Abstract

The copper ore deposit situated in the south-west of Poland is mined by three underground mines owned by KGHM Polish Copper JSC. Exploitation has been accompanied by rock burst hazard since the beginning. Thus, numerous different preventing measures have been developed such as temporary, organizational and long-term ones. However, no one has been able to predict the time, place and energy of a seismic event. The group winning blasting, with maximum number of blasted faces, is the most effective operation to reduce seismic threat. The more faces are blasted the more seismic energy should be reduced. The study aims at assessing the blasting effectiveness in inducing rock bursts and tremors. For this purpose, the seismic activity induced by mining and blasting were investigated. The number of blasting works and blasted faces as well as length of time between subsequent blasting works were analysed and related to provocation effectiveness. The linear correlation and different regressions were calculated to determine these relations. Moreover, the seismic energy reduction in the rock mass was evaluated by means of SRMS Index, which is a factor measured directly before and after blasting. The analyses covered one mine panel in the Polkowice-Sieroszowice copper mine over four-year period.

Highlights

  • Underground copper ore mining in Poland is associated with the Legnica-Głogów Copper District (LGCD) located in the south-western part of the country, where in 1957 the copper ore deposit was discovered and KGHM Polish Copper JSC has been operating since 1961

  • The key preventive measure is monitoring the condition of the rock mass and the effectiveness of rock burst prevention by means of convergence measurements, continuous recording of seismic activity, passive seismic tomography as well as geotechnical and geological observations

  • Observations of seismoacoustic activity induced by group blasting are carried out with the use of the Microprocessor Meter of Crackles (MMC) before and after blasting works, whose results are presented as the Synthetic Index of Rock Mass Stability (SRMS Index) [3]

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Summary

Introduction

Underground copper ore mining in Poland is associated with the Legnica-Głogów Copper District (LGCD) located in the south-western part of the country, where in 1957 the copper ore deposit was discovered and KGHM Polish Copper JSC has been operating since 1961. The company consists of three mines Rudna, Lubin, Polkowice-Sieroszowice and three copper smelters Cedynia, Głogów, Legnica [1] This hazard results from the geological structure and tectonics of the deposit [2]. Observations of seismoacoustic activity induced by group blasting are carried out with the use of the Microprocessor Meter of Crackles (MMC) before and after blasting works, whose results are presented as the Synthetic Index of Rock Mass Stability (SRMS Index) [3]

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