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Priputina Irina PhD Rudko Tadeusz PhD Ruser R. PhD Rutgers Michiel PhD Sancelme Martine PhD Schneider D. PhD Shein Evgeni Prof Shirhshova Ludmila PhD Skierucha Wojciech PhD Sławiński Cezary PhD Sokołowska Zofia Prof Stępniewska Zofia Prof Stępniewski Witold Prof Strizhakova Elena MSc Subocheva Svetlana PhD Świeboda Ryszard PhD Szajnocha Katarzyna MSc IPBPSS, Laboratory of Modelling of Ecosystems priputina@issp.serpukhov.su IA, Laboratory of Physical Properties of Crop rudko@demeter.ipan.lublin.pl Institute of Soil Ecology, GSF- Research Center, Neuherberg, Germany Institute of Public health and the Environment (RIVM), Bilthoven, Netherlands Michiel.Rutgers@rivm.nl Universite Blaise Pascal, Aubiere Cedex, France Laboratoire de Synthese Et Etude de Systemes Interet Biologique besse@chisg1.univ-bpclermont.fr Institute of Soil Ecology, GSF- Research Center, Neuherberg, Germany Moscow State University, Department of Physics and Melioration of Soils, Soil Science Faculty IPBPSS, Laboratory of Mass- and Energy Transfer in Soils shirshova@issp.serpukhov.su IA, Department of Hydrotermophysics of Soil Environment and Agricultural Materials skieruch@demeter.ipan.lublin.pl IA, Department of Hydrotermophysics of Soil Environment and Agricultural Materials cslawin@demeter.ipan.lublin.pl IA, Department of Physical Chemistry of Agricultural Materials sokolows@demeter.ipan.lublin.pl IA, Department of Aeration and Gas Exchange in Soils and Agricultural Materials stepniews@demeter.ipan.lublin.pl Lublin University of Technology stepw@fenix.pol.lublin.pl IPBPSS, Laboratory of Physicochemistry of Soils helene@issp.psn.ru Moscow State University, Chemical Department Medical Academy Lublin, Department of Pharmacy rysio@eskulap.am.lublin.pl Catholic University Lublin 170
Szatanik-Kloc Alicja PhD Usowicz Bogusław DrSc Vasilyeva Galina PhD Walczak Ryszard Prof Wilczek Andrzej MSc Witkowska-Walczak Barbara DrSc Włodarczyk Teresa PhD Wolińska Agnieszka MSc Yevdokimov Il’ya PhD IA, Department of Physical Chemistry of Agricultural Materials akloc@demeter.ipan.lublin.pl IA, Department of Hydrotermophysics of Soil Environment and Agricultural Materials usowicz@demeter.ipan.lublin.pl IPBPSS, Laboratory of Physicochemistry of Soils vasilyeva@issp.serpukhov.su IA, Institute Director, Department of Hydrotermophysics of Soil Environment and Agricultural Materials rwalczak@demeter.ipan.lublin.pl IA, Department of Hydrotermophysics of Soil Environment and Agricultural Materials awilczek@demeter.ipan.lublin.pl IA, Department of Hydrotermophysics of Soil Environment and Agricultural Materials bwitwal@demeter.ipan.lublin.pl IA, Department of Aeration and Gas Exchange in Soil Environment and Agricultural Materials teresa@ demeter.ipan.lublin.pl Catholic University Lublin IPBPSS, Laboratory of Soil Cycles of Nitrogen and Carbon * IPBPSS Institute of Physicochemical and Biological Problems in Soil Science, Russian Academy of Sciences Pushchino Moscow region 142292 RUSSIA ** IA Institute of Agrophysics, Polish Academy of Sciences ul. Doświadczalna 4, 20-290 Lublin POLAND 171
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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
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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
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provides the accessibility of catio
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MODEL RESEARCH ON FORMATION OF SYNT
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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
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Results demonstrated that Pb and Cd
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tion was measured using the Tjurina
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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
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+
Page 128 and 129: According to this, when x/N (1-x) i
Page 130 and 131: 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
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
Page 144 and 145: This is worth noting that significa
Page 146 and 147: adsorbed chemicals to microorganism
Page 148 and 149: were detected in the untreated soil
Page 150 and 151: 0.4 1000 Moisture [Vol.] 0.3 0.2 0.
Page 152 and 153: NITROUS OXIDE EMISSION FROM SOILS W
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
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