong>Journal</strong> <strong>of</strong> Advances in materials research and<br />

Systems Technologies II. Trans Tech publications Ltd Zurich Switzerland vol. 62 pp 159-165.<br />

www. Answers.com (2007) “Microwave Radio Relay 15 th February 2007.<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

Estimation <strong>of</strong> C factor for soil erosion modeling using NDVI in Buyukcekmece<br />

watershed<br />

Ahmet Karaburun<br />

Fatih University,<br />

Department <strong>of</strong> Geography,<br />

Buyukcekmece, Istanbul, 34500, Turkey<br />

E-mail address for correspondence: akaraburun@fatih.edu.tr<br />

__________________________________________________________________________________________<br />

Abstract: In order to take measures in controlling soil erosion it is required to estimate soil loss over area <strong>of</strong><br />

interest. Soil loss due to soil erosion can be estimated using predictive models such as Universal Soil Loss<br />

Equation (USLE) and Revised Universal Soil Loss Equation (RUSLE). The accuracy <strong>of</strong> these models depends on<br />

parameters that are used in equations. One <strong>of</strong> the most important parameters in equations used in both <strong>of</strong><br />

models is C factor that represents effects <strong>of</strong> vegetation and other land covers. Estimating land cover by<br />

interpretation <strong>of</strong> remote sensing imagery involves Normalized Difference Vegetation Index (NDVI), an indicator<br />

that shows vegetation cover. The aim <strong>of</strong> this study is estimate C factor values for Buyukcekmece watershed using<br />

NDVI derived from 2007 Landsat 5 TM Image. The final C factor map was generated using the regression<br />

equation in Spatial Analyst tool <strong>of</strong> ArcGIS 9.3 s<strong>of</strong>tware. It is found that north part <strong>of</strong> watershed has higher C<br />

factor values and almost 60% <strong>of</strong> watershed area has C factor classes between 0.2 and 0.4<br />

Keywords: Erosion, RUSLE, USLE, C factor, Landsat, NDVI,<br />

___________________________________________________________________________<br />

INTRODUCTION<br />

Sediment yield studies play key role for various soil and water conservation planning processes including<br />

reservoir sedimentation analysis, studies on river morphology changes and river bed siltation, and agricultural<br />

project planning. Erosion process result in soil loss from a watershed and it is difficult to estimate soil loss as it<br />

arises from a complex interaction <strong>of</strong> various hydro-geological processes (Singh et al., 2008). Estimating the soil<br />

loss risk and its spatial distribution are the one <strong>of</strong> the key factors for successful erosion assessment. Thus it can<br />

be possible to develop and implement policies to reduce the effect <strong>of</strong> soil loss under varied geographical<br />

conditions (Colombo et al., 2005). The accuracy <strong>of</strong> estimating soil risk depends on model and its factors.<br />

Researchers have developed many predictive models that estimate soil loss and identify areas where<br />

conservation measures will have the greatest impact on reducing soil loss for soil erosion assessments (Angima<br />

et al., 2003).<br />

Those models can be classified into three main categories as empirical, conceptual and physical based models<br />

(Merrit et al.,2003). USLE and its modifications are the examples <strong>of</strong> empirical models and ANSWER,<br />

CREAMS, and MODANSW are the samples <strong>of</strong> conceptual models. Examples for the first two groups comprise<br />

the empirical USLE and its modifications, and some <strong>of</strong> the more comprehensive models like ANSWERS,<br />

CREAMS, and MODANSW. ANSWERS and CREAMS are basically conceptual and eventbased. European Soil<br />

Erosion Models, EUROSEM/KINEROS, EUROSEM/MIKE SHE and SHESED-UK are the physically-based<br />

models that have been developed at catchment or small subbasin scales (Fistikoglu and Harmancioglu, 2002).<br />

Universal Soil Loss Equation (USLE) was designed to predict longtime average soil losses in run<strong>of</strong>f from<br />

specific field areas in specified cropping and management systems. The USLE (Wischmeier and Smith, 1978)<br />

estimates the average annual soil loss from:<br />

A = R.K.LS.C.P<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

where A is the estimated soil loss per year R is the run<strong>of</strong>f factor, K is the soil erodibility factor, LS is the slope<br />

length and steepness factor, C is the cover and management factor and P is the support practice factor<br />

(Wischmeier and Smith, 1978). The R factor expresses the erosivity occurring from rainfall and run<strong>of</strong>f at a<br />

particular location. An increase in the intensity and amount <strong>of</strong> rainfall results in an increase in the value <strong>of</strong> R.<br />

The K factor expresses inherent erodibility <strong>of</strong> the soil or surface material. The value <strong>of</strong> "K" is defined as a<br />

function <strong>of</strong> the particle-size distribution, organic-matter content, structure, and permeability <strong>of</strong> the soil or surface<br />

material. The LS factor expresses the effect <strong>of</strong> topography, specifically hillslope length and steepness, on soil<br />

erosion. An increase in hillslope length and steepness results in an increase in the LS factor. The C covermanagement<br />

factor is used to express the effect <strong>of</strong> plants and soil cover. Plants can reduce the run<strong>of</strong>f velocity<br />

and protect surface pores. The C-factor measures the combined effect <strong>of</strong> all interrelated cover and management<br />

variables, and it is the factor that is most readily changed by human activities. The P factor is the support<br />

practice factor. It expresses the effects <strong>of</strong> supporting conservation practices, such as contouring, buffer strips <strong>of</strong><br />

close-growing vegetation, and terracing on soil loss at a particular site. A good conservation practice will result<br />

in reduced run<strong>of</strong>f volume, velocity and less soil erosion. The USLE concept has more recently been modified<br />

and adapted by a large number <strong>of</strong> researchers by including additional data and incorporating research results.<br />

Revised Universal Soil Loss Equation (RUSLE) was developed by integrating several recent techniques and<br />

additional data that improves the accuracy <strong>of</strong> factors <strong>of</strong> USLE model (Renard and Freimund, 1994; Renard et al.<br />

1997; Yoder and Lown, 1995). Thus RUSLE was extended to include forest, rangelands and disturbed areas<br />

compared to USLE. The Revised Soil Loss Equation (RUSLE) followed the same formula as the USLE, but it<br />

has a subfactor for evaluating the cover-management factor, a new equation for slope length and steepness, and<br />

new conservation practice values. It is also applicable to non-agricultural conditions such as construction sites.<br />

The RUSLE model is widely used as a predictive model for estimating soil erosion potential and effects <strong>of</strong><br />

different management practices for over 40 years (Renard et al., 1997).<br />

One <strong>of</strong> the most important parameters in USLE and RUSLE equations is the cover management factor (C) that<br />

represents effects <strong>of</strong> vegetation and other land covers. The C factor reflects the effect <strong>of</strong> cropping and<br />

management practices on the soil erosion rate. The C factor indicates how conservation plans will affect the<br />

average annual soil loss and how that soil-loss potential will be distributed in time during construction activities,<br />

crop rotations, or other management schemes (Van der Knijff et al., 2000). Vegetation cover protects the soil by<br />

dissipating the raindrop energy before reaching the soil surface. As such, soil erosion can be effectively limited<br />

with proper management <strong>of</strong> vegetation, plant residue, and tillage (Lee, 2004). In both <strong>of</strong> USLE and RUSLE, the<br />

C factor is computed using empirical equations that contain field measurements <strong>of</strong> ground cover. (Wischmeier<br />

and Smith, 1978; Renard et al., 1997). Since the satellite image data provide up to date information on land<br />

cover, the use <strong>of</strong> satellite images in the preparation <strong>of</strong> land cover maps is widely applied in natural resource<br />

surveys (Deng et al., 2008; Serra et al.,2008; Yuan,2008).<br />

The traditional method for spatial estimation <strong>of</strong> C factor is assigning values to land cover classes using classified<br />

remotely sensed images <strong>of</strong> study areas. At the end <strong>of</strong> supervised or unsupervised classification, land cover<br />

classes are derived from image for study area and then C factors that are obtained from USLE/RUSLE guide<br />

tables or computed using field observation for each land cover classes are assigned to each pixel in land cover<br />

class (Karaburun, 2009; Efe et al., 2008; Morgan, 1995; Folly et al., 1996; Juergens and Fander, 1993). Since all<br />

pixels in a vegetation class have the same C factor value, those pixels can not represent variation <strong>of</strong> this<br />

vegetation class over the study area (Wang et al., 2002). Researchers developed many methods to estimate C<br />

factor using NDVI for soil loss assessment with USLE/RUSLE (De Jong 1994; De Jong et al., 1999; De Jong<br />

and Riezebos, 1997; Wang et al., 2002; Lin et al. 2002). These methods employ regression model to make<br />

correlation analysis between C factor values measured in field or obtained from guide tables and NDVI values<br />

derived from remotely sensed images. The unknown C factor values <strong>of</strong> land cover classes can be estimated using<br />

equation obtained from linear regression analyses. The aim <strong>of</strong> this study is to estimate C factor values <strong>of</strong> land<br />

cover classes using NDVI values by regression analysis for erosion modeling in Buyukcekmece Watershed.<br />

Study Area<br />

Buyukcekmece watershed is located in the west <strong>of</strong> Istanbul and adjacent to the Marmara Sea (Fig.1) and it<br />

contains most important water sources and a dam provides drinking water for Istanbul. The Buyukcekmece<br />

watershed is one <strong>of</strong> the largest watersheds in Istanbul having an area <strong>of</strong> about 63000 ha and located 50<br />

kilometers west <strong>of</strong> the center <strong>of</strong> Istanbul. Agriculture is one <strong>of</strong> the most dominant land use patterns in<br />

Buyukcekmece watershed, occupying about 42000 hectares <strong>of</strong> land which makes around 67 % <strong>of</strong> the total<br />

surface <strong>of</strong> watershed. Forest area <strong>of</strong> watershed is located in the west side and covers about 8000 hectares. The<br />

upper side <strong>of</strong> watershed is forest and receives annual average rainfall about 750 mm with annual average<br />

temperature 17 0 C. The climate <strong>of</strong> watershed is influenced by Mediterranean climate and Black Sea climate.<br />

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Fig.1 Study area<br />

Normalized Difference Vegetation Index (NDVI)<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

METHODOLOGY<br />

Remote sensing techniques are employed for monitoring and mapping condition <strong>of</strong> ecosystems <strong>of</strong> any part <strong>of</strong><br />

earth. Vegetation cover is the one <strong>of</strong> most important biophysical indicator to soil erosion. Vegetation cover can<br />

be estimated using vegetation indices derived from satellite images. Vegetation indices allow us to delineate the<br />

distribution <strong>of</strong> vegetation and soil based on the characteristic reflectance patterns <strong>of</strong> green vegetation. The<br />

Normalized Difference Vegetation Index (NDVI), one <strong>of</strong> the vegetation indices, measures the amount <strong>of</strong> green<br />

vegetation. The spectral reflectance difference between Near Infrared (NIR) and red is used to calculate NDVI.<br />

The formula can be expressed as (Jensen, 2000);<br />

NDVI = (NIR – red) / (NIR + red)<br />

The NDVI has been used widely in remote sensing studies since its development (Jensen, 2005). NDVI values<br />

range from -1.0 to 1.0, where higher values are for green vegetation and low values for other common surface<br />

materials. Bare soil is represented with NDVI values which are closest to 0 and water bodies are represented<br />

with negative NDVI values (Lillesand et al., 2004: Jasinski, 1990; Sader and Winne, 1992). More than 20<br />

vegetation indices have been proposed and used at present. Since NDVI provides useful information for<br />

detecting and interpreting vegetation land cover it has been widely used in remote sensing studies (Gao, 1996:<br />

Myneni and Asrar, 1994; Sesnie et al., 2008).<br />

A time-series <strong>of</strong> NDVI were derived from Landsat 5 TM images acquired on April, May, June and August 2007.<br />

An average NDVI <strong>of</strong> watershed area was calculated using those NDVI images (Fig.2).<br />

79


C Factor Estimation<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Fig.2 Average NDVI map <strong>of</strong> Buyukcekmece watershed<br />

Soil loss is very sensitive to vegetation cover with slope steepness and length factor (Renard and Ferreira 1993;<br />

Benkobi et al., 1994; Biesemans et al., 2000). Vegetation cover protects the soil by dissipating the raindrop<br />

energy before reaching soil surface. The value <strong>of</strong> C depends on vegetation type, stage <strong>of</strong> growth and cover<br />

percentage (Gitas et al., 2009). The C factor values vary between 0 and 1 based on types <strong>of</strong> land covers. Since<br />

NDVI values have correlation with C factor (De Jong, 1994; Tweddales et al., 2000; De Jong et al., 1999; De<br />

Jong and Riezebos, 1997). Many researchers used regression analysis to estimate C factor values for land cover<br />

classes in erosion assessment (Lin et al., 2002; 2006; Symeonakis and Drake, 2004; Van der Knijff et al., 2002).<br />

The goal <strong>of</strong> regression analysis is to estimate the unknown values <strong>of</strong> dependent variable based upon values <strong>of</strong> an<br />

independent variable using a mathematical model. The linear or non-linear regression equations are constructed<br />

using correlation analysis between NDVI values obtained from remotely sensed image and corresponding C<br />

factor values obtained from USLE/RUSLE guide tables or computed using field observation.<br />

Fig.3 Workflow <strong>of</strong> C factor estimating using NDVI<br />

The study assumes that there exists a linear correlation between NDVI and C factor and uses bare soil and forest<br />

NDVI values as reference values (Fig.3). Sample NDVI values were collected for bare soil and forest land cover<br />

classes from average NDVI image. Since C factor values range from 0 for well-protected soil to 1 for bare soil<br />

(Pierce et al.,1986; Vicenta et al., 2007) the C factor values for bare soil and forest land cover were set to 1 and<br />

0, respectively in the regression analysis. Fig.4 shows the graph <strong>of</strong> the regression equation. The line in Fig.4 is<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

the regression line that describes relationship between C and NDVI values and R shows the correlation<br />

coefficient <strong>of</strong> regression analysis.<br />

The regression equation was found as;<br />

C factor = 1.02 – 1.21 * NDVI<br />

The final C factor map was generated using the regression equation in Spatial Analyst tool <strong>of</strong> ArcGIS 9.3<br />

s<strong>of</strong>tware. The graphs <strong>of</strong> regression analysis and C factor are given in Fig. 4 and Fig.5 respectively.<br />

RESULTS<br />

As can be seen from Table 1, Buyukcekmece experienced lowest mean NDVI values in August. Since watershed<br />

consists <strong>of</strong> agricultural areas the mean NDVI values <strong>of</strong> April, May and June are close to each other. Mean NVDI<br />

values <strong>of</strong> August are lowest because there is no vegetation on agricultural areas.<br />

Table 1 NDVI values <strong>of</strong> Landsat images<br />

Image Date Max NDVI Min NDVI Mean NDVI<br />

April 2007 1 -1 0,395<br />

May 2007 1 -1 0,40<br />

June 2007 1 -1 0,31<br />

August 2007 0,66 -0,43 0,09<br />

Fig.4 Linear regression <strong>of</strong> NDVI and C factor values<br />

As seen from Fig.5 the north part <strong>of</strong> watershed is represented by 0-0.1 C factor class since it is occupied by<br />

forest. Water bodies like Buyukcekmece Lake are represented by 0.9-1.0 C factor class. The agricultural areas <strong>of</strong><br />

watershed are represented by C factor classes from 0.2 to 0.4<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Fig.5 C factor map <strong>of</strong> Buyukcekmece Watershed<br />

The estimated C factor values through regression equation were divided into ten categorical classes and those<br />

classes vary between 0-0.1 and 1.0. The pixel numbers <strong>of</strong> those classes are shown in Fig.6. Since agricultural<br />

areas cover almost 60% <strong>of</strong> watershed area the C factor classes 0.2-0.3 and 0.3-0.4 contain the highest pixel<br />

number respectively. As shown in Fig.6, 0.2-0.3 class has about 28% <strong>of</strong> total pixels while 0.3-0.4 has about 15%<br />

<strong>of</strong> total pixels. The 0.9-1.0 class has the lowest pixel number.<br />

Fig.6 Pixel distribution <strong>of</strong> the C factor map based on NDVI<br />

CONCLUSION<br />

An attempt has been made to estimate C factor values <strong>of</strong> land cover classes using NDVI values for modeling soil<br />

erosion using ArcGIS 9.3 s<strong>of</strong>tware. A regression analysis was performed between NDVI and C factor using an<br />

assumption. C factor values were assigned to pixels <strong>of</strong> NDVI image through regression equation. Based on an<br />

assumption, the C factor map <strong>of</strong> Buyukcekmece watershed was produced to use in soil erosion methods such as<br />

USLE and RUSLE based on an assumption that NDVI and C factor values are correlated with each other. The<br />

results revealed that large parts <strong>of</strong> areas were assigned to C factor classes that vary between 0.2 and 0.4.<br />

It should be noted that C factor values can be precisely estimated using empirical equations that contain field<br />

measurements <strong>of</strong> land cover classes. However, this study shows that NDVI based regression method <strong>of</strong>fers an<br />

optimal method to estimate C factor values <strong>of</strong> land cover classes <strong>of</strong> large areas in a short time.<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

Physiological properties studies on essential oil <strong>of</strong> Jasminum grandiflorum L. as<br />

affected by some vitamins<br />

Rawia.A.Eid, Lobna, S. Taha*, and Soad , M.M. Ibrahim<br />

Department <strong>of</strong> Ornamental Plants and Woody Trees,<br />

National Research Centre, Dokki, Cairo, Egypt<br />

*E-mail address for correspondence: lobnasalah82@yahoo.com<br />

____________________________________________________________________________________<br />

Abstract : A field experiment was conducted out during 2008 and 2009 seasons at Gezayh village, Imbaba<br />

district, Giza Governorate, Egypt. The aim <strong>of</strong> this work is to study the effect <strong>of</strong> foliar application <strong>of</strong> various<br />

concentrations (50, 100 and 150 ppm) <strong>of</strong> ascorbic acid, Thiamin and α –tocopherol separately or<br />

collectively on some flower characters (flower yield and weight <strong>of</strong> flowers), oil pattern (essential oil<br />

concrete percent, yield and some constituents <strong>of</strong> oil), physiochemical properties <strong>of</strong> oil and some chemical<br />

composition <strong>of</strong> Jasminum grandiflorum L. Promoting results were obtained with foliar application <strong>of</strong> all<br />

treatments, especially those <strong>of</strong> Ascorbic acid + Thiamin + α –tocopherol at 100 ppm <strong>of</strong> each or α –<br />

tscopherol at 150 ppm alone on flower yield, weight <strong>of</strong> flowers, oil concrete percent and oil yield as well<br />

as chemical constituents (soluble, non-soluble sugars and carbohydrates). Gas liquid chromatography <strong>of</strong><br />

the oil <strong>of</strong> control plants and those which showed increase in the oil percent revealed that the major<br />

components, i.e. Benzyl Benzoate, benzyl acetate, eugenol, trans-methyl jasmonate and cis jasmone<br />

pronouncedly increased depending on the applied vitamin (ascorbic acid, Thiamin and α –tocopherol)<br />

which also showed a stimulatory effect on physiochemical properties <strong>of</strong> oil such as refractive index,<br />

specific gravity, ester number and acid number as good conductor <strong>of</strong> oil quality.<br />

Keywords: Ascorbic acid, Thiamin , α –tocopherol, jasmin<br />

_____________________________________________________________________________________<br />

INTRODUCTION<br />

Jasmine (Jasminum grandiflorum L.) is an ornamental plant <strong>of</strong> Oleacae. It is semi-evergreen to deciduous<br />

shrub reaching a length <strong>of</strong> 8 meters, <strong>of</strong>ten with pendulous branches. The leaves are odd-pinnate wit 7 to 9<br />

leaflets and used medicinally in skin diseases, odontalgia, otalgia, wounds, etc. (Kulkarmi and Ansari,<br />

2004; Sharma et al., 2005).<br />

The flowers are white with faint, pinkish streaks, delightfully fragment, and borne in lax, terminal<br />

inflorescences. These flowers are not only essential to the perfumery industry but also have been highly<br />

appreciated by orientals since time immemorial. The pretty jasmine flower originated in the lower valleys<br />

<strong>of</strong> the Himalayas <strong>of</strong> northern India (Braja et al ., 1990). The shrub is widely cultivated in the plains and<br />

on the hills specially in Kashmir, Afghanistan, Persia, France, China, Japan and Egypt (Frank and Amelio,<br />

1999).<br />

Jasmine oil has great value for treating sever depression, respiratory tract, for muscle pain and for toning<br />

the skin. This oil is expensive. It takes approximately 800 kilos <strong>of</strong> petals or 10000 flowers, to make 1 kilo<br />

<strong>of</strong> concrete jasmine. Egypt is the main producer <strong>of</strong> jasmine oil.<br />

Plants have a small molecule antioxidants (e.g. ascorbic acid, vitamin C), glutathion and tocopherol<br />

(vitamin E) that they have signaling roles in plant development. In general, the energy metabolism<br />

pathway could be affected by one or another <strong>of</strong> these substances (Robinson, 1973; Pallanca and<br />

Smirn<strong>of</strong>f, 2000).<br />

Ascorbate is the most abundant antioxidant in plants but little was known about its biosynthesis.<br />

Smirrn<strong>of</strong>f et al., (2001) proposed a biosynthetic pathway and identified novel some enzymes. They also<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

reported that ascorbate is synthesized from L-galactose via GDP-mannose and GDP-L-galactose. El-<br />

Kobisy et a.,l (2005) stated that Ascorbic acid is synthesized in the higher plants and affects plant growth<br />

and development, it is product <strong>of</strong> D-glucose metabolism which affects some nutritional cycles activity in<br />

higher plants and play an important role in the electron transport system. Ascorbic acid (vitamin C) is<br />

known as a growth regulating factor which influences many biological processes, Price (1966). Robinson<br />

(1973) reported that Ascorbic acid acts as co-enzymatic reactions by which carbohydrates; proteins are<br />

metabolized and involved in photosynthesis and respiration processes.<br />

Ascorbic acid is an important antioxidant, which reacts not only with H2O2 but also with O2, OH and lipid<br />

hydroperoxidase (CSIR, 1992; Jacobs et al., 2000). A high level <strong>of</strong> endogenous ascorbate is essential<br />

effectively to maintain the antioxidant system that protects plants from oxidative damage (Cheruth, 2009).<br />

Tarraf et al., (1999) on lemongrass (Cympapogom citrates L.) and Farahat et al (2007) on Cupressus<br />

semperviren L. reported that foliar application <strong>of</strong> ascorbic acid caused pronounced increases in vegetative<br />

growth and chemical constituents as well as essential oil percent, oil yield per plant.<br />

Thiamin (vitamin B1) is a necessary ingredient for the biosynthesis <strong>of</strong> the coenzyme Thiamin<br />

pyrophosphate, so it plays an important role in carbohydrate metabolism. It is an essential nutrient for both<br />

plants and animals.<br />

In plants, it is synthesized in the leaves and is transported to the roots where it controls growth. Thiamin is<br />

an important c<strong>of</strong>actor for the translocation reactions <strong>of</strong> the pentose phosphate cycle, which provides<br />

pentose phosphate for nucleotide synthsis and for the reduced NADP required for various synthetic<br />

pathways (Kawasaki, 1992). Youssef and Talaat (2003) reported that pronounced increases in vegetative<br />

growth and chemical constituents <strong>of</strong> rosemary plants by foliar application <strong>of</strong> thiamine.<br />

Alpha-tocopherol (vitamin E) is low molecular weight lipophilic antioxidant which mainly protect<br />

membrane from oxidative damage (Asada, 1999). Zhang et al., (2000) reported a positive correlation<br />

between α-tocopherol and shoot or root growth in two grass species grown under drought. Tocopherols<br />

were proposed to function in relation to their antioxidant properties being prominent in protection <strong>of</strong><br />

polysaturated fatty acids from lipid peroxidation (Bosch, 1995). Recently, tocopherol had an antioxigenic<br />

property when added to green lubricating oil as rapeseed oil (Xiao et al., 2008).<br />

The aim <strong>of</strong> the present study was to reveal the best level to apply <strong>of</strong> ascorbic, thiamin and α-tocopherol<br />

which could improve the flower characters, chemical constituents and essential oil production <strong>of</strong> Jasminum<br />

grandiflorum L.<br />

Materials and methods<br />

A field experiments were conducted out at Gezayh village, Imbaba district, Giza Governorate, Egypt during<br />

two successive seasons <strong>of</strong> 2008 and 2009. The aim objective <strong>of</strong> this study was to investigate the effect <strong>of</strong><br />

foliar application <strong>of</strong> ascorbic acid, Thiamin and α –tocopherol on yield <strong>of</strong> flowers, oil pattern and chemical<br />

constituents <strong>of</strong> Jasminum grandiflorum L. cv. The investigated soil characterized by coarse sand 54%,<br />

fine sand 1%, silt 23 %, clay 22%, pH 7.5, EC 3.79 dSm -1 , and (N 35.3, P 22.6 and K 5.6 mg/100 g soil).<br />

Thirty three years old trees <strong>of</strong> jasmine were planted 2X2 m apart (1000 tree /fed). The experimental area<br />

was irrigated by flood irrigation system.<br />

Trees were sprayed twice with freshly prepared solutions <strong>of</strong> ascorbic acid, thiaminand α-tocopherol each at<br />

50, 100 and 150 ppm, and combination <strong>of</strong> the different concentrations <strong>of</strong> the three factors had been also<br />

carried out, in addition to the untreated plants (control) which were sprayed with tap water. Foliar<br />

application <strong>of</strong> ascorbic acid, thiamine and α-tocopherol carried out two times <strong>of</strong> 30 days intervals, starting<br />

at one month after March at both seasons.<br />

During the flowering period <strong>of</strong> each season, the following data were recorded: flowers yield/tree (kg) and<br />

weight <strong>of</strong> 100 flowers (g). Jasmine concrete was extracted from the flowers using a solvent extraction<br />

system <strong>of</strong> N-hexane according to Guenther (1961).<br />

Flowers are placed in vessel and covered with the solvent such as hexan, it gently heated electrically while<br />

the solvent extracts the fragments molecules <strong>of</strong> the plant. The fragment chemicals are transferred to the<br />

alcohol which is removed by low heat distillation. The essential oil was dried over anhydrous sodium<br />

sulfate and stored at 4-6 o C. The essential oil was subjected to Gc/Ms analysis and its components were<br />

identified by matching their relative retention times in conjunction <strong>of</strong> discriminating Ms ions against a<br />

computer library file <strong>of</strong> large number <strong>of</strong> data obtained under identical experimental conditions (Adams,<br />

1995). Gc/Ms Analysis was carried out on finningan Mat SSQ 7000 mass sepctometer directly coupted to<br />

a varion 3400 gas chromatography equipped with DB-5 (0.25 mm i.d. dX30m, 0.25 coating thickness,<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

fused silica capillary column using helium as the carrier gas at flow rate <strong>of</strong> 1.017 ml/min injector<br />

temperature, 220 o C transfer/line, 250 o C oven temperature programmed, 60 to 250 o C at 3 o C/min.<br />

Some jasmine oil characters i.e. refractive index at 20 o C, specific gravity at 15 o C, acid number and ester<br />

number were determined according to Guenther (1961). Also, total carbohydrates and soluble and non<br />

soluble sugars % in the flowers were estimated according to Herbert et al (1971). The recorded data<br />

(means <strong>of</strong> the two growing seasons) were statistically analyzed using the completely randomized design in<br />

factorial arrangement according to the procedure <strong>of</strong> Snedecor and Cochran (1980), where the means <strong>of</strong><br />

the studied treatments were compared using LSD test at 0.05 <strong>of</strong> probability.<br />

Flower characters<br />

RESULTS AND DISCUSSION<br />

Data presented in Table (1) reveled that all treatments <strong>of</strong> ascorbic acid, thiamine and α-tocopherol<br />

separately or collectively significantly increased flower yield/tree and weight <strong>of</strong> flowers (100 flowers (gm))<br />

<strong>of</strong> Jasminum grandiflorum L. trees compared with untreated plants. The highest increases in flower yield<br />

and fresh weight <strong>of</strong> flowers were observed in plants treated with Asc. 100 ppm + thiamin 100 ppm + αtocopherol<br />

100 ppm followed by α-tocopherol 150 ppm. The increments were 76.68 and 75.21 %, for<br />

flower yield than the corresponding values <strong>of</strong> control plants, the fresh weight <strong>of</strong> f lowers increased by 56.69<br />

and 53.42 % than the corresponding values <strong>of</strong> the control plants. Similar results were obtained by El-<br />

Quesni et al (2009) who revealed that foliar application <strong>of</strong> Ascorbic acid and α-tocopherol on Hibiscus rosa<br />

, Sineses L. plants significantly increased number <strong>of</strong> flower/plant and fresh weight <strong>of</strong> flowers gm/plant<br />

compared with untreated plants. The stimulatory effects <strong>of</strong> ascorbic acid may be attributed to its role in the<br />

regulation <strong>of</strong> cell division, differentiation and enhancement <strong>of</strong> leaf expansion (Noctor and Foyer, 1998).<br />

The effect <strong>of</strong> thiamin was showed by Kawasaki (1992) who reported that thiamin (vitamin B1) is an<br />

essential nutrient for plant growth. It is synthesized in the leaves and is translocated to the roots where it<br />

controls growth. In addition, α-tocopherol interacts with the polyunsaturated acyl groups <strong>of</strong> lipids, stabilize<br />

membranes, protect chloroplast from photooxidation and help to provide an optimal environment for<br />

photosynthetic machinery (Jaleel et a.l, 2006 and Jaleel et al., 2007).<br />

Essential oil concrete percent and oil yield<br />

Data given in Table (1) show that the foliar application <strong>of</strong> Ascorbic acid , thiamin, α-tocopherol or the<br />

combination <strong>of</strong> them significantly increased both jasmine concrete essential oil percent and oil yield as<br />

gm/tree compared to control plants. The highest increment was obtained with treatments <strong>of</strong> Ascorbic acic<br />

100 ppm + thiamin 100 ppm + α-tocopherol 100 ppm or α-tocopherol 150 ppm alone. It could be deduced<br />

from the present results that both concrete essential oil percent and oil yield (g/tree) responded to foliar<br />

application <strong>of</strong> vitamins. In support, Hasnaa et al (2009) on Pelargonium graveolens L. indicated that αtocopherol<br />

treatments at 50 and 100 mg/l significantly increased concrete essential oil percent and yield.<br />

This might be due to Alfa-tocopherol could cause a pronounced enhancement <strong>of</strong> both synthesis and<br />

accumulation <strong>of</strong> oil. Also, Gamal El-Din (2005) on sunflower plants, reported that ascorbic acid<br />

significantly increased oil percentage <strong>of</strong> seeds.<br />

Essential oil constituents<br />

Data represented in Table 2 indicates that oil <strong>of</strong> treated and control plant mainly consisted from benzyl<br />

benzaoat as major constituent (20.1-26.6 %), followed by benzyl acetate (4.8-7.7%) , benzyl alcohol (1.3-<br />

2.7%), eugenol (2.0-4.0%), trans-methyl Jasmonate (5.0-7.8%), cis jasmone (2.3-7.1%) and jasmine lactone<br />

(3.1-8.5%). On the other hand, Gas liquid chromatography showed that oil consists <strong>of</strong> other constituents<br />

such as n-acetyl and methyl anthranilate. Benzyl benzoate content was pronouncedly increased at<br />

treatment (150 ppm) <strong>of</strong> Ascorbic acid, thiamin or α-tocopherol. The highest increment was obtained with<br />

their combination treatment at concentration <strong>of</strong> 100 or 150 ppm. Similar trend was found in case <strong>of</strong> benzyl<br />

acetate, benzyl alcohol, eugenol, trans-methyl jasmonate and cis jasmone contents. However, treatment <strong>of</strong><br />

Ascorbic acid 100+ Thiamin 100 ppm + α-tocopherol 100 ppm gave the highest content <strong>of</strong> n-acetyl.<br />

Highest content <strong>of</strong> methyl anthranilate was obtained with α-tocopherol (100 ppm). These results were in<br />

agreement with those obtained by Youssef and Iman (2003) on Rosmarinus <strong>of</strong>ficinals L. who found that oil<br />

composition responded greatly to foliar spray <strong>of</strong> the vitamins nicotineamide, ascorbic and thiamin at<br />

different rates <strong>of</strong> application. Hasnaa et al., (2009) reported that Gas-liquid chromatography <strong>of</strong> the oil <strong>of</strong><br />

Pelargonium graveolens L. revealed that the major components, i.e. citronellol and linalool pronouncedly<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

increased depending on the applied stigmasterol or α-tocopherol. Therefore, one can conclude the positive<br />

response <strong>of</strong> jasmin oil constituents depended on the level <strong>of</strong> applied ascorbic acid, thiamin and αtocopherol.<br />

Essential oil physiochemical properties<br />

Results in Table 3 showed that refractive index <strong>of</strong> jasmine oil at 20 o C under treatments (ascorbic acid,<br />

thiamin, α-tocopherol and their combination) ranged from 1.41 to 1.50 in comparison with 1.3 in the<br />

control treatment. α-tocopherol (100 or 150 ppm) or Ascorbic acid + thiamin + α-tocopherol (50, 100 or<br />

150 ppm) resulted in the highest refractive index value <strong>of</strong> jasmine oil. Refractive index <strong>of</strong> oil increases<br />

with increase in the number <strong>of</strong> double bonds (iodine value). In general, the refractive indices <strong>of</strong> oils relate<br />

to the degree <strong>of</strong> unsaturation in a linear way (Rudan-Tasic & Kl<strong>of</strong>utar, 1999). Also, the specific gravity is<br />

a good indicative <strong>of</strong> purity <strong>of</strong> oil and depends on the number <strong>of</strong> double bonds. At any given temperature,<br />

specific gravity increases as the mean molecular weight decreases with increase in degree <strong>of</strong> unsaturation<br />

(higher iodine value). In our study, we can notice that specific gravity <strong>of</strong> oil under treatments ranged from<br />

0.93 to 0.99 in comparison with 0.82 in the control treatment (Table 4).<br />

Results showed that the ester no. <strong>of</strong> jasmine oil were 50.0 to 55.8 with tested treatments, compared with<br />

48.2 in the control. The acid no. <strong>of</strong> jasmine oil was 40.3 to 50.8 with various treatments, compared with<br />

45.3 in the control. The acid value is an indirect measure <strong>of</strong> free fatty acid contents present in oil. Hence it<br />

is not desirable, because they render unpleasant odor and deteriorate the quality <strong>of</strong> the product (Muhammad<br />

et al., 1999). However, the fragrance <strong>of</strong> jasmine is characterized by "jasmonoid" compounds, whose<br />

biosynthesis from unsaturated fatty acids. Under study, the results in Table 4, indicates that both Ascorbic<br />

acid and thiamin at 50, 100 and 150 ppm reduced the acid number than that <strong>of</strong> control treatment. In<br />

support, Ismail et al, 2007 indicated that refractive index <strong>of</strong> jasmine oil at 20 o C is 1.04, specific gravity <strong>of</strong><br />

oil at 15 o C is 0.4113, ester no. is 46.34 and the Acid no. <strong>of</strong> jasmine oil is 43.03 in untreated plants.<br />

Chemical constituents<br />

Data presented in Table 4 show that all treatments <strong>of</strong> Ascorbic acid, thiamin and α-tocopherol separately or<br />

collectively significantly increased soluble sugars, nonsoluble sugars and total carbohydrate %. The<br />

highest increment was observed in case <strong>of</strong> treatment Ascorbic acid + thiamin + α-tocopherol each at 100<br />

ppm followed by α-tocopherol 150 ppm. The increments were 54.6 and 52.11 % for soluble sugars, 73.29<br />

and 69.59 % for nonsoluble sugars and 48.84 and 40.78 % for total carbohydrates than the corresponding<br />

values <strong>of</strong> the control plants., these results could be explained by the findings obtained by Price (1966) who<br />

reported that ascorbic acid increased nucleic acid content, especially RNA and protein content <strong>of</strong> wheat<br />

grains. It also influenced by synthesis <strong>of</strong> enzymes, and proteins, in addition, it acts as co-enzyme in<br />

metabolic changes (Reda et al., 1977; Fadl et al, 1978 and Abdel-Halim, 1995). These results are also in<br />

agreement with those obtained by Kawasaki (1992) who reported that thiamine (vitamine B1) is a<br />

necessary ingredient for the biosynthesis <strong>of</strong> the co-enzyme thiamin pyrophosphate , in this latter form it<br />

plays an important role in carbohydrate metabolism. El-Bassiouny et al., (2005) reported that foliar spray<br />

with α-tocopherol on faba bean plant induced increments in yield components. Also , El-Quesni et al.,<br />

