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)
Authors:
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.
Область исследования:
(Archived) Without section
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.
Similar articles
On geochemical specialization of basaltic magmas of the Soviet sector of the Pacific Ocean ore belt
1969 Yu. N. Kapkov, E. M. Kwiatkowski, V. I. Yakovlev
Determination of ore density and heavy element content from two conjugate measurements of scattered u-radiation
1969 V. A. Artsybashev, G. A. Ivanyukovich
On the upward migration of nickel and copper in the formation of salt halos in moraine sediments
1969 N. F. Mayorov