NDLI: Solods under conditions of excessive surface and ground moisture in Western Siberia: Properties, hydrology, and genesis

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Solods under conditions of excessive surface and ground moisture in Western Siberia: Properties, hydrology, and genesis

Content Provider	Springer Nature Link
Author	Zaidelman, F. R. Pakhomova, Ye. Yu. Ustiv, M. T.
Copyright Year	2011
Abstract	Depending on conditions of formation, solods should be differentiated into two groups: solods of ground overmoistening and solods of surface overmoistening. Criteria are offered to distinguish soils according to the ratio between the clay in the B2 horizon and that in the A2 horizon, as well as according to the changes in the soil pH. Formation of gley under conditions of stagnant to percolative water regime is a necessary and sufficient cause for light-colored acid eluvial horizons to form in their profile. In the main properties of the solid phase (acidity, total chemical composition, and distribution of silt), gley solods are identical to soddy-podzolic and chernozem-like podzolic gley soils.
Starting Page	1
Ending Page	10
Page Count	10
File Format	PDF
ISSN	01476874
Journal	Moscow University Soil Science Bulletin
Volume Number	66
Issue Number	1
e-ISSN	19347928
Language	English
Publisher	Allerton Press, Inc.
Publisher Date	2011-04-06
Publisher Place	Heidelberg
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	gley formation solod solonetz excessive moistening eluvial horizons Historical Geology Paleontology
Content Type	Text
Resource Type	Article

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