(2009) indicated that foliar application <strong>of</strong> Asc. acid and α-tocopherol separately to hibiscus plants<br />

significantly increased total soluble sugars through flowering stage.<br />

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Table 1: Flower characters, oil percent and oil yield (g/tree) <strong>of</strong> Jasminum grandiflorum L. plants as<br />

affected by Ascorbic acid, thiamin and α-tocopherol. (Average <strong>of</strong> the two seasons)<br />

Treatments<br />

Conc.<br />

ppm<br />

Flower yield<br />

kg/tree<br />

91<br />

Weight <strong>of</strong> 100<br />

flowers (gm)<br />

Concrete<br />

(%)<br />

Oil yield<br />

(g/tree)<br />

Control 0.87 6.8 0.13 1.13<br />

Ascorbic acid 50 1.74 8.70 0.20 3.48<br />

100 2.89 11.90 0.25 7.23<br />

150 3.15 13.40 0.29 9.14<br />

Thiamin 50 1.05 8.3 0.18 2.29<br />

100 1.85 9.0 0.23 4.26<br />

150 2.34 10.5 0.19 4.45<br />

α-tocopherol 50 2.11 10.3 0.22 4.64<br />

Ascorbic acid 50 + Thiamin 50 +<br />

α-tocopherol 50 ppm<br />

Ascorbic acid 100 + Thiamin 100 +<br />

α-tocopherol 100 ppm<br />

Ascorbic acid 150 + Thiamin 150 +<br />

α-tocopherol 150 ppm<br />

100 3.00 12.0 0.28 8.40<br />

150 3.51 14.6 0.32 11.23<br />

3.11 13.6 0.26 8.09<br />

3.73 15.7 0.34 12.68<br />

2.15 14.2 0.32 6.88<br />

LSD 5% 0.31 0.25 0.01 0.05


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 2: Major constituents <strong>of</strong> essential oil from Jasminum grandiflorum L. as affected by Ascorbic acid, thiamin and α-tocopherol.<br />

Order Retention<br />

time<br />

1 0.532<br />

(Average <strong>of</strong> the two seasons)<br />

Treatments<br />

Constituents<br />

Benzyl<br />

Benzoat&Photol<br />

Control<br />

Ascorbic acid Thiamin α-tocopherol<br />

92<br />

ppm<br />

Asorbic acid+Thiamin +<br />

α-tocopherol<br />

50 100 150 50 100 150 50 100 150 50 100 150<br />

20.1 21.2 21.5 23.0 21.5 21.5 23.0 21.5 21.8 23.4 22.5 26.5 26.6<br />

2 0.729 Benzyl Acetate 4.8 5.2 5.9 6.8 5.0 5.8 6.8 5.8 6.4 6.8 6.8 7.5 7.7<br />

3 0.838 Benzyl Alcohol 1.3 1.7 2.1 2.2 1.8 2.1 2.5 1.5 2.1 2.4 1.9 2.7 2.6<br />

4 0.919 Eugenol 2.0 2.1 2.5 2.9 2.0 3.3 2.7 2.2 2.5 3.1 2.5 3.8 4.0<br />

5 1.234<br />

Trans-methyl<br />

Jasmonates<br />

5.0 5.8 6.5 7.1 5.8 6.8 7.0 5.7 6.6 7.6 5.9 7.8 7.6<br />

6 1.641 Cis Jasmone 2.3 2.5 3.3 6.2 1.8 3.7 5.8 2.4 3.4 6.5 2.0 7.0 7.1<br />

7 1.845 Jasmine Lactone 3.1 5.5 6.2 7.4 4.3 5.7 4.5 6.5 7.4 8.5 7.0 7.9 7.5<br />

8 1.941 n-acetyl 0.81 1.0 1.5 1.8 1.1 1.3 1.6 1.4 1.8 2.2 2.2 2.5 1.9<br />

9 1.958<br />

Methyl<br />

anthranilate<br />

1.2 1.7 1.9 2.1 1.3 1.6 1.3 2.6 3.2 3.6 2.8 3.1 3.0


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 3: Physiological properties <strong>of</strong> essential oil from Jasminum grandiflorum L. as affected by Ascorbic acid, thiamin and α-tocopherol.<br />

Properties<br />

(Average <strong>of</strong> the two seasons)<br />

Treatments<br />

Control<br />

Ascorbic acid Thiamin α-tocopherol<br />

93<br />

ppm<br />

Asc.+Thiamin+<br />

α-tocopherol<br />

50 100 150 50 100 150 50 100 150 50 100 150<br />

Refractive index 20 o C 1.31 1.43 1.43 1.43 1.41 1.41 1.42 1.43 1.48 1.49 1.49 1.50 1.50 0.02<br />

Specific gravity 0.82 0.94 0.94 0.94 0.93 0.94 0.94 0.96 0.97 0.97 0.99 0.99 0.99 0.02<br />

Ester number 48.2 50.0 51.3 51.9 50.0 51.2 51.8 50.1 55.2 55.7 55.2 55.6 55.8 0.12<br />

Acid number 45.3 44.2 44.5 44.8 40.7 40.9 40.3 49.2 50.1 50.7 50.2 50.8 50.5 0.022<br />

LSD<br />

5%


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 4: Chemical constituents <strong>of</strong> Jasminum grandiflorum L.flowers (%) as affected by Ascorbic acid,<br />

thiamin and α-tocopherol. (Average <strong>of</strong> the two seasons)<br />

Treatments<br />

Conc.<br />

ppm<br />

94<br />

Soluble<br />

sugars<br />

Non-soluble<br />

sugars<br />

Total<br />

carbohydrate<br />

Control 10.2 2.11 13.2<br />

Ascorbic acid 50 15.2 2.81 19.8<br />

100 16.7 3.57 20.4<br />

150 17.9 4.11 21.5<br />

Thiamin 50 13.3 2.73 17.3<br />

100 13.2 3.84 18.4<br />

150 11.4 3.65 16.2<br />

α-tocopherol 50 17.3 3.41 20.4<br />

Ascorbic acid 50 + Thiamin 50 +<br />

α-tocopherol 50 ppm<br />

Ascorbic acid 100 + Thiamin 100 +<br />

α-tocopherol 100 ppm<br />

Ascorbic acid 150 + Thiamin 150 +<br />

α-tocopherol 150 ppm<br />

100 19.5 5.81 22.2<br />

150 21.3 6.94 22.8<br />

20.4 6.7 22.6<br />

22.5 7.9 25.8<br />

21.0 5.8 24.3<br />

LSD 5% 1.82 0.23 0.13


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Effect <strong>of</strong> zinc and / or iron foliar application on growth and essential oil <strong>of</strong> sweet<br />

basil (Ocimum basilicum L.) under salt stress<br />

H.A.H. Said-Al Ahl* and Abeer A. Mahmoud **<br />

* Department <strong>of</strong> Cultivation and Production <strong>of</strong> Medicinal and Aromatic Plants, National Research<br />

Centre, Dokki, Giza, Egypt.<br />

** Department <strong>of</strong> Botany (Plant Physiology Section), Faculty <strong>of</strong> Agriculture, Cairo University.<br />

*Corresponding Author: saidalahl@yahoo.com<br />

___________________________________________________________________________________<br />

Abstract: The effect <strong>of</strong> salinity and Fe and/or Zn application on the vegetative growth, dry matter yield<br />

and essential oil production and its constituents were studied at the farm station <strong>of</strong> the National<br />

Research Centre, at Shalakan, Kalubia Governorate, Egypt on sweet basil (Ocimum basilicum L.)<br />

during 2006 and 2007 seasons. The highest plant height, number <strong>of</strong> branches, fresh and dry matter<br />

yield as well as essential oil yield was recorded in normal soil which decreased with the increase in the<br />

salinity. Increasing the soil salinity increased essential oil %. The addition <strong>of</strong> micronutrients had an<br />

active effect comparing with control, highest plant height and number <strong>of</strong> branches being with iron<br />

application and zinc gave the highest value <strong>of</strong> fresh weight, whereas a mixture <strong>of</strong> iron + zinc gave the<br />

highest values <strong>of</strong> dry matter and essential oil yield under normal soil condition. In contrast application<br />

a mixture <strong>of</strong> iron + zinc gave the highest essential oil % under soil salinity condition. Concerning<br />

essential oil constituents, linalool and methylchavicol were the major compounds. The concentration <strong>of</strong><br />

linalool and methylchavicol decreased with saline soil treatment. Addition <strong>of</strong> micronutrients decreased<br />

linalool in normal soil; on the contrary there was an increase in linalool content by using soil salinity<br />

treatment. Highest linalool content (52.14%) was recorded in saline soil with spraying mixture <strong>of</strong><br />

zinc+iron. Spraying plants with zinc and /or zinc+ iron increased the content <strong>of</strong> methylchavicol in<br />

normal soil, and it's content (44.01%) was the highest in normal soil with zinc spraying. All the<br />

spraying treatments except mixture <strong>of</strong> zinc+iron increased the content <strong>of</strong> methylchavicol in saline soil.<br />

The highest decrease in linalool (25.687%) and methylchavicol (20.34%) was caused with zinc+iron in<br />

normal and saline soils, respectively.<br />

Key words: sweet basil, Ocimum basilicum L., foliar application, iron, zinc, salt stress, essential oil<br />

________________________________________________________________________________<br />

INTRODUCTION<br />

The Ocimum genus, belonging to the Lamiaceae family, includes herbs and shrubs distributed in<br />

tropical and subtropical regions <strong>of</strong> Asia, Africa and the Americas. The most important species <strong>of</strong><br />

Ocimum genus is O. basilicum L.; this species, usually named common basil or sweet basil, is<br />

considered economically useful because <strong>of</strong> their basic natural characteristics as essential oil<br />

producers (Lawrence, 1993). Sweet basil is a popular culinary herb used in food and oral care<br />

products (La-Chowicz et al., 1996; Machale et al., 1997). The essential oil <strong>of</strong> the plant is also used as<br />

perfumery. Also, basil is well known as a plant <strong>of</strong> a folk medicinal used as carminative, galactogogue,<br />

stomachic and antispasmodic tonic and vermifugem, also, basil tea taken hot is good for treating<br />

nausea, flatulance and dysentery (Ozcan and Chalchat, 2002; Sajjadi, 2006). Basil is used in pharmacy for<br />

diuretic and stimulating properties, in perfumes and cosmetics for its smell; in fact, it is a part <strong>of</strong> many<br />

fragrance compositions (Bariaux et al., 1992; Khatri et al., 1995). Antiviral and antimicrobial activities<br />

<strong>of</strong> this plant have also been reported (Chiang et al., 2005). Available literature data indicates that<br />

there is a great deal <strong>of</strong> diversity in growth characteristics and the composition <strong>of</strong> essential oil <strong>of</strong> the<br />

genus Ocimum. Such observations have been attributed to the abundant cross-pollination that<br />

occurs within this genus resulting in considerable degrees <strong>of</strong> variation in the genotypes<br />

(Lawrence, 1988). The difference in the essential oil compositions in O. basilicum cultivated in<br />

different geographical localities led to the classification <strong>of</strong> basil into chemotypes on the basis <strong>of</strong> the<br />

97


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

prevalent chemical components (Lawrence, 1992) or components having composition greater than<br />

20 percent (Grayer et al., 1996). There are usually considerable variations in the contents <strong>of</strong> the<br />

major components within this species. In a study <strong>of</strong> essential oils <strong>of</strong> different geographical origins,<br />

(Lawrence, 1988) found that the main constituents <strong>of</strong> the essential oil <strong>of</strong> basil are produced by two<br />

different biochemical pathways, the phenylpropanoids (methyl chavicol, eugenol, methyleugenol and<br />

methyl cinnamate) by the shikimic acid pathway, and the terpenes (linalool and geraniol) by the<br />

mevalonic acid pathway. Other latter studies on the basils from other geographical regions have<br />

added new chemotypes to that list based on the established classification scheme (Grayer,<br />

1996; Lawrence, 1992).<br />

Salinity is one <strong>of</strong> the major factors that affect plant growth; it is a serious problem in many areas <strong>of</strong><br />

world's causing considerable loss in agricultural production (Bray et al., 2000; Shao et al., 2008; Wu et<br />

al., 2007). Soil salinity resulting from natural processes or from crop irrigation with saline water,<br />

occurs in many arid and semi-arid regions <strong>of</strong> the world (Lauchli and Epstein, 1990). The deleterious<br />

effects <strong>of</strong> salinity on plant growth are associated with (1) low osmotic potential <strong>of</strong> soil solution (water<br />

stress), (2) nutritional imbalance, (3) specific ion effect (salt stress), or (4) a combination <strong>of</strong> these<br />

factors (Yildirim and Taylor, 2005). Saline soil are generally dominated by sodium ions, with the<br />

dominant anions being chloride and sulphate, they have a high sodium absorption rate with a high pH<br />

and electrical conductivities (>4 dsm -1 ) (Flowers and Flowers, 2005).<br />

In saline soils, the solubility <strong>of</strong> micronutrients is particularly low, and plants grown on such soil <strong>of</strong>ten<br />

suffer from deficiencies in these elements. Soil salinity may reduce micronutrients uptake due to<br />

stronger competition by salt cations at the root surface (Marschner and Romheld, 1994; Page et al.,<br />

1990). Soluble ferrous fe tended to become oxidized to ferric oxide which was insoluble as well as the<br />

limitation <strong>of</strong> iron uptake by root cell cytosol (Nikolic and Kastori, 2000) and inhibit iron transport to<br />

shoots and its transfer from apoplasm to cytoplasm in shoot tissues (Nikolic and Romheld, 2002). Zinc<br />

is necessary for root cell membrane integrity (Welch et al., 1982). As suggested by Parker et al. (1992),<br />

root cell membrane permeability is increased under zinc deficiency which might be related to the<br />

functions <strong>of</strong> zinc in cell membranes. From this point <strong>of</strong> view, external zinc concentrations could<br />

mitigate the adverse effect <strong>of</strong> NaCL by inhibiting Na and /or Cl uptake or translocation. Alpaslan et al.<br />

(1999) concluded that in the salt affected areas, zinc application could alleviate possible Na and Cl<br />

injury in plants. Foliar spraying under these conditions could be much more efficient than any<br />

application <strong>of</strong> nutrients to the soil (Horesh and Levy, 1981).<br />

Iron (Fe) is a c<strong>of</strong>actor for approximately 140 enzymes that catalyze unique biochemical reactions<br />

(Brittenham, 1994). Hence, iron fills many essential roles in plant growth and development, including<br />

chlorophyll synthesis, thylakoid synthesis and chloroplast development (Miller et al., 1995). Iron is<br />

required at several steps in the biosynthetic pathways. Zinc (Zn ) is an essential element for plant that<br />

act as a metal component <strong>of</strong> various enzymes or as a functional structural or regulatory c<strong>of</strong>actor and for<br />

protein synthesis, photosynthesis, the synthesis <strong>of</strong> auxin, cell division, the maintance <strong>of</strong> membrane<br />

structure and function, and sexual fertilization (Marschner, 1995).<br />

Moreover, little is known about salinity interaction with iron and zinc deprivation, the present study<br />

aimed to decrease salinity stress is a main issue in this study to ensure increasing production. Also, the<br />

present study describes the composition <strong>of</strong> the essential oils <strong>of</strong> sweet basil cultivated in Egypt.<br />

MATERIALS AND METHODS<br />

A field experiment was conducted at the farm station <strong>of</strong> the National Research Centre, at Shalakan,<br />

Kalubia Governorate, Egypt during the two successive seasons <strong>of</strong> 2006 and 2007. The physical and<br />

chemical properties <strong>of</strong> the soil sample were determined according to Jackson, 1973, Table 1.<br />

Seeds <strong>of</strong> Ocimum basilicum L. were provided by the Medicinal and Aromatic Plants Division,<br />

Horticultural Research Institute, Agricultural Research Center, Ministry <strong>of</strong> Agriculture, Egypt. The<br />

seeds <strong>of</strong> basil were sown in the nursery on 1 st March <strong>of</strong> both seasons. After 45 days from seed sowing,<br />

uniform seedlings were transplanted into plots 3x3.5m. on rows, with 60cm a part and 20 cm between<br />

the seedlings. The experimental layout was split plot design in a complete randomized block design<br />

with three replications. The main plots were devoted to the two levels <strong>of</strong> soil salinity (normal soil and<br />

saline soil), while the sub ones were assigned for three sources <strong>of</strong> second factor (Fe, Zn, and a mixture<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

<strong>of</strong> Fe + Zn). The experimental treatments consisted <strong>of</strong> 8 treatments, which represented all combinations<br />

between soil salinity conditions (normal soil, S1 = 0.73 ppm and saline soil, S2 = 4.95 ppm) and foliar<br />

application treatments (F0= control, F1= 250 ppm iron as a foliar spray <strong>of</strong> the chelated Fe-EDTA (Fe<br />

8.5%), F2= 250 ppm Zn-EDTA (Zn16%) and F3= 250 ppm mixture <strong>of</strong> zinc and iron) were sprayed at<br />

interval times <strong>of</strong> 45, 60, 120 and 150 days from transplanting.<br />

Growth characters and chemical constituent's determinations were carried out at the first and second<br />

cuts after 90 and 180 days from transplanting, respectively before flowering. The following data were<br />

recorded. Plant height (cm), number <strong>of</strong> branches / plant, fresh and dry weights <strong>of</strong> herb (g / plant or ton /<br />

feddan). The essential oil percentage was determined in the air dried herb using a modified Clevenger<br />

apparatus according to Guenther (1961). Essential oil percentage was determined and expressed as (%),<br />

while essential oil yield per plant was expressed as ml plant -1 . The essential oils <strong>of</strong> each treatment at<br />

the first and second cuts were collected and dehydrated over anhydrous sodium sulphate and kept in a<br />

refrigerator until GLC analysis. The GLC analysis <strong>of</strong> the essential oil samples was carried out in the<br />

second season using gas chromatography instrument stands at the Central Laboratory <strong>of</strong> the National<br />

Research Center with the following specifications. Instrument: Hewlett Packard 6890 series, Column:<br />

HP (Carbwax 20M) 25m length × 0.32mm I.D, Film thickness: 0.3Mm, Sample size: 1µl, oven<br />

temperature: 60-190 °C, Program: 60 °C/2min, 8 °C/min, 190 °C/25min. Injection port temperature:<br />

240 °C, Detector temperature (FID): 280 °C, Carrier gas: nitrogen, Flow rate: N2 30 ml/min; H2 30<br />

ml/min; air 300 ml/min. Main compounds <strong>of</strong> the essential oils were identified by matching their<br />

retention times with those <strong>of</strong> the authentic samples injected under the same conditions. The relative<br />

percentage <strong>of</strong> each compound was calculated from the area <strong>of</strong> the peak corresponding to each<br />

compound.<br />

Data were exposed to the proper statistical analysis <strong>of</strong> variance according to LeClerg et al. (1966) as<br />

well as Snedecor and Cochran (1990). The means represented in the study following by the same<br />

alphabetical letters were not significantly different at the probability level <strong>of</strong> 0.05, Least Significant<br />

differences (L.S.D) were used compare between means according to Waller and Duncan (1969) at<br />

probability 5%.<br />

A. Growth characters and yield<br />

Effect <strong>of</strong> soil salinity<br />

RESULTS AND DISCUSSIONS<br />

Tables (2-5) show the effect <strong>of</strong> soil salinity on plant height, number <strong>of</strong> branches, fresh and dry weights<br />

<strong>of</strong> herb (g/plant or ton/fed.) <strong>of</strong> the basil plants. These growth characters decreased significantly with<br />

soil salinity conditions in both cuts during two seasons. The inhibitory effect <strong>of</strong> salinity was also found<br />

by (Abd El-Hady, 2007; Abd El-Wahab, 2006; Baghalian et al., 2008; Belaqziz et al., 2009; Ozturk et<br />

al., 2004; Razmjoo et al., 2008; Shalan et al., 2006; Turhan and Eris, 2007). Saline conditions reduce<br />

the ability <strong>of</strong> plants to absorb water causing rapid reductions in growth rate, and induce many<br />

metabolic changes (Epstein, 1980). Also, salt stress with osmotic, nutritional and toxic effects prevents<br />

growth in many plant species (Cheeseman, 1988; Hasegawa et al., 1986). Therefore, the reduction in<br />

growth was explained by lower osmotic potential in the soil, which leads to decreased water uptake,<br />

reduced transpiration, and closure <strong>of</strong> stomata, which is associated with the reduced growth (Ben-Asher<br />

et al., 2006; Levitt, 1980). In general, the mechanisms <strong>of</strong> salinity effect on plant growth were reported<br />

by Meiri and Shalhavet (1973) who attributed the effect <strong>of</strong> salinity to the following points: (a) the<br />

distribution <strong>of</strong> salts within the plant cells may result in turgor reduction and growth retardations. Also,<br />

salinity affects root and stomatal resistance to water flow, (b) the balance between root and shoot<br />

hormones changes considerably under saline conditions, (c) salinity changes the structure <strong>of</strong> the<br />

chloroplasts and mitochondria and such changes may interfere with normal metabolism and growth, (d)<br />

salinity increases respiration and reduces photosynthesis products available for growth.<br />

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Effect <strong>of</strong> micronutrients<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Basil plants sprayed with zinc and/or iron under normal and saline soils conditions were superior if<br />

compared without sprayed plants (tables, 2-5). Results also indicated that treated plants with iron were<br />

much superior in plant height and number <strong>of</strong> branches compared with other treatments. However,<br />

plants treated by zinc were produced fresh and dry weights <strong>of</strong> herb (g/plant or ton/fed.) greater than<br />

those other treatments. While, plants treated with mixture <strong>of</strong> zinc and iron gave the heaviest dry weight<br />

in the first cut, but treated plants with zinc or iron were produced dry weights <strong>of</strong> herb greater than those<br />

<strong>of</strong> other treatments in the second cut during first and second seasons, respectively. The stimulatory<br />

effect <strong>of</strong> zinc and/or iron were recorded by (Aziz and El- Sherbeny, 2004; Pande et al., 2007; Said-Al<br />

Ahl, 2005; Said-Al Ahl and Omer, 2009).<br />

The stimulation effects <strong>of</strong> applying zinc and iron on vegetative growth may be attributed to the well<br />

known functions <strong>of</strong> zinc and iron in plant life, as described in the Introduction. Moreover, zinc is a<br />

component <strong>of</strong> carbonic anhydrase, as well as several dehydrogenases and auxin production which in<br />

turn enhanced the elongation processes, besides the function <strong>of</strong> zinc in CO2 assimilation. Consequently,<br />

the fresh and dry weights <strong>of</strong> herb could be increased (Marschner, 1995). However, iron deficiency<br />

inhibited leaf growth, cell number, size and cell division, as well as chlorophyll, protein, starch and<br />

sugar content. Thus, the fresh and dry weights <strong>of</strong> herb could be decreased. Iron is necessary for the<br />

biosynthesis <strong>of</strong> chlorophyll and cytochrome, besides the function <strong>of</strong> iron in the metabolism <strong>of</strong><br />

chloroplast RNA, leading to increase in the biosyntheses materials (produced and accumulated),<br />

consequently, the growth was enhanced (Marschner, 1995).<br />

Effect <strong>of</strong> interaction<br />

The interaction between normal soil and saline soil conditions with zinc and/or iron application<br />

resulted in a significant increment <strong>of</strong> plant height and number <strong>of</strong> branches in the two cuts for both<br />

seasons (Tables, 2-5). Fresh weight <strong>of</strong> herb (g/plant or ton/fed.) was significantly increased in the<br />

second cut and non significant in the first cut in both seasons, but dry weight <strong>of</strong> herb (g/plant or<br />

ton/fed.) increased significantly in both cuts, except, this increment was insignificant in the second cut<br />

at first season. The maximum plant height and number <strong>of</strong> branches mean values were recorded from<br />

the combination <strong>of</strong> iron spraying and non soil salinity in all cuttings <strong>of</strong> both seasons. The highest fresh<br />

and dry weights <strong>of</strong> herb (g/plant or ton/fed.) resulted from zinc spraying and non soil salinity, or<br />

mixture (zinc and iron) spraying and non soil salinity, respectively in all cuttings <strong>of</strong> both seasons.<br />

While, the minimum growth characters values were resulted from the soil salinity condition without<br />

any treatment.<br />

B. Essential oil production<br />

Effect <strong>of</strong> soil salinity<br />

Tables (4, 5) explain that soil salinity conditions significant increased essential oil %. The increase in<br />

essential oil % due to salinity conditions was found by (Al-Amier and Craker, 2007; Baghalian et al.,<br />

2008; Baher et al., 2002; Hendawy and Khalid, 2005; Prasad et al., 2006; Tabatabale and Zari, 2007).<br />

In contrast, essential oil yield was significant decreased at the first and second cuts <strong>of</strong> both seasons.<br />

The results were similar in both the two seasons. Similar results were found by (Abd El-Wahab, 2006;<br />

Baghalian et al., 2008; Ozturk et al., 2004; Razmjoo et al., 2008). The reduction <strong>of</strong> essential oil yield<br />

by salinity due to a decrease in growth characters.<br />

The stimulation <strong>of</strong> essential oil production under salinity could be due to a higher oil gland density and<br />

an increase in the absolute number <strong>of</strong> glands produced prior to leaf emergence (Charles et al., 1990).<br />

Salt stress may also affect the essential oil accumulation indirectly through its effects on either net<br />

assimilation or the partitioning <strong>of</strong> assimilate among growth and differentiation processes (Charles et<br />

al., 1990).<br />

Penka (1978) showed that the formation and accumulation <strong>of</strong> essential oil in plants was explained as<br />

due to the action <strong>of</strong> environmental factors. It might be claimed that the formation and accumulation <strong>of</strong><br />

essential oil was directly dependent on perfect growth and development <strong>of</strong> the plants producing oils.<br />

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The decrease in oil production might be due to the decrease in plant anabolism. Morales et al. (1993)<br />

suggested that, an increase in oil content in some <strong>of</strong> the salt stressed plants might be attributed to<br />

decline the primary metabolites due to the effects <strong>of</strong> salinity, causing intermediary products to become<br />

available for secondary metabolites synthesis.<br />

Effect <strong>of</strong> micronutrients<br />

Data in Tables (4, 5) indicate that the essential oil (% or yield) <strong>of</strong> basil sprayed with zinc + iron was<br />

higher than the other treatments, followed by plants treated with zinc, and then plants treated with iron,<br />

whereas plants untreated (control) was lower in this respect in the two cuts during the two seasons. The<br />

increase in essential oil due to zinc and /or iron was also found by (El-Sawi and Mohamed, 2002;<br />

Maurya, 1990; Pande et al., 2007; Said-Al Ahl, 2005; Said-Al Ahl and Omer 2009; Subrahmanyam et<br />

al., 1992). From previous studies, biosynthesis <strong>of</strong> secondary metabolites is not only controlled<br />

genetically but it also is affected strongly by environmental influences (Naghdi Badi et al., 2004). In<br />

line with the foregoing, environmental variables affect essential oil, Marschner (1995) found that iron<br />

has important functions in plant metabolism, such as activating catalase enzymes associated with<br />

superoxide dismutase, as well as in photorespiration and the glycolate pathway. Also, in iron-deficient<br />

plants, the activities <strong>of</strong> some enzymes are impaired and may <strong>of</strong>ten be responsible for gross changes in<br />

metabolic processes. Moreover, zinc is an essential micronutrient that acts either as a metal component<br />

<strong>of</strong> various enzymes or as a functional, structural, or regulatory c<strong>of</strong>actor associated with saccharide<br />

metabolism, photosynthesis, and protein synthesis (Marschner, 1995). Carbon dioxide and glucose are<br />

precursors <strong>of</strong> monoterpene biosynthesis. Saccarides are also a source <strong>of</strong> energy and reducing power for<br />

terpenoid synthesis. As zinc is involved in photosynthesis and saccaride metabolism, and as CO2 and<br />

glucose is the most likely sources <strong>of</strong> carbon utilized in terpene biosynthesis, the role <strong>of</strong> zinc in<br />

influencing essential oil accumulation seems particularly important (Srivastava et al., 1997).<br />

Effect <strong>of</strong> interaction<br />

From data in Tables (4, 5), it can be concluded that the interaction treatments between foliar spray with<br />

micronutrients (Zn, Fe and mixture <strong>of</strong> Zn + Fe) and soil salinity significantly increased essential oil %<br />

and essential oil yield in both cuts during two seasons, except essential oil % at first cut was increased<br />

insignificantly <strong>of</strong> both seasons if comparing with none and soil salinity conditions. The highest value <strong>of</strong><br />

essential oil % was obtained by spraying with zinc + iron under soil salinity conditions. Whereas,<br />

plants sprayed with zinc + iron under none soil salinity gave the highest value <strong>of</strong> essential oil yield in<br />

both cuts during two seasons.<br />

C. Chemical composition <strong>of</strong> essential oils<br />

Table (6) show the data belonging to qualitative and quantitative constituents <strong>of</strong> essential oils distilled<br />

from the basil herb before flowering stage collected from the first and second cuts during the season <strong>of</strong><br />

2007. The essential oil composition <strong>of</strong> 8 treatments, along with the quantitative data is listed in Table 6.<br />

Twenty-four compounds were identified. Comparison <strong>of</strong> the analytical data <strong>of</strong> the oils revealed marked<br />

differences in qualitative and quantitative composition. Considering the main components, <strong>of</strong> the all<br />

treatments were characterized by high contents <strong>of</strong> linalool (38.28-52.14%) and methylchavicol (20.34-<br />

27.67%), and moderate amounts <strong>of</strong> 1,8-cineol (6.04-9.22%), germacrene D (2.32-4.38%), and very<br />

variable amounts <strong>of</strong> cis-bisabolene (0.00-2.53%), geraniol (0.59-2.02%), nerol (0.89-1.78%), cadinol<br />

(0.00-1.75%) and 1,4 terpineol (0.66-1.70%), and a lower amounts <strong>of</strong> α-thujene, β-pinene, α-pinene,<br />

camphene, sabinene, myrcene, ocimene, limonene, selinene, nerolidole, cadinene, caryophyllene,<br />

eugenol, camphor and α-terpinene considered as traces.<br />

The results in table (6) show that iron treatment gave the highest content <strong>of</strong> (methylchavicol,<br />

germacrene D, α-pinene and α-thujene); zinc treatment gave the highest content <strong>of</strong> (1, 8-cineol, βpinene,<br />

camphor, nerolidole and camphene) as well as iron + zinc treatment gave the highest content <strong>of</strong><br />

(linalool, sabinene, nerol, eugenol, selinene and cadinole). However, control treatment gave the same<br />

result <strong>of</strong> (limonene, α-terpinene, 1,4 terpineol, caryophyllene, cis-bisabolene, cadinene and ocimene)<br />

under the soil salinity conditions.<br />

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According to major compounds it was obviously cleared that soil salinity treatment decreased both <strong>of</strong><br />

linalool and methylchavicol compared to that <strong>of</strong> control Also, linalool was decreased with spraying<br />

treatments comparing to that <strong>of</strong> control, while there was an increase in methylchavicol by using zinc<br />

and mixture <strong>of</strong> zinc + iron whereas iron treatment had the lowest in this regard comparing to that <strong>of</strong><br />

control in normal soil. However, under saline soil condition, the results indicate that linalool was<br />

increased with spraying treatments comparing to that <strong>of</strong> control and mixture <strong>of</strong> iron + zinc followed by<br />

zinc and then iron gave the highest content <strong>of</strong> linalool. Whereas, methyl chavicol was increased with<br />

spraying <strong>of</strong> iron and zinc, but decreased by iron + zinc comparing to that <strong>of</strong> control and iron followed<br />

by zinc and then control treatment gave the highest content <strong>of</strong> methylchavicol. The highest content <strong>of</strong><br />

linalool was obtained by using zinc + iron under saline soil compared to the other interaction ones and<br />

the lowest value in this respect obtained in normal soil from the same treatment. However, zinc<br />

treatment gave the highest content <strong>of</strong> methylchavicol in normal soil but, under soil salinity, zinc+iron<br />

treatment gave the lowest value in this respect in all cases.<br />

The present study was in accordance by EL-Keltawi and Croteau (1987) on spearmint and marjoram<br />

who indicated that irrigation <strong>of</strong> both plants with saline solution consisting <strong>of</strong> calcium chloride and<br />

sodium chloride reduced essential oil. They added that under salinity in spearmint the content <strong>of</strong><br />

limonene was increased and carvone was concomitantly decreased relative to controls irrigated with<br />

water only. In case <strong>of</strong> marjoram, salt stress led to increase the content <strong>of</strong> sabinene which was<br />

accompanied by a decrease in the content <strong>of</strong> sabinene hydrate. Hendawy and Khalid (2005) on salvia<br />

<strong>of</strong>ficinalis reprted that treatment <strong>of</strong> 2500 ppm soil salinity increased α–thujone, camphor and 1,8-<br />

cineol but it decreased the component <strong>of</strong> β–thujone compared with the control treatment.<br />

Said-Al Ahl and Omer (2009) indicated that linalool was increased in the herb and seeds <strong>of</strong> coriander,<br />

but dodecenal <strong>of</strong> herb was decreased with treatment <strong>of</strong> zinc and mixture <strong>of</strong> zinc + iron compared to<br />

control. Also, Said-Al Ahl et al. (2010) indicated that soil salinity treatments at 1500 and 4500 ppm<br />

levels increased the content <strong>of</strong> linalool and on the contrary there was decreased in eugenol content by<br />

using 1500 and 4500 ppm <strong>of</strong> soil salinity in the Ocimum basilicum var. purpurascens.<br />

The essential oil <strong>of</strong> basil in this study belonging to linalool and methylchavicol chemotype,<br />

characterized by the simultaneous presence <strong>of</strong> linalool and methylchavicol, can be ascribed to those<br />

plants in which essential oil constituents are produced by two different biosynthetic pathways. In fact,<br />

methylchavicol has a common biosynthesis originating from the precursor (L-phenylalanine and<br />

cinnamic acid), whereas linalool follows another biogenetic pathway from mevalonic acid via geranyl<br />

pyrophosphate (Nikanen, 1989). It is known that climatic conditions and water available in the soil can<br />

change the vegetal secondary metabolism and, consequently ,alter the composition <strong>of</strong> essential oils,<br />

throughout the seasons <strong>of</strong> the year. Chemical variations in essential oils were associated with seasons<br />

for Ocimum selloi (Moraes et al., 2002) and with time <strong>of</strong> day for Ocimum gratissimum (Vasconcelos<br />

Silva et al., 1999(.<br />

.<br />

Table 1. The physical and chemical properties <strong>of</strong> the experimental soil.<br />

Physical and chemical properties Normal soil Saline soil<br />

Sand (%) 46.8 49.6<br />

Silt (%) 28.2 26<br />

Clay (%) 25.0 24.4<br />

Soil texture Sandy loam Sandy loam<br />

pH 8.12 8.45<br />

E.C (m. mohs/cm) 0.73 4.95<br />

Organic matter (%) 0.95 0.40<br />

N (mg kg -1 ) 0.09 0.05<br />

P (mg kg -1 ) 20.0 0.45<br />

K (mg kg -1 ) 208.0 2.04<br />

Zn (ppm) 1.2 0.65<br />

Iron (ppm) 20.0 1.32<br />

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Table 2. Effect <strong>of</strong> soil salinity, foliar spray with micronutruients and their interactions on plant height, branches number and herb fresh weight <strong>of</strong> Ocimum<br />

basilicumL. plants at first cut in 2006 and 2007 seasons.<br />

Treatments<br />

Plant height (cm) Branches number plant -1 Fresh weight g plant -1<br />

Season 1 Season 2 Season 1 Season 2 Season 1 Season 2<br />

S1 55.43 a ± 7.831 55.61 a ± 7.972 11.91 a ± 2.188 11.24 a ± 1.898 110.44 a ± 9.481 110.24 a ± 10.077<br />

S2 36.27 b ± 3.939 37.11 b ± 5.451 7.18 b ± 1.395 7.68 b ± 1.589 54.43 b ± 6.849 53.25 b ± 5.940<br />

