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Mountain-meadow soils of the highlands in the Western Caucasus

  • Genesis and Geography of Soils
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Abstract

The published and author’s data on soil-forming conditions, morphology, substance composition and physicochemical properties, total chemical and mineralogical composition, and micromorphology of mountain-meadow soils of the Western Caucasus Range are analyzed. On the basis of the analytical data obtained, the transformation of minerals and features of chemical element profile patterns developed in the course of soil formation are characterized. The main processes accompanying the transformation of mineral and organic parts of the soil mass and migration of soil-formation products are described. Soil formation is shown to be accompanied by two major elementary soil processes developing with participation of soil biota: humus accumulation and clay formation. Ways to improve the classification of mountain-meadow soils are proposed.

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  1. Dokuchaev Soil Science Institute, Pyzhevskii per. 7, Moscow, 119017, Russia

    E. N. Molchanov

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Original Russian Text © E.N. Molchanov, 2010, published in Pochvovedenie, 2010, No. 12, pp. 1433–1448.

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Molchanov, E.N. Mountain-meadow soils of the highlands in the Western Caucasus. Eurasian Soil Sc. 43, 1330–1343 (2010). https://doi.org/10.1134/S1064229310120033

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