Geochemistry and chemical evolution of saline lakes of Western Mongolia

Opis bibliograficzny
Parent link:Geochemistry International
Vol. 52, iss. 5.— 2014.— [P. 388-403]
Korporacja: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Kolejni autorzy: Shvartsev S. L. Stepan Lvovich, Kolpakova M. N. Marina Nikolaevna, Isupov V. P., Vladimirov A. G., Ariunbileg S.
Streszczenie:Title screen
This paper presents data on the major and trace element composition of saline lakes of western Mongolia. The main geochemical types of lakes distinguished in the study are soda-, chloride-, and sulfaterich lakes. Lake water equilibria with major carbonate, sulfate, chloride, and other rock-forming minerals were calculated. The results show that the major factors controlling the formation of each lake type include evaporation and water-rock interaction processes, and the latter factor plays a critical role in freshwater and soda lakes and only a minor role in chloride lakes. Special attention was given to the soda lakes and the factors controlling lake water chemistry.
Режим доступа: по договору с организацией-держателем ресурса
Wydane: 2014
Hasła przedmiotowe:
Dostęp online:http://dx.doi.org/10.1134/S0016702914030070
Format: Elektroniczne Rozdział
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=656103

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