Geochemistry and chemical evolution of saline lakes of Western Mongolia / S. L. Shvartsev [et al.]
Уровень набора: Geochemistry InternationalЯзык: английский.Резюме или реферат: 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..Примечания о наличии в документе библиографии/указателя: [References: p. 402-403 (47 tit.)].Аудитория: .Тематика: электронный ресурс | труды учёных ТПУ | подземные воды | хлорид кальция | численное моделирование | система вода-порода | насыщение | вечная мерзлота | геохимия | природные воды | рассолы | соленые озера | формирование | Монголия Ресурсы он-лайн:Щелкните здесь для доступа в онлайнTitle screen
[References: p. 402-403 (47 tit.)]
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.
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