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

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

Detalles Bibliográficos
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.]
Autor Corporativo: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Outros autores: Kolpakova M. N. Marina Nikolaevna, Shvartsev S. L. Stepan Lvovich, Borzenko S. V., Isupov V. P., Shatskaya S. S.
Summary: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.
Publicado: 2016
Series:Hydrogeochemistry
Subjects:
электронный ресурс
труды учёных ТПУ
геохимические особенности
Кулундинская равнина
озера
Алтайский край
биологические процессы
Acceso en liña:http://dx.doi.org/10.1088/1755-1315/33/1/012007
http://earchive.tpu.ru/handle/11683/34017
Formato: Electrónico Capítulo de libro
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=649465

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