LATERAL DISTRIBUTION AND MIGRATION OF CHEMICAL ELEMENTS IN SWAMP WATERS WITHIN THE BAKCHAR AND IKSA RIVER BASINS (WESTERN SIBERIA)
Abstract
The ecological-geochemical assessment of the Bakchar and Iksa river basins is based on the analysis of lateral distribution and migration of chemical elements in swamp waters. The active accumulation of Na+, Fetotal, Mg2+, NH4+, Cl– and NO3– was revealed within the facies of the Bakchar bog; Fetotal, NH4+; NO3– and Cl– accumulate within the facies of the Iksa drained bog, and Na+ within the facies of the Samara mire. Intensive removal of Mg2+ is typical of the Bakchar bog; removal of Fetotal and NO3– takes place in the Samara mire, while the Iksa drained bog is characterized by no elements removal. The intensity of lateral migration of the studied elements decreases in the series «the Iksa bog – the Bakchar bog – the Samara mire». Migration of chemical elements in the Bakchar bog and the Samara mire has rising geochemical structure, and the Iksa bog has a pike-shaped distribution of geochemical elements.
About the Authors
E. S. Ivanova
Siberian Research Institute of Agriculture and Peat – branch of SFRCA RAS; National Research Tomsk State University.
Russian Federation
Russian Federation
Junior Scientific Researcher.
Tomsk.
Y. A. Kharanzhevskaya
Siberian Research Institute of Agriculture and Peat – branch of SFRCA RAS; National Research Tomsk State University.
Russian Federation
Russian Federation
Senior Scientific Researcher.
Tomsk.
A. A. Mironov
Ugra State University.
Russian Federation
Russian Federation
Department of Chemistry, Associate Professor, Ph.D. in Biology.
Khanty-Mansiysk.
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Review
For citations:
Ivanova E.S., Kharanzhevskaya Y.A., Mironov A.A. LATERAL DISTRIBUTION AND MIGRATION OF CHEMICAL ELEMENTS IN SWAMP WATERS WITHIN THE BAKCHAR AND IKSA RIVER BASINS (WESTERN SIBERIA). Vestnik Moskovskogo universiteta. Seriya 5, Geografiya. 2017;(4):55-64. (In Russ.)
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