NDLI: Differential water capacity of soils of various genesis

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Differential water capacity of soils of various genesis

Content Provider	Springer Nature Link
Author	Sudnitsyn, I. I.
Copyright Year	2015
Abstract	The differential water capacity of the main zonal soils of European Russia and Georgia is determined for the first time. This parameter in the A horizon of these soils rises in the sequence soddy-podzolic soil–gray forest soil–brown semidesert soil–chernozem–light chestnut soil–solonchak–krasnozem within the range of hygroscopic moisture and at equal total potential (or tension) of soil moisture. This is related to a rise in the content of physical clay, humus, or water-soluble salts in the soils. Close correlations are revealed between the logarithm of the absolute value of the total moisture potential (tension) and soil moisture content; between the parameters of this correlation and the specific soil surface; and between the specific soil surface and the content of physical clay in the soil.
Starting Page	174
Ending Page	179
Page Count	6
File Format	PDF
ISSN	01476874
Journal	Moscow University Soil Science Bulletin
Volume Number	70
Issue Number	4
e-ISSN	19347928
Language	English
Publisher	Allerton Press
Publisher Date	2016-01-06
Publisher Place	New York
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	total soil moisture potential hygroscopic moisture specific soil surface physical clay water-soluble salts Historical Geology Paleontology
Content Type	Text
Resource Type	Article

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