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M. S. Kotova
M. S. Kotova

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Articles

Article
  • Date submitted
    1975-08-07
  • Date accepted
    1975-10-05

Protection of surface and ground waters in the permafrost zone in connection with open-pit mining of placer deposits

Article preview

Development of alluvial deposits of minerals is almost always connected with the necessity to include large volumes of surface water in the working cycle of mining enterprises. In the process of open pit mining, process water is enriched with a large amount of suspended material, the content of which in some cases reaches 15-20 g/L. A significant part of these process waters is returned to the river network. Annually within the Magadan region only from washing of metal-bearing placers 1-1,2 billion m3 of process water enters the river network. ...

How to cite: Novozhilov V.N., Kotova M.S., Dvoskin G.A., Shemyakin V.N. Protection of surface and ground waters in the permafrost zone in connection with open-pit mining of placer deposits // Journal of Mining Institute. 1976. Vol. 70. Iss. 2. p. 116-119.
Article
  • Date submitted
    1970-08-11
  • Date accepted
    1970-10-07

Pollution of mine water at open-pit mines in the Tikhvin mining district

Article preview

In the open-pit method of bauxite mining at the quarries of the Tikhvin Alumina Refinery, as a result of erosion by surface and underground waters of sandy-clay and bauxite rocks that make up the ledges of the sides, working platforms, dumps, as well as the bottom and walls of drainage ditches, there is pollution of mine water.

How to cite: Novozhilov V.N., Kotova M.S., Krylov V.N. Pollution of mine water at open-pit mines in the Tikhvin mining district // Journal of Mining Institute. 1971. Vol. 62. Iss. 2. p. 107-109.
Article
  • Date submitted
    1964-08-29
  • Date accepted
    1964-10-07

About changes in composition and mineralization of pore waters during their squeezing from clays

Article preview

In recent years, more and more attention of researchers is attracted to the study of sedimentation waters of clayey rocks.It has been noted that as the solutions are squeezed by the application of individual load steps, mineralization in subsequent portions of the solution continuously decreases. This regularity was tried to explain by the action of filtration effect, influence of membrane equilibrium, different dissolving capacity of different categories of bound water. Currently, an increasing number of researchers are inclined to the fact that the difference in mineralization of subsequent portions of the solution indicates the existence near the surface of the solid phase of some part of the solution with a reduced concentration of dissolved salts - the so-called bound solution.

How to cite: Kotova M.S. About changes in composition and mineralization of pore waters during their squeezing from clays // Journal of Mining Institute. 1965. Vol. 48. Iss. 2. p. 88-91.