LSD at � 0.05 5.1220 0.6758 2.2470 1.0230 6.0970 7.8010<br />

F0 38.24 d ± 6.538 37.45 d ± 7.113 7.68 c ± 2.891 7.23 c ± 2.285 71.25 b ± 28.708 69.83 b ± 28.388<br />

F1 52.69 a ± 12.539 53.69 a ± 10.499 11.10 a ± 3.705 11.17 a ± 2.792 85.27 a ± 29.959 84.00 a ± 30.361<br />

F2 44.15 c ± 11.738 44.04 c ± 11.247 9.29 b ± 1.385 9.46 b ± 0.499 88.43 a ± 33.338 87.52 a ± 33.179<br />

F3 48.32 b ± 11.649 50.25 b ± 12.007 10.10 ab ± 3.188 9.99 b ± 2.357 84.80 a ± 31.976 85.63 a ± 33.696<br />

LSD at � 0.05 1.8820 2.0190 1.0550 0.5440 6.9310 4.5900<br />

S1xF0 44.07 d ± 2.001 43.87 c ± 0.998 10.15 c ± 1.550 9.29 cd ± 0.543 97.17 ± 4.908 95.50 ± 5.500<br />

S1xF1 64.09 a ± 0.460 63.17 a ± 1.607 14.40 a ± 1.058 13.70 a ± 0.265 112.33 ± 4.646 111.50 ± 5.074<br />

S1xP2 54.73 c ± 2.194 54.22 b ± 1.338 10.18 c ± 1.154 9.89 c ± 0.271 118.60 ± 5.769 117.63 ± 5.119<br />

S1xF3 58.83 b ± 2.021 61.17 a ± 1.607 12.90 b ± 1.258 12.07 b ± 0.902 113.67 ± 5.508 116.33 ± 3.215<br />

S2x F0 32.42 g ± 1.040 31.03 e ± 1.380 5.20 e ± 0.346 5.17 f ± 0.153 45.33 ± 4.619 44.17 ± 2.843<br />

S2xF1 41.29 e ± 1.728 44.20 c ± 1.814 7.80 d ± 0.721 8.63 de ± 0.404 58.20 ± 4.952 56.50 ± 3.148<br />

S2xF2 33.56 g ± 1.822 33.87 e ± 1.963 8.40 d ± 1.039 9.04 d ± 0.063 58.27 ± 3.900 57.41 ± 2.342<br />

S2 xF3 37.80 f ± 1.836 39.33 d ± 0.577 7.30 d ± 0.520 7.90 e ± 0.173 55.93 ± 5.100 54.93 ± 0.902<br />

LSD at � 0.05 2.6620 2.8550 1.4920 0.7693 N.S N.S<br />

Means with different letters within each column are significant at 0.05 level and means in the same column with the same letters are not significant. Mean<br />

±Sd (standard deviation)<br />

Since: S = Soil salinity, i. e. S1 = 0.73 dsm -1 , S2 =4.95 dsm -1 ; F = Foliar spray with micronutrients, i. e. F0 = control, F1 = iron 250ppm, F2 = zinc 250ppm,<br />

F3= mixture <strong>of</strong> iron + zinc<br />

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Table 3. Effect <strong>of</strong> soil salinity, foliar spray with micronutruients and their interactions on plant height, branches number and herb fresh weight <strong>of</strong> Ocimum<br />

basilicum L. plants in at second cut in 2006 2007 seasons.<br />

Treatments<br />

Plant height (cm) Branches number plant -1 Fresh weight g plant -1<br />

Season 1 Season 2 Season 1 Season 2 Season 1 Season 2<br />

S1 70.53 a ± 7.733 69.46 a ± 7.137 15.41 a ± 1.874 14.79 a ± 2.192 138.78 a ± 15.292 133.63 a ± 12.583<br />

S2 51.08 b ± 5.595 51.75 b ± 5.683 11.03 b ± 2.116 11.17 b ± 2.248 67.75 b ± 9.697 71.65 b ± 11.697<br />

LSD at � 0.05 3.3340 1.9350 1.3940 2.2600 5.3080 2.7990<br />

F0 53.17 c ± 7.047 51.70 d ± 7.200 10.63 c ± 2.815 10.38 b ± 2.681 84.81 c ± 35.643 84.58 d ± 32.444<br />

F1 69.32 a ± 10.901 68.02 a ± 8.634 14.44 a ± 3.247 14.18 a ± 2.717 106.50 b ± 35.681 107.30 b ± 30.040<br />

F2 59.01 b ± 12.088 60.36 c ± 10.843 13.95 ab ± 0.580 13.48 a ± 0.949 116.50 a ± 45.873 114.67 a ± 34.373<br />

F3 61.70 b ± 13.336 62.35 b ± 12.282 13.84 b ± 3.299 13.88 a ± 3.279 105.25 b ± 38.621 104.00 c ± 39.100<br />

LSD at � 0.05 2.9820 1.2510 0.5352 0.9621 1.9870 2.6340<br />

S1xF0 59.47 c ± 1.295 58.23 e ± 0.979 13.20 c ± 0.200 12.70 bc ± 1.082 117.29 c ± 2.350 114.17 d ± 1.443<br />

S1xF1 79.01 a ± 2.968 75.87 a ± 0.594 17.39 a ± 0.344 16.50 a ± 1.323 139.00 b ± 1.000 134.67 c ± 2.517<br />

S1xP2 69.89 b ± 1.723 70.22 c ± 1.235 14.23 b ± 0.521 13.09 bc ± 1.299 158.33 a ± 2.887 146.00 a ± 2.000<br />

S1xF3 73.73 b ± 2.802 73.53 b ± 0.924 16.81 a ± 0.812 16.87 a ± 0.231 140.50 b ± 0.500 139.67 b ± 2.082<br />

S2x F0 46.87 d ± 1.848 45.17 g ± 0.764 8.07 e ± 0.115 8.05 e ± 0.777 52.33 f ± 2.517 55.00 g ± 2.000<br />

S2xF1 59.63 c ± 2.570 60.17 d ± 1.041 11.50 d ± 0.500 11.87 cd ± 0.777 74.00 d ± 3.606 79.93 e ± 1.675<br />

S2xF2 48.13 d ± 2.721 50.50 f ± 0.866 13.67 bc ± 0.577 13.87 b ± 0.325 74.67 d ± 1.528 83.33 e ± 2.082<br />

S2 xF3 49.67 d ± 1.528 51.17 f ± 1.041 10.87 d ± 0.231 10.90 d ± 0.361 70.00 e ± 1.000 68.33 f ± 1.155<br />

LSD at � 0.05 4.2170 1.7690 0.7569 1.3610 2.8090 3.7260<br />

Means with different letters within each column are significant at 0.05 level and means in the same column with the same letters are not significant. Mean ±Sd<br />

(standard deviation)<br />

Since: S = Soil salinity, i. e. S1 = 0.73 dsm -1 , S2 =4.95 dsm -1 ; F = Foliar spray with micronutrients, i. e. F0 = control, F1 = iron 250ppm, F2 = zinc 250ppm,<br />

F3= mixture <strong>of</strong> iron + zinc<br />

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Table 4. Effect <strong>of</strong> soil salinity, foliar spray with micronutruients and their interactions on plant height, branches number and herb fresh weight <strong>of</strong> Ocimum<br />

basilicum L. plants at first cut in 2006 and 2007 seasons.<br />

Treatments<br />

Dry weight g plant -1 Essential oil % Essential oil yield plant -1<br />

Season 1 Season 2 Season 1 Season 2 Season 1 Season 2<br />

S1 30.16 a ± 5.739 26.49 a ± 3.998 0.70 b ± 0.089 0.69 b ± 0.083 0.21 a ± 0.064 0.19 a ± 0.046<br />

S2 14.71 b ± 2.475 15.02 b ± 2.636 0.76 a ± 0.088 0.76 a ± 0.096 0.11 b ± 0.028 0.12 b ± 0.032<br />

LSD at � 0.05 2.0730 1.1370 0.0095 0.0123 0.0145 0.0034<br />

F0 16.63 d ± 6.445 16.30 c ± 6.123 0.60 d ± 0.043 0.59 c ± 0.033 0.10 d ± 0.033 0.10 d ± 0.033<br />

F1 22.02 c ± 6.580 19.90 b ± 4.769 0.72 c ± 0.039 0.74 b ± 0.037 0.16 c ± 0.042 0.15 c ± 0.034<br />

F2 24.67 b ± 9.694 22.85 a ± 6.791 0.76 b ± 0.048 0.75 b ± 0.064 0.18 b ± 0.062 0.17 b ± 0.039<br />

F3 26.42 a ± 11.314 23.97 a ± 7.731 0.83 a ± 0.037 0.82 a ± 0.041 0.21 a ± 0.085 0.19 a ± 0.054<br />

LSD at � 0.05 1.1730 1.2150 0.0325 0.0398 0.0080 0.0174<br />

S1xF0 22.47 d ± 0.896 21.83 d ± 1.258 0.57 ± 0.025 0.57 ± 0.027 0.13 de ± 0.003 0.12 de ± 0.013<br />

S1xF1 27.97 c ± 1.002 24.17 c ± 1.443 0.70 ± 0.040 0.72 ± 0.031 0.20 c ± 0.005 0.18 c ± 0.018<br />

S1xP2 33.50 b ± 0.500 28.97 b ± 1.704 0.72 ± 0.006 0.70 ± 0.000 0.24 b ± 0.006 0.20 b ± 0.012<br />

S1xF3 36.70 a ± 1.468 31.00 a ± 1.000 0.80 ± 0.021 0.78 ± 0.017 0.29 a ± 0.014 0.24 a ± 0.009<br />

S2x F0 10.80 f ± 0.985 10.77 f ± 0.580 0.63 ± 0.025 0.62 ± 0.021 0.07 f ± 0.007 0.07 f ± 0.004<br />

S2xF1 16.07 e ± 1.007 15.63 e ± 0.404 0.75 ± 0.025 0.75 ± 0.044 0.12 e ± 0.006 0.12 e ± 0.004<br />

S2xF2 15.83 e ± 0.764 16.73 e ± 0.404 0.80 ± 0.006 0.81 ± 0.042 0.13 de ± 0.006 0.13 de ± 0.010<br />

S2 xF3 16.13 e ± 0.709 16.93 e ± 0.058 0.85 ± 0.025 0.85 ± 0.017 0.14 d ± 0.002 0.14 d ± 0.004<br />

LSD at � 0.05 1.6580 1.7180 1.4920 0.7693 N.S N.S<br />

Means with different letters within each column are significant at 0.05 level and means in the same column with the same letters are not significant. Mean ±Sd<br />

(standard deviation)<br />

Since: S = Soil salinity, i. e. S1 = 0.73 dsm -1 , S2 =4.95 dsm -1 ; F = Foliar spray with micronutrients, i. e. F0 = control, F1 = iron 250ppm, F2 = zinc 250ppm,<br />

F3= mixture <strong>of</strong> iron + zinc<br />

105


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 5. Effect <strong>of</strong> soil salinity, foliar spray with micronutruients and their interactions on herb dry weight, essential oil % and essential oil yield <strong>of</strong> Ocimum<br />

basilicum L. plants at second cut in 2006 and 2007 seasons.<br />

Treatments<br />

Dry weight g plant -1 Essential oil % Essential oil yield plant -1<br />

Season 1 Season 2 Season 1 Season 2 Season 1 Season 2<br />

S1 40.49 a ± 3.288 39.68 a ± 3.623 0.66 b ± 0.083 0.66 b ± 0.075 0.27 a ± 0.051 0.26 a ± 0.050<br />

S2 21.40 b ± 2.424 21.39 b ± 2.220 0.73 a ± 0.083 0.73 a ± 0.080 0.16 b ± 0.030 0.16 b ± 0.030<br />

LSD at � 0.05 1.6190 3.1310 0.0393 0.0156 0.0231 0.0271<br />

F0 26.75 b ± 9.464 25.94 b ± 8.688 0.58 c ± 0.044 0.58 c ± 0.041 0.15 c ± 0.048 0.15 c ± 0.041<br />

F1 32.58 a ± 10.394 32.23 a ± 10.213 0.71 b ± 0.026 0.70 b ± 0.025 0.23 b ± 0.069 0.22 b ± 0.068<br />

F2 32.67 a ± 10.671 32.08 a ± 10.420 0.72 b ± 0.069 0.72 b ± 0.082 0.23 ab ± 0.055 0.22 b ± 0.050<br />

F3 31.78 a ± 11.570 31.87 a ± 10.905 0.78 a ± 0.038 0.77 a ± 0.039 0.25 a ± 0.080 0.24 a ± 0.073<br />

LSD at � 0.05 1.7420 0.8172 0.0303 0.0281 0.0164 0.0113<br />

S1xF0 35.33 ± 1.528 33.83 b ± 0.764 0.55 g ± 0.045 0.55 e ± 0.027 0.19 c ± 0.021 0.19 d ± 0.006<br />

S1xF1 42.00 ± 1.000 41.50 a ± 1.500 0.69 de ± 0.030 0.69 c ± 0.023 0.29 b ± 0.018 0.29 b ± 0.019<br />

S1xP2 42.33 ± 0.577 41.57 a ± 0.751 0.66 e ± 0.010 0.65 d ± 0.021 0.28 b ± 0.008 0.27 c ± 0.011<br />

S1xF3 42.30 ± 1.572 41.80 a ± 0.700 0.75 bc ± 0.031 0.74 b ± 0.017 0.32 a ± 0.016 0.31 a ± 0.012<br />

S2x F0 18.17 ± 0.764 18.04 d ± 1.066 0.61 f ± 0.006 0.62 d ± 0.015 0.11 e ± 0.005 0.11 f ± 0.007<br />

S2xF1 23.17 ± 1.756 22.97 c ± 0.950 0.72 cd ± 0.010 0.71 bc ± 0.023 0.17 d ± 0.012 0.16 e ± 0.009<br />

S2xF2 23.00 ± 2.000 22.60 c ± 1.039 0.78 ab ± 0.015 0.79 a ± 0.012 0.18 cd ± 0.015 0.18 de ± 0.010<br />

S2 xF3 21.27 ± 0.643 21.93 c ± 0.902 0.81 a ± 0.006 0.81 a ± 0.012 0.17 cd ± 0.004 0.18 de ± 0.010<br />

LSD at � 0.05 N.S 1.1560 0.0428 0.0398 0.0232 0.0159<br />

Means with different letters within each column are significant at 0.05 level and means in the same column with the same letters are not significant. Mean ±Sd<br />

(standard deviation)<br />

Since: S = Soil salinity, i. e. S1 = 0.73 dsm -1 , S2 = 4.95 dsm -1 ; F = Foliar spray with micronutrients, i. e. F0 = control, F1 = iron 250ppm, F2 = zinc 250ppm,<br />

F3= mixture <strong>of</strong> iron + zinc<br />

106


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 6. Effect <strong>of</strong> soil salinity and foliar spray with micronutruients on essential oil constituents <strong>of</strong> Ocimum basilicum L. plants<br />

in 2007 seasons.<br />

Soil salinity<br />

Compounds Saline soil (4.95 dsm )<br />

-1<br />

Normal soil (0.73 dsm )<br />

-1<br />

F0<br />

F1<br />

F2<br />

F3<br />

F0<br />

F1<br />

F2<br />

α–thujene--<br />

--<br />

--<br />

--<br />

--<br />

0.02<br />

0.01<br />

α-pinene<br />

0.42<br />

0.19<br />

0.32<br />

0.40<br />

0.29<br />

0.40<br />

0.01<br />

camphene--<br />

--<br />

--<br />

--<br />

--<br />

0.02<br />

0.46<br />

sabinene--<br />

--<br />

0.08<br />

0.07<br />

--<br />

0.01<br />

0.35<br />

β-pinene<br />

0.86<br />

0.94<br />

0.93<br />

1.21<br />

0.75<br />

1.18<br />

1.69<br />

myrcene--<br />

--<br />

--<br />

--<br />

0.45<br />

0.84<br />

1.33<br />

limonene<br />

0.37<br />

0.70<br />

0.76<br />

0.97<br />

0.64<br />

0.10<br />

0.11<br />

1 ,8-cineol 7.79<br />

9.40<br />

6.36<br />

7.99<br />

6.63<br />

8.39<br />

9.22<br />

α - terpinene 1.03<br />

0.93<br />

0.91<br />

0.93<br />

0.35<br />

0.10<br />

0.32<br />

ocimene--<br />

0.42<br />

0.36<br />

0.36<br />

0.48<br />

0.12<br />

0.41<br />

Linalool<br />

39.85<br />

32.42<br />

27.68<br />

25.68<br />

38.28<br />

46.54<br />

49.33<br />

camphor--<br />

--<br />

0.27<br />

0.06<br />

0.02<br />

0.22<br />

0.29<br />

1,4-terpineol 1.05<br />

1.34<br />

0.78<br />

0.73<br />

1.70<br />

0.66<br />

0.89<br />

methylchavicol 35.64<br />

30.84<br />

44.01<br />

38.52<br />

21.48<br />

27.67<br />

23.66<br />

nerol<br />

1.00<br />

1.89<br />

1.29<br />

1.11<br />

0.89<br />

1.22<br />

1.09<br />

geroniol<br />

0.75<br />

1.23<br />

1.13<br />

1.18<br />

2.02<br />

0.85<br />

0.59<br />

eugenol--<br />

--<br />

--<br />

--<br />

--<br />

--<br />

--<br />

caryophyllene-- 0.44<br />

0.24<br />

0.37<br />

0.18<br />

0.12<br />

0.01<br />

germacrene D 2.19<br />

3.89<br />

1.80<br />

2.88<br />

2.32<br />

4.38<br />

4.08<br />

cadinene--<br />

0.09<br />

--<br />

0.10<br />

0.11<br />

--<br />

--<br />

cis-bisabolene 1.71<br />

1.98<br />

1.74<br />

2.04<br />

2.53<br />

--<br />

--<br />

nerolidole<br />

0.08<br />

0.41<br />

0.60<br />

0.25<br />

0.44<br />

0.43<br />

0.45<br />

selinene<br />

0.42<br />

0.60<br />

0.05<br />

0.86<br />

0.01<br />

0.09<br />

0.74<br />

t-cadinol<br />

3.25<br />

3.91<br />

4.02<br />

4.76<br />

--<br />

1.38<br />

1.61<br />

Identified<br />

compounds<br />

96.31<br />

91.62<br />

93.33<br />

90.47<br />

91.42<br />

99.26<br />

93.13<br />

F = Foliar spray with micronutrients, i. e. F0 = control, F1 = iron 250ppm, F2 = zinc 250ppm, F3 = mixture <strong>of</strong> iron + zinc<br />

107<br />

F3<br />

--<br />

--<br />

--<br />

0.47<br />

0.30<br />

0.05<br />

0.01<br />

6.04<br />

0.31<br />

0.40<br />

52.14<br />

0.14<br />

0.78<br />

20.34<br />

1.78<br />

1.07<br />

0.42<br />

--<br />

3.63<br />

--<br />

--<br />

0.30<br />

0.91<br />

1.75<br />

91.35


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

CONCLUSIONS<br />

It may be concluded that Ocimum basilicum (linalool and methylchavicol chemo type) is tolerant to<br />

soil salinity, thus we may recommend its cultivation in slain soil <strong>of</strong> Egypt. Foliar spraying with iron<br />

and /or zinc under these conditions could be much more efficient than not application <strong>of</strong> nutrients. So,<br />

we recommended that, foliar application <strong>of</strong> iron and /or zinc to raise the salt stress tolerance <strong>of</strong> sweet<br />

basil (Ocimum basilicum L.).<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

Growth and yield <strong>of</strong> Foeniculum vulgare var.azoricum as influenced by some<br />

vitamins and amino acids<br />

S.F. Hendawy and Azza A.Ezz El-Din*<br />

Cultivation and Production <strong>of</strong> Medicinal and Aromatic Plants Dept.<br />

National Research Centre, Dokki, Cairo -12622, Egypt<br />

E-mail address for correspondence :azzaamin2001@hotmail.com<br />

___________________________________________________________________________________<br />

Abstract :This investigation was carried out in Saft El-Laban farm, Giza during two successive<br />

seasons <strong>of</strong> 2006/2007 and 2007/2008 to study the effect <strong>of</strong> foliar application <strong>of</strong> ascorbic acid and<br />

thiamine in a rate <strong>of</strong> 0, 25 , 50 and 75 mgL -1 . for each as well as amino acids i.e aspartic and phenyl<br />

alanin in a rate <strong>of</strong> 0, 100, 200 and 300 ppm for each on growth, yield and chemical composition <strong>of</strong><br />

fennel plants. The obtained results could be summarized as follows: ascorbic acid at 75 mgL -1 .<br />

recorded the best value <strong>of</strong> plant height, number <strong>of</strong> branches, number <strong>of</strong> flower heads and seed weight<br />

per plant. No significant difference was shown between aspartic acid and ascorbic acid. Phenyl alanin<br />

at 300 ppm resulted the highest essential oil percent (2.78%) compared with control (2.00%).<br />

Key words: Foeniculum vulgare, ascorbic acid, aspartic, phenylalanine, thiamine, essential oil<br />

__________________________________________________________________________________<br />

INTRODUCTION<br />

Foeniculum vulgare (Fennel) belonging to the family Apiaceae is a perennial herb native to the<br />

Mediterranean Region. It is widely cultivated and extensively used as a culinary spice. The plant is<br />

aromatic and is used as a pot herb. The leaves have diuretic properties and the roots are regarded as<br />

purgatives. Dried fruits <strong>of</strong> fennel posses a pleasant aromatic taste and used for flavouring soups, meat<br />

dishes and sauces. The fruits are considered to be usefull in treatment <strong>of</strong> diseases <strong>of</strong> the chest, spleen<br />

and kidney (Singh and Kale 2008).<br />

The anti-inflammatory, analgesic and antioxidant activities <strong>of</strong> the fruits <strong>of</strong> fennel have been reported by<br />

(Choi and Hwang 2004).<br />

The oil <strong>of</strong> fennel regulates the peristaltic functions <strong>of</strong> the gastrointestinal tract and relevies the spasms<br />

<strong>of</strong> intestines (Fathy et al 2002).<br />

Amino acids are fundamental ingredients in the process <strong>of</strong> protein synthesis. Glycine and Glutamic<br />

acids play an important role in formation <strong>of</strong> vegetative tissue and chlorophyll. They also have a<br />

chelating effect on micronutrients through making their absorption and transportation easier for the<br />

plant. They are precursors or activators <strong>of</strong> phytohormones and growth substances. L. Methionine is a<br />

precursor <strong>of</strong> ethylene and growth factors such as espermine and espermidine (Singh 1999).<br />

Gamal El-Din et al (1997) found that foliar application <strong>of</strong> ornithine and phenylalanine 50, 100 mgL -1 .<br />

on Cymbopgon citrates led to significantly increase in vegetative growth, number <strong>of</strong> leaves and tillers<br />

as well as fresh and dry weight <strong>of</strong> herb. El-Sherbeny and Hassan (1987) reported that phenylalanine<br />

or tryptophan at 200 or 250 mgL -1 significantly increased growth parameters and alkaloid content <strong>of</strong><br />

datura plants.<br />

Moursy et al (1988) indicated that phenylalanine or ornithine increased the fresh and dry weight <strong>of</strong><br />

callus explants <strong>of</strong> Datura stramonium L. Refaat and Naguib (1998) found that spraying peppermint<br />

plant with alpha-alanine at 25 and 50 ppm increased fresh and dry weight <strong>of</strong> the plant and essential oil<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

content. Harridy (1986) mentioned that the higher alkaloid percentage and yield <strong>of</strong> Catharanthus<br />

roseus resulted from foliar application <strong>of</strong> some amino acids. Similar trend was observed by Awad<br />

(1986), studying methionen on Hyoscyamus muticus. Talaat and Youssef (2002) found a pronounced<br />

increase in vegetative growth <strong>of</strong> basil plant as a result <strong>of</strong> lysine and ornithine treatments.<br />

Little information are available about the role <strong>of</strong> vitamins in regulating the biosynthesis <strong>of</strong> essential oil<br />

in plants. Robinson (1973) reported that vitamin B complex and vitamin C act as co-enzmes in the<br />

enzymatic reactions by which carbohydrates, fats and proteins are metabolized and involved in<br />

photosynthesis and respiration. Taraf et al (1999) reported that foliar application <strong>of</strong> nicotine amide to<br />

lemongrass plants significantly promoted vegetative growth as well as essential oil percent, oil yield<br />

per plant, total carbohydrates and crude proteins.<br />

Ascorbic acid (vitamin C) is known as a growth regulating factor which influences many biological<br />

processes. Price (1966) reported that ascorbic acid (vit.C) increases nucleic acid content, especially<br />

RNA. It also influenced the synthesis <strong>of</strong> enzymes, nucleic acids and protein, in addition it acts as coenzyme<br />

in metabolic changes. Abd El-Halim (1995) reported that foliar application <strong>of</strong> ascorbic acid on<br />

tomato plants significantly increased growth parameters (stem length, number <strong>of</strong> branches, leaves,<br />

flowers and fruit set as well as dry weight <strong>of</strong> shoot per plant) in comparison with control plants.<br />

Thiamine (Vitamin B1) is a necessary ingredient for biosynthesis <strong>of</strong> the coenzyme thiamine<br />

pyrophosphate, in this latter form it plays an important role in carbohydrate metabolism. It is an<br />

essential nutrient for both plant and animal. In plants, it is synthesized in the leaves and is transported<br />

to the roots where it controls growth. Thiamine is an important c<strong>of</strong>actor for the transketolation reaction<br />

<strong>of</strong> the pentose phosphate for nucleotide synthesis and for the reduced NADP required for various<br />

synthetic pathways. It acts as co-enzyme oxidative carboxylation <strong>of</strong> � -keto acids (e.g. � ketoglutarate,<br />

pyruvate, the � -keto analogs <strong>of</strong> the branched-chain amino acids: leucine isoleucine and<br />

valine) Kawasaki (1992). In this concern, Reda et al (1977) reported that thiamine treatment<br />

significantly increased the total yield <strong>of</strong> chromones as well as khellin and visnagin yield (mg plant -1 ) in<br />

the fruits <strong>of</strong> Ammi visnaga. Ascorbic acid seemed to retard the growth <strong>of</strong> Ammi Visnaga but the yield<br />

<strong>of</strong> different chromones in the fruits under the effect <strong>of</strong> ascorbic acid (50 and 100 mg/1) was about three<br />

folds that <strong>of</strong> the corresponding control.<br />

The aim <strong>of</strong> this study is to investigate the effect <strong>of</strong> some vitamins and amino acids on growth, yield and<br />

oil composition <strong>of</strong> fennel plants.<br />

Field experiments:<br />

MATERIALS AND METHODS<br />

Field experiments were carried out at Saft El-Laban farm, Giza, Egypt during two successive growing<br />

seasons (2007 and 2008) to study foliar application <strong>of</strong> some vitamins i.e ascorbic acid and thiamine and<br />

amino acids i.e aspartic and phenylalanine on growth, yield and chemical composition <strong>of</strong> fennel plants.<br />

Seeds <strong>of</strong> Foeniculum vulgare var. azoricum were obtained from Sekem Group Company, Egypt.<br />

The mechanical and chemical analysis <strong>of</strong> the soil were carried out according to the method <strong>of</strong><br />

Chapman and Pratt (1978), which were presented in Table (1).<br />

114


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table (1): Physical and chemical analysis <strong>of</strong> the experimental soil.<br />

Physical properties Chemical parameters<br />

Soil type loamy<br />

Course sand 4.9%<br />

Fine sand 30.7%<br />

Silt 27.5%<br />

Clay 27.5%<br />

Organic matter 2.1%<br />

115<br />

pH<br />

Available N<br />

Available P2O5<br />

Available K2O<br />

Fe<br />

Mn<br />

Zn<br />

Cu<br />

Na<br />

Mg<br />

7.8<br />

13.8 mg/100g<br />

0.482 mg/100g<br />

3.01 mg/100g<br />

1.1 ppm<br />

0.53 ppm<br />

21 ppm<br />

21 ppm<br />

29 ppm<br />

2.4 ppm<br />

Seeds were sown directly in soil on 12 th <strong>of</strong> October 2006, and on the 2 nd <strong>of</strong> October 2007. The<br />

experimental unit area was 4 m 2 and the treatments were arranged in completely randomized block<br />

design with three replicates for each treatment. Each plot contained 3 rows <strong>of</strong> 60 cm apart and the<br />

distance between plants was 30 cm. Calcium super phosphate (15.5% P2O5), at 100 kg/ feddan,<br />

ammonium sulphate (20.5%N) at 150 kg/ feddan and potassium sulphate (48% K2O) at 100kg/feddan<br />

were applied. Phosphorus fertilizer was added at the time <strong>of</strong> soil preparation while nitrogen fertilizer<br />

was added at two separated side dressings, the first one on 15 th. December and the second on 15 th.<br />

February in both seasons.<br />

The treatments were as follows:<br />

Treat. 1: Control (Sprayed with water)<br />

Treat.2: Sprayed with aspartic acid at 100 ppm.<br />

Treat.3: Sprayed with aspartic acid at 200 ppm.<br />

Treat.4: Sprayed with aspartic acid at 300 ppm.<br />

Treat.5: Sprayed with Phenyl alanin at 100 ppm.<br />

Treat.6: Sprayed with Phenyl alanin at 200 ppm..<br />

Treat.7: Sprayed with Phenyl alanin at 300 ppm.<br />

Treat.8: Sprayed with thiamine at 25 mg/L.<br />

Treat.9: Sprayed with thiamine at 50 mg/L.<br />

Treat.10:Sprayed with thiamine at 75 mg/L.<br />

Treat.11:Sprayed with ascorbic acid at 25 mg/L.<br />

Treat.12:Sprayed with ascorbic acid at 50 mg/L.<br />

Treat.13:Sprayed with ascorbic acid at 75 mg/L.<br />

The plants were sprayed with vitamins or amino acids twice, the first one on 15 th December and the<br />

second on 15 th February, early in the morning, while the control plants were sprayed with distilled<br />

water.<br />

Plant height (cm), plant fresh weight or (aerial parts)g plant -1 plant dry weight (aerial parts), g plant-1<br />

flowers head number, no <strong>of</strong> branches, no. <strong>of</strong> suckers and seed weight per plant were recorded through<br />

the two growth seasons. Essential oil percentage was determined in the fruits.


Chemical analysis:<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Samples <strong>of</strong> dried seeds were subjected to water distillation for determination <strong>of</strong> their essential oil<br />

content using clevenger's apparatus Marotti and Piccaglia (1992).<br />

Oil samples were subjected to Gas Chromatographic Analysis to identify their oil composition adopting<br />

the following condition:<br />

Apparatus: Thermo Quest Trace GC 2000 Series-Finnegan<br />

Standard material: Piano paraffines SUPELCO product.<br />

Column: 60m x 0.32 mm SPB TM -5<br />

Detector: FID; Operating mode Splitless; Base temp. 300 o C<br />

Mobile phase: Nitrogen 30ml/min<br />

Oven Program: Initial temp. 40 o C, rate <strong>of</strong> increase 3 o C/minute; Final temp. 240 o C; Hold time 10<br />

minutes.<br />

The results <strong>of</strong> all the parameters were statistically analysed adopted the method <strong>of</strong> (Snedecor and<br />

Cochran 1980).<br />

RESULTS AND DISCUSSION<br />

Table (2&3) showed the effect <strong>of</strong> foliar application <strong>of</strong> vitamins i.e, ascorbic acid (vitamin C) and<br />

thiamine (vitamin B1) as well as amino acids i.e, aspartic acid and phenylalanine on growth and yield<br />

<strong>of</strong> Foeniculum vulgare var. azoricum during 2007 and 2008. The data indicate that application <strong>of</strong><br />

aspartic acid increased plant height (cm) up to<br />

116


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table(2): Effect <strong>of</strong> foliar application <strong>of</strong> ascorbic acid and thiamine and amino acids, aspartic and phenylalanine on growth, yield and chemical composition<br />

Foeniculum vulgare var. azoricum plants; First season (2007).<br />

Treatments<br />

Plant height<br />

(cm)<br />

Aerial parts<br />

fresh weight<br />

g plant -1<br />

Aerial parts<br />

dry weight<br />

g plant -1<br />

117<br />

Number <strong>of</strong><br />

flower heads<br />

plant -1<br />

Number <strong>of</strong><br />

branches<br />

plant -1<br />

Number <strong>of</strong><br />

suckers plant -1<br />

Seed weight<br />

g plant -1<br />

Control 0ppm 128.0 650.0 98.48 30.0 8.0 2.0 38.0 2.00<br />

Aspartic<br />

Phenylalanine<br />

Thiamine<br />

Ascorbic acid<br />

100 ppm<br />

200 ppm<br />

300 ppm<br />

Mean<br />

L.S.D. (5%)<br />

100 ppm<br />

200 ppm<br />

300 ppm<br />

Mean<br />

L.S.D. (5%)<br />

25 mg L -1<br />

50 mg L -1<br />

75 mg L -1<br />

Mean<br />

L.S.D. (5%)<br />

25 mg L -1<br />

50 mg L -1<br />

75 mg L -1<br />

Mean<br />

L.S.D. (5%)<br />

158.0<br />

173.0<br />

178.0<br />

169.7<br />

5.12<br />

145.0<br />

155.0<br />

158.0<br />

152.7<br />

4.60<br />

167.0<br />

185.0<br />

184.0.<br />

178.7<br />

5.90<br />

170.0<br />

194.0<br />

185.0<br />

183.0<br />

6.33<br />

710.0<br />

745.0<br />

768.0<br />

741.0<br />

28.16<br />

705.0<br />

715.0<br />

734.0<br />

718.0<br />

24.16<br />

714.0<br />

735.0<br />

772.0<br />

740.3<br />

27.00<br />

766.0<br />

780.0<br />

790.0<br />

778.7<br />

23.51<br />

107.58<br />

112.88<br />

116.36<br />

112.3<br />

2.94<br />

110.16<br />

111.72<br />

114.69<br />

112.2<br />

N.S.<br />

105.00<br />

108.09<br />

113.53<br />

108.9<br />

3.10<br />

117.85<br />

120.00<br />

121.54<br />

119.8<br />

2.80<br />

L.S.D. (5%) for foliar appli. 6.12 21.60 2.34 2.18 0.90 0.36 2.85 0.074<br />

38.0<br />

42.0<br />

48.0<br />

42.7<br />

2.41<br />

35.0<br />

39.0<br />

42.0<br />

38.7<br />

2.38<br />

35.0<br />

42.0<br />

48.0<br />

41.7<br />

2.21<br />

38.0<br />

45.0<br />

50.0<br />

44.3<br />

2.26<br />

10.0<br />

12.0<br />

12.0<br />

11.3<br />

0.90<br />

12.0<br />

14.0<br />

15.0<br />

13.7<br />

1.10<br />

10.0<br />

12.0<br />

13.0<br />

11.7<br />

0.80<br />

11.0<br />

13.0<br />

15.5<br />

13.0<br />

1.11<br />

3.0<br />

3.0<br />

5.0<br />

3.7<br />

0.40<br />

3.0<br />

4.0<br />

4.0<br />

3.7<br />

N.S.<br />

4.0<br />

5.0<br />

5.0<br />

4.7<br />

0.35<br />

4.0<br />

6.0<br />

6.0<br />

5.3<br />

0.38<br />

45.0<br />

49.0<br />

52.0<br />

48.7<br />

2.34<br />

40.0<br />

45.0<br />

48.0<br />

44.3<br />

2.47<br />

48.0<br />

55.0<br />

58.0<br />

53.7<br />

2.35<br />

52.0<br />

58.0<br />

61.0<br />

57.0<br />

2.71<br />

Oil%<br />

2.20<br />

2.32<br />

2.45<br />

2.3<br />

0.090<br />

2.43<br />

2.51<br />

2.58<br />

2.5<br />

0.092<br />

2.44<br />

2.48<br />

2.53<br />

2.5<br />

0.075<br />

2.48<br />

2.55<br />

2.67<br />

2.6<br />

0.070


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table(3). Effect <strong>of</strong> foliar application <strong>of</strong> ascorbic acid and thiamine and amino acids, aspartic and phenylalanine on growth, yield and chemical composition<br />

