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GAZHA SOILS OF RUSSIA.

Г. И. Черноусенко

First published: 2019-06-20https://doi.org/10.5593/sgem2019/3.2/s13.031View metrics

Abstract

The article discusses the morphological, micromorphological, and chemical properties of gazha (gypsiferous) soils in the subboreal zone of Russia. The concept of gazha is explained, and the factors and conditions of its formation are analyzed. The analysis of the microfabrics of the gazha horizons indicates that they are mainly composed of small gypsum crystals of pseudorhombohedral shape with possible participation of few gypsum druses. The organization of gypsum crystals in the form of whirl-shaped clusters indicates the processes of cryogenic sorting (freezing out) of the crystals, which is typical of the soils in the permafrost zone. Gypsum druses prevail in the lower part of the soil profiles. Mineralogical analysis confirms the monomineral composition of these horizons; salts are represented by gypsum.

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  • Citations
  • CrossRef - Citation Indexes: 6
  • Scopus - Citation Indexes: 5
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  • Mendeley - Readers: 1

Publication details

Title
GAZHA SOILS OF RUSSIA.
Authors
Г. И. Черноусенко
Proceedings
SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings; 19th International Multidisciplinary Scientific GeoConference SGEM2019, Water Resources. Forest, Marine and Ocean Ecosystems
Publisher
STEF92 Technology
Year
2019
Pages
231-238
SWS Citekey
Chernousenko201913231238
ISSN
1314-2704
ISBN
978-619-7408-82-9
Language
en
Publication type
Conference Paper
Keywords
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Number of times cited according to Crossref: 6

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