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Doklady Earth Sciences

, Volume 483, Issue 1, pp 1380–1383 | Cite as

The Hydrodynamic Regime of Groundwaters in Coal and Oil-Shale Mining Leases

  • A. V. Mokhov
GEOLOGY
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Abstract

The data on the underworking of water objects and piezometric surveys have allowed scientists to reveal a correlation between hydrodynamic conditions in groundwaters and the stressed and strained state of rock masses at the sites of underground mining of coal and oil-shale deposits. The hydraulic fracturing of the downward filtration current within the layers of clay rocks and upon their contact with sand- and limestone layers was found, along with a discontinuous distribution of hydrostatic pressure in the section of the water-conducting subsidence cracks resulting in groundwater accumulation on clay layers.

Notes

ACKNOWLEDGMENTS

The publication was prepared within a State Assignment for the Southern Science Center, Russian Academy of Sciences, project no. 01201363185.

REFERENCES

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    A. V. Mokhov, Dokl. Earth Sci. 452 (1), 904–906 (2013).CrossRefGoogle Scholar
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    F. P. Strel’skii, L. L. Bokii, and A. D. Prokhorov, Ugol’, No. 8, 61–63 (1983).Google Scholar
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    Yu. A. Norvatov, Investigation and Prediction for Technogenic Mode of Underground Waters (under Development of Mineral Deposits) (Nedra, Leningrad, 1988) [in Russian].Google Scholar

Copyright information

© Pleiades Publishing, Ltd. 2018

Authors and Affiliations

  1. 1.Southern Science Center, Russian Academy of SciencesRostov-on-DonRussia

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