Foeniculum vulgare var. azoricum plants; Second season (2008).<br />

Treatments<br />

Plant height<br />

(cm)<br />

Aerial parts<br />

fresh weight<br />

g plant -1<br />

Aerial parts<br />

dry weight<br />

g plant -1<br />

118<br />

Number <strong>of</strong><br />

flower heads<br />

plant -1<br />

Number <strong>of</strong><br />

branches<br />

plant -1<br />

Number <strong>of</strong><br />

suckers plant -1<br />

Seed weight<br />

g plant -1<br />

Control 0ppm 132.0 675.0 102.27 30.0 9.0 3.0 37.0 2.00<br />

Aspartic<br />

Phenylalanine<br />

Thiamin<br />

Ascorbic acid<br />

100 ppm<br />

200 ppm<br />

300 ppm<br />

Mean<br />

L.S.D. (5%)<br />

100 ppm<br />

200 ppm<br />

300 ppm<br />

Mean<br />

L.S.D. (5%)<br />

25 mg L -1<br />

50 mg L -1<br />

75 mg L -1<br />

Mean<br />

L.S.D. (5%)<br />

25 mg L -1<br />

50 mg L -1<br />

75 mg L -1<br />

Mean<br />

L.S.D. (5%)<br />

155.0<br />

170.0<br />

174.0<br />

166.3<br />

5.05<br />

148.0<br />

156.0<br />

160.0<br />

154.7<br />

4.63<br />

165.0<br />

182.0<br />

189.0<br />

178.7<br />

5.82<br />

170.0<br />

194.0<br />

185.0<br />

183.0<br />

6.12<br />

714.0<br />

733.0<br />

756.0<br />

734.3<br />

26.00<br />

724.0<br />

733.0<br />

754.0<br />

737.0<br />

21.32<br />

722.0<br />

730.0<br />

775.0<br />

742.3<br />

25.14<br />

755.0<br />

784.0<br />

788.0<br />

775.7<br />

23.51<br />

108.18<br />

111.06<br />

114.55<br />

111.3<br />

2.88<br />

113.13<br />

114.53<br />

117.81<br />

115.2<br />

2.56<br />

106.18<br />

107.35<br />

113.97<br />

109.2<br />

2.94<br />

116.15<br />

120.62<br />

121.23<br />

119.3<br />

2.14<br />

L.S.D. (5%) for foliar appli. 6.08 22.30 2.55 2.01 0.85 0.24 2.78 0.078<br />

36.0<br />

43.0<br />

48.0<br />

42.3<br />

2.11<br />

36.0<br />

41.0<br />

45.0<br />

40.7<br />

2.08<br />

37.0<br />

44.0<br />

49.0<br />

43.3<br />

2.03<br />

38.0<br />

48.0<br />

52.0<br />

46.0<br />

2.06<br />

10.0<br />

13.0<br />

14.0<br />

12.3<br />

0.75<br />

13.0<br />

14.0<br />

15.0<br />

14.0<br />

0.84<br />

13.0<br />

14.0<br />

14.0<br />

13.7<br />

0.70<br />

12.0<br />

15.0<br />

15.0<br />

14.0<br />

0.90<br />

3.0<br />

5.0<br />

5.0<br />

4.3<br />

N.S.<br />

4.0<br />

5.0<br />

6.0<br />

5.0<br />

N.S.<br />

4.0<br />

6.0<br />

6.0<br />

5.3<br />

0.25<br />

5.0<br />

6.0<br />

7.0<br />

6.0<br />

0.22<br />

43.0<br />

49.0<br />

53.0<br />

48.3<br />

2.28<br />

42.0<br />

47.0<br />

50.0<br />

46.3<br />

2.40<br />

48.0<br />

53.0<br />

57.0<br />

52.7<br />

2.25<br />

54.0<br />

60.0<br />

63.0<br />

59.0<br />

2.65<br />

Oil%<br />

2.20<br />

2.35<br />

2.40<br />

2.3<br />

0.095<br />

2.41<br />

2.48<br />

2.78<br />

2.5<br />

0.084<br />

2.48<br />

2.51<br />

2.58<br />

2.5<br />

0.086<br />

2.47<br />

2.53<br />

2.64<br />

2.5<br />

0.071


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

300 ppm, but this increment had no significant effect comparing with 200 ppm. The maximum value <strong>of</strong><br />

this character was obtained by applying ascorbic acid at the rate <strong>of</strong> 50 mgL -1 . This was true during both<br />

seasons except thiamine and ascorbic acid in the second one, whereas the three applied doses were<br />

significant up to 75 mgL -1 . Wahba et al 2002 reported that aspartic acid as foliar spray (25, 50 and 75<br />

ppm) increased the vegetative growth, flowering parameters and yield <strong>of</strong> courms <strong>of</strong> Anthoglyza<br />

aethiopica.<br />

Fresh and dry weight <strong>of</strong> aerial parts significantly increased by increasing all treatments up to 300 ppm<br />

for asp. and phenyl. and 75 mg for vit. B1 and vit. C during the 1 st . season. In the 2 nd . season, the higher<br />

dose applied from vitamins and amino acids, the maximum fresh and dry weight more obtained. The<br />

highest weights were recorded with spraying ascorbic acid at 75 mgL -1 . Gamal El-Din and Abd El-<br />

Wahed (2005) stated that all amino acids treatments (ornithine, proline and phenlyalanin) significantly<br />

increased plant height, number <strong>of</strong> branches, number <strong>of</strong> flower heads and fresh and dry weights <strong>of</strong> aerial<br />

part <strong>of</strong> chamomile plant.<br />

Applying ascorbic acid significantly increased number <strong>of</strong> flower heads in fennel plants up to the higher<br />

dose. The same effect was observed when spraying aspartic acid, phenylalanine and thiamine.<br />

Ascorbic acid is not only an important antioxidant, it also appears to link flowering time,<br />

developmental senescence, programmed cell death and responses to pathogens (Pastori et al 2003;<br />

Barth et al 2004 and Pavet et al 2005). Furthermore, it affects nutritional cycle's activity in higher<br />

plants and plays an important role in the electron transport system Liu et al (1997). El-Banna et al<br />

(2006) found stimulatory effects <strong>of</strong> vitamin C on potato. Golan-Goldhirsh et al (1995) indicated that<br />

soybean treated with ascorbic acid increased photosynthesis process. Talaat (2003) detected that<br />

ascorbic foliar application on sweet paper increased content <strong>of</strong> macro-nutrients (N, P and K).<br />

Increasing aspartic acid doses significantly increased seed weight g plant -1 up to 300 ppm. Spraying<br />

vitamin C at 75 mgL -1 . resulted in the maximum seed weight. Attoa et al (2002) found that aspartic<br />

acid at 75 ppm increased both the fixed oil and total glucosinolate contents <strong>of</strong> Iberis amara. The<br />

maximum oil % was achieved from 300 ppm <strong>of</strong> phenylalanine (2.78%) compared with control (2.00%).<br />

Table (4) showed the effect <strong>of</strong> foliar application <strong>of</strong> ascorbic acid and thiamine and amino acids,<br />

aspartic and phenylalanine on essential oil composition <strong>of</strong> Foeniculum vulgare var. azoricum. The<br />

analysis <strong>of</strong> essential oil <strong>of</strong> fennel showed the presence <strong>of</strong> 7 componds as main constituents. The major<br />

one was found to be anethol (trans-1- methoxy-4- (Prop-1- enly) benzene; C10H12O).<br />

It ranged from 61.55 to 77.31%, followed by fenchone with values <strong>of</strong> 6.14 to 13.62%. Estragol<br />

occupied the third place and recorded 4.21% to 9.54%. Braun and Franz (1999) found that anethole,<br />

estragole, fenchone and Limonene are the major constituents <strong>of</strong> fennel essential oil. They represent<br />

99% <strong>of</strong> herb oil and 93% <strong>of</strong> the fruits oil. Mahfouz and Sharaf El-Din (2007) reported that Anethole<br />

was the main component in F.vulgare oil. It reached the highest value with half dose <strong>of</strong> N, P and K<br />

(mineral fertilization 357 kg ammonium sulphate + 238 kg calcium super-phosphate +60 kg potassium<br />

sulphate ha -1 ) and inoculation with Basillus megatherium).<br />

119


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table(4). Effect <strong>of</strong> foliar application <strong>of</strong> ascorbic acid and thiamine and amino acids, aspartic and phenylalanine on oil composition <strong>of</strong> Foeniculum vulgare var. azoricum .<br />

Treatments � -pinene � -pinene Myrcene Limonene Fenchone Estragol Anethol Un-Known<br />

Total identified<br />

compounds<br />

Control 0 2.24 0.44 1.55 7.33 10.24 9.54 61.55 7.11 92.89<br />

Aspartic 100 ppm 1.15 traces 2.11 6.54 9.15 8.71 62.14 10.2 89.8<br />

200 ppm 1.36 0.16 0.06 6.65 9.13 8.82 64.21 9.61 90.39<br />

300 ppm 1.34 0.21 0.18 7.02 9.24 7.16 65.02 9.83 90.17<br />

Phenylalanine 100 ppm 1.44 0.33 0.16 9.14 10.38 6.23 62.34 9.98 90.02<br />

200 ppm 1.45 0.25 0.95 7.25 12.45 6.31 68.11 3.23 96.77<br />

300 ppm 1.48 0.24 0.38 7.93 12.36 6.01 68.42 3.76 96.24<br />

Thiamine 25 mg L -1<br />

50 mg L -1<br />

75 mg L -1<br />

1.01 0.29 0.36 6.54 10.14 6.42 64.32 9.53 90.47<br />

1.06 0.41 0.41 6.72 11.21 6.13 65.16 9.08 90.92<br />

1.18 0.45 0.45 6.72 10.25 6.02 66.17 8.76 91.24<br />

Ascorbic 25 mg L -1<br />

50 mg L -1<br />

75 mg L -1<br />

1.32 0.38 0.85 5.13 13.62 4.32 72.22 2.16 97.84<br />

1.35 0.36 0.93 5.14 6.14 4.21 77.31 4.56 95.44<br />

1.38 0.25 0.99 5.16 8.36 4.45 74.16 5.25 94.75<br />

120


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Khalil et al (2008) stated that the major components in fennel seed oil are anethole, more than 45%<br />

and limonene, more than 12%. Abd El-Wahab and Mehasen (2009) reported that anethole content<br />

recorded higher percentage in Indian fennel than local fennel in all sowing time (7, 15 and 21 Nov. )<br />

and sowing locations (El-Minia, Assuit, Sohag and Qena governorates) under upper Egypt conditions.<br />

CONCLUSION<br />

We recommended that among all applied treatments, ascorbic acid at 75 mg L -1 resulted in the best<br />

values <strong>of</strong> growth parameters, while phenylalanine at concentration <strong>of</strong> 300 ppm recorded the highest<br />

essential oil percent compared with control.<br />

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Braun, M., Franz, G., 1999. Quality criteria <strong>of</strong> bitter fennel oil in the German pharmacopoeia. Pharm.<br />

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Chapman, H.D., Pratt, R.F., 1978. Methods Analysis for Soil, Plant and Water. Univ. <strong>of</strong> California,<br />

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El-Banna, E.N., Ashour, S.A., Abd El-Salam, H.Z., 2006. Effect <strong>of</strong> foliar application with organic<br />

compounds on growth, yield and tuber quality <strong>of</strong> potato (Solanum tuberosum L.) J. Agric. Sci.<br />

Mansoura Univ., 31, 1165-1175.<br />

El-Sherbeny, S.Z., Hassan, A.E., 1987. Physiological studies on Datura stramonium L., the effect <strong>of</strong><br />

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Egypt, 12, 101-110.<br />

Fathy, M.S., Shehata, A.H, Kaleel, A.E, Ezzat, S.M., 2002. An acylated Kaempferol glycoside from<br />

flowers <strong>of</strong> Foeniculum vulgare and F.dulce. Molecules, 7, 245-251.<br />

Gamal El-Din, K.M., Abd El-Wahed, M.S.A., 2005. Effect <strong>of</strong> some amino scids on growth and<br />

essential oil content <strong>of</strong> chamomile plant. Inter. J. <strong>of</strong> Agric. Biol., 7, 376-380.<br />

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Gamal El-Din, K.M., Tarraf, S.A., Balbaa, L.K., 1997. Physiological studies on the effect <strong>of</strong> some<br />

amino acids and microelements on growth and essential oil content in lemongrass<br />

(Cymbopogon citrates Hort). J. Agric. Sci. Mansoura Univ., 22, 4229-4241.<br />

Golan-Goldhirsh, A., Mozafar, A., Oerti, J.J., 1995. Effect <strong>of</strong> ascorbic acid on soybean seedlings grown<br />

on medium containing a high concentration <strong>of</strong> copper. J. Plant Nutr., 18, 1735-1741.<br />

Harridy, I.M.A., 1986. Physiological studies on periwinkle plant (Catharanthus roseus G. Don). Ph.D<br />

Thesis, Fac. <strong>of</strong> Agric., Cairo Univ. pp. 94-96.<br />

Kawasaki, T., 1992. Modern Chromatographic Analysis <strong>of</strong> Vitamins, 2 nd ed., vol. 6-, Marcel Dekker,<br />

Inc., New York, U.S.A., pp. 319-354.<br />

Liu, W., Hu, W.Y, Hao, J.J., Chen, G., 1997. The relationship between ascorbic acid and changes <strong>of</strong><br />

several physiological and biochemical indexes in isolated wheat leaves under NaCl stress.<br />

Plant Physiol., communications, 33, 423-425.<br />

Mahfouz, S.A., Sharaf El-Din, M.A., 2007. Effect <strong>of</strong> mineral vs. bi<strong>of</strong>ertilizer on growth, yield and<br />

essential oil content <strong>of</strong> fennel (Foeniculum vulgare Mill). Int. Agrophysics, 21, 361-366.<br />

Marotti, J., Piccaglia, R., 1992. The influence <strong>of</strong> distillation conditions on the essential oil composition<br />

<strong>of</strong> three varieties <strong>of</strong> Foeniculum vulgare Mill. J. <strong>of</strong> Essential Oil Res. 4, 569-576.<br />

Moursy, H.A. L., Hussein, M.S., El-Bahr., K.M., 1988. Effect <strong>of</strong> some alkaloid precursors on the<br />

growth and alkaloid production <strong>of</strong> Datura stramonium cultured in vitro. Egypt. J. Bot., 31,<br />

153-165.<br />

Pastori, G.M., Kiddle, G., Antoniw, J., Bernard, S., Veljovic – Jovanovic, S., Verrier, P.J., Noctor, G.,<br />

Foyer, C.H., 2003. Leaf vitamin C contents modulate plant defense development through<br />

hormone signaling. The Plant Cell, 15, 939-951.<br />

Pavet, V., Olmos, E., Kiddle, G., Mowla, S., Kumar, S., Antoniw, J., Alvarez, M.E., Foyer, C.H., 2005.<br />

Ascorbic acid deficiency activates cell death and disease resistance responses in Arabidopsis.<br />

Plant Physiol; 139, 1291-1303.<br />

Price, C.E., 1966. Ascorbate stimulation <strong>of</strong> RNA synthesis. Nature, 212, 1481.<br />

Reda, F., Fadl, M., Abdel-Alla, R.S., El-Moursi, A., 1977. Physiological studies on Ammi visnaga L.:<br />

The effect <strong>of</strong> thiamine and ascorbic acid on growth and chromone yield. Egypt. J. Pharm. Sci.,<br />

18, 19-27.<br />

Refaat, A.M., Naguib, Y.N, 1998. Peppermint yields and oil quality as affected by application <strong>of</strong> some<br />

amino acids. Bull. <strong>of</strong> Fac. <strong>of</strong> Agric., Cairo Univ., 1, 89-98.<br />

Robinson, F.A., 1973. Vitamins. In Phytochemistry. Vol. III: 195-220. Lawrence, Miller, P., (ed) Van-<br />

Nostrand Reinhold Co., New York.<br />

Singh, B., Kale, R.K., 2008. Chemomodulatory action <strong>of</strong> Foeniculum vulgare (fennel) on skin and<br />

forestomach papillomagenesis, enzymes associated with xenobiotic metabolism and<br />

antioxidant status in murine model system. Food and Chem.. Toxi., 46, 3842-3850.<br />

Singh, B.K., 1999. Plant Amino Acids: Biochemistry and Biotechnology. Marcel Dekker Inc., New<br />

York, U.S.A, pp.648.<br />

Snedecor, G.W., Cochran, W.C., 1980. Statistical methods' 7 th Ed., Iowa State Univ., Ames, Iowa,<br />

U.S.A., pp. 507.<br />

Talaat, I.M., Yussef, A.A., 2002. The role <strong>of</strong> the amino acids lysine and ornithine in growth and<br />

chemical constituents <strong>of</strong> Basil plant. Egypt. J. Appl. Sci, 17, 83-95.<br />

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Talaat, N.B., 2003. Physiological studies on the effect <strong>of</strong> salinity, ascorbic acid and putrescine <strong>of</strong> sweet<br />

paper plant. Ph.D Thesis, Fac. <strong>of</strong> Agric., Cairo Univ.<br />

Taraf, S.A., Gamal El-Din, K.M., Balbaa, L.K., 1999. The response <strong>of</strong> vegetative growth and essential<br />

oil <strong>of</strong> lemongrass (Cymbopogon citrates Hort) to foliar application <strong>of</strong> ascorbic acid,<br />

nicotinamid and some micronutrients. Arab Univ. <strong>of</strong> Agric. Sci., 7, 247-259.<br />

Wahba, H., Mohamed, S.M., Attoa, G.E., Farahat, A.A., 2002. Response <strong>of</strong> Antholyza aethiopica to<br />

foliar spray with some amino acids and mineral nutrition with sulphur. Annals Agric. Sci., Ain<br />

Shams Univ., 47, 929-944.<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Effect <strong>of</strong> water stress and potassium humate on the productivity <strong>of</strong> oregano plant<br />

using saline and fresh water irrigation<br />

H.A.H. Said-Al Ahl* and M.S. Hussein<br />

Department <strong>of</strong> Cultivation and Production <strong>of</strong> Medicinal and Aromatic Plants,<br />

National Research Centre, Dokki, Giza, Egypt.<br />

Postal code: 12622<br />

*E-mail address for correspondence: saidalahl@yahoo.com<br />

_________________________________________________________________________________<br />

Abstract: To study the response <strong>of</strong> oregano (Origanum vulgare L.) plants to soil moisture regimes<br />

using fresh and saline water irrigation and potassium humate fertilization, a pot experiment was<br />

conducted during two successive seasons (2007/2008 and 2008/2009) under the natural conditions <strong>of</strong><br />

the greenhouse <strong>of</strong> the National Research Center, Dokki, Giza, Egypt. Herb fresh weight g plant -1 and<br />

the content and yield ml plant -1 <strong>of</strong> essential oil were decreased significantly by using saline water<br />

irrigation compared to fresh water irrigation. Herb fresh weight g plant -1 and essential oil yield ml<br />

plant -1 <strong>of</strong> Origanum vulgare L were significantly decreased with the rise in water stress levels.<br />

Whereas, there was significant increase in essential oil % by using lower level <strong>of</strong> available soil<br />

moisture (30% ASM) followed by 90% ASM and then 60% ASM contained the highest values <strong>of</strong><br />

essential oil %. Fresh herb and essential oil production increased significantly with K-humate<br />

application. The maximum <strong>of</strong> herb fresh and essential oil yields were obtained from plants irrigated<br />

with 90% available soil moisture fresh water combined with k-humate fertilizer 1.5 g pot -1 . Essential<br />

oil % recorded their maximum value from plants irrigated with 60% ASM fresh water combined with<br />

1.5 g pot -1 K-hum ate. Totally, 20 compounds were identified in essential oils <strong>of</strong> three populations by<br />

means <strong>of</strong> GLC. Carvacrol was the dominant compound (46.44–77.96%) for all essential oil samples,<br />

followed by p-cymene (5.31–19.30%) and γ-terpinene (3.38–16.42%). The composition <strong>of</strong> essential oil<br />

<strong>of</strong> oregano was affected by soil moisture regimes using fresh and saline water irrigation and potassium<br />

humate fertilization.<br />

Keywords: Origanum vulgare L., essential oil, potassium humate, soil moisture regime, saline<br />

irrigation, carvacrol<br />

_________________________________________________________________________________<br />

INTRODUCTION<br />

The genus Origanum belongs to the family <strong>of</strong> Lamiaceae (Labiatae) and includes many species that are<br />

commonly found as wild plants in the Mediterranean areas (Skoula and Harborne, 2002). Because <strong>of</strong><br />

special compositions <strong>of</strong> essential oil the leaves <strong>of</strong> Origanum plants are widely used as a very popular<br />

spice for food production. Origanum vulgare L. is the widest spread among all the species within the<br />

genus which distributed all over, Europe, West and Central Asia up to Taiwan, North Africa, and<br />

America (Goliaris et al., 2002; Ietswaart, 1980). Traditionally, leaves and flowers <strong>of</strong> oregano are used<br />

in Lithuania mostly for their beneficial properties to cure cough, sore throats, relieve digestive<br />

complaints, and probably stimulate the appetite (Ien et al., 2008). The volatile oil <strong>of</strong> oregano has been<br />

used traditionally for respiratory disorders, indigestion, dental caries, rheumatoid arthritis and urinary<br />

tract disorders (Ertas et al., 2005). The essential oil <strong>of</strong> oregano is composed <strong>of</strong> carvacrol as dominant<br />

component, followed by p-cymene, γ- terpinene, germacrene D, and thymol (Azizi et al., 2009;<br />

Dorman and Deans, 2004; Horne et al., 2001; Said-Al Ahl et al., 2009 a, b; Veldhuizen et al., 2007).<br />

Recently, this spice plant has drawn more attention <strong>of</strong> consumers due to the antimicrobial, antifungal,<br />

insecticidal and antioxidative effects <strong>of</strong> this herb on humanhealthy (Bakkali et al., 2008; Jaloszynski et<br />

al., 2008; Kulisic et al., 2004; Lopez et al., 2007; Soylu et al., 2007).<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

The commercial value <strong>of</strong> an aromatic and <strong>of</strong> a medicinal plant could be reflected by the composition <strong>of</strong><br />

their essential oils. The quality <strong>of</strong> oregano is determined mainly by the essential oil content and its<br />

composition. Both parameters may vary considerably depending on genotypes and cultivation<br />

conditions (D’antuono et al., 2000; Novak et al., 2003). In addition, the essential oil content <strong>of</strong> oregano<br />

leaves and its components seem to be strongly influenced by environmental problems, especially<br />

water/salt stress (Charles et al., 1990) and deficiency and inadequate mineral nutrients (Stutte, 2006).<br />

Salinity is one <strong>of</strong> the major factors that affect plant growth; it is a serious problem in many areas <strong>of</strong> the<br />

world causing considerable loss in agricultural production (Bray et al., 2000; Shao et al., 2008; Wu et<br />

al., 2007). Soil salinity resulting from natural processes or from crop irrigation with saline water,<br />

occurs in many arid and semi-arid regions <strong>of</strong> the world (Lauchli and Epstein, 1990). In Egypt, saline<br />

water is used for irrigation in some areas. In the same time, under the arid climatic conditions<br />

prevailing in Egypt and associated with the perennial irrigation practices, imperfect drainage system,<br />

continuous increase <strong>of</strong> water–table level and the relatively high salinity levels <strong>of</strong> water sources<br />

particularly in the new reclaimed land, the salinization <strong>of</strong> Egyptian soils rapidly going to be an acute<br />

problem.<br />

Similar to other Lamiaceae species, however, uniformity in essential oil content and composition and<br />

consistency in growth and development are especially susceptibility to environmental stress due to<br />

plant heterogeneity. Thus, crop yields and quality in major oregano production regions that are<br />

frequently subject to dry periods can fluctuate (Al-Amier and Craker, 2007). The use <strong>of</strong> irrigation over<br />

the past several years to promote crop growth has increased the salt content <strong>of</strong> the soil, frequently<br />

forcing growers to apply 10% to 20% excess water to lower salt concentrations in the root zone (Arndt<br />

et al., 2001; Mohamed et al., 2002; Takabayashi and Dick 1996; Takabayashi et al., 1994). Water<br />

stress in plants from a lack <strong>of</strong> moisture or from drought induced by salt stress is associated with many<br />

metabolic changes, including essential oil metabolites. In addition, the water supply is one <strong>of</strong> the most<br />

determinative cultivation conditions which significantly affect the yield and essential oil content <strong>of</strong><br />

various spices and herb crops (Aziz et al., 2008; Mohamed et al., 2002; Singh and Ramesh, 2000;<br />

Singh et al., 2000, 2002; Zehtab- Salmasi et al., 2001). In most cases Origanum plants must be<br />

irrigated during the cultivation period to obtain a good yield. For example during cultivation <strong>of</strong><br />

Origanum dictamnus in Crete (Greece), irrigation was necessary for two harvests in 1 year (Skoula and<br />

Kamenopoulos, 1997). Practically, the time at which the plants are irrigated is important for the<br />

efficiency <strong>of</strong> irrigation. For example, appropriate irrigation strategies showed a great potential for<br />

improvement <strong>of</strong> the yield <strong>of</strong> monoterpenes in field-grown spearmint and rosemary (Delfine et al.,<br />

2005). Dunford and Vazquez (2005) reported that herb yield <strong>of</strong> Mexican oregano (Lippia Berlandieri<br />

Schauer) increased significantly with increasing moisture and the amount <strong>of</strong> water received by the plant<br />

did not have a significant effect on the thymol and carvacrol content <strong>of</strong> the oil.<br />

The improvement <strong>of</strong> plant nutrition can contribute to increased resistance and production when the crop<br />

is submitted to water stress. However, the content <strong>of</strong> essential oils and their composition are affected by<br />

fertilization.<br />

Humic acid (HA) is one <strong>of</strong> the major components <strong>of</strong> humus. Humates have long been used as a soil<br />

conditioner, fertilizer and soil supplement (Albayrak and camas, 2005). Humic acid can be used as<br />

growth regulate-hormone level improve plant growth and enhance stress tolerance (Albayrak and<br />

Camas, 2005; Piccola et al., 1992; Tan and Nopamornbodi, 1979). Fortun et al., 1989 and Kononova,<br />

1966 reported that humic acid improve soil structure and change physical properties <strong>of</strong> soil, promote<br />

the chelation <strong>of</strong> many elements and make these available to plants, aid in correcting plant chlorisis,<br />

enhancement <strong>of</strong> photosynthesis density and plant root respiration has resulted in greater plant growth<br />

with humate application (Chen and Avid, 1990; Smidova, 1960). Increase the permeability <strong>of</strong> plant<br />

membranes due to humate application resulted in improve growth <strong>of</strong> various groups <strong>of</strong> beneficial<br />

microorganisms, accelerate cell division, increased root growth and all plant organs for a number <strong>of</strong><br />

horticultural crops and turfgrasses, as well as, the growth <strong>of</strong> some trees, Russo and Berlyn (1990),<br />

Sanders et al. (1990) and Pioncelot (1993).<br />

So far, there is no report on the yield and composition <strong>of</strong> the essential oil <strong>of</strong> Origanum vulgare L.<br />

plants cultivated under this experimental condition in literature.<br />

The aim <strong>of</strong> the present research was to investigate to evaluate oregano plants grown under osmotic<br />

stress conditions and using organic fertilizer treatments to raise the tolerant <strong>of</strong> this plant to stress<br />

conditions, and also to provide information on the composition <strong>of</strong> Origanum vulgare volatile oil and<br />

its variability among osmotic stress conditions.<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

MATERIALS AND METHODS<br />

A pot trail study was carried out during the two successive seasons <strong>of</strong> 2007/2008 and 2008/2009 under<br />

the natural conditions <strong>of</strong> the greenhouse <strong>of</strong> the National Research Center, Dokki, Giza, Egypt. The<br />

physical and chemical analyses <strong>of</strong> the soil were determined according to Jackson, 1973. The soil<br />

texture was sandy loam, having a physical composition as follows: 45.70% sand, 28.40% silt, 25.90%<br />

clay and 0.85% organic matter. The results <strong>of</strong> soil chemical analysis were as follows: pH= 8.05; E.C<br />

(dsm -1 ) = 0.81; and total nitrogen =0.09 %; available phosphorus =2.26mg/100gram; potassium= 18.85<br />

mg/100gram; field capacity (F.C.) and wilting point (W.P.) were determined according to the pressure<br />

membrane methods described by Black, 1965. Field capacity, permanent wilting point, available soil<br />

moisture (A.S.M) and bulk density (B.D.), as means over the two seasons were 34.0 %, 16.0 % 18.0 %<br />

and 1.36 g/cm 3 , respectively.<br />

Seeds <strong>of</strong> oregano were obtained from Jellitto Standensamen Gmbh, Schwarmstedt, Germany. The<br />

seeds were sown in the nursery on 15 th November during both seasons. The seedlings were transplanted<br />

into pots (30 cm diameter, 50 cm depth) on the 15 th February <strong>of</strong> each season. Each pot contained three<br />

seedlings and was placed in full sun light. Each pot was filled with 10 kg <strong>of</strong> air dried soil. The soil<br />

related to the typic torrifluvents (based on USDA, 1996). Two levels <strong>of</strong> potassium humate (0.0 and 1.5<br />

g pot -1 ) was applied to the soil with water irrigation application at three equal portions before each cut<br />

in both seasons. Potassium humate which was used in this study is produced by Leili Agrochemistry<br />

Co., LTD, China and its properties are shown in Table (1). Then after one month from transplanting,<br />

irrigation treatments were applied to the oregano plants (90, 60 and 30% available soil moisture) equal<br />

to 32.20., 26.80 and 21.40 soil moisture. The pots were separated into two sets, the first set irrigated<br />

with tap water (0.40 dsm -1 ), and the second set irrigated with Nacl solution (4 dsm -1 ). Pots were<br />

weighted daily and when soil moisture percentage reached the aforementioned points, pots were<br />

irrigated to reach field capacity (34.0% soil moisture). The differences between the needed soil<br />

moisture for the previous treatments and field capacity were calculated and added to the pots in the<br />

different treatments. The experimental layout was factorial experiment in complete randomized design<br />

(CRD) with three replications. Each replicate contained ten pots, while the pot contained three plants.<br />

Herbal fresh weight (g plant -1 ) <strong>of</strong> each replicate was determined in the first, second and third cuts at<br />

31 May, 31 July and 30 September, respectively before flowering stage in both seasons. Essential oil<br />

content was determined by hydro-distillation for 3 hours by submitting fresh herb (100 g) for each<br />

replicate at each cut in both seasons in modified Clevenger apparatus (Guenther, 1961). Essential oil<br />

percentage <strong>of</strong> each replicate was determined and expressed as (%), while essential oil yield per plant<br />

was expressed as ml plant -1 . The essential oils <strong>of</strong> each treatment were collected and dehydrated over<br />

anhydrous sodium sulphate and kept in a refrigerator until gas-liquid chromatography (GLC) analyses.<br />

The GLC analysis <strong>of</strong> the essential oil samples was carried out in the second season using a Hewlett<br />

Packard gas chromatograph apparatus at the Central Laboratory <strong>of</strong> the National Research Center<br />

(NRC) with the following specifications: instruments: Hewlett Packard 6890 series, column; HP<br />

(Carbwax 20M, 25m length x 0.32mm I.D), film thickness: 0.3mm, sample size: 1µl, oven temperature:<br />

60-190°C, Program temperature: 60°C/2min, 8°C/min, 190°C/25min, injection port<br />

temperature:240°C, carrier gas: nitrogen, detector temperature (FID): 280°C, flow rate: N2 3ml/min.,<br />

H2 3ml/min., air 300ml/min. Main compounds <strong>of</strong> the essential oil were identified by matching their<br />

retention times with those <strong>of</strong> the authentic samples that were injected under the same conditions. The<br />

relative percentage <strong>of</strong> each compound was calculated from the peak area corresponding to each<br />

compound. Except for the constituents <strong>of</strong> the essential oils, the data <strong>of</strong> this experiment were statistically<br />

analyzed according to Snedcor and Cochran (1981).<br />

A.Herb fresh yield<br />

RESULTS AND DISCUSSIONS<br />

Effect <strong>of</strong> water stress using fresh or saline water irrigation<br />

Data in Table (2) clear the effect <strong>of</strong> water stress and potassium humate on the productivity <strong>of</strong> oregano<br />

plant using saline and fresh water irrigation. Under water stress, increase in available soil moisture<br />

significantly enhanced the fresh herb yield in all cuts <strong>of</strong> both seasons. Increasing water amounts<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

increased herb fresh weight. The highest mean values due to irrigation treatments were recorded with<br />

plants that received the highest amounts <strong>of</strong> water. The pronounced effect <strong>of</strong> increased irrigation on<br />

fresh herb yield may be attributed to the availability <strong>of</strong> sufficient moisture around the root concentrated<br />

and thus a greater proliferation <strong>of</strong> root biomass resulting in the higher absorption <strong>of</strong> nutrients and water<br />

leading to production <strong>of</strong> higher vegetative biomass (Singh et al., 1997). On the other hand, increasing<br />

levels <strong>of</strong> water stress reduce growth and yield due to reduction in photosynthesis and plant biomass.<br />

Under increasing water- stress levels photosynthesis was limited by low Co2 availability due to<br />

reduced stomatal and mesophyll conductance. Drought stress is associated with stomatal closure and<br />

thereby with decreased Co2 fixation. The superiority <strong>of</strong> the plants that received the highest rate <strong>of</strong><br />

irrigation treatments in producing the heaviest total plant fresh weight was in agreement with that <strong>of</strong> El-<br />

Naggar et al. (2004); Moeini Alishah et al. (2006); Said-Al Ahl and Abdou (2009); Said-Al Ahl et al.<br />

(2009 a, c) .<br />

Data tabulated in Table (2) show that fresh weight <strong>of</strong> herb (g plant -1 ) decreased significantly with<br />

increment <strong>of</strong> saline irrigation conditions in all cuts during both seasons. The inhibitory effect <strong>of</strong><br />

salinity was also found by (Abd El-Hady, 2007; Abd El-Wahab, 2006; Baghalian et al., 2008; Belaqziz<br />

et al., 2009; Ozturk et al., 2004; Razmjool et al., 2008; Shalan et al., 2006; Turhan and Eris, 2007).<br />

Saline conditions reduce the ability <strong>of</strong> plants to absorb water causing rapid reductions in growth rate,<br />

and induce many metabolic changes (Epstein, 1980). Also, salt stress with osmotic, nutritional and<br />

toxic effects prevents growth in many plant species (Cheeseman, 1988; Hasegawa et al., 1986).<br />

Therefore, the reduction in growth was explained by lower osmotic potential in the soil, which leads to<br />

decreased water uptake, reduced transpiration, and closure <strong>of</strong> stomata, which is associated with the<br />

reduced growth (Ben-Asher et al., 2006; Levitt, 1980). In general, the mechanisms <strong>of</strong> salinity effect on<br />

plant growth were reported by Meiri and Shalhavet (1973) who attributed the effect <strong>of</strong> salinity to the<br />

following points: (a) the distribution <strong>of</strong> salts within the plant cells may result in turgor reduction and<br />

growth retardations. Also, salinity affects root and stomatal resistance to water flow, (b) the balance<br />

between root and shoot hormones changes considerably under saline conditions, (c) salinity changes<br />

the structure <strong>of</strong> the chloroplasts and mitochondria and such changes may interfere with normal<br />

metabolism and growth, (d) salinity increases respiration and reduces photosynthesis products available<br />

for growth.<br />

Effect <strong>of</strong> potassium humate application<br />

Also, data reported in Table (2) showed that foliar application <strong>of</strong> humic acid caused significantly<br />

positive trend in increasing herb fresh yield (g plant -1 ). Similar results were reported by Said-Al Ahl et<br />

al. (2009, b) on Origanum vulgare and Zaghloul et al. (2009) on Thuja orientalis who indicated that<br />

spraying the plants with potassium humate increased growth compared with control plants due to the<br />

direct effect <strong>of</strong> humic acid on solubilization and transport <strong>of</strong> nutrients. These results are in accordance<br />

with those obtained by Norman et al. (2004) on marigolds and peppers and number <strong>of</strong> fruits <strong>of</strong><br />

strawberries. Chen and Avaid (1990) added that humic substances have a very pronounced influence on<br />

the growth <strong>of</strong> plant roots thought enhance root initiation which known as root stimulator. Humic acid<br />

improve growth <strong>of</strong> plant foliage and roots where, Vaughan (1974) proposed that humic acids may<br />

primarily increase root growth by increasing cell elongation or root cell membrane permeability,<br />

therefore increased water uptake by increased plant roots, as well as it can produce root systems by<br />

increasing branching and number <strong>of</strong> fine roots, as a result potentially increase nutrients uptake by<br />

increase root surface area (Rauthan and Schnitzer, 1981).<br />

Effect <strong>of</strong> interaction<br />

There was a significant difference in most <strong>of</strong> interaction treatments between water or salt stress and<br />

potassium humate application. Increment the available soil moisture using saline or fresh water<br />

combined with potassium humate enhanced the fresh herb yield. The irrigation applied at 90%<br />

available soil moisture using fresh water irrigation, combined with potassium humate gave the best<br />

result <strong>of</strong> fresh herb yield in the all cuts during both seasons.<br />

