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.
|Журнал||IOP Conference Series: Earth and Environmental Science|
|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)