大采空区顶板“活化-再平衡”规律研究

    Study on the laws of “activation-rebalance” of large goaf roof

    • 摘要: 工作面开采时小煤柱无法承受失稳破断的顶板压力,导致趋于稳定的相邻大采空区顶板结构“活化”失稳,大采空区附近应力场变化易诱发冲击地压等灾害。本文以门克庆煤矿3104工作面、3106工作面及3107工作面为背景,综合运用现场监测与理论分析,探究大采空区顶板覆岩破断演化规律,阐明其“活化-再平衡”机理。研究结果表明:①3107工作面第二次见方期间,大采空区侧104 J以上微震事件较第一次增加7次,能量激增约28倍,表明顶板“活化”失稳;至第三次见方,大能量事件减至1次,能量骤降93.9%,顶板恢复“再平衡”状态。②3107工作面回采时,78~198 m岩层微震频次约为3104工作面、3106工作面的4倍,但其总能量却低一个数量级,证实大采空区顶板“活化”失稳未向高位岩层延伸。③建立了小煤柱开采下采空区顶板“活化”失稳力学模型与判据,揭示了下位基本顶发生回转“活化”失稳,而中位关键层未达失稳条件,保持稳定。

       

      Abstract: During the mining of the working face, the small coal pillar cannot bear the roof pressure of the instability and breaking, which leads to the “activation” instability of the roof structure of the adjacent large goaf roof, and the change of the stress field near the large goaf is easy to induce rock burst and other disasters. Based on the background of 3104, 3106 and 3107 working faces in Menkeqing Coal Mine, this paper comprehensively uses field monitoring and theoretical analysis to explore the fracture evolution law of roof overburden in large goaf and clarify its “activation-rebalance” mechanism. The research shows that: ① during the second square of the 3107 working face, the microseismic events above 104 J on the side of the large goaf increased by 7 times compared with the first time, and the energy surged by about 28 times, indicating that the roof is “activation” and unstable. By the third time, the large energy event is reduced to 1 time, the energy plummeted by 93.9%, and the roof returned to the “rebalance” state. ② During 3107 working face stoping, the microseismic frequency of 78-198 m strata is about 4 times that of 3104 and 3106 working faces, but its total energy is one order of magnitude lower, which confirms that the instability of roof “activation” in large goaf does not extend to high strata. ③ The mechanical model and criterion of roof “activation” and instability in goaf under small coal pillar mining are established. It is revealed that the rotary “activation” and instability of the lower basic roof occurs, while the middle key stratum does not reach the instability condition and remains stable.

       

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