Formation of chemical composition of drainage waters of Korshunovskoye iron ore deposit
Abstract
One of the main reasons for changes in the chemical composition of groundwater during drainage of developed deposits is the intensification of the overflow of pressure, more mineralized water of deep horizons, or squeezing (due to the growth of intra-class stresses) pore water from weakly permeable layers and blocks with a general decrease in head in the upper aquifers.
Область исследования:
(Archived) Without section
References
- Gavryukhina A.A. Formation of groundwater under the influence of artificial load (on the example of Moscow). M., Nauka, 1984.
- Gureev I.E. Formation of mine waters at development of Belozersk iron ore deposit and questions of their rational use. Author's abstract of Cand. Kiev, Izd. of the Institute of Geological Sciences of the Academy of Sciences of the Ukrainian SSR, 1981.
- Mironenko V.A., Rumynin V.G., Uchayev V.K. Protection of groundwater in mining areas. L., Nedra, 1980.
- Plotnikov N.I. Dewatering at development of ore deposits and environmental protection. - Mining Journal, 1978, No. 2.
Similar articles
Hydrochemical zonality and formation of groundwater chemistry of the upper hydrogeologic floor of the northern part of the Onego-Dvinskiy interfluve
1985 T. V. Saltanova
Formation of the chemical composition of groundwater in the foothill troughs of Algeria
1985 Lanur Aissa
Landscape-hydrogeochemical zonality of groundwater of the hypergenesis zone (on the example of the Prionezhye region)
1985 S. M. Sudarikov