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REY geochemistry in groundwater from Paratunka geothermal area (Kamchatka peninsula, Far East of Russia)статья
Информация о цитировании статьи получена из
Web of Science,
Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 12 января 2022 г.
- Авторы: Bragin Ivan V., Kharitonova Natalia A., Chelnokov George A., Aseeva Anna V., Chudaev Oleg V.
- Журнал: Environmental Earth Sciences
- Том: 77
- Год издания: 2018
- Издательство: Springer Verlag
- Местоположение издательства: Germany
- Первая страница: 375
- Последняя страница: 389
- DOI: 10.1007/s12665-018-7571-7
- Аннотация: New data on geochemistry of the Paratunka deposit of mineral waters—Russian biggest geothermal system is presented in this paper. Studied waters are thermal (T = 45–80 °C), alkaline (ph = 7.9–8.7), belong to Ca–Na Cl–SO4 type with reducing environment (Eh = − 150 to − 180 mV) leading to Ce- (+ 0.31) and Eu- (+ 0.8) anomalies. Evolution of chemical type of thermal water from Na–SO4 to Ca–Cl is discussed from the point of water–rock interaction and marine water intrusion as well. REY concentrations are extremely low due to alkaline pH (∑REY = 25–165 ppt). First reliable data on REY concentration in alkaline thermal water, surrounding river water and suspended matter of these waters gave an opportunity to discuss cerium, europium and yttrium anomalies in terms of sorption/desorption processes and pH/Eh dependencies, confirmed by thermodynamic calculations of the REE migration forms.
- Добавил в систему: Харитонова Наталья Александровна