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MINING PROCESSES
Название Evaluation of safety of full ore extraction under aquifer by determining fractured water-conducting zone height in Oktyabrsky Mine
DOI 10.17580/gzh.2024.03.03
Автор Darbinyan T. P., Zherlygina E. S., Andreev A. A., Popov A. K.
Информация об авторе

NorNickel’s Polar Division, Norilsk, Russia

T. P. Darbinyan, Director, Department of Mining Practice, Candidate of Engineering Sciences

 

Research Center for Geomechanics and Mining Practice Problems, Empress Catherine II Saint-Petersburg Mining University, Saint-Petersburg, Russia
E. S. Zherlygina, Senior Researcher, Geodynamic Safety Laboratory, Candidate of Engineering Sciences, Zherlygina_ES@pers.spmi.ru
A. A. Andreev, Head of Projects
A. K. Popov, Engineer, Laboratory for Ground Pressure at Metalliferous and Nonmetal Deposits

Реферат

The long-term operating experience of mines reveals some adverse factors to affect safety of mining under water bodies. It is highly risky if water inflow jumps during mining in such conditions. The main criterion of safety in this regard is selected to be the safe mining depth under a water body. The safe mining depth can be expressed numerically in terms of the height of a zone of mining-induced water-conducting fractures. The authors propose an approach based on the calculation procedure of the fractured water-conducting zone height which is numerically equivalent to the safe mining depth since “the safe mining depth under water bodies is a minimum depth below which mining operations induce no water inrushes in underground openings from undermined water objects”. Since water inrushes occur in water-conducting fractures, it is valid to consider their propagation height as a value of the safe mining depth. The procedure is proposed by Professor V. N. Gusev, Surveying Department of the Saint-Petersburg Mining University. At the research stage and in the course of pre-projects works at ore mining companies, the procedure can be applied to various geological and geotechnical conditions. If the knowledge of geology of the impermeable rock mass is insufficient, the procedure can help perform an aggregative estimate of risk of water ingress to mined-out voids from an undermined water-bearing object. Using this estimate, it is possible to identify a portion of a deposit (ore body) which is safely mineable irrespective of the structure and properties of the impermeable rock mass, even in the most unfavorable conditions.

Ключевые слова Water object, safe mining depth, fractured water-conducting zone height, protective activities
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