2013
DOI: 10.1016/j.ijrmms.2012.08.007
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Structural aspects of gas and dolomite outburst in Rudna copper mine, Poland

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Cited by 27 publications
(25 citation statements)
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“…At the same time, the concentration of methane inside the measuring chamber after comminuting sample 16v2 increased by 0.29%, which corresponds to a release of 2.58 cm 3 of methane from a sample weighing 1 kg. Another gas released from the sample was nitrogen, which-as the main component of the gas mixture contained in the pore pressure of the dolomite-was found in the post-outburst masses collected from the spot in the "Rudna" mine where the tragic incident happened in 2009 (Wierzbicki and Młynarczuk 2013).…”
Section: Resultsmentioning
confidence: 99%
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“…At the same time, the concentration of methane inside the measuring chamber after comminuting sample 16v2 increased by 0.29%, which corresponds to a release of 2.58 cm 3 of methane from a sample weighing 1 kg. Another gas released from the sample was nitrogen, which-as the main component of the gas mixture contained in the pore pressure of the dolomite-was found in the post-outburst masses collected from the spot in the "Rudna" mine where the tragic incident happened in 2009 (Wierzbicki and Młynarczuk 2013).…”
Section: Resultsmentioning
confidence: 99%
“…The classical theory of gas and rock outbursts assumes that the value of the energy of the gas accumulated in the rock pores has to be high enough for the gas to do work when destroying the rock and transporting it down the excavation Sobczyk 2014;Skoczylas 2014;Tian et al 2016). The high porosity values of dolomite (from 15.6 to 16.8%) and the pore pressure of gas exceeding 5.3 MPa were among the main reasons for the outburst of dolomite and other rocks that occurred in the "Rudna" copper mine in Poland in September 2009 (Wierzbicki and Młynarczuk 2013).…”
Section: Discussionmentioning
confidence: 99%
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“…According to the majority of theories and scientific research, a rock and gas outburst is triggered mainly by the energy of gases released from a rock mass and a necessary condition for it to occur is the presence of gas pockets in a rock mass (Li et al [10], Jiang et al [7]). Additional factors that contribute to the occurrence of an outburst are among others different structural properties of a rock mass in its restricted areas, changes of tensions of a rock mass due to its exploitation as well as a working face approaching faults (Shepherd et al [15], Xue et al [18], Lianchong et al [11], Wierzbicki and Młynarczuk [17]). …”
Section: Introductionmentioning
confidence: 99%