B. Essential oil production<br />

Effect <strong>of</strong> water stress using fresh or saline water irrigation<br />

In all cuts in both seasons, both water quantities using saline and fresh water irrigation and potassium<br />

humate application and their interaction affected the content <strong>of</strong> essential oils in oregano (Tables 3, 4).<br />

The mean values <strong>of</strong> essential oils due to water irrigation treatments showed that increasing water<br />

supply from 30% to 60% available soil moisture increased essential oil percentage. Increasing water<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

supply from 60% to 90% available soil moisture decreased percentage <strong>of</strong> essential oils. In other words,<br />

the medium stress condition (60% available soil moisture treatment) accelerated the production <strong>of</strong><br />

essential oils, while the severe stress conditions due to water (40% available soil moisture treatment)<br />

decreased the biosynthesis <strong>of</strong> the essential oils. On the contrary, essential oil yield increased with<br />

increment <strong>of</strong> available soil moisture (Table 4).<br />

Table (3) explains that salt condition significant decreased essential oil % at all cuts in both seasons.<br />

With similar, essential oil yield also was significant decreased at all cuts <strong>of</strong> both seasons as a result <strong>of</strong><br />

salt stress (Table 4). The inhibitory effect <strong>of</strong> high level <strong>of</strong> salinity was also found by many investigators<br />

(Abd El-Wahab, 2006; Baghalian et al., 2008; Ozturk et al., 2004; Razmjoo et al., 2008; Shalan et al.,<br />

2006). The reduction <strong>of</strong> essential oil yield by salinity may be due to a decrease in growth characters<br />

and/or essential oil %. Salt stress may also affect the essential oil accumulation indirectly through its<br />

effects on either net assimilation or the partitioning <strong>of</strong> assimilate among growth and differentiation<br />

processes (Charles et al., 1990).<br />

Penka (1978) showed that the formation and accumulation <strong>of</strong> essential oil in plants was explained as<br />

due to the action <strong>of</strong> environmental factors. It might be claimed that the formation and accumulation <strong>of</strong><br />

essential oil was directly dependent on perfect growth and development <strong>of</strong> the plants producing oils.<br />

The decrease in oil production might be due to the decrease in plant anabolism.<br />

Effect <strong>of</strong> potassium humate application<br />

Essential oil percent and yield (ml plant -1 ) in oregano herb were significantly increased as a result <strong>of</strong><br />

foliar application with K-humate (Tables 3, 4). Said-Al Ahl et al. (2009, b) and Zaghloul et al. (2009)<br />

reported that humate application lead to increase oil content in Origanum vulgare and Thuja orientalis,<br />

respectively. From the above mentioned results, it could be concluded that foliar application <strong>of</strong> Khumate<br />

promoted growth and possessed the best oil percentage and yield (ml plant -1 ) in oregano plant.<br />

Effect <strong>of</strong> interaction<br />

Generally, the maximum essential oil content was observed in the fresh herb <strong>of</strong> plants that irrigated<br />

using fresh water at 60% ASM and sprayed with 1% K-humate in the all cuts during both seasons. In<br />

addition, spraying oregano plants with K-humate caused an increase in the essential oil yield (Table 4).<br />

Generally, the highest essential oil yield (ml plant -1 ) was obtained from plants irrigated using fresh<br />

water at 90% ASM and sprayed at 1% K-humate in all cuts <strong>of</strong> both seasons. The increment <strong>of</strong> essential<br />

oil yield may be obtained as a result <strong>of</strong> increment herb weight and/or essential oil %.<br />

Essential oil composition <strong>of</strong> oregano<br />

Totally, 20 constituents were identified for the oregano essential oil (Tables 5, 6). Carvacrol content<br />

was the dominant constituent <strong>of</strong> the essential oil for all samples tested, ranging from 46.44% to<br />

77.96%. The second major constituent was p-cymene (ranging from 5.31% to 19.30%) and the third<br />

one was γ-terpinene (ranging from 3.38% to 16.42%). The other main constituents were α-pinene (0-<br />

5.39%), α-terpinene (0-5.39%), α-thujene (0-5.05%), germacrene D (0-2.91%), thymol (0-2.76%),<br />

caryophyllene (0-2.70%), terpineol-4-ol (0-1.56%) and β-pinene (0-1.19%). Other constituents such as<br />

linalool, limonene, borneol, α-terpineol, bornyl acetate, carvacrol acetate, elemene, cadinene and<br />

caryophyllene oxide were present in amount less the 1%.<br />

In second cut <strong>of</strong> second season, among water and saline stress, the carvacrol percentage <strong>of</strong> essential oil<br />

was increased by raising amount <strong>of</strong> fresh water irrigation and irrigation at 90% ASM gave a higher<br />

value (77.96%), 60% ASM (67.17%) and 30% ASM gave a lower value (60.36%), but there was<br />

decrease in this regard by raising amount <strong>of</strong> saline water irrigation and irrigation at 30% ASM gave a<br />

higher content (58.02%), 90% ASM (57.79%) and 60% ASM gave a lower content (46.44%). Whereas,<br />

p-cymene was decreased by raising amount <strong>of</strong> fresh and saline water irrigation and a higher content <strong>of</strong><br />

this component was resulted from irrigation at 30% ASM (15.63 and 16.94% using fresh and saline<br />

water, respectively), 60% ASM fresh water and 90% ASM saline water (11.64 and 16.03%,<br />

respectively) and a lower content (8.76 and 13.29%, resulted from 90% ASM fresh water and 60%<br />

ASM saline water, respectively). Correspondingly, the percentage <strong>of</strong> γ-terpinene was decreased by<br />

raising amount <strong>of</strong> fresh water irrigation and irrigation at 30% ASM gave a higher value (7.65%), 60%<br />

ASM (6.61%) and 90% ASM gave a lower value (3.56%), but there was increase in this regard by<br />

raising amount <strong>of</strong> saline water irrigation and irrigation at 90% ASM gave a higher content (12.94%),<br />

30% ASM (11.63%) and 60% ASM gave a lower content (11.32%), Table (5). It is clear that saline<br />

water irrigation increased the biosynthesis <strong>of</strong> p-cymene and γ-terpinene, while the apposite was true<br />

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with carvacrol. It is well known p-cymene transforms to thymol or carvacrol and the environmental<br />

conditions affect the rate <strong>of</strong> transformation (Aziz et al., 2008; Omer, 1999).<br />

From Table (6) it can be observed the differences between three major constituents <strong>of</strong> essential oil <strong>of</strong><br />

oregano supplying with a water level <strong>of</strong> 90% available soil moisture and without / with 1.5 g K-humate<br />

pot -1 in three cuttings, carvacrol was higher for plants irrigated with a fresh water alone in second cut<br />

and compared to other treatments but, the plants irrigated with a saline water alone in first cut<br />

contained a lower content. On the contrary p-cymene and γ-terpinene were the highest by using saline<br />

water irrigation and with K-humate in first cut and the lowest content from the plants irrigated with<br />

fresh water alone in third cut. Irrigation with 90% ASM with fresh water without potassium humate in<br />

second cut gave the maximum value <strong>of</strong> carvacrol content (77.96%), while irrigation with 90% ASM<br />

with fresh water without potassium humate in first cut gave the highest values for both p-cymene<br />

(10.99%) and γ-terpinene (8.41%). Under saline water irrigation the maximum values for both pcymene<br />

(19.30%) and γ-terpinene (16.42%) were obtained as a result <strong>of</strong> 90% ASM with potassium<br />

humate in first cut, while 90% ASM with potassium humate in second cut gave the highest value <strong>of</strong><br />

carvacrol (63.17%).<br />

Table (7) indicates that saline water irrigation decreased the mean value <strong>of</strong> carvacrol and on the<br />

contrary there was increased in p-cymene and γ-terpinene mean values by using saline water irrigation.<br />

Whereas, mean values <strong>of</strong> carvacrol, p-cymene and γ-terpinene were increased by application <strong>of</strong> Khumate.<br />

Also, mean values <strong>of</strong> carvacrol, p-cymene and γ-terpinene were affected by cuttings. For<br />

carvacrol, third cut recorded the highest mean value followed by second cut and then first cut.γterpinene<br />

has adverse behavior, first cut resulted the highest mean value followed by second cut and<br />

then third cut. However, the highest mean value <strong>of</strong> p-cymene resulted from second cut and third cut<br />

recorded the lowest mean value.<br />

Second cut was effective in raising the productivity <strong>of</strong> the essential oil yield. Table (8) show that saline<br />

water irrigation decreased the mean value <strong>of</strong> carvacrol and on the contrary there was increased in pcymene<br />

and γ-terpinene mean values by using saline water irrigation. Among soil moisure levels, the<br />

carvacrol mean value <strong>of</strong> essential oil was the highest at 90% ASM and 60% ASM obtained the lowest<br />

mean value. Also, the mean values <strong>of</strong> p-cymene and γ-terpinene were the highest for 30% ASM<br />

followed by 60% ASM and then 90% ASM.<br />

CONCLUSIONS<br />

Our study showed that herbal production and essential oil content <strong>of</strong> Origanum vulgare L. can be<br />

significantly affected by environmental and agronomical conditions including potassium humate<br />

fertilization and soil moisture regime using fresh and saline water irrigation. Application <strong>of</strong> potassium<br />

humate increase herb fresh yield and essential oil content <strong>of</strong> oregano herbage. Herbal fresh yield and<br />

essential oil % and oil yield ml plant -1 were significant decreased by using a saline water irrigation<br />

compared to fresh water. Supplying plants with a water level <strong>of</strong> 90% available soil moisture was<br />

effective in raising the productivity <strong>of</strong> herb and yield <strong>of</strong> essential oil, but 60% available soil moisture<br />

was effective in essential oil percentage, whereas 30% available soil moisture significantly decreased<br />

herbal fresh yield and essential oil % and oil yield ml plant -1 .The interaction between 90% available<br />

soil moisture <strong>of</strong> fresh water and with 1.5 g pot -1 k-hum ate gave the best results for herb and yield <strong>of</strong><br />

essential oil. Essential oil % recorded their maximum value from plants irrigated with 60% ASM <strong>of</strong><br />

fresh water combined with 1.5 g pot -1 K-humate. Whereas percentage <strong>of</strong> main compounds <strong>of</strong> essential<br />

oil such as carvacrol, γ-terpinene and p-cymene affected by these treatments. Supplying plants with a<br />

water level <strong>of</strong> 90% available soil moisture <strong>of</strong> fresh water alone in second cut contained the highest<br />

value <strong>of</strong> carvacrol, but p-cymene and γ-terpinene recorded their maximum values by irrigating<br />

Origanum vulgare with a saline water level <strong>of</strong> 90% available soil moisture and with k-humate in first<br />

cut.<br />

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TABLES<br />

Table 1. Guaranteed analysis and physical data <strong>of</strong> Humic total<br />

Guaranteed analysis<br />

Humic acid 80%<br />

Potassium (K2O) 10-12%<br />

Zn, Fe, Mn, etc., 100ppm<br />

Physical Data<br />

Appearance Black powder<br />

pH 9-10<br />

Water solubility < 98%<br />

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Table 2. Effect <strong>of</strong> water stress using saline and fresh water irrigation, K-humate fertilizer and their interaction treatments on the herb fresh weight <strong>of</strong> oregano<br />

plants during the two seasons.<br />

K-humate<br />

132<br />

First Season<br />

Water<br />

Herb fresh weight (g plant<br />

and salt<br />

stress<br />

-1 )<br />

Without<br />

K-humate<br />

First cut<br />

K-humate Mean<br />

Without<br />

K-humate.<br />

Second cut<br />

K-humate. Mean<br />

Without<br />

K-humate<br />

Third cut<br />

K-humate Mean<br />

S1 2.41 4.58 3.49 3.72 6.45 5.08 1.05 1.58 1.31<br />

S2 4.18 7.77 5.97 7.50 10.07 8.78 3.13 5.02 4.08<br />

S3 5.71 10.53 8.12 8.96 17.43 13.20 4.38 7.30 5.84<br />

S4 1.58 2.02 1.80 2.03 2.48 2.25 0.61 0.75 0.68<br />

S5 2.02 2.49 2-25 2.76 3.01 2.88 0.94 1.24 1.09<br />

S6 2.72 3.21 2-96 3.59 4.42 4.00 1.83 2.02 1.92<br />

Mean 3.10 5.10 4.76 7.31 6.03 1.99 2.98<br />

L.S.D. at 5% K-humate =0.056<br />

K-humate = 0.046<br />

K-humate = 0.034<br />

Stress = 0.098<br />

Stress = 0.079<br />

Stress = 0.059<br />

Interaction =0.138<br />

Interaction = 0.113<br />

Interaction =0.083<br />

S1 2.47 4.58 3.53 3.69<br />

Second Season<br />

6.45 5.07 1.03 5.03 3.03<br />

S2 4.19 7.69 5.94 7.53 10.17 8.85 3.10 7.20 5.15<br />

S3 5.70 10.75 8.23 8.88 17.28 13.08 4.44 0.58 2.51<br />

S4 1.49 2.02 1.75 1.97 2.43 2.20 0.58 0.71 0.64<br />

S5 2.05 2.42 2.23 2.72 3.05 2.88 0.94 1.10 1.02<br />

S6 2.61 3.15 2.88 3.65 4.39 4.02 1.88 2.07 1.97<br />

Mean 3.08 5.10 4.74 7.29 1.99 2.78<br />

L.S.D. at 5% K-humate =0.050<br />

K-humate = 0.042<br />

K-humate = 0.039<br />

Stress = 0.087<br />

Stress = 0.073<br />

Stress = 0.067<br />

Interaction =0.123<br />

Interaction =0.103<br />

Interaction =0.055<br />

S-stress; S1, S2, S3= irrigation <strong>of</strong>: 30, 60, 90% available soil moisture using fresh water; S4, S5, S6= irrigation <strong>of</strong>: 30, 60, 90% available soil moisture using<br />

saline water


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 3. Effect <strong>of</strong> water stress using saline and fresh water irrigation, K-humate fertilizer and their interaction treatments on the herb fresh volatile oil (%) <strong>of</strong><br />

oregano plants during the two seasons.<br />

K-humate<br />

133<br />

First Season<br />

Water<br />

Volatile oil (%)<br />

and salt<br />

stress<br />

Without<br />

K-humate<br />

First cut<br />

K-humate Mean<br />

Without<br />

K-humate.<br />

Second cut<br />

K-humate. Mean<br />

Without<br />

K-humate<br />

Third cut<br />

K-humate Mean<br />

S1 0.533 0.633 0.583 0.450 0.533 0.491 0.416 0.433 0.425<br />

S2 0.650 0.750 0.700 0.533 0.633 0.583 0.500 0.583 0.541<br />

S3 0.600 0.683 0.641 0.500 0.600 0.550 0.466 0.533 0.500<br />

S4 0.366 0.383 0.375 0.316 0.366 0.341 0.233 0.266 0.250<br />

S5 0.450 0.483 0.466 0.433 0.483 0.458 0.383 0.400 0.391<br />

S6 0.433 0.466 0.450 0.433 0.466 0.450 0.350 0.383 0.366<br />

Mean 0.505 0.566 0.444 0.513 0.391 0.433<br />

L.S.D. at 5% K-humate = 0.0157<br />

K-humate = 0.0143<br />

K-humate = 0.0184<br />

Stress = 0.0275<br />

Stress = 0.0247<br />

Stress = 0.0319<br />

Interaction =N.S<br />

Interaction = 0.0349<br />

Interaction =0.0451<br />

S1 0.516 0.633 0.575 0.433<br />

Second Season<br />

0.533 0.483 0.400 0.433 0.416<br />

S2 0.633 0.766 0.700 0.533 0.616 0.575 0.500 0.583 0.541<br />

S3 0.616 0.666 0.641 0.500 0.583 0.541 0.450 0.533 0.491<br />

S4 0..383 0.416 0.400 0.300 0.383 0.341 0.250 0.316 0.283<br />

S5 0.483 0.500 0.491 0.466 0.466 0.466 0.366 0.383 0.375<br />

S6 0.433 0.450 0.441 0.416 0.433 0.425 0.366 0.383 0.375<br />

Mean 0.511 0.572 0.541 0.441 0.502 0.388 0.438<br />

L.S.D. at 5% K-humate = 0.0150<br />

K-humate = 0.0190<br />

K-humate = 0.0178<br />

Stress = 0.0260<br />

Stress = 0.0329<br />

Stress = 0.0308<br />

Interaction =0.0368<br />

Interaction =0.0466<br />

Interaction =0.0436<br />

S-stress; S1, S2, S3= irrigation <strong>of</strong>: 30, 60, 90% available soil moisture using fresh water; S4, S5, S6= irrigation <strong>of</strong>: 30, 60, 90% available soil moisture using<br />

saline water


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 4. Effect <strong>of</strong> water stress using saline and fresh water irrigation, K-humate fertilizer and their interaction treatments on the volatile oil yield (ml plant -1 )<br />

<strong>of</strong> oregano plants during the two seasons.<br />

K-humate<br />

134<br />

First Season<br />

Water<br />

Oil yield (ml plant<br />

and salt<br />

stress<br />

-1 )<br />

Without<br />

K-humate<br />

First cut<br />

K-humate Mean<br />

Without<br />

K-humate.<br />

Second cut<br />

K-humate. Mean<br />

Without<br />

K-humate<br />

Third cut<br />

K-humate Mean<br />

S1 0.0128 0.0289 0.0209 0.0167 0.0353 0.0260 0.0044 0.0068 0.0056<br />

S2 0.0271 0.0582 0.0427 0.0400 0.0528 0.0464 0.0153 0.0293 0.0223<br />

S3 0.0342 0.0725 0.0534 0.0448 0.0916 0.0682 0.0204 0.0389 0.0296<br />

S4 0.0058 0.0077 0.0068 0.0064 0.0091 0.0078 0.0014 0.0016 0.0015<br />

S5 0.0091 0.0121 0.0106 0.0120 0.0146 0.0133 0.0036 0.0050 0.0043<br />

S6 0.0118 0.0150 0.0134 0.0156 0.0206 0.0181 0.0064 0.0078 0.0071<br />

Mean 0.0168 0.0324 0.0226 0.0373 0.0086 0.0149<br />

L.S.D. at 5% K-humate = 0.00076<br />

K-humate = 0.0048<br />

K-humate = 0.0005<br />

Stress = 0.00281<br />

Stress = 0.0083<br />

Stress = 0.0009<br />

Interaction =0.00188<br />

Interaction = 0.0118<br />

Second Season<br />

Interaction =0.0013<br />

S1 0.0154 0.0290 0.0222 0.0160 0.0344 0.0252 0.0041 0.0065 0.0053<br />

S2 0.0265 0.0589 0.0427 0.0387 0.0627 0.0507 0.0155 0.0294 0.0224<br />

S3 0.0351 0.0717 0.0534 0.0444 0.1008 0.0726 0.0799 0.0384 0.0591<br />

S4 0.0057 0.0337 0.0197 0.0059 0.0093 0.0076 0.0014 0.0023 0.0018<br />

S5 0.0099 0.0121 0.0110 0.0127 0.0142 0.0134 0.0036 0.0046 0.0041<br />

S6 0.0113 0.0142 0.0128 0.0152 0.0190 0.0171 0.0069 0.0079 0.0074<br />

Mean 0.0173 0.0366 0.0270 0.0221 0.0401 0.0186 0.0148<br />

L.S.D. at 5% K-humate = 0.0073<br />

K-humate = 0.0012<br />

K-humate = 0.0171<br />

Stress = 0.0126<br />

Stress = 0.0021<br />

Stress = 0.0297<br />

Interaction =0.0178<br />

Interaction =0.0030<br />

Interaction =0.0420<br />

S-stress; S1, S2, S3= irrigation <strong>of</strong>: 30, 60, 90% available soil moisture using fresh water; S4, S5, S6= irrigation <strong>of</strong>: 30, 60, 90% available soil moisture using<br />

saline water


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 5. Essential oil composition (%) <strong>of</strong> Origanum vulgare L. plants grown under different levels <strong>of</strong><br />

Available soil moisture using fresh and saline water irrigation at second cut in 2009 season.<br />

Compounds<br />

135<br />

Treatments<br />

Irrigation with fresh water Irrigation with saline water<br />

30% ASM 60% ASM 90% ASM 30% ASM 60% ASM 90% ASM<br />

���thujene -- -- 0.33<br />

���pinene -- 0.11 0.08<br />

���pinene 0.56 0.61 0.11<br />

��terpinene<br />

0.45 0.28 0.38<br />

P-cymene<br />

15.63 11.64 8.76<br />

limonene<br />

γ- terpinene<br />

linalool<br />

borneol<br />

Terpinene-4-ol<br />

��terpineol<br />

thymol<br />

Bornyl acetate<br />

carvacrol<br />

Carvacrol acetate<br />

elemene<br />

0.70 0.46 0.30<br />

7.65 6.61 3.56<br />

0.64 0.35 0.54<br />

0.90 0.76 0.03<br />

0.85 0.51 0.40<br />

0.19 0.20 0.27<br />

1.87 1.55 0.98<br />

0.16 0.19 0.06<br />

60.36 67.17 77.96<br />

0.59 0.41 0.59<br />

0.29 0.21 0.36<br />

�caryophyllene 0.14 0.45 0.40<br />

germacrene D<br />

cadinene<br />

caryephyllene oxide<br />

Identified compounds<br />

0.59 1.61 0.83<br />

0.05 0.09 0.01<br />

-- -- 0.01<br />

91.62 93.21 95.96<br />

Irrigation <strong>of</strong>: 30, 60, 90% ASM– <strong>of</strong> available soil moisture<br />

-- 5.05<br />

-- 2.70<br />

-- 0.75<br />

1.62 5.39<br />

16.94 13.29<br />

-- 0.49<br />

11.63 11.32<br />

-- 0.41<br />

-- 1.89<br />

-- 1.56<br />

-- --<br />

-- 2.76<br />

-- --<br />

58.02 46.44<br />

-- --<br />

-- 0.45<br />

1.27 2.57<br />

1.52 1.66<br />

-- --<br />

-- 0.87<br />

91.00 97.59<br />

1.15<br />

0.11<br />

0.25<br />

1.53<br />

16.03<br />

--<br />

12.94<br />

0.18<br />

--<br />

0.37<br />

--<br />

0.96<br />

0.24<br />

57.79<br />

0.30<br />

--<br />

1.02<br />

1.07<br />

0.05<br />

0.16<br />

94.05


Compounds<br />

���thujene<br />

���pinene<br />

���pinene<br />

��terpinene<br />

P-cymene<br />

limonene<br />

γ- terpinene<br />

linalool<br />

borneol<br />

Terpinene-4ol<br />

��terpineol<br />

thymol<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 6. Essential oil composition (%) <strong>of</strong> Origanum vulgare L. plants grown with 90% Available soil<br />

moisture using fresh and saline water irrigation and/or k-humate application during three cuts in 2009<br />

season.<br />

Bornyl acetate<br />

carvacrol<br />

Carvacrol<br />

acetate<br />

elemene<br />

�caryophyllene<br />

germacrene D<br />

cadinene<br />

caryephyllene<br />

oxide<br />

Identified<br />

compounds<br />

Treatments<br />

Irrigation with fresh water<br />

Irrigation with saline water<br />

Without K-humate With K-humate<br />

Without K-humate With K-humate<br />

Cut 1 Cut 2 Cut 3 Cut 1 Cut 2 Cut 3 Cut 1 Cut 2 Cut 3 Cut 1 Cut 2 Cut 3<br />

0.21 0.33 0.33 0.31 0.31 1.32 1.50 1.15 1.45 0.77 0.37 1.07<br />

0.23<br />

0.81<br />

0.46<br />

10.99<br />

0.90<br />

8.41<br />

0.40<br />

0.45<br />

0.41<br />

0.20<br />

1.51<br />

0.21<br />

66.04<br />

0.21<br />

0.14<br />

0.36<br />

0.66<br />

0.07<br />

--<br />

92.67<br />

0.08<br />

0.11<br />

0.38<br />

8.76<br />

0.30<br />

3.56<br />

0.54<br />

0.03<br />

0.40<br />

0.27<br />

0.98<br />

0.06<br />

77.96<br />

0.59<br />

0.36<br />

0.40<br />

0.83<br />

0.01<br />

0.01<br />

95.96<br />

0.18<br />

1.04<br />

0.58<br />

5.31<br />

0.53<br />

3.38<br />

0.24<br />

0.23<br />

0.52<br />

--<br />

0.91<br />

0.18<br />

77.04<br />

0.28<br />

0.23<br />

0.22<br />

2.45<br />

0.31<br />

0.19<br />

94.15<br />

0.39<br />

0.65<br />

0.49<br />

9.21<br />

0.36<br />

7.33<br />

0.31<br />

0.40<br />

0.61<br />

0.27<br />

1.27<br />

0.45<br />

67.51<br />

0.81<br />

0.45<br />

0.70<br />

0.48<br />

--<br />

--<br />

91.90<br />

0.31<br />

--<br />

--<br />

10.73<br />

--<br />

5.33<br />

0.36<br />

--<br />

0.43<br />

0.63<br />

1.01<br />

0.30<br />

74.54<br />

0.89<br />

0.45<br />

0.35<br />

0.47<br />

0.02<br />

--<br />

96.13<br />

136<br />

1.74<br />

0.66<br />

0.56<br />

5.41<br />

--<br />

5.00<br />

0.63<br />

0.39<br />

0.68<br />

--<br />

1.33<br />

0.37<br />

71.74<br />

0.51<br />

0.43<br />

0.90<br />

2.00<br />

0.80<br />

0.43<br />

94.90<br />

1.51<br />

1.19<br />

1.27<br />

13.08<br />

--<br />

13.56<br />

--<br />

--<br />

0.71<br />

--<br />

1.52<br />

--<br />

52.41<br />

--<br />

--<br />

2.70<br />

0.79<br />

0.73<br />

--<br />

91.97<br />

0.11<br />

0.25<br />

1.53<br />

16.03<br />

--<br />

12.94<br />

0.18<br />

--<br />

0.37<br />

--<br />

0.96<br />

0.24<br />

57.79<br />

0.30<br />

--<br />

1.02<br />

1.07<br />

0.05<br />

0.16<br />

94.05<br />

0.18<br />

0.41<br />

--<br />

11.95<br />

--<br />

11.41<br />

--<br />

0.12<br />

0.40<br />

0.08<br />

1.03<br />

--<br />

60.11<br />

0.19<br />

--<br />

1.15<br />

2.91<br />

0.30<br />

0.11<br />

91.50<br />

0.88<br />

--<br />

1.64<br />

19.30<br />

--<br />

16.42<br />

--<br />

--<br />

--<br />

--<br />

1.61<br />

--<br />

54.29<br />

--<br />

--<br />

1.77<br />

--<br />

--<br />

--<br />

96.68<br />

0.40<br />

--<br />

0.15<br />

17.40<br />

--<br />

9.58<br />

--<br />

--<br />

0.65<br />

--<br />

1.45<br />

--<br />

63.17<br />

0.65<br />

0.11<br />

0.75<br />

1.60<br />

--<br />

0.01<br />

96.29<br />

0.60<br />

0.11<br />

0.34<br />

12.08<br />

0.41<br />

10.52<br />

0.18<br />

0.11<br />

0.25<br />

0.19<br />

1.18<br />

0.18<br />

61.29<br />

0.29<br />

0.18<br />

1.71<br />

2.45<br />

0.28<br />

0.17<br />

93.59


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 7. Important differences in three main compounds <strong>of</strong> Origanum vulgare L. essential oil. The<br />

plants were grown with 90% Available soil moisture using fresh and saline water irrigation and/or k-<br />

humate application during three cuts in 2009 season.<br />

Compounds<br />

137<br />

Treatments<br />

Water irrigation K-humate Cuttings<br />

Mean <strong>of</strong><br />

Fresh<br />

Mean <strong>of</strong><br />

Saline<br />

Mean <strong>of</strong><br />

Without<br />

Mean <strong>of</strong><br />

With<br />

Mean <strong>of</strong><br />

Cut 1<br />

Mean <strong>of</strong><br />

Cut 2<br />

Mean <strong>of</strong><br />

Cut 3<br />

carvacrol 72.47 58.13 65.18 65.42 60.22 63.36 67.79<br />

P-cymene 8.40 14.37 11.02 12.35 13.14 13.23 8.68<br />

γ- terpinene 5.50 12.40 8.87 9.03 11.43 7.85 7.57<br />

Total 86.37 85.50 85.07 86.80 84.79 84.44 84.04<br />

Table 8. Important differences in three main compounds <strong>of</strong> Origanum vulgare L. essential oil. The<br />

plants were grown under different levels <strong>of</strong> Available soil moisture using fresh and saline water<br />

irrigation at second cut in 2009 season.<br />

Compounds<br />

Mean <strong>of</strong> 30%<br />

ASM<br />

Treatments<br />

Soil moisture Water irrigation<br />

Mean <strong>of</strong> 60%<br />

ASM<br />

Mean <strong>of</strong> 90%<br />

ASM<br />

Mean <strong>of</strong> Fresh Mean <strong>of</strong><br />

Saline<br />

carvacrol 59.19 56.80 64.87 68.49 54.08<br />

P-cymene 16.28 12.46 12.39 12.01 15.42<br />

γ- terpinene 9.64 8.96 8.25 5.94 11.96<br />

Total 85.11 78.22 85.51 86.44 81.46


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

Influence <strong>of</strong> Foliar Application <strong>of</strong> Pepton on Growth, Flowering and Chemical<br />

Composition <strong>of</strong> Helichrysum bracteatum Plants under Different Irrigation<br />

Intervals.<br />

Soad , M.M. Ibrahim, Lobna, S. Taha* and M.M. Farahat<br />

Department <strong>of</strong> Ornamental Plant and Woody Trees,<br />

National Research Centre, Dokki, Cairo, Egypt<br />

*E-mail address for correspondence: lonbasalah82@yahoo.com<br />

___________________________________________________________________________________<br />

Abstract: Two field experiments were carried out at Research and Production Station, Nubaria <strong>of</strong><br />

National Research Center, Egypt, during 2007 and 2008 seasons. The purpose <strong>of</strong> this study is to<br />

investigate the influence <strong>of</strong> foliar spraying with peptone (0, 250, 500 and 1000 ppm) on growth,<br />

flowering and chemical composition under three irrigation intervals (2, 4 and 6 days) on Helichrysum<br />

bracteatum. Irrigation intervals treatments have a depressing effect on different growth characters<br />

(plant height, number <strong>of</strong> branches/plant, leaf area and fresh and dry weight <strong>of</strong> leaves) by increasing<br />

irrigation intervals. The same manner was observed and concerning flowering parameters and<br />

chemical constituents (total soluble sugars, total soluble indoles and free amino acids). On the<br />

contrary, three pigments content and total soluble phenols. Data also, showed that all growth<br />

parameters and flowering parameters (number <strong>of</strong> flower/plant, flower diameter and fresh and dry<br />

weights <strong>of</strong> flowers) were significantly promoted by increasing the concentration <strong>of</strong> pepton from 250 to<br />

500 and 1000 ppm as well as chemical constituents. The most promising results were obtained from<br />

plants treated with pepton 1000 ppm and irrigated every 2 days. These treatments may be<br />

recommended for decreasing the hazard effect on growth <strong>of</strong> Helichrysum bracteatum under different<br />

irrigation intervals.<br />

Keywords: foliar pepton, irrigation intervals, growth parameters, chemical composition.<br />

_________________________________________________________________________________<br />

INTRODUCTION<br />

Straw flower, Hardy Annual or Everlasting (Helichrysum bracteatum). Family Asteraceae is an easy<br />

annual plant to grow with yellow, orange, pink, deep rose, red, wine, magento, purplor white blooms.<br />

The true petals are found in the center <strong>of</strong> each flower and they are surrounded by colorful, straw like<br />

bracts. The flowers bloom from summer to early autumn. Harvest flowers for drying before they open<br />

fully. Seeds need light to germinate, plant in porous soil. It endemic to Austalia, growing in open<br />

scrub and grassland areas. And using in Dried Arrangement, Border, Rock garden and Cutting Bed.<br />

Water is the major component <strong>of</strong> the plant body. It constituents about 80 to 90 % <strong>of</strong> fresh weight <strong>of</strong><br />

most herbaceous plant organs and over 50 % <strong>of</strong> the fresh weight <strong>of</strong> woody parts. Water affects<br />

markedly, either directly or indirectly, most plant physiological processes. Hence, with the exception<br />

<strong>of</strong> some kinds <strong>of</strong> seeds, dehydration <strong>of</strong> plant tissues below some critical level is accompanied by<br />

irreversible changes in structure and ultimately by plant death. The importance <strong>of</strong> water in living<br />

organisms results from its unique physical and chemical properties, which also determine its functions<br />

in plant physiology, water is a major constituent <strong>of</strong> the protoplasm, it acts as a solvent for many solid<br />

and gaseous substances, forming a continuous liquid phase throughout the plant, it takes part in many<br />

important physiological reactions, it maintains cell turgor, which exerts an impact on many<br />

physiological processes. Several authors indicated the promotive effect <strong>of</strong> the high levels <strong>of</strong> wate<br />

supply on growth parameters including, Farahat (1990) on Schinus molle, Schinus terebinthifolius and<br />

Myoporum acuminatum, Sayed (2001) on Khaya senegalensis, Uday et al (2007), and Soad (2005) on<br />

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Simmodsia chinensis, Azza and Sahar (2006)on Melia azedarach and Azza et al (2007) on Bauhinia<br />

variegata.<br />

Amino acids as organic nitrogenous compounds are the building blocks in the synthesis <strong>of</strong> proteins,<br />

Davies (1982). Amino acids are particularly important for stimulation cell growth. They act as buffers<br />

which help to maintain favorable pH value within the plant cell, since they contain both acid and basic<br />

groups; they remove the ammonia from the cell. This function is associated with amide formation, so<br />

they protect the plants from ammonia toxicity. They can serve as a source <strong>of</strong> carbon and energy, as<br />

well as protect the plants against pathogens. Amino acids also function in the synthesis <strong>of</strong> other<br />

organic compounds, such as protein, amines, purines and pyrimidiens, alkaloids vitamins, enzymes,<br />

terpenoids and others, Goss (1973) and Hass (1975), stated that the biosynthesis <strong>of</strong> cinamic acids<br />

(which are the starting materials for the synthesis <strong>of</strong> phenols) are derived from phenylalanine and<br />

tyrosine. Tyrosine is hydroxyl phenol amino acid that is used to build neurotran smitters and<br />

hormones. Several other authors indicated that promotive effect <strong>of</strong> amino acids on ornamental and<br />

medicinal plants including, Mohamed and Khalil (1992) on Antirrhinum majus, Matthiola incana and<br />

Callistephus chinensis, Hussein et al (1992) on Datura metel, Mohamed and Whaba (1993) on<br />

Rosmarinus <strong>of</strong>ficinalis, Abou Dahab and Nahed (2006) on Philodendron erubescens and Nahed and<br />

Balbaa (2007) on Saliva farinacea.<br />

Therefore, the present investigation was planned to explore the ability <strong>of</strong> helichrysum plants <strong>of</strong><br />

tolerating various degrees <strong>of</strong> drought, and possible alleviating <strong>of</strong> the harmful effects by the use <strong>of</strong><br />

pepton.<br />

MATERIALS AND METHODS<br />

Two field experiments were carried out at National Research Centre (Research and Production Station,<br />

Nubaria), during two successive seasons <strong>of</strong> 2006/2007 and 2007/2008 to investigate the effect <strong>of</strong><br />

irrigation and foliar application <strong>of</strong> peptone on growth, flowering and chemical constituents <strong>of</strong><br />

Helichrysum bracteatum plants. Helichrysum seeds were supplied from Research and Production<br />

Station, Nubaria. The soil is sand in texture with pH 8.0 , EC 0.92 dSm -1 (at 25 o C), organic carbon<br />

