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2. ENVIRONMENTAL ChEMISTRy & TEChNOLOGy 2.1. Lectures

2. ENVIRONMENTAL ChEMISTRy & TEChNOLOGy 2.1. Lectures

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Chem. Listy, 102, s265–s1311 (2008) Environmental Chemistry & Technology<br />

Table I<br />

Calculated values from calibration plots<br />

T h e S t o i c h i o m e t r y o f t h e T e r n a r y<br />

S p e c i e s o f 1 2 - M o l y b d a t o p h o s p h a t e<br />

w i t h R h o d a m i n e B<br />

The molar ratio of components in the ion associate<br />

was expressed from the method of continuous variations1<strong>2.</strong><br />

n<br />

y = 0.1421x + 0.0104 R 2 = 0.9987<br />

X Δ α a 0.40 × 10 –6 mol dm –3 1.24 × 10 –5 g dm –3<br />

X Δ β a 1.18 × 10 –6 mol dm –3 3.66 × 10 –5 g dm –3<br />

X m b 0.79 × 10 –6 mol dm –3 <strong>2.</strong>44 × 10 –5 g dm –3<br />

X 3σ c 0.83 × 10 –6 mol dm –3 <strong>2.</strong>56 × 10 –5 g dm –3<br />

ε σ d 142123 ± 3767 mol –1 cm –1 dm 3<br />

x<br />

1− x<br />

max<br />

= .The resulting value of n was n = = 1<br />

max<br />

0,<br />

5<br />

1−<br />

0,<br />

5<br />

Fig. 1. The point 0 on the jobs curve corresponds with the<br />

maximal concentration of the Rhodamine b and zero concentration<br />

of phosphate, the point 1 with the maximal concentration<br />

of phosphate and zero concentration of Rhodamine b. points<br />

belong to the total absorbance of solution, points belong to the<br />

Rhodamine b blank<br />

This molar ratio corresponds with the ratio between phosphate<br />

and Rhodamine B as 1 : 1. Which describes the composition<br />

of the ion associate such as H 2 P[Mo 3 O 10 ] 4 – . RhB + in<br />

1 mol dm –3 H 2 SO 4 .<br />

A p p l i c a t i o n s F o r t h e R e a l S a m p l e s<br />

o f W a t e r<br />

For all kinds of water, the method of standard additions<br />

in six concentration levels which are 1, 2, 4, 6,<br />

7 × 10 –6 mol dm –3 was used. The concentration of phosphate<br />

was found 0.1 ± 0.02 mg dm –3 triplicate the values in the<br />

.<br />

s431<br />

Fig. <strong>2.</strong> The supposed structure of the ion associate<br />

river water and 0.16 ± 0.007 mg dm –3 phosphate in the drinking<br />

water. The determination could not be carried out by<br />

this approach for mineral water because of increased contents<br />

of silicate in solution. The optimal concentration of<br />

6.7 × 10 –4 mol dm –3 tartaric acid is not effective for masking<br />

but the necessary higher concentration of tartaric acid would<br />

interfere with the determination of phosphate. The concentration<br />

of phosphate in the analyzed sea water was under the<br />

detection limit and the method of standard addition can not<br />

be used.<br />

REFEREnCES<br />

1. Klein G., Perera P.: Eutrophication and health. WHO<br />

and EC, Luxembourg 200<strong>2.</strong><br />

<strong>2.</strong> Pitter P.: Hydrochemie. VŠCHT, Praha 1999.<br />

3. Marczenko Z.: Separation and spectrophotometric<br />

deter-mination of elements. Ellis-Horwood, Chichester<br />

1986.<br />

4. Malát M.: Absorpční anorganická fotometrie. Academia,<br />

Praha 1973.<br />

5. Xiao L. H., Jia Z. Z.: Anal. Chim. Acta 55, 580 (2006).<br />

6. Sommer L., Doležal J.: Scripta fac. Sci. nat. Univ. Purk.<br />

Brun 19, 159 (1989).<br />

7. Kratochvíla J., Sommer L.: Scripta Fac. Sci. nat. Univ.<br />

Purk. Brun 10, 53 (1980).<br />

8. Kartikeyan S., Rao T. P., Iyer C. S. P., Damodaran A. D.:<br />

Microchimica Acta 71, 113 (1994).<br />

9. Graham R. C.: Data Analysis for the Chemical Science.<br />

VCH Publisher, new York 1993.<br />

10. ČSn ISO 8466-1: Kalibrace a hodnocení analytických<br />

metod a určení jejich charakteristik -Část 1: Statistické<br />

hodnocení lineární kalibrační funkce (březen 1994).<br />

11. Miller J. n., Miller J. C.: Statistics and Chemometrics<br />

for Analytical Chemistry. Pearson Education Limited,<br />

new York 2005.<br />

1<strong>2.</strong> Sommer L., Hniličková M.: Bull. Soc. Chim. France<br />

1959, 36.<br />

13. MacDougall D.: Anal. Chem. 52, 2242 (1980).

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