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The permafrost hydrogeology in the Mir diamond pipe area

https://doi.org/10.31242/2618-9712-2019-24-3-7

Abstract

This study presents unique permafrost and groundwater conditions in the Mir diamond pipe area, based on comprehensive analysis of the hydrogeology of western Yakutia. Permafrost in this area is anomalously thick and has a two-layered structure. The upper layer is perennially frozen ground containing local cryopeg lenses, while the lower layer is cryotic ground saturated with brines that have temperatures below 0°C. Subpermafrost aquifers which pose the most serious hazards for mining operations are briefly described. Mine dewatering is shown to be complicated by intensive degassing of subpermafrost brines, as well as by the formation of local cones of piezometric surface depression around the wells. Attention is drawn to the development of a zone of secondary rock fissuring around the mine. This process, along with the high dissolving capacity of drainage water, promotes the formation of underground channels and caves and thus the increased water flow into the mine. It is noted that subpermafrost brines hold promise for balneological and mineral extraction purposes. Measures are proposed to efficiently solve the groundwaterrelated problems in the Mir mine for its further development.

About the Authors

Viktor Vasilyevich Shepelev
P.I. Melnikov Permafrost institute SB RAS
Russian Federation

Shepelev Viktor Vasilyevich, doctor of geological and mineralogical sciences, Professor, Academician
of Academy of Sciences of Republic of Sakha (Yakutia), Principal Researcher, P.I. Melnikov Permafrost
institute SB RAS, 36 Merzlotnaya Str., Yakutsk, 677010, Russia, https://orcid.org/0000-0003-3434-6969, sheply@mpi.ysn.ru;



Mikhail Nikolayevich Zhelezniak
P.I. Melnikov Permafrost institute SB RAS
Russian Federation

Zhelezniak Mikhail Nikolayevich, doctor of geological and mineralogical sciences, Director, P.I. Melnikov Permafrost institute SB RAS, 36 Merzlotnaya Str., Yakutsk, 677010, Russia,
https://orcid.org/0000-0003-4124-6579, fe@mpi.ysn.ru;



Nadezhda Anatolyevna Pavlova
P.I. Melnikov Permafrost institute SB RAS
Russian Federation

Pavlova Nadezhda Anatolyevna, candidate of geological and mineralogical sciences, Leading Researcher, P.I. Melnikov Permafrost institute SB RAS, 36 Merzlotnaya Str., Yakutsk, 677010, Russia,
https://orcid.org/0000-0001-5473-7778, pavlova@mpi.ysn.ru



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Review

For citations:


Shepelev V.V., Zhelezniak M.N., Pavlova N.A. The permafrost hydrogeology in the Mir diamond pipe area. Arctic and Subarctic Natural Resources. 2019;24(3):80-87. (In Russ.) https://doi.org/10.31242/2618-9712-2019-24-3-7

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ISSN 2618-9712 (Print)
ISSN 2686-9683 (Online)