0.89 %, and nutrients (N % 0.036, P% 0.012, K% 0.016 and Fe 265 ppm).seeds were sown on the 1 st<br />

week <strong>of</strong> September, after 45 days from sowing uniform seedlings about 8 cm height with 2 pairs <strong>of</strong><br />

leaves were transplanted into the open field. The experiment was set up in a split plot design with three<br />

replicates (each replicate contained 6 plants) containing three treatments <strong>of</strong> irrigation intervals (2, 4 and<br />

6 days) occupied the main plots and three pepton concentrations (250, 500 and 1000 ppm) in addition<br />

to the untreated plants (control) were assigned to the subplots. The seedlings were planted in row at 50<br />

cm, distance. Drip irrigation system was applied in the experiment using drippers (4L/h) for two hours<br />

every two days. The plants were fertilized with 4g ammonium nitrate (33% N), 2g potassium sulphate<br />

(48 % K2O) and 4 g calcium super phosphate (15.5 % P2O5) / plant after 15 days from transplanting.<br />

The grown plants received the normal cultural practices during the growth seasons.<br />

Plants were sprayed with pepton (based on the energizing power <strong>of</strong> free amino acids, produced by<br />

A.P.C. Europe Co. Avsan Julain-Spain). Plants were sprayed twice with pepton until run-<strong>of</strong>f occurred;<br />

the first spraying was in the second week <strong>of</strong> March. One month later the second spray was performed.<br />

At the first week <strong>of</strong> May 2006/2007 and 2007/2008, the following data were recorded: plant height<br />

(cm), number <strong>of</strong> branches /plant, leaf area (cm 2 ) fresh and dry weights <strong>of</strong> leaves (g), number <strong>of</strong><br />

flowers/ plant, flower diameter (cm) and fresh and dry weight <strong>of</strong> flower (g). total soluble sugars were<br />

determined in the methanolic extract by using the phenol-sulphoric method according to Dubois et al<br />

(1956), photosynthetic pigments including Chlorophyll (a+b) as well as carotenoids content were<br />

determined in fresh leaves as mg/gm fresh weight, according to the procedure achieved by Saric et al<br />

(1976). The total indoles were determined in the methanolic extract, using P-dimethyl<br />

aminobenzaldhyed test " Erlic's reagent" according to Larsen et al (1962). Total soluble phenols were<br />

determined calorimetrically by using Folin Ciocalte a reagent A.O.A.C. (1985). Free amino acid<br />

content was determined according to Rosen (1957).<br />

The data were statistically analyzed for each season and then a combined analysis <strong>of</strong> the two seasons<br />

was carried out according to the procedure outlined by Steel and Torrie (1980).<br />

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Growth parameters:<br />

RESULTS AND DISCUSSION<br />

Data presented in Table (1) indicated that significant increasing in all growth parameters by reducing<br />

the interval between irrigations. The highest values <strong>of</strong> plant height, number <strong>of</strong> branches/ plant, leaf<br />

area and fresh and dry weights <strong>of</strong> leaves were obtained at the plants irrigated every 2 days, while the<br />

lowest values occurred by irrigation at the longest intervals (6 days). Moreover, the differences<br />

between each two successive irrigation intervals were significant. Numerically, plant height and fresh<br />

weights <strong>of</strong> leaves were increased by (29.7 and 49.21%) and by (19.58 and 24.40 %) as a results <strong>of</strong> 2<br />

and 4 irrigation intervals (days), respectively, in comparison with the long interval (6 days). According<br />

to the previous results, El-Monayeri et al (1983) reported that, this may be due to the vital roles <strong>of</strong><br />

water supply at adequate amount for different physiological processes such as photosynthesis,<br />

respiration, transpiration, translocation, enzyme reaction and cells turgidity occurs simultaneously.<br />

Such reduction could be attributed to decrease in the activity <strong>of</strong> meristemic tissues responsible for<br />

elongation. As well as the inhibition photosynthesis efficiency under efficient water condition<br />

Siddique (1999). These results are in agreement with those obtained by Burman et al (1991) on<br />

Azadirachta indica, Soad (2005) on Simmondsia chinensis and Azza et (2006) on Melia azedarach.<br />

145


Table (1) Some growth parameters <strong>of</strong> Helichrysum bracteatum plants as affect with irrigation intervals and foliar application <strong>of</strong> pepton (average <strong>of</strong> two seasons).<br />

Pepton<br />

treatments<br />

(ppm)<br />

Plant height (cm) Number <strong>of</strong> branhes/plant Leaf area (cm2) Fresh weight <strong>of</strong> leaves (g) Dry weight <strong>of</strong> leaves (g)<br />

Irrigation intervals days (A)<br />

2 4 6 Mean 2 4 6 Mean 2 4 6 Mean 2 4 6 Mean 2 4 6 Mean<br />

Control 48.07 43.13 37.83 43.01 20.67 17.33 14.00 17.33 5.26 4.99 3.75 4.67 17.63 14.51 11.87 14.67 3.52 2.9 2.37 2.93<br />

P1 250 57.87 54.77 43.40 52.01 25.33 22.00 21.33 22.89 6.76 6.16 4.7 5.87 19.83 17.66 13.08 16.86 3.96 3.53 2.61 3.37<br />

P2 500 62.83 58.87 47.50 56.40 29.00 24.33 23.00 25.44 7.65 6.58 5.29 6.50 24.04 18.83 15.00 19.29 4.81 3.76 3.00 3.86<br />

P3 1000 68.7 62.10 54.30 61.70 33.33 26.33 26.33 28.66 7.72 6.70 6.18 6.87 25.82 21.80 18.59 22.07 5.16 4.36 3.71 4.41<br />

Mean 59.37 54.72 45.76 27.08 22.50 21.17 6.85 6.11 4.98 21.83 18.20 14.64 4.36 3.64 2.93<br />

LSD 5%<br />

Irrigation<br />

A<br />

1.66<br />

2.29 0.13 0.86<br />

Pepton B 1.84 1.57 0.06 0.86 0.17<br />

Interaction<br />

AB<br />

NS<br />

NS 0.11 1.49<br />

146<br />

0.17<br />

0.30


Concerning the effect <strong>of</strong> peptone on saga growth, data presented in Table (1) revealed that foliar<br />

application <strong>of</strong> peptone significantly promoted plant height, number <strong>of</strong> branches/plant, leaf area and<br />

fresh and dry weight <strong>of</strong> leaves. Increasing peptone concentration from 250 to 500 and 1000 pm to<br />

Helichrysum bracteatum plants significantly increased all growth parameters over control plants. The<br />

increments effect on plant height and number <strong>of</strong> branches/plant by (20.92, 13.13 and 43.00 %) and<br />

32.1, 46.8 and 65.54%), respectively compared with control plants. The positive effect <strong>of</strong> amino acids<br />

on yield may be due to the vital effect <strong>of</strong> these amino acids stimulation on the growth <strong>of</strong> plant cells.<br />

The positive effect <strong>of</strong> amino acids on growth was stated by Goss (1973) who indicated that amino acids<br />

can serve as a source <strong>of</strong> carbon and energy when carbohydrates become defficient in the plant, amino<br />

acids are determinate, releasing the ammonia and organic acid form which the amino acid was<br />

originally formed. The organic acids then enter the Kreb's cycle, to be broken down to release energy<br />

through respiration. Thon et al (1981) pointed out that amino acids provide plant cells with an<br />

immediately available source <strong>of</strong> nitrogen, which generally can be taken by the cells more rapidly than<br />

in organic nitrogen. The results are characteristically accompanied by Youssef et al (2004) on lemon<br />

basil, Gamal El-Din et al (1997) on lemon grass, Talaat Youssef (2002) on basil plant, El-Fawakhry<br />

and El-Tayeb (2003) on chrysanthemum, Refaat and Naguib (1998) on peppermint plant, Youssef et al<br />

(2004) on datura plant and Mona and Talaat (2005) on Pelargonium graveolens plant, the found that<br />

amino acids significantly increased vegetative growth.<br />

The interaction between different factors (irrigation and peptone ) was almost for all vegetative growth<br />

parameters except plant height and number <strong>of</strong> branches/plant. The highest values due to the irrigation<br />

regime and peptone were obtained due to irrigated every 2 days and concentration 1000 ppm <strong>of</strong> foliar<br />

spray <strong>of</strong> pepeton. The lowest sensitivity <strong>of</strong> peptone –sufficient plants to drought stress is related to the<br />

notion that some amino acids (e.g. phenylalanine, ornithine) can affect plant growth and development<br />

through their influence on gibberelline biosynthesis Waller and Nawachi (1978). Amino acids acting<br />

as the building blocks <strong>of</strong> proteins can serve in number <strong>of</strong> additional functions in regulation <strong>of</strong><br />

metabolism, transport and storage nitrogen Bidwell (1979) and Fowden (1973).<br />

Flowering Characters:<br />

Data presented in table (2) show that all decreasing irrigation intervals from 6 to 2 days significantly<br />

increased flower diameter, number <strong>of</strong> flowers/plant and fresh and dry weights <strong>of</strong> flowers. The<br />

increments on fresh and dry weights <strong>of</strong> flowers/plant by 26.93 and 31.02% respectively for the 2 days<br />

compared with 6 days. Our results are computable with those obtained by Ruhi Bastug et al (2006) on<br />

gladiolus plants, Kittas et al (2004) on Rose and Banker et al (2008) on wheat and stated that the high<br />

level <strong>of</strong> irrigation lead to the increment <strong>of</strong> flowering parameters and quality.<br />

Data presented in table (2) show that foliar spray <strong>of</strong> sage plants with pepton at 1000 ppm resulted in the<br />

highest values flowering parameters. The maximum and values were observed for number <strong>of</strong><br />

flowers/plant and fresh and dry weights <strong>of</strong> flowers/plant by 38.45, 38.51 and 38.07 %, respectively<br />

over control plants. These results are characteristically accompanied by Karima and Abd El-Wahed<br />

(2005) who found that using amino acids led to significant increases in number <strong>of</strong> flowers, diameters <strong>of</strong><br />

flower and fresh and dry weights <strong>of</strong> flowers/plant <strong>of</strong> Matricaria chamomilla L. plant. Also, Nahed<br />

and Balbaa (2007) on Saliva fFarincea stated that application <strong>of</strong> tyrosine 100 ppm significant<br />

promotion in all flowering parameters at flowering stage.<br />

Regarding the interaction effects, data in Table (2) show that flowering parameters were significantly<br />

augmented. It is also clear from the obtained data that irrigation interval 2 days combined with foliar<br />

spray <strong>of</strong> sage plants with 1000 ppm peptone resulted in the highest pronounced effects on all flowering<br />

parameters.<br />

Chemical Constituents:<br />

Pigment content<br />

Data in Table (3) recorded that, the content <strong>of</strong> three photosynthetic pigments (Chlorophyll a, b and<br />

carotenoids) were increased by the gradual increasing in irrigation intervals. Accordingly it can be<br />

stated that irrigation every 6 days was the most effective irrigation treatment for promoting the<br />

synthesis and accumulation <strong>of</strong> the three photosynthetic pigments. In harmony with these results were<br />

those obtained by Soad (2005) and Azza et al (2007).<br />

147


The three photosynthetic pigments took similar trend in response to peptone levels. The three<br />

concentrations used <strong>of</strong> peptone 250, 500 and 1000 ppm caused an increase in the contents <strong>of</strong><br />

Chlorophyll a, b and carotenoids in regard to those <strong>of</strong> untreated seedlings. Hussein et al (1992) found<br />

that higher concentration <strong>of</strong> adenine and cytosine increased the photosynthetic pigments <strong>of</strong> datura<br />

plants.<br />

148


Table (2) Flowering parameters <strong>of</strong> Helichrysum bracteatum plants as affect with irrigation intervals and foliar application <strong>of</strong> pepton (average <strong>of</strong> two seasons).<br />

Pepton<br />

treatments<br />

(ppm)<br />

Number <strong>of</strong> flowers/plant Flower diameter (cm) Fresh weight <strong>of</strong> flowers (g) Dry weight <strong>of</strong> flowers (g)<br />

Irrigation intervals days (A)<br />

2 4 6 Mean 2 4 6 Mean 2 4 6 Mean 2 4 6 Mean<br />

Control 11.83 11.30 8.83 10.65 3.23 3.13 2.17 2.84 27.20 25.96 20.32 24.49 8.70 7.79 6.09 7.53<br />

P1 250 15.63 14.23 11.13 13.66 3.32 3.48 2.75 3.18 35.96 32.74 25.61 31.44 11.50 9.82 7.68 9.67<br />

P2 500 16.60 16.00 12.50 15.03 3.76 3.56 2.87 3.40 38.18 36.54 28.75 34.49 12.21 11.06 8.63 10.63<br />

P3 1000 20.50 16.77 14.70 17.32 4.82 3.54 2.91 3.76 47.15 38.53 33.81 39.83 14.78 11.56 10.14 12.16<br />

Mean 16.14 14.58 11.79 3.78 3.43 2.68 37.12 33.44 27.12 11.80 10.06 8.14<br />

LSD 5%<br />

Irrigation<br />

A<br />

0.97 0.05 2.39 0.82<br />

Pepton B 0.51 0.04 1.12 0.39<br />

Interaction<br />

AB<br />

0.89 0.08 1.94 0.67<br />

149


Table (3) Chemical constituents <strong>of</strong> Helichrysum bracteatum plants as affect with irrigation intervals and foliar application <strong>of</strong> pepton (average <strong>of</strong> two seasons).<br />

Pepton<br />

treatments<br />

(ppm)<br />

Chl a (mg/g F.W.) Chl b (mg/g F.W.) Chl a+b (mg/g F.W.) Carotenoids (mg/g F.W.)<br />

Irrigation intervals days<br />

2 4 6 Mean 2 4 6 Mean 2 4 6 Mean 2 4 6 Mean<br />

Control 1.629 2.062 1.921 1.871 0.335 0.667 0.394 0.465 1.964 2.729 2.315 2.336 0.849 0.972 0.972 0.931<br />

P1 250 1.782 2.126 2.372 2.093 0.455 0.935 0.583 0.658 2.237 2.581 2.955 2.591 1.079 1.186 1.027 1.097<br />

P2 500 2.187 2.497 2.858 2.514 0.634 0.983 0.654 0.757 2.821 3.480 3.512 3.271 1.458 1.316 1.425 1.400<br />

P3 1000 1.851 2.444 2.750 2.348 0.524 0.976 0.614 0.705 2.375 3.420 3.364 3.053 1.269 1.634 1.286 1.396<br />

Mean 1.862 2.282 2.475 0.487 0.890 0.561 2.349 3.053 3.037 1.164 1.277 1.178<br />

LSD 5%<br />

Irrigation<br />

A<br />

0.036 0.018 0.054 0.110<br />

Pepton B 0.031 0.010 0.041 0.010<br />

Interactio<br />

n AB<br />

0.054 0.018 0.072 0.018<br />

150


The present data are in agreement with the findings <strong>of</strong> Hussein (2003) on Foeniculum vulgare L. plants<br />

and Nahed and Laila (2007) on Saliva farinacea plants, they reported that foliar application <strong>of</strong> amino<br />

acids (Tryptophan) caused an increase in photosynthetic pigments contents. The accumulation <strong>of</strong><br />

photosynthetic pigments as a result <strong>of</strong> these nitrogen compounds may be due to the important role <strong>of</strong><br />

nitrogen in the biosynthesis <strong>of</strong> Chlorophyll molecules, Meyeret et al (1968).<br />

In this respect, interaction between irrigation intervals and pepton applications, the data revealed that<br />

the combination <strong>of</strong> both factors on Chlorophyll a, b and carotenoids was more effective than the effect<br />

<strong>of</strong> each factors, all the interaction <strong>of</strong> used treatments increased significantly photosynthetic pigments in<br />

the leaves <strong>of</strong> Helichrysum bracteatum plants.<br />

Total soluble sugars content:<br />

Data recorded in Table (4) indicated that total soluble sugars content as affected by different irrigation<br />

intervals treatments, followed the same manner obtained previously on photosynthetic pigments, were<br />

gradually decreased by increasing the intervals <strong>of</strong> irrigation. These results were in accordance with<br />

those recorded by Azza et al (2007).<br />

Pepton at all used concentration caused an increasing in total soluble sugars content as compared with<br />

untreated seedlings. This result could be explained by the findings obtained by Refaat and Naguib<br />

(1998) reported that application <strong>of</strong> all amino acids (alanine, cytosine, guanine, thiamine and L-tyrosine)<br />

increased the total carbohydrates percentage in peppermint leaves. The promotive affected <strong>of</strong> the<br />

amino acids on the total carbohydrates content may be due to their important role on the biosynthesis <strong>of</strong><br />

Chlorophyll molecules which in turn affected carbohydrate content.<br />

As far the interaction between irrigation intervals and peptone applications the higher values were<br />

provided when adding 1000 ppm peptone and irrigation every 4 days.<br />

Total soluble indoles:<br />

According to the data illustrated in Table (4) the total indoles levels which were determined in leaves<br />

<strong>of</strong> Helichrysum bracteatum plants were increased by decreasing irrigation intervals.<br />

Concerning pepton, total indoles levels were decreased by the increase in peptone levels. The highest<br />

values <strong>of</strong> total indoles were obtained from interaction treated plants with peptone at 1000 ppm and<br />

irrigated every 4 days.<br />

151


Table (4) Chemical constituents <strong>of</strong> Helichrysum bracteatum plants as affect with irrigation intervals and foliar application <strong>of</strong> pepton (average <strong>of</strong> two seasons).<br />

Pepton treatments<br />

(ppm)<br />

Total soluble sugars (mg/g F.W.) Total indoles (mg/g F.W.) Total phenoles (mg/g F.W.)<br />

Irrigation intervals days<br />

152<br />

Total free amino acids (mg/g<br />

F.W.)<br />

2 4 6 Mean 2 4 6 Mean 2 4 6 Mean 2 4 6 Mean<br />

Control 0.948 2.245 1.338 1.510 1.225 1.117 1.292 1.211 1.165 1.354 0.908 1.142 0.971 0.685 0.714 0.790<br />

P1 250 1.659 3.143 1.511 2.104 0.816 0.718 0.635 0.723 1.216 1.659 1.510 1.462 1.132 0.835 0.742 0.903<br />

P2 500 1.983 3.459 1.941 2.461 1.184 0.966 0.784 0.978 1.242 1.733 1.535 1.503 1.242 1.027 0.814 1.028<br />

P3 1000 2.045 3.580 2.865 2.830 1.246 0.482 0.813 0.847 1.364 2.506 1.594 1.821 1.375 1.091 0.910 1.125<br />

Mean 1.659 3.107 1.914 1.118 0.821 0.881 1.247 1.813 1.387 1.180 0.910 0.795<br />

LSD 5%<br />

Irrigation<br />

A<br />

0.018 0.009 0.008 0.007<br />

Pepton B 0.013 0.008 0.010 0.008<br />

Interaction<br />

AB<br />

0.022 0.014 0.018 0.013


Total soluble phenols:<br />

The results in Table (4) emphasized that amounts <strong>of</strong> total soluble phenols were significantly increased<br />

by increasing irrigation intervals. These results are in accordance with those obtained by Azza et al<br />

(2006) on Taxodium distichum. Concerning peptone, total soluble phenols levels were increased by<br />

increasing irrigation intervals and peptone concentration the highest values were provided when adding<br />

1000 ppm and interval 4 days.<br />

Total free amino acids:<br />

From the given data in Table (4) it can be concluded that decreasing irrigation intervals caused an<br />

increase <strong>of</strong> total free amino acids content. In regard to the effect <strong>of</strong> water stress on amino acids, it has<br />

been indicated that generally total free amino acids increased under water stress, Simpson (1981). This<br />

trend does not apply to Myoporum since long irrigation interval caused a decrease in amino acids.<br />

However, many investigators reported that an increase in amino acids is associated with water stress,<br />

Farahat (1990) on Schinus molle, Schinus terebinthifolius and Myoporum acuminatum). Data<br />

presented in table (4) show that total free amino was significantly increased as a result <strong>of</strong> foliar spray <strong>of</strong><br />

peptone 500 and 1000 ppm. Our results are in agreement with those obtained by Karima and Abdel-<br />

Wahed (2005) on Chamomile plants, Gamal ElDin et al (1997) on lemon grass, Mona and Iman (2005)<br />

on Pelargonium graveolens L. and Nahed and Balbaa (2007) on Saliva fariacea plants. They reported<br />

that application <strong>of</strong> amino acids significantly increased total amino acids.<br />

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155


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

Permeability and Porosity Prediction from Wireline logs Using Neuro-Fuzzy Technique<br />

Wafaa El-Shahat Afify* and Alaa H. Ibrahim Hassan**<br />

*Lecturer <strong>of</strong> <strong>Applied</strong> Geophysics, Faculty <strong>of</strong> <strong>Science</strong>, Benha University<br />

** Senior Reservoir Geologist (Bab Team)<br />

Abu Dhabi Company for Onshore Oil Operations<br />

*E-mail address for correspondence: w_afify@yahoo.com<br />

____________________________________________________________________________________<br />

Abstract: Petroleum reservoir characterization is a process for quantitatively describing various<br />

reservoir properties in spatial variability using all the available field data. Porosity and permeability are the<br />

two fundamental reservoir properties which relate to the amount <strong>of</strong> fluid contained in a reservoir and its<br />

ability to flow. These properties have a significant impact on petroleum fields operations and reservoir<br />

management. In un-cored intervals and well <strong>of</strong> heterogeneous formation, porosity and permeability<br />

estimation from conventional well logs has a difficult and complex problem to solve by statistical methods.<br />

This paper suggests an intelligent technique using fuzzy logic and neural network to determine reservoir<br />

properties from well logs. Fuzzy curve analysis based on fuzzy logic is used for selecting the best related<br />

well logs with core porosity and permeability data. Neural network is used as a nonlinear regression<br />

method to develop transformation between the selected well logs and core measurements. The technique is<br />

demonstrated with an application to the well data in West July oil field, Gulf <strong>of</strong> Suez, Egypt for the<br />

Miocene Upper Rudeis reservoirs (Asal and Hawara formations). The results show that the technique can<br />

make more accurate and reliable reservoir properties estimation compared with conventional computing<br />

methods. This intelligent technique can be utilized as a powerful tool for reservoir properties estimation<br />

from well logs in oil and natural gas development projects.<br />

____________________________________________________________________________________<br />

INTRODUCTION<br />

Reservoir characterization is a process <strong>of</strong> describing various reservoir characteristics using all the<br />

available data to provide reliable reservoir models for accurate reservoir performance prediction. The<br />

reservoir characteristics include permeability, porosity, pore and grain size distributions, facies distribution,<br />

and depositional environment. The types <strong>of</strong> data needed for describing the characteristics are core data,<br />

well logs, well tests, production data and seismic survey. Such information is essential to the determination<br />

<strong>of</strong> the economic viability <strong>of</strong> a particular well or reservoir to be explored. A large number <strong>of</strong> techniques<br />

have been introduced in order to establish an adequate interpretation model over the past fifty years.<br />

Nevertheless, conventional derivation <strong>of</strong> a well log data analysis model normally falls into one <strong>of</strong> the two<br />

main approaches: empirical and statistical. In the empirical approach, mathematical functions relating the<br />

desired permeability based on several well log data inspired by theoretical concepts are used [Wyllie and<br />

Rose, 1950, Kapadia and Menzie, 1985]. This approach has long been favored in the field and much effort<br />

has been made to understand the underlying petroleum engineering principles. However, the unique<br />

geophysical characteristic <strong>of</strong> each region prevents a single formula from being universally applicable.<br />

Statistical techniques are viewed as more practical approaches [Wendt et al., 1986, and Hawkins, 1994].<br />

The common statistical technique used is multiple regression analysis. The simplest form <strong>of</strong> regression<br />

analysis is to find a relationship between the input logs and the petrophysical properties. The derived<br />

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regression equations are then used for well log analysis. However, a number <strong>of</strong> initial assumptions <strong>of</strong> the<br />

model need to be made. Assumptions must also be made as to the statistical characteristics <strong>of</strong> the log data.<br />

Over the past decade, another technique that has emerged as an option for well log analysis is the Artificial<br />

Neural Network (ANN). Research has shown that an ANN can provide an alternative approach to well log<br />

analysis with improvement over the traditional methods [Osborne, 1992, Wong et al., 1995, Fung and<br />

Wong, 1999]. Most <strong>of</strong> the ANN based well log analysis models have used the Multi-layer Neural Network<br />

(MLNN) utilizing the backpropagation learning algorithm. Such networks are commonly known as<br />

Backpropagation Neural Networks (BPNNs). A BPNN is suited to this application, as it resembles the<br />

characteristics <strong>of</strong> regression analysis in statistical approaches. Fuzzy Logic (FL) that is capable to express<br />

the underlying characteristics <strong>of</strong> a system in human understandable rules is also used. A fuzzy set allows<br />

for the degree <strong>of</strong> membership <strong>of</strong> an item in a set to be any real number between 0 and 1. This allows human<br />

observations, expressions and expertise to be modeled more closely. Once the fuzzy sets have been defined,<br />

it is possible to use them in constructing rules for fuzzy expert systems and in performing fuzzy inference.<br />

This approach seems to be suitable to well log analysis as it allows the incorporation <strong>of</strong> intelligent and<br />

human knowledge to deal with each individual case. However, the extraction <strong>of</strong> fuzzy rules from the data<br />

can be difficult for analysts with little experience. This could be a major drawback for use in well log<br />

analysis. If a fuzzy rule extraction technique is made available, then fuzzy systems can still be used for well<br />

log analysis [Wong et al., 1999 and Kuo et al., 1999]. With the emergence <strong>of</strong> intelligent techniques that<br />

combine ANN and fuzzy together have been applied successfully in well log analysis [Huang et al., 2001,<br />

Kadkhodaie Ilkhchi et al., 2008, Khaxar et al., 2007, Johanyák et al.2007]. These techniques used in<br />

building the well log analysis model normally address the disadvantages encountered in ANN and fuzzy<br />

system. This paper suggests an intelligent technique for reservoir characterization using fuzzy logic and<br />

neural network to determine reservoir properties from well log data for the Miocene Upper Rudeis<br />

reservoirs (Asal and Hawara formations), in West July oil field, Gulf <strong>of</strong> Suez, Egypt, Fig.1.<br />

Back propagation neural networks (BPNN).<br />

A neural network (NN) is an intelligent tool for solving complex problems. A BPNN is a supervised<br />

training technique that sends the input values forward through the network then computes the difference<br />

between calculated output and corresponding desired output from the training dataset. The error is then<br />

propagated backward through the net and the weights are adjusted during a number <strong>of</strong> iterations, named<br />

epochs. The training ceases when the calculated output values best approximate the desired values [Bhatt<br />

and Helle, 2002].A flowchart <strong>of</strong> training procedure in a supervised NN is shown in Fig. 2.<br />

Fuzzy logic (FL).<br />

The basic theory <strong>of</strong> fuzzy sets was first introduced by Zadeh, 1965. In recent years, it has been shown that<br />

uncertainty may be due to fuzziness (possibility) rather than probability. FL is considered to be appropriate<br />

to deal with the nature <strong>of</strong> uncertainty in system and human errors, which were not considered in existing<br />

reliability theories. Generally, geological data are not clear-cut and habitually are associated with<br />

uncertainties. For example, prediction <strong>of</strong> core parameters from well log responses is difficult and is usually<br />

associated with error [Nikravesh and Aminzadeh, 2003].FL derives useful information from this error and<br />

applies it as a powerful parameter for increasing the accuracy <strong>of</strong> the predictions. A fuzzy inference system<br />

(FIS) is a method to formulate inputs to an output using FL [Kadkhodaie Ilkhchi et al., 2006].<br />

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Fig.2. A flow chart <strong>of</strong> training procedure in a supervised<br />

neural network.<br />

Fuzzy modeling technique can be classified into three categories, namely the linguistic (Mamdani-type), the<br />

relational equation, and the Takagi, Sugeno and Kang (TSK). Takagi and Sugeno, 1985, is a FIS in which<br />

output membership functions are constant or linear and are extracted by a clustering process. Each <strong>of</strong> these<br />

clusters refers to a membership function. Each membership function generates a set <strong>of</strong> fuzzy if–then rules<br />

for formulating inputs to outputs. A schematic diagram <strong>of</strong> FIS is shown in Fig.3.<br />

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Neuro-fuzzy (NF) model.<br />

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Hybrid NF systems combine the advantages <strong>of</strong> fuzzy systems (which deal with explicit knowledge) with<br />

those <strong>of</strong> NN (which deal with implicit knowledge). On the other hand, Fuzzy Logic (FL) enhances<br />

generalization capability <strong>of</strong> a Neural Network (NN) system by providing more reliable output when<br />

extrapolation is needed beyond the limits <strong>of</strong> the training data. A schematic diagram <strong>of</strong> information flows in<br />

a NF system is shown in Fig.4. The architecture <strong>of</strong> the Neuro-Fuzzy classifier is slightly different from the<br />

architecture used in function approximations [Tommi, 1994]. The two first layers have the identical<br />

function with the approximation. Fig. 5 shows a system using the following fuzzy rules,<br />

Rule 1: If x1 is A1 and x2 is B1, then class is 1.<br />

Rule 2: If x1 is A2 and x2 is B2, then class is 2.<br />

Rule 3: If x1 is A1 and x2 is B3, then class is 1.<br />

Layer 3. Combination <strong>of</strong> firing strengths: If several fuzzy rules have the same consequence class, this layer<br />

combines their firing strengths. Usually, the maximum connective (or operation) is used.<br />

Layer 4. Fuzzy outputs: In this layer, the fuzzy values <strong>of</strong> the classes are available. The values describe how<br />

well the input <strong>of</strong> the system matches to the classes.<br />

Layer 5. Defuzzification: If the crisp classification is needed, the best-matching class for the input is chosen<br />

as output class.<br />

METHODS AND RESULTS<br />

The data used for permeability and porosity determination are the open-hole wireline subsurface well log<br />

data [gamma ray (GR), sonic (DT), density (ROHB), deep resistivity (RD), Neutron (PHIN) logs, water<br />

saturation (SW)], and core data [core permeability and core porosity]. The work in the present research<br />

proceeds as following;<br />

• Removing erroneous and outliers from the raw well log data.<br />

• Organizing data into input data sets including GR, DT, ROHB, RD, PHIN, SW and<br />

output data sets including core permeability and core porosity.<br />

• Normalization <strong>of</strong> input and output data sets (between the ranges 0-1) to renders the data<br />

dimensionless and removes the effect <strong>of</strong> scaling.<br />

• Dividing the data into: training, checking and testing data sets.<br />

• Clustering the input and output data sets using fuzzy c-means (FCM), fuzzy k-means<br />

(FKM) or subtractive clustering methods.<br />

• Fuzzyfication, which involves the conversion <strong>of</strong> numeric data in real world domain to<br />

fuzzy numbers in fuzzy domain, this takes place by building the fuzzy inference system<br />

FIS, which involves setting the membership functions and establishment <strong>of</strong> fuzzy rules.<br />

• Deffuzzification, which is optional, involves the conversion <strong>of</strong> the derived fuzzy<br />

number to the numeric data in real world domain.<br />

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Fig.3. Schematic diagram <strong>of</strong> FIS<br />

Fig.4. Schematic diagram <strong>of</strong> information flow in a NF system<br />

Fig.5. Neural architecture <strong>of</strong> the NF classifier.<br />

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•Organizing data. The data for the neuro-fuzzy model come from one well SG-3105A at West July oil<br />

field, Gulf <strong>of</strong> Suez, Egypt. The selection <strong>of</strong> this well is based on geological considerations; it contains<br />

reasonably good core coverage <strong>of</strong> the Upper Rudeis Formation. Core-log calibration was carefully carried<br />

out to compensate for differences in depth. Table (1), illustrates the statistics <strong>of</strong> the input and output data<br />

sets used in NF modeling.<br />

•Normalizing data. When processing the actual materials, due to the different dimensions <strong>of</strong> the source<br />

rocks evaluation parameter, the volume level <strong>of</strong> actual data vary considerably. If we calculate by using the<br />

raw data directly, the indicating role <strong>of</strong> the data which has a larger volume would become more<br />

outstanding. While the indicator with a lower volume and a higher sensitivity will be underestimated. Thus,<br />

we should preprocess and normalize the raw data. In this work normalizing data takes place by using the<br />

maximum and minimum values <strong>of</strong> the data.<br />

•Fuzzy clustering. It is necessary to classify the input and output datasets into groups using clustering<br />

methods. In this study, a subtractive clustering method, which is a useful and effective way to FL modeling,<br />

is used for extraction <strong>of</strong> clusters and fuzzy if–then rules. The details <strong>of</strong> subtractive clustering could be<br />

found in Chiu [1994], Chen and Wang [1999], Jarrah and Halawani [2001].The important parameter in<br />

subtractive clustering which controls number <strong>of</strong> clusters and fuzzy if–then rules is clustering radius. This<br />

parameter could take values between the range <strong>of</strong> [0, 1]. Specifying a smaller cluster (say 0.1) radius will<br />

usually yield more and smaller clusters in the data resulting in more rules. In contrast, a large cluster radius<br />

(say 0.9) yields a few large clusters in the data resulting in few rules.<br />

The effectiveness <strong>of</strong> a fuzzy model is related to the search for an optimal clustering radius, which is a<br />

controlling parameter for determining the number <strong>of</strong> fuzzy if–then rules. Few rules could not cover the<br />

entire domains, and more rules will complicate the system behavior and may lead to low performance <strong>of</strong><br />

the model. Regarding the permeability model, four centers result from clustering, thus the fuzzy model was<br />

established by four fuzzy if-then rules and four membership functions for input and output data. Porosity<br />

model, on the other hand, contains five centers (clusters), five rules and five membership functions. Figures<br />

6 and 7 shows the subtractive clusters <strong>of</strong> permeability and porosity data.<br />

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•Building the fuzzy inference system FIS. Fuzzy inference is the process <strong>of</strong> formulating the mapping from<br />

a given input to an output using fuzzy logic. The mapping then provides a basis from which decisions can<br />

be made, or patterns discerned. The process <strong>of</strong> fuzzy inference involves setting the membership functions<br />

and establishment <strong>of</strong> fuzzy rules, [Matlab fuzzy logic user’s guide, and 2009].<br />

1- Setting the Membership Functions (MF). A membership function (MF) is a curve that defines how each<br />

point in the input space is mapped to a membership value (or degree <strong>of</strong> membership) between 0 and 1. The<br />

input space is sometimes referred to as the universe <strong>of</strong> discourse, a fancy name for a simple concept. The<br />

only condition a membership function must really satisfy is that it must vary between 0 and 1. The function<br />

itself can be an arbitrary curve whose shape we can define as a function that suits us from the point <strong>of</strong> view<br />

<strong>of</strong> simplicity, convenience, speed, and efficiency. There are many types <strong>of</strong> membership functions built<br />

from several basic functions:<br />

• Piece-wise linear functions<br />

• The Gaussian distribution function<br />

• The sigmoid curve<br />

• Quadratic and cubic polynomial curves<br />

In this study, a Gaussian distribution membership function is used to define the extracted input clusters. A<br />

Gaussian function f (x) shows the normal distribution <strong>of</strong> data (x):<br />

e<br />

f ( X ) �<br />

�<br />

�(<br />

x��<br />

)<br />

2 /<br />

�<br />

2�<br />

2<br />

Where µ and σ are the parameters <strong>of</strong> normal distribution showing the mean and standard deviation <strong>of</strong> data,<br />

respectively. These Gaussian membership functions are constructed from mean and σ values <strong>of</strong> the clusters.<br />

The mean represents the cluster centers and σ is derived from:<br />

σ = (radii � (maximum data – minimum data))/sqrt. The input parameters <strong>of</strong> Gaussian membership<br />

function for permeability and porosity are shown in tables 2A and 3A.<br />

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In the FIS, output membership functions are linear equations constructed from inputs. For example, output<br />

membership function number one (MF1), which is the consequent <strong>of</strong> rule no. 1, is constructed from six<br />

petrophysical inputs as following:<br />

Output MF1 = C1 � GR � C2<br />

� DT � C3<br />

� ROHB � C4<br />

� RD � C5<br />

� PHIN � C6<br />

� SW � C7<br />

In this equation, parameters C 1 , C2,<br />

C3,<br />

C4,<br />

C5<br />

and C 6 are coefficients corresponding to GR, DT,<br />

ROHB, RD, PHIN and SW inputs, respectively. Parameter C 7 is constant in each equation. These<br />

parameters are obtained by linear least-squares estimation. With these explanations there will be seven<br />

parameters for each output membership function, which are shown in tables 2B and 3B for permeability<br />

and porosity, respectively. Figures 8 and 9 represent the FIS generated Gaussian membership<br />

functions <strong>of</strong> input data for permeability and porosity model, respectively.<br />

