Soil formation in permafrost- taiga landscapes and the methodology of lithochemical sampling of cover sediments (on the example of the North of the Siberian Platform)
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Abstract
The North of Siberia is characterized by gentle sloping relief, subarctic climate, and the development of a thick layer of permafrost. Permafrost- taiga soils are formed here throughout the whole territory. The article considers their main types developed on the eluvio-deluvium of pre-Quaternary rocks and the regularities of metal distribution in soil profiles of the area of the eastern slope of the Anabar anteclise.
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References
- Glazovskaya M. A. Geochemical bases of typology and methods of research of natural landscapes. PH of MSU, 1964.
- Lukashev K. I. Geochemical behavior of elements in hypergene migration cycle. Nauka i tekhnika. Minsk, 1964.
- Tyutyunov I. A. Processes of change and transformation of soils and rocks at negative temperature (cryogenesis). PH AS USSR, 1960.
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