Some issues of formation and protection of ferruginous waters
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Abstract
Groundwater containing more than 10 mg/l of iron is commonly referred to ferruginous waters. Such waters occur quite often, but due to the great dependence of iron migration ability on acid-alkaline and gas conditions, these deposits are localized in area and have unstable hydrochemical regime ...
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References
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- Gortikov V.M., Rengarten E.V., Goryunov A.A. Physico-chemical studies of marcial springs of Karelia. - In the book: Physicochemistry of mineral waters and muds. Moscow, Viomedgiz, 1937. 263 p.
- Korotkov A.I., Malov A.I. Hydrochemistry of the Northern Dvina delta. - In the book: Problems of regional hydrochemistry. L., PH of the Geogr. of the USSR, 1979, pp. 106-107.
- Korotkov A.I., Pavlov A.N Hydrochemical method in geology and hydrogeology. L., Nedra, 1972. 185 p.
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