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Moreover, Figure 10 A shows the FIS model generated for permeability and porosity, (Fig.10B).<br />

2- Establishment <strong>of</strong> fuzzy rules. Fuzzy rule statements are used to formulate the conditional statements that<br />

comprise fuzzy logic. A single fuzzy if-then rule assumes the form if x is A then y is B where A and B are<br />

linguistic values defined by fuzzy sets on the ranges (universes <strong>of</strong> discourse) X and Y, respectively. The ifpart<br />

<strong>of</strong> the rule “x is A” is called the antecedent or premise, while the then-part <strong>of</strong> the rule “y is B” is called<br />

the consequent or conclusion.<br />

The generated fuzzy if-then rules for formulating input petrophysical data to permeability are:<br />

1. If (GR is in1mf1) and (DT is in2mf1) and (ROHB is in3mf1) and (RD is in4mf1) and (PHIN is in5mf1)<br />

and (SW is in6mf1) then (K is out1mf1).<br />

2. If (GR is in1mf2) and (DT is in2mf2) and (ROHB is in3mf2) and (RD is in4mf2) and (PHIN is in5mf2)<br />

and (SW is in6mf2) then (K is out1mf2).<br />

3. If (GR is in1mf3) and (DT is in2mf3) and (ROHB is in3mf3) and (RD is in4mf3) and (PHIN is in5mf3)<br />

and (SW is in6mf3) then (K is out1mf3).<br />

4. If (GR is in1mf4) and (DT is in2mf4) and (ROHB is in3mf4) and (RD is in4mf4) and (PHIN is in5mf4)<br />

and (SW is in6mf4) then (K is out1mf4).<br />

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The generated fuzzy if-then rules for formulating input petrophysical data to porosity are:<br />

1. If (GR is in1mf1) and (DT is in2mf1) and (ROHB is in3mf1) and (RD is in4mf1) and (PHIN is in5mf1)<br />

and (SW is in6mf1) then (PHI is out1mf1).<br />

2. If (GR is in1mf2) and (DT is in2mf2) and (ROHB is in3mf2) and (RD is in4mf2) and (PHIN is in5mf2)<br />

and (SW is in6mf2) then (PHI is out1mf2).<br />

3. If (GR is in1mf3) and (DT is in2mf3) and (ROHB is in3mf3) and (RD is<br />

in4mf3) and (PHIN is in5mf3) and (SW is in6mf3) then (PHI is out1mf3).<br />

4. If (GR is in1mf4) and (DT is in2mf4) and (ROHB is in3mf4) and (RD is in4mf4) and (PHIN is in5mf4)<br />

and (SW is in6mf4) then (PHI is out1mf4).<br />

5. If (GR is in1mf5) and (DT is in2mf5) and (ROHB is in3mf5) and (RD is in4mf5) and (PHIN is in5mf5)<br />

and (SW is in6mf5) then (PHI is out1mf5).<br />

A graphical illustration showing steps to formulation <strong>of</strong> petrophysical data inputs to permeability using four<br />

fuzzy if–then rules generated by FIS, is represented in Fig.11. The formulation <strong>of</strong> petrophysical data to<br />

porosity using five fuzzy if-then rules generated by FIS are shown in Fig. 12. Each figure displays a<br />

roadmap <strong>of</strong> the whole fuzzy inference process. The seven plots across the top <strong>of</strong> the figure represent the<br />

antecedent and consequent <strong>of</strong> the first rule. Each rule is a row <strong>of</strong> plots, and each column is a variable. The<br />

rule numbers are displayed on the left <strong>of</strong> each row.<br />

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The structure <strong>of</strong> the NF model is now generated for permeability (Fig.13A) and porosity (Fig.13B). The<br />

input is represented by the left-most node and the output by the right-most node. The node represents a<br />

normalization factor for the rules.<br />

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DISCUSSION<br />

The NF technique is used to determine the porosity and permeability <strong>of</strong> the Upper Rudeis Formation using<br />

the available well data, as well as core permeability and core porosity data, (Fig. 14). The Upper Rudeis<br />

sand is the third most important reservoir in July oil field. The sand was supplied by fans draining the Red<br />

Sea hills to the west <strong>of</strong> July field and deposited in a similar environment to the Lower Rudeis Formation,<br />

Pivnik et al., (2003).<br />

A total <strong>of</strong> 108 data points are used for training, 108 data points are used for checking and 60 data points are<br />

used for testing the NF models <strong>of</strong> the permeability and porosity. The FIS is trained using the training data<br />

set then checked and tested using checking data sets and testing data sets respectively. The testing data set<br />

is used to check the generalization capability <strong>of</strong> the resulting fuzzy inference system. The idea behind using<br />

a checking data set for model validation is that after a certain point in the training, the model begins over<br />

fitting the training data set. In principle, the model error for the checking data set tends to decrease as the<br />

training takes place up to the point that over fitting begins, and then the model error for the checking data<br />

suddenly increases. Over fitting is accounted for by testing the FIS trained on the training data against the<br />

checking data. Usually, these training and checking data sets are collected based on observations <strong>of</strong> the<br />

target system and are then stored in separate files.<br />

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Figure 15 shows the checking and the FIS output. On the other hand, Fig.16. shows testing data and FIS<br />

output. The performance <strong>of</strong> the model is evaluated by the MSE <strong>of</strong> the data sets, as illustrated in Fig.17. and<br />

table (4). The correlation coefficient between the measured and NF predicted K and PHI are 0.825 and<br />

0.957, respectively. A comparison between measured and NF predicted K and PHI versus depth is shown in<br />

Figs. 18 and 19.<br />

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CONCLUSIONS<br />

In this study, the NF intelligent technique is used to estimate reservoir porosity and permeability from<br />

conventional well logs. Fuzzy curve analysis based on fuzzy logic can be used for selecting the<br />

best related parameters with reservoir properties. The NF modeling approach presented in this paper has<br />

been successfully applied for the prediction <strong>of</strong> petrophysical reservoir parameters. This modeling approach<br />

has the significant advantage in that it does not require any previous assumption based on physical or<br />

experimental considerations about the reservoir complexities to construct a reasonable and accurate model<br />

from a set <strong>of</strong> measured data. Excellent correlation coefficients have been obtained for porosity 0.957, and<br />

permeability 0.825, using NF models. The techniques can make more accurate and reliable reservoir<br />

properties estimation and can be utilized a powerful tool for reservoir properties determination from well<br />

logs in petroleum industry, and is applicable in different wells and oil fields.<br />

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ACKNOWLEDGEMENTS<br />

The authors would like to express their gratitude for the Gulf Of Suez Petroleum Company, (GUPCO),<br />

Egypt for supplying the data needed for this work.<br />

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Kadkhodaie Ilkhchi, A., Hossain Rahimpour-Bonab, and Rezaee, M.R., 2008. A committee machine with<br />

intelligent systems for estimation <strong>of</strong> total organic carbon content from petrophysical data: An<br />

example from Kangan and Dalan reservoirs in South Pars Gas Field, Iran <strong>Journal</strong> <strong>of</strong> Computers<br />

and Geosciences, doi:10.1016/j.cageo.2007.12.007<br />

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Egypt, AAPG Bulletin, v. 87, pp. 1015-1030.<br />

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174


Figure 1 - Location map <strong>of</strong> July Oil Field.<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

FIGURES CAPTION<br />

Figure 2 - A flow chart <strong>of</strong> training procedure in a supervised neural network.<br />

Figure 3 - Schematic diagram <strong>of</strong> FIS.<br />

Figure 4 - Schematic diagram <strong>of</strong> information flow in a NF system.<br />

Figure 5 - Neural architecture <strong>of</strong> the NF classifier.<br />

Figure 6 - Subtractive clustering <strong>of</strong> permeability fuzzy model.<br />

Figure 7 - Subtractive clustering <strong>of</strong> porosity fuzzy model.<br />

Figure 8 - Generated Gaussian membership functions for permeability model input data.<br />

Figure 9 - Generated Gaussian membership functions for porosity model input data.<br />

Figure 10 - Diagrams showing formulation <strong>of</strong> input petrophysical data to: (A)<br />

permeability, K and (B) porosity, PHI using fuzzy modeling.<br />

Figure 11 – Rule viewer <strong>of</strong> FIS permeability model.<br />

Figure 12 - Rule viewer <strong>of</strong> FIS porosity model.<br />

Figure 13 - Structure <strong>of</strong> Neuro-Fuzzy model for permeability (A) and porosity (B).<br />

Figure 14 - Petrophysical and core data <strong>of</strong> SG-310-5A well.<br />

Figure 15 - Showing checking data and FIS output, permeability (A) and porosity (B).<br />

Figure 16 - Showing testing data and FIS output, permeability (A) and porosity (B).<br />

Figure 17 - Mean square error (MSE) obtained during training the permeability<br />

model (A) and the porosity model (B).<br />

Figure 18 - Predicted and core permeability.<br />

Figure 19 - Predicted and core porosity.<br />

TABLES CAPTION<br />

Table1 - Statistics <strong>of</strong> input and output data sets.<br />

Table 2 - Showing input (a) and output (b) membership functions parameters derived by<br />

FIS for permeability.<br />

Table 3 - Showing input (a) and output (b) membership functions parameters derived by<br />

FIS for porosity.<br />

Table 4 - MSE <strong>of</strong> the different datasets.<br />

175


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

Response <strong>of</strong> vegetative growth and chemical constituents <strong>of</strong> Schefflera<br />

arboricola L. plant to foliar application <strong>of</strong> inorganic fertilizer (grow-more)<br />

and ammonium nitrate at Nubaria.<br />

Mona, H. Mahgoub *, El-Quesni, Fatma E.M., and Magda,M. Kandil<br />

Department <strong>of</strong> Ornamental plant and Woody trees,<br />

National Research Centre, Dokki, Cairo, Egypt<br />

*E-mail address for correspondence: azza856@yahoo.com<br />

________________________________________________________________________________<br />

Abstract: A pot experiment was carried out during 2007 and 2008 seasons at Research and Production<br />

Station, Nubaria <strong>of</strong> National Research Centre, Dokki, Cairo, Egypt to study the response <strong>of</strong> Schefflera<br />

plants to foliar fertilizer (Grow-more at the rates <strong>of</strong> 0.0, 1.0 cm 3 /L and 2.0 cm 3 /L) and ammonium<br />

nitrate at the rate <strong>of</strong> (0, 100 and 200 kg) and their interaction on vegetative growth expressed as plant<br />

height, stem diameter, number <strong>of</strong> leaves, leaf area, fresh and dry weight <strong>of</strong> (leaves, roots and stem) and<br />

chemical composition significantly affected by application <strong>of</strong> the two factors which were used in this<br />

study.Grow-more and nitrogen fertilizer promoted all morphological characters, photosynthetic<br />

pigments, protein %, nitrogen, phosphorus and potassium.,<br />

Keywords: Schefflera arboricola,Grow-more,ammonium nitrate<br />

__________________________________________________________________________________<br />

INTRODUCTION<br />

Schefflera arboricola L. is flowering plant in the family araliaceae, native to Tiwan and Hainan. It is<br />

also goes by the common name "Dwarf umbrella tree". It is an evergreen shrub growing to 3-4 m<br />

height, <strong>of</strong>ten trailing stems scrambing over other vegetation. The leaves are palmately compound, with<br />

7-9 leaflets, the leaflets 9-20 cm long and 4-10 cm broad (though <strong>of</strong>ten smaller in cultivation). The<br />

flowers are produced in a 20 cm pancil <strong>of</strong> small umbels, each umbel 7-10 mm diameter with 5-10<br />

flowers.<br />

It is commonly grown as houseplant, popular for its tolerance <strong>of</strong> neglect and poor growing condition.<br />

Numerous cultivars have been selected for variation in leaf colour and pattern, <strong>of</strong>ten variegated with<br />

creamy-white to yellow edges or centers, and dwarf forms. Scheffleras are delicate tropical plants<br />

<strong>of</strong>ten used to decorate public places, such as lobbies, shopping malls and waiting rooms. Smaller<br />

Scheffleras are better studied for homes and small <strong>of</strong>fices. Uph<strong>of</strong>(1959). Inorganic fertilizers are the<br />

elements needed in small amounts, they are <strong>of</strong>ten refers to as micronutrients (Kohnke 1995) these<br />

elements are chlorine (Cl), Iron (Fe), Manganese (Mg), Boron (B), Copper (Cu), Zinc (Zn),<br />

Molybdenum (Mo), Nickel (Ni) and Cobalt (Co) most <strong>of</strong> these elements are derived from the soil and<br />

organic sources (Brady and Weil 2000). Micronutrients are also essential for organization and rapid<br />

alternation <strong>of</strong> nutrition compound within plant owing to their great importance in contribution to direct<br />

the enzymes way in metabolism Massoud et al (2005). Therefore, both granular and fluid (liquid) NPK<br />

fertilizers are commonly used as carriers <strong>of</strong> micronutrients including micronutrients with mixed<br />

fertilizer which is a convenient method <strong>of</strong> application and allows more uniform distribution with<br />

conventional application equipment. Micronutrients are essential for plant growth, but are required in<br />

much smaller amounts than those <strong>of</strong> the primary nutrients Brady and Weil (2000).<br />

Nitrate and ammonium are the major source <strong>of</strong> inorganic nitrogen taken up by the roots <strong>of</strong> higher<br />

plants. Most <strong>of</strong> ammonium has to be incorporated into organic compounds in the roots whereas nitrate<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

is readily mobile in the xylem and can also be stored in the vacules <strong>of</strong> roots, shoots and storage organs.<br />

Nitrate accumulation can be considerable importance for cation-anion balance, for osmoregulation,<br />

particularly in so-called nitrophilie species such as Chenopodium album and Urtica dioica (Smirn<strong>of</strong>f<br />

and Stewart, 1985). Dahiya et al (2001) mentioned that further increments in nitrogen level, up to 180<br />

ppm, adversely affected growth and dry matter yield <strong>of</strong> tuberose. While Pal and Biswas (2000) found<br />

that the lower doses <strong>of</strong> fertilizer produced poor quality plant and yield <strong>of</strong> flower and best results were<br />

found when tuberose were fertilized N, P and K at the level <strong>of</strong> 15, 15, 20 g/m 2 , respectively. Also<br />

Paradhan et al (2004) noticed that combined application <strong>of</strong> N at 40 g/m 2 and K at 30 g/m 2 gave the<br />

highest values <strong>of</strong> plant height, number <strong>of</strong> leaves /plant, leaf area, spike length and number <strong>of</strong><br />

flowers/spike. Mahgoub et al (2006) studied the effect <strong>of</strong> the nitrogen levels 30, 40, 50 and 60 g/m 2 as<br />

ammonium nitrate (33.5 % N) and the level <strong>of</strong> 25, 30, 35 and 40 g/m 2 as potassium sulfate (48 % K2O).<br />

They found that Iris bulbs showed higher values for plant height, fresh and dry weight <strong>of</strong> leaves (40 g<br />

N + 30 g K /m 2 ) N level up to 60 g/m 2 showed stimulatory effect on chlorophyll a, b and carotenoids,<br />

60 g N/m 2 increased carbohydrate percentage in the presence <strong>of</strong> 30 g /m 2 K, (40 g N/m 2 + 25 g K /m 2 )<br />

recorded high values <strong>of</strong> N, P and K in Iris leaves.<br />

The aim <strong>of</strong> this work is to study the response <strong>of</strong> Schefflera arboricola plants to foliar fertilizer <strong>of</strong><br />

Grow-more and nitrogen fertilizer and their interactions on growth and some chemical composition.<br />

MATERIALS AND METHODS<br />

The experiments was conducted at Research and Production Station <strong>of</strong> National Research Centre at<br />

Nubaria during two successive seasons 2007 and 2008 to investigate the response <strong>of</strong> Schefflera<br />

arboricola plant to foliar fertilizer micro nutrients and nitrogen fertilizer (ammonium nitrate 33.5 %)<br />

on growth and some chemical composition. On the third week <strong>of</strong> February 2007 and 2008 seasons,<br />

vegetative uniform cutting (20-24 cm length) were taken from Schefflera arboricola plant, cutting<br />

were treated for a minute with 1000 mg/L indole butric acid before planting in pots to enhance rooting.<br />

Rooted cuttings were planted in black plastic pots (10 cm) in diameter (one plant /pot) and grown in<br />

shaded green house media formulated by combination <strong>of</strong> peatmoss and sandy soil (1:1, v/v). The<br />

seedling were transplanted on 20 th April 2007 and 2008 seasons, in plastic pot (30 cm) in diameter<br />

filled with 10 kg <strong>of</strong> peatmoss and sandy soil (1:1, v/v) arranged in a complete randomized design with<br />

three replicates. Each replicate consists <strong>of</strong> three plants. Water requirements were relative humidity<br />

maintained between 45-65%, allow the surface <strong>of</strong> potting media to dry slightly before irrigation. Each<br />

pot was fertilized twice with 1.5 g nitrogen as ammonium nitrate (33.5% N) and 1.0 g potassium<br />

sulphate (48.5 % K2O). The fertilizers were applied at 30 and 60 days after transplanting. Phosphorus<br />

as calcium superphosphate (15.5 % P2O5) was mixed with soil before transplanting at a rate <strong>of</strong> 3.0 g/<br />

pot. Other agricultural processes were performed according to normal practice. Plants were sprayed<br />

with different concentration <strong>of</strong> foliar fertilizer (Gropw-more) Table (1) which produced by Ajemco<br />

International company at the rate <strong>of</strong> (0.0, 1.0 and 2.0 cm 3 /L). Nitrogen as ammonium nitrate was<br />

fertilized with (0, 100 and 200 kg), interaction <strong>of</strong> the two factors had been also carried out, in addition<br />

to untreated plants (control) which were sprayed with tap water. Foliar application <strong>of</strong> Grow-more and<br />

nitrogen was carried out two times <strong>of</strong> 30 days intervals starting at 20 July at both seasons. The<br />

experiments were sat in completely Randomized Design (CRD) with three replicates and two factors.<br />

The following data were recorded on 1 st week <strong>of</strong> December 2007 and 2008 season, the recorded data<br />

were plant height (cm), stem diameter (mm), No. <strong>of</strong> leaves, leaf area (cm 2 ) <strong>of</strong> 4 and 5 base leaves, fresh<br />

and dry weight <strong>of</strong> plant organs (gm). Photosynthetic pigments i.e. chlorophyll (a, b and carotenoids)<br />

were determined exactly 0.1 gm <strong>of</strong> fresh leaves <strong>of</strong> schefflera plant using the Spectrophotometric<br />

method developments by Metzzner et al (1965). Total nitrogen was determined by Chapman and Pratt<br />

(1961), while phosphorus determination carried out Colorimtrically according to King (1951). Potassium<br />

was determined photometrically by flam photometer method as described by Brown and Lillan (1946).<br />

Data obtained were subjected to standard analysis <strong>of</strong> variance procedure, the values <strong>of</strong> LSD were<br />

obtained whenever F value were significantly as 5% levels reported by Snedecor and Cochran (1980).<br />

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Growth characters:<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

RESULTS AND DISCUSSION<br />

Data in Table (2) show that foliar application <strong>of</strong> Grow-more at the concentration <strong>of</strong> 1.0 and 2.0 cm 3 /L<br />

on schefflera plants significantly increased all growth parameters plant height (cm), No. <strong>of</strong> leaves, fresh<br />

and dry weight <strong>of</strong> plant organs (gm), root and stem (gm), stem diameter and leaf area (cm 2 ) than the<br />

untreated plants, the highest values <strong>of</strong> previous characters were found when plants treated with 2.0<br />

cm3/L <strong>of</strong> grow-more followed by 1.0 cm 3 /L. These results are agreement with El-Fouly (2001) who<br />

noticed that the number <strong>of</strong> leaves and leaf area <strong>of</strong> sunflower plants were increased by addition <strong>of</strong> Fe,<br />

Mn, Zn, root size was increased by addition <strong>of</strong> Fe and Mn only. Rabie et al (2002) reported that foliar<br />

fertilizer containing N, P, K, Fe, Mn and Zn pronounced increases in dry weight, macro and<br />

micronutrients content <strong>of</strong> sorghum plants than control plants. Negm and Zahran (2001) found that,<br />

foliar application <strong>of</strong> micronutrients had the significant effect on increasing wheat grain and straw<br />

yields; yield attributes (plant height, spike length and 1000 grains weight). El -Quesni et al (2009)<br />

mentioned that using inorganic fertilizers at the concentrations <strong>of</strong> 1.0 and 2.0 cm 3 /L on syngonium<br />

plants increased plant height, stem diameter, No. <strong>of</strong> leaves/plant, leaf area and fresh and dry weight <strong>of</strong><br />

roots and leaves. These results may be due to micronutrient boron which helps transport vital sugars<br />

through plant membranes and promotes proper cell division, cell wall formation and development, also<br />

due to zinc which promotes seed/grain formation, plant maturity, acts as enzyme activator in protein,<br />

hormone (i.e. IAA) and RNA / DNA synthesis and metabolism. Chlorine also indirectly affects plant<br />

growth by stomatal regulation <strong>of</strong> water loss. Molybdenum has a significant effect on pollen formation,<br />

so fruit and grain formation are affected by molybdenum –deficient plants.<br />

With regard to the effect <strong>of</strong> nitrogen fertilizer on schefflera plants data in Table (2) illustrated that<br />

using nitrogen fertilizer at the rate <strong>of</strong> 100 kg gave significant increases than control plants. 200 kg<br />

nitrogen gave the highest values in all growth parameters under study compared with control plants.<br />

These results are in agreement with Ramesh et al (2002) they mentioned that plant height increased<br />

with increasing the rate <strong>of</strong> nitrogen. In this respect, Paradahan et al (2004) on gladiolus c.v. red<br />

mention that 4 g/m2 N plus K fertilizer at the rate <strong>of</strong> 30 g/m2 recorded highest value <strong>of</strong> number, fresh<br />

and dry weight <strong>of</strong> leaves as plant height . As regarding the interaction treatments, foliar application<br />

micronutrients and nitrogen fertilizer, the data show that significantly increased all growth characters<br />

under study. The highest values <strong>of</strong> growth characters were obtained by grow-more 2.0 cm 3 /L<br />

combined with ammonium nitrate at the rate <strong>of</strong> 200 kg /fed followed by grow-more 2.0 cm3/L and N at<br />

the rate <strong>of</strong> 200 kg/fed.<br />

Data emphasized the interaction effect were significantly affected all growth parameters i.e. plant<br />

height (cm), number <strong>of</strong> leaves, fresh and dry weight <strong>of</strong> (leaves, root and stem) stem diameter and leaf<br />

area <strong>of</strong> schefflera arboricola L. plants. These results may be due to increasing the nitrogen levels<br />

which delays senescence and stimulates growth and also changes plant morphology, particularly if the<br />

nitrogen availably is high in the rooting medium during the early growth (Levin et al, 1989; Olsthoorn<br />

et al 1991), it presumably related to nitrogen induced changes in the phytohormone balance (Sommer<br />

and Six 1982).<br />

Chemical constituents:<br />

Synthetic Pigments:<br />

Data in Table (3) indicated that spraying schefflera plants with grow-more at the rate <strong>of</strong> 1.0 cm3/L<br />

increasing significantly in chl. a, b and total chlorophyll and decreased in total carotenoids content<br />

whereas 2.0 cm3/L gave the highest values in the content <strong>of</strong> plants from Chl. a, Chl. b, total<br />

Chlorophyll and total carotenoids content. These results were agreement with those obtained by<br />

Ratanarat et al (1990), El-Quesni et al (2009) they found that the highest values <strong>of</strong> Chl. a, Chl. b and<br />

total carotenoids in syngonium plants increases by increasing the concentration <strong>of</strong> grow-more up to 2.0<br />

cm3/L. These results may be due to iron, manganese, which promote chlorophyll production and<br />

photosynthesis process, copper which helps in chlorophyll formation. With regard to the effect <strong>of</strong><br />

nitrogen fertilizer on schefflera plants data in Table (3) showed that the two used concentration <strong>of</strong> N<br />

fertilizer increasing Chl. a, b and total Chlorophyll whereas total carotenoids content gave significant<br />

increased by using 200 kg N only. These results are agreement with Mahgoub et al (2006) on Iris<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

bulbs they mentioned that maximizing the rate <strong>of</strong> N up to 60 g/m2 showed the stimulatory effect on<br />

chlorophyll a, b and carotenoids irrespective <strong>of</strong> the K fertilizer level.<br />

Concerning the effect <strong>of</strong> interaction on photosynthetic pigments data show that the highest significant<br />

values was found in plant treated with 2.0 cm2/L grow-more fertilizer plus 200 kg nitrogen fertilizer<br />

followed by 2.0 cm3/L micronutrients and 100 N , respectively. These treatments may be due to<br />

positive effect on growth parameters.<br />

Mineral Ions content:<br />

Data in Table (3) found that foliar application <strong>of</strong> grow-more at the concentration <strong>of</strong> 1.0 and 2.0 cm 3 /L<br />

and nitrogen fertilizer at the rate <strong>of</strong> 100 and 200 kg increased the total amount <strong>of</strong> nitrogen, phosphorus<br />

and potassium ions content on schefflera plants compared with control plants. These results were<br />

agreement with those obtained by Sharma et al (2002) they found that application <strong>of</strong> organic material<br />

either alone or in combination with chemical fertilizers caused substantial increase in total N, available<br />

P, K as well as increased wheat and straw yield Mahgoub et al(2006) on Iris bulbs they found that<br />

using 40 g/m2 N plus 25 g/m 2 K recorded high values <strong>of</strong> N, P and K in Iris leaves. With regard the<br />

effect <strong>of</strong> interaction in mineral ions content data show that significantly increased N, P and K content<br />

<strong>of</strong> schefflera plants were obtained by grow-more 2 cm 3 /L combined with 200 kg N followed by grow<br />

more 2 cm 3 /L.<br />

Data in Table (3) mentioned that total protein percentage increased by (6.46 and 10.53) when plants<br />

treated with 1.0 and 2.0 cm 2 /L grow-more respectively compared with control plants which recorded<br />

(8.68 %). Also nitrogen fertilizer 100 and 200 kg treatments in the total protein increased by (9.68 and<br />

10.09 %) respectively than control plants (8.90 %).<br />

The highest recorded data in total protein percentage were (11.21, 10.69 and 10.19) obtained from 2<br />

cm 3 /L micronutrients plus 200 kg nitrogen fertilizer followed by 2 cm 3 /L and 200 kg N respectively.<br />

These results are in line with those obtained by Negm and Zahran (2001) they mentioned that<br />

micronutrients increased protein grain content in wheat plants and El-Quesni et al (2009) on<br />

syngonium plants. These increments led to positive effect <strong>of</strong> growth parameters and enhancing effect<br />

on plant metabolism which was regarded as a better indicator for foliage plants.<br />

Table (1) Chemical properties <strong>of</strong> micronutrients fertilizer grow-more used in this study.<br />

Growmore<br />

content<br />

N2 P2O5 K2O Fe Zn Mg Ca Cu S B Mo<br />

% 11 6 8 0.15 0.15 0.14 0.02 0.20 0.02 0.01 0.01<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table (2) Effect <strong>of</strong> micronutrient and nitrogen fertilizer on vegetative growth <strong>of</strong> schefflera arboricola<br />

L. plants. (means <strong>of</strong> two seasons 2007 and 2008).<br />

Character<br />

Treatments<br />

Effect <strong>of</strong> micronutrient<br />

Plant<br />

height<br />

Stem<br />

diam<br />

eter<br />

Control 37.61 1.21<br />

Micro 1 cm 3 /L 33.84 1.24<br />

Micro 2 cm 3 /L 42.97 1.46<br />

No.o<br />

f<br />

leave<br />

s<br />

181<br />

Leaf<br />

area<br />

F.W<br />

<strong>of</strong><br />

root<br />

D.W<br />

<strong>of</strong><br />

root<br />

F.W<br />

<strong>of</strong><br />

leave<br />

s<br />

cm mm cm 2 gm<br />

18.6<br />

2<br />

19.9<br />

0<br />

22.2<br />

7<br />

8.87<br />

9.56<br />

11.6<br />

6<br />

39.6<br />

2<br />

41.4<br />

0<br />

45.0<br />

8<br />

17.5<br />

3<br />

36.6<br />

7<br />

41.3<br />

7<br />

75.6<br />

8<br />

76.9<br />

2<br />

84.6<br />

3<br />

D.W<br />

<strong>of</strong><br />

leave<br />

s<br />

26.6<br />

6<br />

26.9<br />

3<br />

29.8<br />

8<br />

F.W<br />

<strong>of</strong><br />

stem<br />

35.7<br />

6<br />

36.6<br />

7<br />

41.3<br />

7<br />

LSD at 5% level 1.41 0.07 1.58 1.54 1.41 2.09 3.69 1.88 2.09 1.48<br />

Effect <strong>of</strong> nitrogen<br />

Control 39.91 1.23<br />

N 100 kg 39.36 1.25<br />

N 200 kg 41.10 1.42<br />

19.8<br />

6<br />

19.5<br />

0<br />

21.4<br />

2<br />

9.10<br />

9.80<br />

11.1<br />

8<br />

41.2<br />

2<br />

41.7<br />

9<br />

43.0<br />

9<br />

18.0<br />

5<br />

19.2<br />

0<br />

20.3<br />

8<br />

77.0<br />

3<br />

78.0<br />

6<br />

82.1<br />

4<br />

26.2<br />

0<br />

27.0<br />

5<br />

29.2<br />

1<br />

30.9<br />

1<br />

37.4<br />

0<br />

39.5<br />

0<br />

LSD at 5% level 1.41 0.07 1.58 1.54 1.40 1.70 3.69 1.88 2.09 1.48<br />

Effect <strong>of</strong> interaction<br />

Control 32.00 1.11<br />

Micro 1 cm 3 /L 41.38 1.28<br />

Micro 2 cm 3 /L 43.34 1.32<br />

N 100 kg 40.17 1.26<br />

N 200 kg 40.67 1.27<br />

Micro 1 cm 3 /L + N<br />

100 kg<br />

Micro 1 cm 3 /L + N<br />

200 kg<br />

Micro 2 cm 3 /L + N<br />

100 kg<br />

Micro 2 cm 3 /L + N<br />

200 kg<br />

38.67 1.24<br />

36.42 1.20<br />

39.25 1.25<br />

46.33 1.80<br />

14.7<br />

3<br />

22.0<br />

2<br />

22.8<br />

3<br />

19.8<br />

3<br />

21.2<br />

8<br />

19.0<br />

0<br />

18.6<br />

6<br />

19.6<br />

7<br />

24.3<br />

2<br />

6.33<br />

10.2<br />

9<br />

10.6<br />

8<br />

10.0<br />

7<br />

10.2<br />

0<br />

9.39<br />

9.00<br />

9.95<br />

14.3<br />

4<br />

33.5<br />

4<br />

43.7<br />

4<br />

46.3<br />

8<br />

42.0<br />

0<br />

43.3<br />

3<br />

41.5<br />

5<br />

38.9<br />

0<br />

41.8<br />

3<br />

47.3<br />

0<br />

12.5<br />

7<br />

20.3<br />

1<br />

21.2<br />

7<br />

19.8<br />

5<br />

20.1<br />

7<br />

18.1<br />

5<br />

17.0<br />

7<br />

19.6<br />

0<br />

23.9<br />

0<br />

67.0<br />

7<br />

81.6<br />

8<br />

82.3<br />

3<br />

80.3<br />

0<br />

79.6<br />

7<br />

76.2<br />

5<br />

72.8<br />

3<br />

77.6<br />

3<br />

93.9<br />

3<br />

21.1<br />

2<br />

28.1<br />

7<br />

29.3<br />

3<br />

27.7<br />

8<br />

28.0<br />

7<br />

26.2<br />

1<br />

25.4<br />

2<br />

27.1<br />

7<br />

33.1<br />

5<br />

28.1<br />

3<br />

40.8<br />

7<br />

41.4<br />

2<br />

39.3<br />

3<br />

39.8<br />

0<br />

35.7<br />

8<br />

33.3<br />

7<br />

37.0<br />

9<br />

45.3<br />

2<br />

LSD at 5% level 2.44 0.11 2.73 2.66 2.44 2.94 6.39 3.01 3.61 2.56<br />

Micro= micronutrients, F.W.=fresh weight,D.W.=dry weight , N= nitrogen<br />

D.W<br />

<strong>of</strong><br />

stem<br />

15.0<br />

1<br />

16.8<br />

5<br />

21.1<br />

2<br />

16.4<br />

1<br />

16.7<br />

3<br />

19.8<br />

9<br />

11.0<br />

7<br />

18.0<br />

0<br />

20.1<br />

7<br />

16.9<br />

8<br />

17.0<br />

0<br />

16.5<br />

4<br />

11.0<br />

0<br />

16.6<br />

7<br />

26.5<br />

3


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table (3) Effect <strong>of</strong> micronutrient and nitrogen fertilizer on chemical constituents <strong>of</strong> schefflera<br />

arboricola L. plants. (means <strong>of</strong> two seasons 2007 and 2008).<br />

Treatments<br />

Character<br />

Effect <strong>of</strong> micronutrient<br />

Chlorophylls Total<br />

Chl. a Chl. b<br />

Chl.<br />

a+b<br />

182<br />

caroten<br />

oids<br />

Mineral ions contents<br />

N P K<br />

mg/g %<br />

Total<br />

protein<br />

Control 0.99 0.30 1.29 0.17 1.47 0.25 3.23 8.68<br />

Micro 1 cm 3 /L 1.12 0.33 1.45 0.18 1.52 0.27 3.26 9.46<br />

Micro 2 cm 3 /L 1.29 0.41 1.70 0.25 1.62 0.33 4.12 10.53<br />

LSD at 5% level 0.08 0.08 0.09 0.09 0.03 0.02 0.33 0.39<br />

Effect <strong>of</strong> nitrogen<br />

Control 1.03 0.33 1.36 0.19 1.51 0.27 3.32 8.90<br />

N 100 kg 1.18 0.34 1.50 0.19 1.52 0.27 3.42 9.68<br />

N 200 kg 1.19 0.38 1.57 0.22 1.59 0.30 3.87 10.09<br />

LSD at 5% level 0.08 0.02 0.09 0.02 0.03 0.02 0.33 0.39<br />

Effect <strong>of</strong> interaction<br />

Control 0.52 0.17 0.69 0.09 1.19 0.15 2.50 5.83<br />

Micro 1 cm 3 /L 1.26 0.40 1.66 0.23 1.63 0.32 3.46 10.17<br />

Micro 2 cm 3 /L 1.31 0.43 1.75 0.26 1.67 0.35 4.00 10.69<br />

N 100 kg 1.22 0.36 1.58 0.21 1.60 0.28 3.63 10.00<br />

N 200 kg 1.24 0.37 1.61 0.22 1.65 0.30 3.55 10.19<br />

Micro 1 cm 3 /L + N 100 kg 1.13 0.31 1.44 0.17 1.47 0.25 3.23<br />

Micro 1 cm 3 /L + N 200 kg 0.96 0.29 1.25 0.13 1.43<br />

9.35<br />

0.22 3.10 8.80<br />

Micro 2 cm 3 /L + N 100 kg 1.18 0.37 1.50 0.18 1.48 0.26 3.39 9.69<br />

Micro 2 cm 3 /L + N 200 kg 1.37 0.47 1.83 0.30 1.70 0.39 4.96 11.21<br />

LSD at 5% level 0.15 0.04 0.15 0.03 0.06 0.04 0.56 0.67<br />

Micro= micronutrients, Chl. Chlorophyll, N= nitrogen


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

REFERENCES<br />

Brady Nyle C. and R. Weil Ray. (2000). Elements <strong>of</strong> The Nature and Properties <strong>of</strong> Soil. Upper saddle<br />

Rover, New Jersy: Prentice-Hill Inc<br />

Brown, J.D. and O. Lilliland, (1946). Rapid determination <strong>of</strong> potassium and sodium in plant material<br />

and soil extracts by flame photometr. Proc.Amer.Hort.Sci., 48: 341-346.<br />

Chapman, H.D. and P.F. Pratt (1961). Methods <strong>of</strong> Analysis for Soil, Plants and Waters. Univ.<br />

