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Demkin Vitaliiy DrSc Dmitrakov Leonid PhD Dmitrakova Ludmila PhD Elzov Maxim MSc Farkas Csilla PhD Forano Claude PhD Ghabbour Elham A. PhD Goerke K. PhD Hajnos Mieczysław DrSc Horabik Józef Prof Józefaciuk Grzegorz DrSc Kerjentzev Anatolyi DrS Khokhlova Olga PhD Koptsik Galina PhD Korsunskaia Ludmila PhD Kossowski Jan PhD Kotowska Urszula MSc Księżopolska Alicja PhD IPBPSS, Laboratory of Archaeological Soil Science demkin@issp.serpukhov.su IPBPSS, Laboratory of Physicochemistry of Soils pinsky@issp.serpukhov.su IPBPSS, Laboratory of Physicochemistry of Soils pinsky@issp.serpukhov.su IPBPSS, Laboratory of Archaeological Soil Science m_eltsov@mail.ru Institute for Soil Science and Agricultural Chemistry of HAS, Budapest, Hungary csilla@rissac.hu Universite Blaise Pascal, Aubicre Cedex, France, Laboratoire des Materiaux Inorganiques forano@chimsrv1.univ-bpclermont.fr Barnett Institute, Northeastern University Department of Chemistry, Boston, MA, 02115, USA Institute of Soil Ecology, GSF- Research Center, Neuherberg, Germany IA, Department of Physical Chemistry of Agricultural Materials mhajnos@demeter.ipan.lublin.pl IA, Laboratory of Physics of Plant Granular Solids jhorabik@demeter.ipan.lublin.pl IA, Department of Physical Chemistry of Agricultural Materials jozefaci@demeter.ipan.lublin.pl Institute of Basic Biological Problems RAS, Puschino IPBPSS, Laboratory of Geochemistry and Soil Mineralogy olgakhl@issp.serpukhov.su Moscow State University koptsik@skop.phys.msu.su IPBPSS, Soil-Ecological Station IA, Department of Hydrotermophysics of Soil Environment and Agricultural Materials j.kossowski@demeter.ipan.lublin.pl IA, Department of Aeration and Gas Exchange in Soil Environment and Agricultural Materials ukot@ demeter.ipan.lublin.pl IA, Department of Physical Chemistry of Agricultural Materials aksiezo@demeter.ipan.lublin.pl 168
Kudeyarova Agniya DrSc Kudeyarov Valery Prof Kurochkina Galina PhD Lamorski Krzysztof MSc Lukina Natalia PhD Maher Barbara Prof Marx M. PhD Matyka-Sarzyńska Dorota PhD Mikhailov Alexei MSc Molenda Marek DrSc Munch J.PhD Nikonov Vyacheslav PhD Oleynik Sergey PhD Pachepsky Yakov Prof Pampura Tamara PhD Piekarz Jarosław MSc Pinsky David DrSc IPBPSS, Laboratory of Geochemistry and Soil Mineralogy vnk@issp.serpukhov.su IPBPSS, Institute Director, IPBPSS, Laboratory of Physicochemistry of Soils pinsky@issp.serpukhov.su IA, Department of Hydrotermophysics of Soil Environment and Agricultural Materials lamorski@demeter.ipan.lublin.pl Institute of North Environmental Problems nikonov@cepl.rssi.ru Lancaster University, Centre for Environmental Magnetism and Paleomagnetism, Department of Geography, UK. Institute of Soil Ecology, GSF- Research Center, Neuherberg, Germany IA, Department of Physical Chemistry of Agricultural Materials dmatyka@demeter.ipan.lublin.pl IPBPSS, Laboratory of Modelling of Ecosystems alexei_mikhailov@mail.ru IA, Laboratory of Physics of Plant Granular Solids mmolenda@demeter.ipan.lublin.pl Institute of Soil Ecology, GSF- Research Center, Neuherberg, Germany Institute of North Environmental Problems nikonov@cepl.rssi.ru IPBPSS, Laboratory of Geochemistry and Soil Mineralogy olgakhl@issp.serpukhov.su USDA-ARS Environmental Microbial Safety Laboratory, Beltsville MD, USA ypachepsky@anri.barc.usda.gov IPBPSS, Laboratory of Physicochemistry of Soils pinsky@issp.serpukhov.su IA, Department of Agrophysical Bases of Soil Environment Management buli@demeter.ipan.lublin.pl IPBPSS, Laboratory of Physicochemistry of Soils pinsky@issp.serpuchov.su 169
Page 2 and 3:
PHYSICS, CHEMISTRY AND BIOGEOCHEMIS
Page 4 and 5:
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
Page 14 and 15:
In present investigation the quartz
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Hence, the micromorphology suggests
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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.
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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
Page 44 and 45:
SOIL SALINITY AND CLIMATE CHANGES I
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POROUS STRUCTURE OF NATURAL BODIES
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These nonuniform classification sys
Page 50 and 51:
Mercury intrusion data are plotted
Page 52 and 53:
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
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
Page 92 and 93:
PHOSPHATE-INDUCED CHANGES IN THE SP
Page 94 and 95:
According to the data of Table 1, t
Page 96 and 97:
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
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+
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 164 and 165: Priputina Irina PhD Rudko Tadeusz P
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