Please use this identifier to cite or link to this item: https://elib.belstu.by/handle/123456789/11800
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dc.contributor.authorSokolovski, I. V.en
dc.contributor.authorBespaly, А. А.en
dc.date.accessioned2017-03-10T07:52:22Z-
dc.date.available2017-03-10T07:52:22Z-
dc.date.issued2013-
dc.identifier.citationSokolovski, I. V. Sod-podzolic groundwater cryptogley and groundwater gley soils of the Belarusian polesye region / I. V. Sokolovski, А. А. Bespaly // Proceedings of BSTU. No. 1. – Minsk : BSTU, 2013. – P. 125-129en
dc.identifier.urihttps://elib.belstu.by/handle/123456789/11800-
dc.description.abstractFindings of investigation of a constitution, compound and properties of sod-podzolic weakly gleyey and gleyey forest soils of the Belarus Polesye region are resulted. It is defined gradation analysis and properties. It is specified, that sod-podzolic weakly gleyey and gleyey soils are formed on fluvioglacial and old alluvial sandy and sandy-loam deposits. The humus content in sod-podzolic soils averages 2– 3%. Soils are characterised middle acidic to subacidic reaction of medium, the degree of soils saturation of the base varies from 33% in a humus horizon to 79% in underlaying horizons. They are formed bracken, bilberry and oxalis phylums of ouk-woods on a given soils.en
dc.format.mimetypeapplication/pdfen
dc.publisherBSTUen
dc.subjectлесные почвыru
dc.subjectдерново-подзолистые почвыru
dc.subjectгрунтово-слабоглееватые почвыru
dc.subjectгрунтово-глееватые почвыru
dc.titleSod-podzolic groundwater cryptogley and groundwater gley soils of the Belarusian polesye regionen
dc.typeArticleen
dc.identifier.udc630*114-
Appears in Collections:2013, № 1

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