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Mountainous meadow-steppe soils in high mountains of the Eastern Caucasus region
The results of comprehensive investigations into the soil-forming conditions, morphology, substantive composition, physicochemical properties, bulk elemental composition, and mineralogy of mountainous meadow-steppe soils of the Eastern Caucasus region are discussed. The analysis of the obtained and...
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Published in: | Eurasian soil science 2009-06, Vol.42 (6), p.591-599 |
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Main Author: | |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that cite this one |
Online Access: | Get full text |
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Summary: | The results of comprehensive investigations into the soil-forming conditions, morphology, substantive composition, physicochemical properties, bulk elemental composition, and mineralogy of mountainous meadow-steppe soils of the Eastern Caucasus region are discussed. The analysis of the obtained and published data has shown that the formation of these soils takes place in a relatively arid high-mountain environment from the coarse-textured eluvium of noncalcareous rocks. Two major pedogenetic processes with the participation of soil biota—humus accumulation and argillization—are responsible for their origin. Suggestions for improving the classification of mountainous meadow-steppe soils are given. |
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ISSN: | 1064-2293 1556-195X |
DOI: | 10.1134/S1064229309060027 |