- Page 2 and 3: PHYSICS, CHEMISTRY AND BIOGEOCHEMIS
- Page 4 and 5: IN MEMORIAM Dr Ludmila Petrovna Kor
- Page 6 and 7: magnetic (ferrimagnetic) oxides, ma
- Page 8 and 9: educed water activity, would favour
- Page 10 and 11: In this paper AT sorption by surfac
- Page 12 and 13: were obtained with clay content, pH
- Page 14 and 15: In present investigation the quartz
- Page 16 and 17: Hence, the micromorphology suggests
- Page 18 and 19: As the indicators of soil aeration
- Page 20 and 21: Stomatal diffusive resistance of th
- Page 22 and 23: indicators of soil aeration conditi
- Page 24 and 25: REFERENCES 1. 2. 3. 4. 5. 6. 7. 8.
- Page 28 and 29: MORPHOLOGICAL AND PHYSICOCHEMICAL P
- Page 30 and 31: conditions, existing at the first p
- Page 32 and 33: INFLUENCE OF TEMPERATURE ON WATER P
- Page 34 and 35: moisture % 100 90 80 70 60 50 40 so
- Page 36 and 37: STATE OF MICROBIAL COMMUNITIES IN M
- Page 38 and 39: million cells/g soil 25 20 15 10 5
- Page 40 and 41: THE INFLUENCE OF COMPOSITION AND PR
- Page 42 and 43: days grew faster than on substrate
- Page 44 and 45: SOIL SALINITY AND CLIMATE CHANGES I
- Page 46 and 47: POROUS STRUCTURE OF NATURAL BODIES
- Page 48 and 49: These nonuniform classification sys
- Page 50 and 51: Mercury intrusion data are plotted
- Page 52 and 53: METHOD AND MATERIALS The shear stre
- Page 54 and 55: wheat flour NaCl salt fine milk Fig
- Page 56 and 57: The shear experiments revealed two
- Page 58 and 59: Variable charge of mineral surfaces
- Page 60 and 61: 3. Huffaker RC and Wallace A 1958 P
- Page 62 and 63: Q V (pH)/N t = α(pH) = n ∑ i= 1
- Page 64 and 65: REFERENCES 1. De Wit, J.C.M, Van Ri
- Page 66 and 67: BM - biomass; NM - necromass; MM -
- Page 68 and 69: thousand times at the absence of co
- Page 70 and 71: . m 131.5 131.0 I Height above sea
- Page 72 and 73: SEASONAL VARIABILITY OF SOIL WATER
- Page 74 and 75: The mean difference (MD) and the ro
- Page 76 and 77:
Acknowledgement This paper presents
- Page 78 and 79:
1992; Selim 1999). The relative imp
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1.0 C rel 0.5 0.0 v=0.7 D=3.28 v=0.
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1.0 a b C rel 0.5 0.0 0 1 2 3 0 1 2
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Comparison of before- and after-pul
- Page 86 and 87:
provides the accessibility of catio
- Page 88 and 89:
MODEL RESEARCH ON FORMATION OF SYNT
- Page 90 and 91:
The analysis of the specific surfac
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PHOSPHATE-INDUCED CHANGES IN THE SP
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According to the data of Table 1, t
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MINERAL-ORGANIC COMPOUND OF SOILS:
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RESULTS AND DISCUSSION An analysis
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INTRODUCTION CHEMICAL DEGRADATION O
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of organic particles and their elec
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HNO 3 -extractable form is very clo
- Page 106 and 107:
Results demonstrated that Pb and Cd
- Page 108 and 109:
tion was measured using the Tjurina
- Page 110 and 111:
OUTPUT FLUXES OF LEAD IN FOREST ECO
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Regional data on Pb concentrations
- Page 114 and 115:
DEVICE FOR EVALUATION OF THE RAPE P
- Page 116 and 117:
SPECTROSCOPIC COMPARISON OF HUMIC A
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ehavior of sequentially extracted H
- Page 120 and 121:
MODERN MONITORING SYSTEMS FOR THE M
- Page 122 and 123:
The control of the measurement syst
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ASORPTION AND SURFACE AREA OF SOILS
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Nm xCBET N = ( 1− x BET − )[ 1+
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According to this, when x/N (1-x) i
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POTENTIAL OF AZOLLA CAROLINIANA TO
- Page 132 and 133:
The decrease of Pb(II) and of Cd(II
- Page 134 and 135:
12. 13. 14. 15. 16. Piechalak, A.,
- Page 136 and 137:
Kloc, 2001]. Nitrogen adsorption is
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This is worth noting that the lower
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N ( h) 1 2 γ ( h) = [ ( ) ( )] ( )
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Exemplary spatial distributions (sa
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This is worth noting that significa
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adsorbed chemicals to microorganism
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were detected in the untreated soil
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0.4 1000 Moisture [Vol.] 0.3 0.2 0.
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NITROUS OXIDE EMISSION FROM SOILS W
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N2O-N [mg kg -1 ] 100 80 60 40 20 0
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LITERATURE 1. 2. 3. 4. 5. 6. 7. 8.
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where v(t) - CO 2 production rate;
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carbon was involved mainly into mic
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Demkin Vitaliiy DrSc Dmitrakov Leon
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Priputina Irina PhD Rudko Tadeusz P