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E. M. Starichkov
E. M. Starichkov
St. Petersburg State Mining Institute
St. Petersburg State Mining Institute

Articles

Geology
  • Date submitted
    2001-07-16
  • Date accepted
    2001-08-05
  • Date published
    2002-02-01

To the geochemistry of bottom sediments of Lake Pyasino (Norilsk District)

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The water system of the Pyasina River is the only one carrying wastewater from the entire Norilsk industrial district. Studies will make it possible to assess the scale and degree of pollution, as well as the dynamics of unfavorable factors along the entire length of this water artery (more than 800 km). The aim of the work is to study the distribution patterns of heavy metals in the modern sediments of the coastal areas of the Arctic basin on the example of the water system of the Norilsk district. It has been revealed that bottom sediments of the Pyasino Lake have an average lead content of 22.7 g/t (MAC - 20 g/t), arsenic - 47 g/t, which is 20 times higher than the norm (MAC - 2 g/t). Nickel content is characterized by extremely high concentrations, about 150 g/t (MAC - 4 g/t), which makes it the major pollutant of bottom sediments of the lake. Strontium content on average does not exceed permissible 268.7 g/t (MAC - 350 g/t), though maximum concentration (southern part of the lake) reaches 600 g/t, which is approximately twice the norm. Zinc concentration is 144 g/t (MAC - 230 g/t), Chromium content is on average 200'g/t (MAC - 50 g/t), which is four times higher than the maximum permissible concentration; Cobalt content is 71 g/t (MAC - 250 g/t). Maximum allowable content of copper varies from 150 to 200 g/t, and the average content of copper in bottom sediments of Pyasino Lake is 234 g/t, which is within the allowable limits, but the south-western part of the lake is characterized by the increased concentration of 494 g/t. Manganese and iron are within the MAC.

How to cite: Starichkov E.M. To the geochemistry of bottom sediments of Lake Pyasino (Norilsk District) // Journal of Mining Institute. 2002. Vol. № 2 150. p. 18-21.
Problems of rational use of mineral resources
  • Date submitted
    2000-10-15
  • Date accepted
    2000-11-06
  • Date published
    2001-05-01

Technogenic geochemical anomalies in mining areas

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The paper considers the main factors affecting the assessment and forecast of the environmental situation in the exploration and development of ore deposits. The data on the composition of soils, water and bottom sediments in some large mining areas (Norilsk, Komsomolsk, etc.) are presented. It is shown that the variability of mineral and chemical composition of ores and host rocks within the subsurface is one of the most important factors both for solving the problem of rational use of mineral deposits and for predicting the environmental consequences of their mining.

How to cite: Gavrilenko V.V., Marin Y.B., Smolenskii V.V., Starichkov E.M. Technogenic geochemical anomalies in mining areas // Journal of Mining Institute. 2001. Vol. № 5 149. p. 149-151.