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

Bibliographische Detailangaben
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 33 : Contemporary Issues of Hydrogeology, Engineering Geology and Hydrogeoecology in Eurasia.— 2016.— [012007, 6 p.]
Körperschaft: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Weitere Verfasser: Kolpakova M. N. Marina Nikolaevna, Shvartsev S. L. Stepan Lvovich, Borzenko S. V., Isupov V. P., Shatskaya S. S.
Zusammenfassung:Title screen
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.
Veröffentlicht: 2016
Schriftenreihe:Hydrogeochemistry
Schlagworte:
Online-Zugang:http://dx.doi.org/10.1088/1755-1315/33/1/012007
http://earchive.tpu.ru/handle/11683/34017
Format: Elektronisch Buchkapitel
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=649465
Beschreibung
Zusammenfassung:Title screen
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.
DOI:10.1088/1755-1315/33/1/012007