Salt and gypsum pedofeatures as indicators of soil processes

Pedofeatures of salts and gypsum in arid and semi-arid soils indicate the salinization process and its dynamics. Mineralogical and morphological features of these pedofeatures, their distribution in the soil profile as well as confinement to individual components of microstructure are indicators of...

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Bibliographic Details
Main Author: I. A. Yamnova
Format: Article
Language:Russian
Published: V.V. Dokuchaev Soil Science Institute 2016-11-01
Series:Бюллетень Почвенного института им. В.В. Докучаева
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Online Access:https://bulletin.esoil.ru/jour/article/view/238
Description
Summary:Pedofeatures of salts and gypsum in arid and semi-arid soils indicate the salinization process and its dynamics. Mineralogical and morphological features of these pedofeatures, their distribution in the soil profile as well as confinement to individual components of microstructure are indicators of soil processes, both modern and relict. The paper presents the results of a comprehensive morpho-mineralogical analysis of the newly formed salt and gypsum pedofeatures in saline soils in the south of European Russia and Cis-Baikal region as well as Transcaucasia, Central Asia, Kazakhstan and Mongolia.
ISSN:0136-1694
2312-4202