California, Div. Agric. Sci. Berkely, USA, pp: 445.<br />

Dahiya, S.S., S.. Mohansundram, Sukhbi-Singh, S. Dahiya- Dsgnd Singh (2001). Effect <strong>of</strong> nitrogen<br />

and phosphorus on growth and dry matter yield <strong>of</strong> tuberose (Polianthus tuberose L.).<br />

Haryama <strong>Journal</strong> <strong>of</strong> Horticultural <strong>Science</strong>, 30:3-4, 198-200.<br />

El-Fouly, M.M.; O.A. N<strong>of</strong>al and Z.M. Mobarak (2001). Effects <strong>of</strong> soil treatment with iron, manganese<br />

and zinc on growth and micronutrient uptake <strong>of</strong> sunflower plants grown in high-pH soil.<br />

<strong>Journal</strong> <strong>of</strong> Agronomy and Crop <strong>Science</strong>. 186(4): 245-251.<br />

King, E.J. (1951). Microanalysis in Medical Biochemistry, 4 th E dn. J. and Ehar Chill. Ltd., London.<br />

Kohnk, Helmut and D. Franzmier, (1995). Soil <strong>Science</strong> Simplified. USA: Waveland Press Inc.<br />

Levin, S.A., H.A. Mooney and C. Field (1989). The dependence <strong>of</strong> plant root: shoot ratios on internal<br />

nitrogen concentration. Ann. Bot. (London)64, 71-75.<br />

Mahgoub, H.M.; Rawia, A. Eid, and Bedour, H. Abou Leila (2006). Response <strong>of</strong> Iris bulbs growth in<br />

sandy soil to nitrogen and potassium fertilization. <strong>Journal</strong> <strong>of</strong> applied <strong>Science</strong>s Research, 2(11):<br />

899-903.<br />

Massoud, A.M.; M.Y. Abou Zaid and M.A. Bakry (2005). Response <strong>of</strong> pea plants grown in silty clay<br />

soil to micronutrients and Rhizobium incubation. Egypt.J.Appl. Sci., 20: 329-346.<br />

Metzzner, H., H. Rava and H. Senger (1965). Unter suchungen zur synchronis iebekiety pigments<br />

mangel von chlrella. Planta, 65: 186-190.<br />

Negm, A.Y. and F.A. Zahran (2001). Optimization time <strong>of</strong> micronutrient application to wheat plants<br />

grown on sandy soils. Egyptian <strong>Journal</strong> <strong>of</strong> Agricultural Research 79(3): 813-823.<br />

Ol sthoorn,A.F.M.; W.G.Keltjens,B.Van Braen and M.C.G.Hopman (1991).Infleunce <strong>of</strong> ammonium on<br />

fine root development and rhizosphere PH <strong>of</strong> douglas seedlings in sand plant soil 133:75-<br />

81.<br />

Pal, A.K. and B.Biswas (2005). Response <strong>of</strong> fertilizer on growth and yield <strong>of</strong> tuberose (Poliathus<br />

tuberose L.) c.v. Calcutta single in the plains <strong>of</strong> west Bengal. J. Interacadimica, Nadia, India,<br />

9: 1, 33-<br />

Paradhan, A.; J.N. Mishra and P.C. Lenka (2004). Effect <strong>of</strong> N and K growth and yield <strong>of</strong> gladiolus.<br />

Orissa <strong>Journal</strong> <strong>of</strong> Horticulture. Orissa Horticultural Society, Bhubaneswar, India. 32: 74-77.<br />

Rabie, M.H.; I.A. Ibrahim, I. A. Attia and E.A. Zahran (2002). Effect <strong>of</strong> enriched starch phosphate and<br />

carbamate as natural foliar fertilizers on yield and mineral content <strong>of</strong> sorghum. Egyptian<br />

<strong>Journal</strong> <strong>of</strong> Agricultural Research . 80(3): 971-984.<br />

Ramesh Kumar, Sheo Ghind and D.S.Yadov (2002). <strong>Studies</strong> on N and P requirement <strong>of</strong> tuberose<br />

(Polianthus tuberosa Linn) c.v. single in hilly soils. Haryana <strong>Journal</strong> <strong>of</strong> Horticultural <strong>Science</strong>,<br />

Haryana Society <strong>of</strong> Haryana, H::Sar, India, 31:1/2, 52-54.<br />

Ratanarat, S.; W. Masangsan; P. Vacleesirisak; C. Distsantia and V. Phanuvas (1990). Effects <strong>of</strong> ion<br />

foliar spray and specific Rhizobium strains on yield components <strong>of</strong> three peanut cultivars. In:<br />

Proceedings 8 th National Ground.nut Research.Meeting.3-5May 1989,Roi-Et,Thiland.<br />

Sharma, S.R; S.C.Bh Andari; H.S. Purohit (2002). Effect <strong>of</strong> organic manure and mineral nutrients<br />

on nutrient uptake and yield <strong>of</strong> cowpea. <strong>Journal</strong> <strong>of</strong> Indian Society <strong>of</strong> Soil <strong>Science</strong>. 50(4): 475-<br />

480.<br />

183


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Smirn<strong>of</strong>f ,N and G.R. Stewart (1985). Nitrate assimilation ion and translocation by higher plants.<br />

Comparative physiology and ecological consequences. Physiol. Plant 64:133-140.<br />

Snedecor, G.W. and W.G. Cochran.1980 Statistical Method 7 th Ed<br />

.IowstateUniv.Press,Iowa,USA.<br />

Sommer, K.andR.six(1982).Ammonium als stickst<strong>of</strong>f qelle beim anbau von<br />

Fttergerste.Landw.Forsch.38:151-161.<br />

Uph<strong>of</strong>, J.C. Th. (1959). Dictionary <strong>of</strong> Economic plants, Weinheim. An excellent and very<br />

comprehensive guide but it only gives very short descriptions <strong>of</strong> the uses without any details<br />

<strong>of</strong> how to utilize the plants.<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

ISSN 1943-2429<br />

© 2010 <strong>Ozean</strong> Publication<br />

STATISTICAL MODELLING FOR OUTLIER FACTORS<br />

Ahmet Kaya<br />

Ege University, Tire Kutsan Vocational High School Computer Programming Department,<br />

Tire-İzmir, Turkey.<br />

e-mail address for correspondence: ahmet.kaya@ege.edu.tr<br />

____________________________________________________________________________________<br />

Abstract. Error in data is one <strong>of</strong> the facts that cause the parameter estimations to be subjective. If the<br />

erroneous case is proved statistically, then these cases are called outliers. Outliers are defined as the few<br />

observations or records which appear to be inconsistent with the rest <strong>of</strong> the group <strong>of</strong> the sample and more<br />

effective on prediction values. Isolated outliers may also have positive impact on the results <strong>of</strong> data<br />

analysis, data mining and estimated model. In this study, we are concerned with outliers in time series<br />

which have two special cases, innovational outlier (IO) and additive outlier (AO). The occurence <strong>of</strong> AO<br />

indicates that action is required, possibly to adjust the measuring instrument or mistake made by person<br />

in observation or record. However, if IO occurs, no adjustment <strong>of</strong> the measurement operation is required.<br />

Also in the study, a multi-factor ( 3 42<br />

2<br />

) modelling was done in order to fit the effects <strong>of</strong> model in data<br />

analysis AR(1) coefficients, (0.5, 0.7, 0.9) outlier type (AO, IO), serie wideness (50, 100, 200, 500) and<br />

criterion value sensibility (% 99 (C=3.00), % 95 (C=3.50), % 90 (C=4.00)) factors statistically by<br />

making use <strong>of</strong> a simulation study. The results <strong>of</strong> the variance analysis on outlier factors were also<br />

emphasized.<br />

Key Words: ARMA, Outliers in Time Series, AO, IO, Modelling outlier factors.<br />

___________________________________________________________________________________<br />

INTRODUCTION<br />

Real data and databases may <strong>of</strong>ten include some erroneous parts. These situations, which damage the<br />

characteristics <strong>of</strong> data are called “abnormal condition”, and the values, which cause these “abnormal<br />

condition” are called outliers. The outliers, which are really independent, are the situations that cause the<br />

parameter estimation values in modelling to be subjective, they damage the processes even though they<br />

are set properly, and it is an obligation to destroy or to eliminate the effects. They diminish the reliability<br />

<strong>of</strong> the results. In this case, outliers is the name given to the data or data sets, which are inharmonious with<br />

the rest <strong>of</strong> the serie, cause the parameter estimation values to be subjective, and damage the settled<br />

processes.<br />

The outliers are values which seem either too large or too small as compared to rest <strong>of</strong> the observations<br />

(Gumbel, 1960).<br />

An outlying observation, or outlier, is one that appears to deviate markedly from other members <strong>of</strong> the<br />

sample in which it occurs (Grubbs, 1969).<br />

The detection <strong>of</strong> influential subsets or multiple outliers is more difficult, owing to masking and swamping<br />

problems. Masking occurs when one outlier is not detected because <strong>of</strong> the presence <strong>of</strong> others, while<br />

swamping occurs when a non-outlier is wrongly identified owing to the effect <strong>of</strong> some hidden outliers<br />

(Pena and Yohai, 1995).<br />

Data analysis is done by adapting the data to a time series model which is composed <strong>of</strong> observations.<br />

Outliers in time series were first studied by Fox in 1972. Fox has developed a criterion to fix the outliers<br />

which is called likelihood ratio criteria, and defined the outliers as the first and second type outliers. The<br />

simulations made have proved that the most effective method among these is the consecutive method,<br />

185


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

developed by Chang(1982), Chang and Tiao(1983). Hillmer(1983) Tsay(1986), Pena(1987), Abraham<br />

and Yatawara(1988), Bruce and Martin(1989) had some studies which contributed the theorical structure<br />

<strong>of</strong> the consecutive method. Besides, Abraham and Yatawara(1988) have studied on lagrange multiplier<br />

method or score based outlier tests. Pena(1987), Abraham and Chuang(1989) and Bruce and<br />

Martin(1989) have studied about the tests depending on the elimination <strong>of</strong> the outlier values during<br />

outlier detection and effective observations in time series (Ljung, 1993).<br />

Isolating Outliers<br />

The main reason for isolating outliers is associated with data quality assurance. The main exceptional<br />

values are more likely to be incorrect. According to the definition given by Wand and Wang (1996),<br />

unreliable data represents an unconformity between the state <strong>of</strong> the database and the state <strong>of</strong> the real<br />

world. For a variety <strong>of</strong> database applications, the amount <strong>of</strong> erroneous data may reach to ten percent and<br />

even more.<br />

It is well known that outliers can seriously affect any inferences drawn if they are not treated<br />

appropriately. Their detection and treatment, however, can lead to considerably greater computational<br />

process. For that reason, removal <strong>of</strong> outliers effect can improve the quality <strong>of</strong> data used for statistical<br />

inferences. Isolated outliers may also have positive impact on the results <strong>of</strong> data analysis and data mining.<br />

Simple statistical estimates, like sample mean and standard deviation can be significantly biased by<br />

individual outliers that are far away from the middle <strong>of</strong> the distribution.<br />

Outlier Detection<br />

The purpose <strong>of</strong> outlier detection is to discover the unusual data, whose behavior is very exceptional when<br />

compared to the rest <strong>of</strong> the data set. Examining the extraordinary behavior <strong>of</strong> outliers helps to uncover the<br />

valuable knowledge hidden behind them and to help the decision makers to make pr<strong>of</strong>it or improve the<br />

service quality. Hence, mining aiming to detect outlier is an important data mining research with<br />

numerous applications, which include credit card fraud detection, discovery <strong>of</strong> criminal activites in<br />

electronic commerce, weather prediction, marketing, statistical applications and so on.<br />

Detection methods are divided into two parts: univariate and multivariate methods. In univariate methods,<br />

observations are examined individually and in multivariate methods, associations between variables in<br />

the same dataset are taken into account.<br />

Classical outlier detection methods are powerful when the data contain only one outlier. However, these<br />

methods decrease drastically if more than one outliers are present in the data (Hadi, 1992).<br />

Although manual inspection <strong>of</strong> scatter plots is the most common approach to outlier detection, this is not<br />

the most effective method. Since the multidimensionality <strong>of</strong> databases provides a significant advantage to<br />

automated perceptions <strong>of</strong> outliers over the manual analysis <strong>of</strong> visualized data. Unlike the case <strong>of</strong> human<br />

decision-making, the parameters <strong>of</strong> the automated detection <strong>of</strong> outliers can be completely controlled,<br />

making it an objective tool for data analysis. Outlier detection in a database is to enhance the performance<br />

<strong>of</strong> data mining algorithms (Last and Kendal, 1995).<br />

Before we address the issue <strong>of</strong> identifying these outliers, we must emphasize that not all are wrong<br />

numbers. They may justifiably be part <strong>of</strong> the group and may lead to better understanding <strong>of</strong> the<br />

phenomena being studied. When an outlier is detected, the analyst is faced with number <strong>of</strong> questions<br />

(David,1978) :<br />

� Is the measurement process out <strong>of</strong> control?<br />

� Is the model wrong?<br />

� Is some transformation required?<br />

� Is there an identifiable subset <strong>of</strong> observations that is important in its different behavior?<br />

OUTLIER MODEL<br />

A mathematical definition <strong>of</strong> a stationary time series is that a time series is said to be stationary if there is<br />

no systematic change in mean (no trend) if there is no systematic change in variance, and if strictly<br />

periodic variations have been removed (Chatfield, 1991).<br />

Now, Consider a stationary autoregressive moving average (ARMA) process <strong>of</strong> order ( p<br />

, q)<br />

186


t<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

�( B ) z � �(<br />

B)<br />

e<br />

(1)<br />

�(<br />

B)<br />

� 1�<br />

� B � ... ��<br />

B<br />

1<br />

q<br />

� ( B)<br />

� 1�<br />

� B � ... ��<br />

B ,<br />

1<br />

t<br />

p<br />

q<br />

p<br />

,<br />

B<br />

e t is a sequence <strong>of</strong> independent and identically distributed random variables with mean zero and<br />

variance<br />

2<br />

� .<br />

Model (2) can also be written as<br />

t<br />

t<br />

k<br />

187<br />

z<br />

t<br />

� z<br />

t�k<br />

� ( B) z � e<br />

(3)<br />

2<br />

where � ( B) � �(<br />

B)<br />

/ �(<br />

B)<br />

�1<br />

��<br />

B ��<br />

B �...<br />

.<br />

1<br />

When estimating the impact <strong>of</strong> an AO (4) and <strong>of</strong> an IO (5), respectively, in a hypothetical situation in<br />

which all <strong>of</strong> time series parameters are known. Two types <strong>of</strong> outliers in time series introduced by Fox<br />

(1972), are additive and innovational.<br />

The additive outlier-AO model:<br />

It is the type <strong>of</strong> outliers that affects a single observation and occurs as a result <strong>of</strong> a mistake made by<br />

person in observation or record. This model, defined as “total outlier” in the literature, is shown as<br />

follows:<br />

y z � �x<br />

t<br />

t<br />

t<br />

2<br />

� (4)<br />

where y t is the observed value, � is the magnitude <strong>of</strong> outlier and<br />

Innovational outlier-IO model:<br />

x t<br />

�1 t � T �<br />

� �<br />

�<br />

�0<br />

Otherwise�<br />

It is the type <strong>of</strong> outliers that affects the subsequent observations starting from its position, in other words<br />

that occurs as a result <strong>of</strong> natural randomness. The model, defined as “randomness outlier” in the literature,<br />

is shown as follows:<br />

� ( B)<br />

yt ( et<br />

� �xt<br />

)<br />

�(<br />

B)<br />

� (5)<br />

Thus the AO case may be called a gross error model, since only the level <strong>of</strong> the T’th observation is<br />

affected. On the other hand, an IO represents an extraordinary shock at time point T influencing<br />

z T , zT<br />

�1,...<br />

through the dynamic system described by �( B) � �(<br />

B)<br />

/ �(<br />

B)<br />

(Chang, Tiao and Chen,<br />

1988).<br />

The occurence <strong>of</strong> AO indicates that action is required, possibly to adjust the measuring instrument or at<br />

least to print an error massage on the database. However, if IO occurs no adjustment <strong>of</strong> the measurement<br />

operation is required (Muirhead, 1986).<br />

The existence <strong>of</strong> AO can seriously bias the estimates <strong>of</strong> the ARMA coefficients and variance, whereas IO<br />

in general has much smaller effect (Chang Tiao and Chen, 1983).<br />

Most <strong>of</strong>ten only AO’s are troublesome, whereas IO’s <strong>of</strong>ten have very little effect. This is understandable,<br />

since an IO can be seen as an extreme disturbance, but an AO is always an observation separate from the<br />

rest <strong>of</strong> data. For example think <strong>of</strong> the residual <strong>of</strong> an AR(1) model. An IO only affects residual, at the date<br />

(2)


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

<strong>of</strong> outlier. An AO, on the other hand, affects the next residual as well, thus inflating two consecutive<br />

residuals. This effect has several consequences for any further analysis <strong>of</strong> the residuals.<br />

According to some researchers, if there exist an AO type outlier in an observation set, its effects must be<br />

removed, however, in case an IO type outlier exists, it is accepted as it occured as a result <strong>of</strong> natural<br />

randomness and its effects must not be removed. Since natural randomness is a situation, which already<br />

exists in all phases <strong>of</strong> life, the notion <strong>of</strong> “these effects must be tolerated” is the valid thought.<br />

Distinguishing an AO From an IO:<br />

There is usually little information available in practice about what type the possible outlier might be<br />

possible might be AO or IO is more appropriate for a given situation. When a test <strong>of</strong> an inappropriate type<br />

is used, the detecting power the test could be substantially reduced. Furthermore, even if it is known that<br />

an outlier has occurred at a particular point, the possibly adverse effect <strong>of</strong> the outlier may not be easy to<br />

remove unless its nature is properly identified (Chang Tiao and Chen, 1988).<br />

Outliers’ Characteristics:<br />

In order to show the characteristics <strong>of</strong> and AO model, the data are “uncontrolled” concentration readings<br />

<strong>of</strong> a chemical process recorded at every two-hour interval, titled “Box-Jenkins A Series” was used. (See,<br />

Box-Jenkins, 1976).<br />

In case <strong>of</strong> AO, only the level <strong>of</strong> the T’th observation is affected. (See the table-1, and the graph-1)<br />

Moreover IO represents an extraordinary shock at time point T influcing z T , zT<br />

�1,...<br />

through the<br />

dynamic system described by �( B) � �(<br />

B)<br />

/ �(<br />

B)<br />

. (See the table-2, and chart-2).<br />

AO Description:<br />

Table 1, Box-Jenkins A Series observations from 38 to 48.<br />

1 2 3 4 5 AO 5 4 3 2 1<br />

38 39 40 41 42 43 44 45 46 47 48<br />

17.7 17.4 17.8 17.6 17.5 16.5 17.8 17.3 17.3 17.1 17.4<br />

When Table-1 observations which is shown above have been investigated, it can be seen that finding<br />

additive outlier don’t change the tendency <strong>of</strong> observations. Observations taken before T (occurence <strong>of</strong><br />

outlier) time same tendency as observations taken after. Thus, we conclude that this outlier is AO,<br />

because only level <strong>of</strong> the T’th observation is affected. This conclusion can be seen from the chart-1which<br />

is shown below.<br />

Chart 1, Box-Jenkins A series observations from 38 to 48<br />

188


IO Description:<br />

<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 2, Box-Jenkins A series observations from 59 to 69.<br />

1 2 3 4 5 IO 5 4 3 2 1<br />

59 60 61 62 63 64 65 66 67 68 69<br />

17.2 16.6 17.1 16.9 16.6 18.0 17.2 17.3 17.0 16.9 17.3<br />

When Table-2 observations which is shown above have been investigated, it can be seen that finding<br />

innovational outlier changes the tendency <strong>of</strong> observations. Observations taken from before T time<br />

different from after, it can be seen that observations value has been changed. Thus, we conclude that this<br />

outlier is IO, because at time point T influcing consecutive observations. z T , zT<br />

�1,...<br />

. This conclusion<br />

can be seen from the chart-2 which is shown below.<br />

Outlier Detection Algorithm:<br />

Chart 2, Box-Jenkins A Series observation from 59 to 69<br />

� Read observations from defined file.<br />

� Read estimated ARMA parameters, using statistical package programs.<br />

� Read calculated � j ’s from the estimated model.<br />

� Read ê t ’s to use<br />

2<br />

ˆ � a and find outliers.<br />

189


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

� Read critical values C which can be 3.00, 3.50 and 4.00.<br />

� Do<br />

1.<br />

2<br />

Calculate the ˆ � a from the ê t ’s.<br />

2. Increase the index <strong>of</strong> the current value by one<br />

3. Calculate � 1.<br />

T , � 2.<br />

T .<br />

4. If � C then display T, IO.<br />

1.<br />

T �<br />

2.<br />

T �<br />

5. If � C then display T, AO.<br />

otherwise no outlier&stop<br />

6. Calculate effect <strong>of</strong> IO or AO and update on new value in file.<br />

7. Reallocate new ê T ’s<br />

� End Do.<br />

� Go Reading new observations from updated file and perform algoritm again.<br />

SIMULATION PROCESS<br />

A computer simulation is an attempt to model a real-life or hypothetical situation on a computer so that it<br />

can be studied to see how the system works. By changing variables, predictions may be made about the<br />

behaviour <strong>of</strong> the system Computer simulation has become a useful part <strong>of</strong> modelling many natural<br />

systems in physics, chemistry and biology, and human systems in economics and social sciences as well<br />

as in engineering to gain insight into the operation <strong>of</strong> those systems. Traditionally, the formal modeling <strong>of</strong><br />

systems has been via a mathematical model, which attempts to find analytical solutions enabling the<br />

prediction <strong>of</strong> the behaviour <strong>of</strong> the system from a set <strong>of</strong> parameters and initial conditions. Computer<br />

simulation is <strong>of</strong>ten used as an adjunct to, or substitution for, modeling systems for which simple closed<br />

form analytic solutions are not possible. There are many different types <strong>of</strong> computer simulation, the<br />

common feature they all share is the attempt to generate a sample <strong>of</strong> representative scenarios for a model<br />

in which a complete enumeration <strong>of</strong> all possible states would be prohibitive or impossible<br />

(http://en.wikipedia.org/wiki/Simulation# Computer_simulation)<br />

In this study I conducted a simulation study to obtain some inferences about the different AR(1)<br />

coefficients, series size, outlier types, and sensitivity coefficients. Table 1 shows the probability <strong>of</strong><br />

finding Additive Outlier-AO, and Innovational Outlier-IO, based on 10000 realizations <strong>of</strong> the AR(1) with<br />

� � 0.<br />

5,<br />

0.<br />

7,<br />

0.<br />

9 and the critical values are C � 3. 00,<br />

C � 3.<br />

50,<br />

C � 4.<br />

00 , For sizes<br />

n � 50,<br />

100,<br />

200,<br />

500 . The fact that critical value C � 3.<br />

00 is close to the 1%, C � 3.<br />

50 to the<br />

5% and C � 4.<br />

00 to the 10% significance level. The location <strong>of</strong> outliers is set in the middle <strong>of</strong> the<br />

observational period, spesifically T � 26 when n � 50 , T � 51 when n �100<br />

, T � 101 when<br />

n � 200 , and T � 251 when n � 500 (Kaya, 2004).<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

Table 3. Finding AO and IO probability<br />

based on 10000 replications <strong>of</strong> an AR(1) process.<br />

� n<br />

C=3.0<br />

AO IO<br />

C=3.5<br />

AO IO<br />

C=4.0<br />

AO IO<br />

50 0.34 0.38 0.33 0.37 0.322 0.35<br />

1 2 4 0 4<br />

100 0.44 0.48 0.42 0.46 0.431 0.46<br />

2 2 8 6 4<br />

0.5 200 0.57 0.61 0.55 0.59 0.540 0.57<br />

7 0 9 6 9<br />

500 0.62 0.66 0.61 0.65 0.609 0.64<br />

2 2 4 0 1<br />

50 0.52 0.56 0.52 0.55 0.512 0.55<br />

9 2 5 5 1<br />

100 0.62 0.66 0.61 0.65 0.607 0.64<br />

2 0 9 3 3<br />

0.7 200 0.65 0.68 0.63 0.66 0.622 0.65<br />

1 8 9 8 6<br />

500 0.75 0.78 0.74 0.77 0.723 0.75<br />

0 7 3 6 7<br />

50 0.64 0.67 0.63 0.67 0.621 0.66<br />

2 6 8 2 1<br />

100 0.69 0.72 0.68 0.72 0.681 0.71<br />

1 8 8 1 5<br />

0.9 200 0.79 0.83 0.79 0.83 0.782 0.81<br />

5 6 1 0 5<br />

500 0.90 0.94 0.89 0.93 0.875 0.90<br />

1 5 2 2 7<br />

STATISTICAL ANALYSIS<br />

Statistics is an increasingly important subject which is useful in many types <strong>of</strong> scientific investigation. It<br />

has become the science <strong>of</strong> collecting, analysing and interpreting data in the best possible way. Statistics is<br />

particularly useful in situations where there is experimental uncertainty and is <strong>of</strong>ten defined as the science<br />

<strong>of</strong> making decisions in the face <strong>of</strong> uncertainty. We begin with some scientific examples in which<br />

experimental uncertainty is present. Most formal statistical models used in different area have been<br />

linear, based on the principles <strong>of</strong> statistical inference, analysis <strong>of</strong> variance, regression and other models.<br />

Formal models may be a variety <strong>of</strong> different forms described by equation models and implemented using<br />

some special programming language which are Pascal, C, C+, C++, and also other special languages,<br />

such as LISP and PROLOG (Kaya and İkiz,2001).<br />

Models can be used for member <strong>of</strong> different purpose in research and management <strong>of</strong> production systems.<br />

Some uses are (Bywater and Cacho, 1994);<br />

� Classification <strong>of</strong> existing data<br />

� Identification <strong>of</strong> type <strong>of</strong> data in research<br />

� Taking results <strong>of</strong> experiments<br />

� Constructing and testing hypothesis<br />

� Estimating parameters<br />

� Concluding experimental results<br />

� Designing experimental production systems<br />

� Determining best production systems<br />

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<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

MODELLING<br />

By using the simulation results a variance analysis study was made for putting forward how the factors<br />

like Model AR(1) Coefficients (M), (0.5, 0.7, 0.9), Series Size (W), (50, 100, 200, 500), Critical value<br />

sensitiveness (C), (C=3.00, C=3.50, C=4.00), Outlier Type (T) (AO, IO) are effective statistically in<br />

detecting outliers. The factors to solve such problems are;<br />

Model AR(1) coefficient (M)<br />

Series sizes (W)<br />

Critical value sensitiveness (C)<br />

Outlier type (T)<br />

The factor levels were selected properly and the model equation for multi-factored 3 42<br />

2<br />

experiment<br />

layout was designed as given below:<br />

Y � � M �W<br />

� C �T<br />

� �<br />

ijkl<br />

� (6)<br />

i<br />

i �1, 2,<br />

3;<br />

j �1,<br />

2,<br />

3,<br />

4;<br />

k �1,<br />

2,<br />

3;<br />

l �1,<br />

2<br />

j<br />

k<br />

l<br />

ijkl<br />

In this model Y ijkl represents the probability <strong>of</strong> outlier detection, � represents general average, i M<br />

represents AR(1) coefficients, j W represents the series sizes, C k represents critical value sensitiveness,<br />

T l represents outlier type, and � ijkl represents the error term.<br />

Table 4. Analysis <strong>of</strong> variance for Table 1.<br />

SOURCE DF Sum<br />

<strong>of</strong><br />

Square<br />

s<br />

AR(1) 2 0.8443<br />

1<br />

Series Size 3 0.6340<br />

9<br />

Critical 2 0.0054<br />

Value<br />

9<br />

Outlier 1 0.0231<br />

Type<br />

1<br />

Error 63 0.0324<br />

6<br />

Total 71 1.5394<br />

8<br />

192<br />

Mean<br />

Square<br />

0.4221<br />

6<br />

0.2113<br />

6<br />

0.0027<br />

5<br />

0.0231<br />

1<br />

0.0005<br />

2<br />

F P<br />

819. 0.000<br />

86<br />

410. 0.000<br />

20<br />

5.33 0.007<br />

44.8<br />

5<br />

CONCLUDING REMARKS<br />

0.000<br />

From the results <strong>of</strong> this experiment, some main important conclusions were emerged:<br />

� The data used in this study were obtained from the simulation experiments performed.<br />

Simulation results were reorganized and remodeled under a suitable experimental design. The<br />

type <strong>of</strong> factorial design was ( 3 4 2)<br />

2<br />

that is 2 factors each at 3 levels and two factors at 1 level<br />

each. Different AR(1) (0.5, 0.7, 0.9), sensitivity coefficients (3.00, 3.50, 4.00), series size n (50,<br />

100, 200, 500), outlier types (AO-IO) and were statistically significant.<br />

� AR(1) coefficients are the values that show the strength <strong>of</strong> the dependence among the<br />

observations. Therefore, it is easier to make outlier analysis on dependent observation sets. In<br />

other words, outlier detection is easier in series having more dependency among the<br />

observations.


<strong>Ozean</strong> <strong>Journal</strong> <strong>of</strong> <strong>Applied</strong> <strong>Science</strong>s 3(1), 2010<br />

� AO, known as the outlier value that occurs because <strong>of</strong> the user is detected more difficultly than<br />

IO, the outlier value that occurs as a result <strong>of</strong> natural randomness. The presence <strong>of</strong> AO in data<br />

causes loss <strong>of</strong> autocorrelation in outlier position. For that reason, finding IO is easier than<br />

finding AO.<br />

� For the sample lengths <strong>of</strong> n =50, 100, 200 and 500, the probability <strong>of</strong> detecting error is<br />

considered important. So data analysis being easier for large data is detained as a result.<br />

� Since the critical value sensitiveness is found as important and it is a factor showing the<br />

tolerance bounderies <strong>of</strong> the outlier analysis in outlier detection phase, it must be emphasized<br />

carefully.<br />

� The proposed procedure is demonstrated to be useful for estimating time series parameters when<br />

there is the possibility <strong>of</strong> outliers. It can be applied to all invertible models. Moreover, it is<br />

flexible and easy to interpret, and it can be implemented with very few modifications to existing<br />

s<strong>of</strong>tware packages capable <strong>of</strong> dealing with ARMA and transfer function models. In practice, we<br />

suggest that this procedure can be used in conjuction with other diagnostic tools for time series<br />

analysis to produce even better results (Chang, Tiao and Chen, 1988).<br />

Suggestions and Inferences:<br />

1. Before making the statistical tests on an observation set, outlier analysis must be done. By this way,<br />

test statistics can produce more healthy results.<br />

2. There are two types <strong>of</strong> outliers, possible to encounter. The effect <strong>of</strong> first type <strong>of</strong> outliers, which are<br />

caused by people, equipments and machines, must be eliminated. Since the second type <strong>of</strong> outliers<br />

occurs because <strong>of</strong> the natural randomness, the elimination <strong>of</strong> the effects <strong>of</strong> them is optional.<br />

3. The model, which is appropriate for the observation values must be used. If an inappropriate model is<br />

applied, the values which are not outliers may be considered as outliers.<br />

4. Outlier detection processes in time series are mutually attached with the autocorrelation powers <strong>of</strong><br />

the observations. For the observation sets, whose autocorrelation is low, the effect “hiding”, in which<br />

the outlier is not considered as an outlier, and the effect “dragging”, in which a non-outlier<br />

observation is considered as an outlier can be obtained.<br />

5. Since outlier detection processes are also used in quality control processes, which are concerned with<br />

finding error, their importance is increasing everyday.<br />

6. While detecting an outlier, the following components <strong>of</strong> the process are determined as important:<br />

a. Generosity <strong>of</strong> the error,<br />

b. Series size,<br />

c. Strong autocorrelation,<br />

d. Criterion value sensitiveness.<br />

REFERENCES<br />

Abraham, B. Chuang, A. 1989. Outlier Detection and Time Series Modelling, American Statistical<br />

Association and the American Society for Quality Control.<br />

Box, G.E.P and Jenkins, G.M. 1976. Time Series Analysis, Forecasting and Control, San Francisco,<br />

Holden-Day.<br />

Chang, I., Tiao, G.C., and Chen C. 1988. Estimation <strong>of</strong> Time Series Parameters in the Presence <strong>of</strong><br />

Outliers, American Statistical Association and American Society for Quality Control.<br />

(Technometrics) Vol. 30, No.2.<br />

Chang, I. and Tiao, G.C. 1983. Estimation <strong>of</strong> Time Series Parameters in the Presence <strong>of</strong> Outliers.<br />

Technical Report 8. Statistics Research Center, University <strong>of</strong> Chicago, Chicago.<br />

Chatfield, C. 1991. The Analysis <strong>of</strong> Time Series, An Introduction. Chapman and Hall. London.<br />

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Collett, D. and Lewis, T. 1976. The Subjective Nature <strong>of</strong> Outliers Rejection Procedures, <strong>Applied</strong> Statist.<br />

25, No.3, 228.<br />

Cox, D.R. and Snell, E.J. 1980. <strong>Applied</strong> Statistics-Principles and Examples, Great Britain.<br />

David, F. Andrews and Pregibon. 1978. Finding the Outliers that Matter, J.R. Statist. Soc. B, 40, No 1.<br />

85-93.<br />

Elash<strong>of</strong>f, J.D. 1972. A model for Quadratic Outliers in Linear Regression, <strong>Journal</strong> <strong>of</strong> American<br />

Statistical Association, 67, 478-485.<br />

Grubbs, F.E. 1969. Procedures for Detecting Outlying Observations in Samples, Technometrics, 11, 1-<br />

21.<br />

Gumbel, E.J. 1960. Discussion on Rejection <strong>of</strong> Outliers by Anscombe, F. J. Technometrics , 2, 165-166.<br />

Hadi, A.S. 1992. Identifying Multiple Outliers in Multivariate Data, J.R. Statist. Soc. B. 54, No.3, 761-<br />

771.<br />

Hawkins, D.W. 1980. Identification <strong>of</strong> Outliers, Chapman and Hall, Great Britain.<br />

Johnson, R.A and Wichern, D.W. 1988. <strong>Applied</strong> Multivariate Statistical Analysis, Prentice Hall, New<br />

Jersey, ABD.<br />

Last, M., and Kandel, A.: Automated Detection <strong>of</strong> Outliers in Real World Data,<br />

www.ise.bgu.ac.il/faculty/mlast/papers.<br />

Ljung, G.M.1993. On Outlier Detection in Time Series, J.R. Statist. Soc. B, 55, No. 2, 559-567.<br />

Muirhead, C.R. 1986. Distinguishing Outlier Types in Time Series, J.R. Statist.. Soc. B, 48, 39-47.<br />

Pena, D. and Yohai, V.J. 1995. The Detection <strong>of</strong> Influential Subsets in Linear Regression by Using an<br />

Influential Matrix, J.R. Statist. Soc. B 57, No. 1, (1995) 145-156.<br />

Prescott, P. 1975. An Approximate Test for Outliers in Linear Models, Technometrics, 17, 129-132.<br />

Wand, Y., and Wang, R.Y. 1996. Anchoring Data Quality Dimension in Ontological Foundations.<br />

Communications <strong>of</strong> the ACM, 39, 11, 86-95.<br />

Kaya, A. 1999. An Investigation The Analysis <strong>of</strong> Outliers in Time Series, Ph.D Thesis, Dokuz Eylül<br />

University, İzmir, Turkey.<br />

Fox, A. J. 1972. Outliers in Time Series, <strong>Journal</strong> <strong>of</strong> the Royal Statistical Society, Ser. B. 43, 350-363.<br />

Kaya, A. 2004. Modelling Outlier Factors in Data Analysis, ADVIS ) (Advances in Information<br />

Systems), LNCS 3261, 88-95.<br />

Taplin, R.H. 1993. Robust Likelihood Calculation for Time Series, <strong>Journal</strong> <strong>of</strong> the Royal Statistical<br />

Society. Ser. B. 55, No. 4, pp. 829-836.<br />

Kaya, A. and İkiz, F. 2001. İstatistiksel Stok Kontrolde Bilgisayar Modellemesi üzerine bir çalışma,<br />

V. Ekonometri ve istatistik Sempozyumu, Adana.<br />

Bywater , A.C. Cacho, O.J. 1994. Use <strong>of</strong> Simulation Model in Research. Proceedings <strong>of</strong> the New<br />

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194

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