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

Аннотация

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.

Язык оригинала	Английский
Номер статьи	012007
Журнал	IOP Conference Series: Earth and Environmental Science
Том	33
Номер выпуска	1
DOI	https://doi.org/10.1088/1755-1315/33/1/012007
Состояние	Опубликовано - 15 апр 2016
Событие	International Conference on Modern Problems of Hydrogeology, Geology Engineering and Hydrogeoecology of Eurasia, SPGE 2015 - Tomsk, Российская Федерация Продолжительность: 23 ноя 2015 → 27 ноя 2015

ASJC Scopus subject areas

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

Доступ к документу

10.1088/1755-1315/33/1/012007

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Цитировать

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

Y1 - 2016/4/15

N2 - 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.

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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