Some issues of formation and protection of ferruginous waters
Authors:
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 ...
Область исследования:
(Archived) Without section
References
- Hydrogeology of the USSR / Edited by I.K.Zaitsev. M., Nedra, 1971. Vol. 27. 295 p.
- 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.
- Ovchinnikov A.M., Mineral Waters. M., Gosgeoltekhizdat, 1963, 375 p.
Similar articles
Investigation of groundwater self-purification processes in the Slantsev mining district
1980 A. I. Korotkov, V. N. Shemyakin, S. V. Tsivyan
Investigation of mass transfer processes in groundwater by methods of mathematical modeling
1980 G. N. Genzel, V. A. Mironenko
Investigation of groundwater self-purification processes in the section of tailing ponds of the Phosphorit Combine
1980 A. I. Korotkov, N. S. Petrov, V. N. Shemyakin