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PHYSICS, CHEMISTRY AND BIOGEOCHEMIS
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IN MEMORIAM Dr Ludmila Petrovna Kor
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magnetic (ferrimagnetic) oxides, ma
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educed water activity, would favour
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In this paper AT sorption by surfac
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were obtained with clay content, pH
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In present investigation the quartz
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Hence, the micromorphology suggests
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As the indicators of soil aeration
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Stomatal diffusive resistance of th
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indicators of soil aeration conditi
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REFERENCES 1. 2. 3. 4. 5. 6. 7. 8.
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Table 1. Breakdown of numbers and t
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MORPHOLOGICAL AND PHYSICOCHEMICAL P
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conditions, existing at the first p
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INFLUENCE OF TEMPERATURE ON WATER P
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moisture % 100 90 80 70 60 50 40 so
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STATE OF MICROBIAL COMMUNITIES IN M
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million cells/g soil 25 20 15 10 5
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THE INFLUENCE OF COMPOSITION AND PR
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days grew faster than on substrate
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SOIL SALINITY AND CLIMATE CHANGES I
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POROUS STRUCTURE OF NATURAL BODIES
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These nonuniform classification sys
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Mercury intrusion data are plotted
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METHOD AND MATERIALS The shear stre
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wheat flour NaCl salt fine milk Fig
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The shear experiments revealed two
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Variable charge of mineral surfaces
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3. Huffaker RC and Wallace A 1958 P
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Q V (pH)/N t = α(pH) = n ∑ i= 1
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REFERENCES 1. De Wit, J.C.M, Van Ri
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BM - biomass; NM - necromass; MM -
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thousand times at the absence of co
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. m 131.5 131.0 I Height above sea
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SEASONAL VARIABILITY OF SOIL WATER
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The mean difference (MD) and the ro
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Acknowledgement This paper presents
- Page 78 and 79: 1992; Selim 1999). The relative imp
- Page 80 and 81: 1.0 C rel 0.5 0.0 v=0.7 D=3.28 v=0.
- Page 82 and 83: 1.0 a b C rel 0.5 0.0 0 1 2 3 0 1 2
- Page 84 and 85: Comparison of before- and after-pul
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- Page 88 and 89: MODEL RESEARCH ON FORMATION OF SYNT
- Page 90 and 91: The analysis of the specific surfac
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- Page 94 and 95: According to the data of Table 1, t
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- Page 98 and 99: RESULTS AND DISCUSSION An analysis
- Page 100 and 101: INTRODUCTION CHEMICAL DEGRADATION O
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- Page 112 and 113: 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
- Page 118 and 119: 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
- Page 124 and 125: ASORPTION AND SURFACE AREA OF SOILS
- Page 126 and 127: Nm xCBET N = ( 1− x BET − )[ 1+
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- 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
- Page 138 and 139: This is worth noting that the lower
- Page 140 and 141: N ( h) 1 2 γ ( h) = [ ( ) ( )] ( )
- Page 142 and 143: Exemplary spatial distributions (sa
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- Page 154 and 155: N2O-N [mg kg -1 ] 100 80 60 40 20 0
- Page 156 and 157: LITERATURE 1. 2. 3. 4. 5. 6. 7. 8.
- Page 158 and 159: where v(t) - CO 2 production rate;
- Page 160 and 161: carbon was involved mainly into mic
- Page 162 and 163: Demkin Vitaliiy DrSc Dmitrakov Leon
- Page 164 and 165: Priputina Irina PhD Rudko Tadeusz P