Mineral water formation in the eastern part of the Cheboksary deposit

The results of multidisciplinary uranium-isotopic and microelement hydrochemical studies were used to establish that mineral waters in the eastern part of the Cheboksary reservoir have formed from mixing of strata waters of Tatarskie deposits with a deep water, entering through fractured-weakened zo...

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Bibliographic Details
Published in:Water resources 2010-11, Vol.37 (6), p.752-758
Main Authors: Ivanov, A. F, Tikhonov, A. I, Mironova, N. E
Format: Article
Language:English
Subjects:
Aquatic Pollution
Deep water
Earth and Environmental Science
Earth Sciences
Geology
Groundwater
Hydrogeology
Hydrology
Hydrology/Water Resources
Mineral water
Reservoirs
Uranium
Waste Water Technology
Water Management
Water Pollution Control
Water Resources and the Regime of Water Bodies
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Summary:The results of multidisciplinary uranium-isotopic and microelement hydrochemical studies were used to establish that mineral waters in the eastern part of the Cheboksary reservoir have formed from mixing of strata waters of Tatarskie deposits with a deep water, entering through fractured-weakened zones of deep faults of the Gor'kii-Kil'mezskaya lineament zone.
ISSN:0097-8078
1608-344X
DOI:10.1134/S0097807810060023