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Please use this identifier to cite or link to this item: http://dspace.bsu.edu.ru/handle/123456789/20289
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dc.contributor.authorUmarova, A. B.-
dc.contributor.authorShein, E. V.-
dc.contributor.authorKukharuk, N. S.-
dc.date.accessioned2017-10-16T07:26:52Z-
dc.date.available2017-10-16T07:26:52Z-
dc.date.issued2014-
dc.identifier.citationUmarova, A.B. Soil water retention curve of agrogray soils: influence of anisotropy and the scaling factor / A. B. Umarova, E. V. Shein, N. S. Kukharuk // Eurasian Soil Science. - 2014. - №8(13).-P. 1238-1244.ru
dc.identifier.urihttp://dspace.bsu.edu.ru/handle/123456789/20289-
dc.description.abstractThe soil water characteristic or soil water retention curve (WRC) of medium-loamy gray forest soil horizons was studied in cylinder-shaped samples of disturbed and undisturbed structure. The sample height varied within 2-4 cm and the diameter within 4.5-10 cm. The soil monoliths were sampled in three profiles: vertically, along the slope, and across the slope in accordance with the intrasoil paleorelief formed by the fun-nel-shaped surface of the second humus horizon. The experimental WRC were approximated with the van Genuchten equationru
dc.language.isoenru
dc.subjectagricultureru
dc.subjectsoil scienceru
dc.subjectwater retention curveru
dc.subjectsamplingru
dc.subjectasymmetryru
dc.subjectanisotropy in the soil propertiesru
dc.subjectmodelingru
dc.subjectloose soil samplesru
dc.subjectsoil monolithsru
dc.titleSoil water retention curve of agrogray soils: influence of anisotropy and the scaling factorru
dc.typeArticleru
Appears in Collections:Статьи из периодических изданий и сборников (на иностранных языках) = Articles from periodicals and collections (in foreign languages)

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