Geochemical features of Kulunda plain lakes (Altay region, Russia)

M. N. Kolpakova, S. L. Shvartsev, S. V. Borzenko, V. P. Isupov, S. S. Shatskaya

Division for Geology

Research output: Contribution to journal › Conference article

Abstract

Geochemical specifics of lake water of the Kulunda Steppe territory (Altay region, Russia) are studied. The results show that in the territory mainly chloride and less soda lakes with sodium compound are developed. It is presented that calcite and soda saturation indexes (SI) of lake water increase with growth of pH, but decrease in such minerals as gypsum and barite. The opposite situation is typical for SI depending on the salinity. It is revealed that evaporation, secondary mineral formation and various biological processes have the greatest impact on accumulation of elements in solution.

Original language	English
Article number	012007
Journal	IOP Conference Series: Earth and Environmental Science
Volume	33
Issue number	1
DOIs	https://doi.org/10.1088/1755-1315/33/1/012007
Publication status	Published - 15 Apr 2016
Event	International Conference on Modern Problems of Hydrogeology, Geology Engineering and Hydrogeoecology of Eurasia, SPGE 2015 - Tomsk, Russian Federation Duration: 23 Nov 2015 → 27 Nov 2015

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ASJC Scopus subject areas

Environmental Science(all)
Earth and Planetary Sciences(all)

Cite this

Kolpakova, M. N., Shvartsev, S. L., Borzenko, S. V., Isupov, V. P., & Shatskaya, S. S. (2016). Geochemical features of Kulunda plain lakes (Altay region, Russia). IOP Conference Series: Earth and Environmental Science, 33(1), [012007]. https://doi.org/10.1088/1755-1315/33/1/012007

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AU - Kolpakova, M. N.

AU - Shvartsev, S. L.

AU - Borzenko, S. V.

AU - Isupov, V. P.

AU - Shatskaya, S. S.

PY - 2016/4/15

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AB - Geochemical specifics of lake water of the Kulunda Steppe territory (Altay region, Russia) are studied. The results show that in the territory mainly chloride and less soda lakes with sodium compound are developed. It is presented that calcite and soda saturation indexes (SI) of lake water increase with growth of pH, but decrease in such minerals as gypsum and barite. The opposite situation is typical for SI depending on the salinity. It is revealed that evaporation, secondary mineral formation and various biological processes have the greatest impact on accumulation of elements in solution.

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Access to Document

10.1088/1755-1315/33/1/012007