Perkolační teorie a její využití pro interpretaci retenční čáry půdní vlhkosti
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41210%2F04%3A6616" target="_blank" >RIV/60460709:41210/04:6616 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Percolation Theory and its Applicaton for Interpretation of Soil Water Retention Curves
Popis výsledku v původním jazyce
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 ahomogeneous 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 sizesin 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
Název v anglickém jazyce
Percolation Theory and its Applicaton for Interpretation of Soil Water Retention Curves
Popis výsledku anglicky
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 ahomogeneous 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 sizesin 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
Klasifikace
Druh
C - Kapitola v odborné knize
CEP obor
DF - Pedologie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)
Ostatní
Rok uplatnění
2004
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název knihy nebo sborníku
Invited Presentations College on Soil Physics
ISBN
92-95003-26-8
Počet stran výsledku
12
Strana od-do
209-220
Počet stran knihy
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Název nakladatele
The Abdus Salam International Centre for Theoretical Physics
Místo vydání
Trieste
Kód UT WoS kapitoly
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