Содержание и распределение химических элементов в системе «вода–почва–растение» Алгинского гидроминерального комплекса (Западное Забайкалье)

Authors

  • Светлана Геннадьевна Дорошкевич Geological Institute of the Siberian Branch of the Russian Academy of Sciences
  • Михаил Константинович Чернявский Geological Institute of the Siberian Branch of the Russian Academy of Sciences

DOI:

https://doi.org/10.17308/geo.2018.4/2261

Keywords:

chemical elements in water, soil, plants, lake, thermal water source, floodplain and steppe landscape, West Trans Baikal

Abstract

The results of studying the distribution of chemical elements in the biogeochemical system of the Algin hydromineral complex are presented. The chemical composition of the source water and the lake water is different: the source water is dominated by Cr, Cs, Ni, Gd, Ag, Dy, Pb, Ce, Pr, Y, Eu, Co, Sn and Tl; t he la kes water i s dom inated by As, Sb, Ge, Zr, W , Mo, Li, V , Th, Sr, H f, U, Ga, Cu, Rb, Yb, Cd, Al, Nd, Ba, Be, Mn, La, Er, Sm and Ti. The amount of Na, Cs, Sr, Ba, Br, Al, Y, Zr, Ti, V, Cd, As and Se in soils and vegetation depends on their water content.

Author Biographies

  • Светлана Геннадьевна Дорошкевич, Geological Institute of the Siberian Branch of the Russian Academy of Sciences

    Candidate of Biological Sciences, Senior researcher of the laboratory of Hydrogeology and Geoecology of the Geological Institute of the Siberian Branch of the Russian Academy of Sciences, Ulan-Ude

  • Михаил Константинович Чернявский, Geological Institute of the Siberian Branch of the Russian Academy of Sciences

    Candidate of Geographical Sciences, Researcher of the laboratory of Hydrogeology and Geoecology of the Geological Institute of the Siberian Branch of the Russian Academy of Sciences, Ulan-Ude

References

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Published

2018-10-17

Issue

Section

Geography

How to Cite

Содержание и распределение химических элементов в системе «вода–почва–растение» Алгинского гидроминерального комплекса (Западное Забайкалье). (2018). Proceedings of Voronezh State University. Series: Geography. Geoecology, 4, 15-25. https://doi.org/10.17308/geo.2018.4/2261