Floor stability in the first layer of mine workings when the stope is run through an impact zone of a geological fault
P.V. Grechishkin1 , V.V. Sementsov2, N.Yu. Troshkov1, D.V. Osminin2, S.S. Onishchenko1
1 Kemerovo Branch, VNIMI JSC, Kemerovo, Russian Federation
2 VostNII Research Center JSC, Kemerovo, Russian Federation
Russian Mining Industry №3S / 2024 стр. 20-25
Abstract: The article discusses specific features of rock pressure manifestation in mine workings of the first layer in the impact zone of a geological fault and the bearing pressure from stoping operations. Factors are defined that cause the occurrence of such phenomena. The issue regarding classification of these phenomena, which are not defined in the "Guidelines for forecasting dynamic phenomena..." is stated. Specific features of the rock pressure are given depending on the structure and physical and mechanical properties of coal in different layers during slice mining of the seam. The experience of monitoring dynamic phenomena and creation of optimal methods to control the floor stability in the first layer of mine workings are described for the stoping operations in conditions of the Kuznetsk coal basin. Results of perennial instrumental survey of the rock mass using the Angel-M system with the electrometric mine equipment function applying the induced electromagnetic radiation method are described, as well as analysis of the seismic situation in the investigated area. A new term is proposed for classification of the recorded dynamic phenomena. A layout of boreholes for directional hydrofrac of the deep-buried rocks above the intermediate drift during the stoping period was designed, which allowed to effectively reduce the negative impact caused by the weight of the poorly caving rocks.
Keywords: stability of floor in mine workings, stope, geological faulting, rock pressure
For citation: Grechishkin P.V., Sementsov V.V., Troshkov N.Yu., Osminin D.V., Onishchenko S.S. Floor stability in the first layer of mine workings when the stope is run through an impact zone of a geological fault. Russian Mining Industry. 2024;(3S):20–25. (In Russ.) https://doi.org/10.30686/1609-9192-2024-3S-20-25
Article info
Received: 03.05.2024
Revised: 18.06.2024
Accepted: 27.06.2024
Information about the authors
Pavel V. Grechishkin – Cand. Sci. (Eng.), Director, Kemerovo Branch, VNIMI JSC, Kemerovo, Russian Federation; e-mail: This email address is being protected from spambots. You need JavaScript enabled to view it.
Vyacheslav V. Sementsov – Cand. Sci. (Eng.), Executive Director, First Deputy CEO, VostNII Research Center JSC, Kemerovo, Russian Federation
Nikolay Yu. Troshkov – Deputy Director, Kemerovo Branch, VNIMI JSC, Kemerovo, Russian Federation
Dmitry V. Osminin – Cand. Sci. (Eng.), Head of the Mining Geomechanics Laboratory, VostNII Research Center JSC, Kemerovo, Russian Federation
Sergey S. Onishchenko – Engineer, Laboratory of Geomechanics and Mine Surveying Methods, Kemerovo Branch, VNIMI JSC, Kemerovo, Russian Federation
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