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https://elib.belstu.by/handle/123456789/11800
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DC Field | Value | Language |
---|---|---|
dc.contributor.author | Sokolovski, I. V. | en |
dc.contributor.author | Bespaly, А. А. | en |
dc.date.accessioned | 2017-03-10T07:52:22Z | - |
dc.date.available | 2017-03-10T07:52:22Z | - |
dc.date.issued | 2013 | - |
dc.identifier.citation | Sokolovski, 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. 125-129 | en |
dc.identifier.uri | https://elib.belstu.by/handle/123456789/11800 | - |
dc.description.abstract | Findings 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.mimetype | application/pdf | en |
dc.publisher | BSTU | en |
dc.subject | лесные почвы | ru |
dc.subject | дерново-подзолистые почвы | ru |
dc.subject | грунтово-слабоглееватые почвы | ru |
dc.subject | грунтово-глееватые почвы | ru |
dc.title | Sod-podzolic groundwater cryptogley and groundwater gley soils of the Belarusian polesye region | en |
dc.type | Article | en |
dc.identifier.udc | 630*114 | - |
Appears in Collections: | 2013, № 1 |
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