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Subject Item
n2:RIV%2F60460709%3A41210%2F04%3A6616%21RIV%2F2005%2FMSM%2F412105%2FN
rdf:type
n5:Vysledek skos:Concept
dcterms:description
The soil porous system has traditionally been deduced from the soil-water retention curve with the assumption of homogeneity and free accessibility of pores, defined as capillary tubes,from the sink /source of water. But real soil fabric is modeled as a homogeneous one. To examine the differences between homogeneous and heterogeneous soil porous systems, we studied two types of soils: sandy soil and coarse sandy soil. We applied image processing filters and the ARC/info gRID module to analyze pore sizes in both soils from their electron microscope images taken at two diffeent magnifications. We used the resulting pore-size distribution data to generate 3-D porous media consisting of pores and throats. The homogeneous pore structure was created as a mono-modal por-throat network with one pore-size distribution. The heterogeneous por structure was designed as a bi-modal pore-throat network with two por-size distributions, where the pore sizes were hierarchically arranged in the modes of the network. We The soil porous system has traditionally been deduced from the soil-water retention curve with the assumption of homogeneity and free accessibility of pores, defined as capillary tubes,from the sink /source of water. But real soil fabric is modeled as a homogeneous one. To examine the differences between homogeneous and heterogeneous soil porous systems, we studied two types of soils: sandy soil and coarse sandy soil. We applied image processing filters and the ARC/info gRID module to analyze pore sizes in both soils from their electron microscope images taken at two diffeent magnifications. We used the resulting pore-size distribution data to generate 3-D porous media consisting of pores and throats. The homogeneous pore structure was created as a mono-modal por-throat network with one pore-size distribution. The heterogeneous por structure was designed as a bi-modal pore-throat network with two por-size distributions, where the pore sizes were hierarchically arranged in the modes of the network. We The soil porous system has traditionally been deduced from the soil-water retention curve with the assumption of homogeneity and free accessibility of pores, defined as capillary tubes,from the sink /source of water. But real soil fabric is modeled as a homogeneous one. To examine the differences between homogeneous and heterogeneous soil porous systems, we studied two types of soils: sandy soil and coarse sandy soil. We applied image processing filters and the ARC/info gRID module to analyze pore sizes in both soils from their electron microscope images taken at two diffeent magnifications. We used the resulting pore-size distribution data to generate 3-D porous media consisting of pores and throats. The homogeneous pore structure was created as a mono-modal por-throat network with one pore-size distribution. The heterogeneous por structure was designed as a bi-modal pore-throat network with two por-size distributions, where the pore sizes were hierarchically arranged in the modes of the network. We
dcterms:title
Perkolační teorie a její využití pro interpretaci retenční čáry půdní vlhkosti Percolation Theory and its Applicaton for Interpretation of Soil Water Retention Curves Percolation Theory and its Applicaton for Interpretation of Soil Water Retention Curves
skos:prefLabel
Perkolační teorie a její využití pro interpretaci retenční čáry půdní vlhkosti Percolation Theory and its Applicaton for Interpretation of Soil Water Retention Curves Percolation Theory and its Applicaton for Interpretation of Soil Water Retention Curves
skos:notation
RIV/60460709:41210/04:6616!RIV/2005/MSM/412105/N
n3:strany
209;220
n3:aktivita
n12:Z
n3:aktivity
Z(MSM 412100004)
n3:dodaniDat
n14:2005
n3:domaciTvurceVysledku
n19:3693929
n3:druhVysledku
n4:C
n3:duvernostUdaju
n17:S
n3:entitaPredkladatele
n10:predkladatel
n3:idSjednocenehoVysledku
579084
n3:idVysledku
RIV/60460709:41210/04:6616
n3:jazykVysledku
n9:eng
n3:klicovaSlova
Pore-size analysis, images of soil structure, mono-modal and bi-modal porous system, soil water retention curve, percolation theory, two-phase displacement
n3:klicoveSlovo
n8:images%20of%20soil%20structure n8:Pore-size%20analysis n8:mono-modal%20and%20bi-modal%20porous%20system n8:two-phase%20displacement n8:soil%20water%20retention%20curve n8:percolation%20theory
n3:kontrolniKodProRIV
[A53C060E219A]
n3:mistoVydani
Trieste
n3:nazevEdiceCisloSvazku
ictp lecture notes, 18
n3:nazevZdroje
Invited Presentations College on Soil Physics
n3:obor
n15:DF
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
1
n3:rokUplatneniVysledku
n14:2004
n3:tvurceVysledku
Kodešová, Radka
n3:zamer
n18:MSM%20412100004
s:numberOfPages
12
n11:hasPublisher
The Abdus Salam International Centre for Theoretical Physics
n13:isbn
92-95003-26-8
n16:organizacniJednotka
41210