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 It is shown that the water conducting cracks are formed in the undermined rocks in the areas of water-resistant strata (WRS) containing so called «abnormal» («unusual») zones. It is noted that the «abnormality» of the geological section in the analyzed cases of accidents of groundwater inflows into the mines during the development of Verkhnekamsky and other salt deposits was established post factum based on a retrospective analysis of the possible causes of accidents. It is concluded that the methods of protection of WRS, recommended by the current regulations, can not be effectively implemented in the presence of abnormal zones. This problem is associated with the difficulties in detecting anomalous zones during exploration and the imperfection of methods of classifying abnormal zones as dangerous zones. It is almost impossible to obtain the necessary data on the qualitative and quantitative parameters of the abnormal zones with the actually used methods of exploration of salt deposits. Therefore there is a high chance, that the project technical solutions (backfilling ratios, pillars’ dimensions, rooms’ dimensions, etc.), aimed to prevention of water conducting cracks development, will not correspond to the actual mining and geological conditions. It is concluded that the greatest danger is posed by abnormal zones characterized by changes in the structure, composition and strength characteristics of rocks, and located above the permanent edges of mine fields. In this situation, in conditions of the Verkhnekamskoye deposit, the formation of water conducting cracks in WRS should be considered as an event that will inevitably occur during the operation of the mine or after its closure. In the given paper, measures are proposed to prevent the formation of water conducting cracks over permanent edges of mine fields.

For citation: Zubov V. P., Kovalski E. R., Antonov S. V., Pachgin V. V. Improving the safety of mines in developing Verkhnekamsk potassium and magnesium salts. Gornyy informatsionno-analiticheskiy byulleten'. 2019;5:22-33. [In Russ]. DOI: 10.25018/0236-1493-2019-05-0-22-33

: 5
ISBN: 0236-1493
УДК: 622.831
DOI: 10.25018/0236-1493-2019-05-0-22-33
Authors: Zubov V. P., Kovalski E. R., Antonov S. V., Pachgin V. V.

Authors' Information:
V.P. Zubov (1), Doctor of Technical Sciences, Head of Chair, e-mail: spggi_zubov@mail.ru,
E.R. Kovalski (1), Candidate of Technical Sciences, Assistant Professor, e-mail: e.r.kovalsky@gmail.com,
S.V. Antonov, Mining Engineer, General Director,
K-Potash Service LLC, 238434, e-mail: info@k-potash.ru,
V.V. Pachgin (1), Mining Engineer, e-mail: pachginv@gmail.com,
1) Saint Petersburg Mining University, 199106, Saint-Petersburg, Russia
Corresponding author: V.P. Zubov, e-mail: spggi_zubov@mail.ru.

Key words:
Water-resistant strata, water conducting cracks, abnormal zones, mining borders, borders of mine fields, breakthrough of groundwater into a mine.


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