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贺虎, 窦林名, 巩思园, 周澎, 薛再君. 覆岩关键层运动诱发冲击的规律研究[J]. 岩土工程学报, 2010, 32(8).
引用本文: 贺虎, 窦林名, 巩思园, 周澎, 薛再君. 覆岩关键层运动诱发冲击的规律研究[J]. 岩土工程学报, 2010, 32(8).
Rock burst rules induced by cracking of overlying key stratum[J]. Chinese Journal of Geotechnical Engineering, 2010, 32(8).
Citation: Rock burst rules induced by cracking of overlying key stratum[J]. Chinese Journal of Geotechnical Engineering, 2010, 32(8).

覆岩关键层运动诱发冲击的规律研究

Rock burst rules induced by cracking of overlying key stratum

  • 摘要: 基于岩层运动关键层理论,研究了覆岩关键层破断规律,从力学机理上分析了覆岩关键层正“O-X”型破断时,矿山压力达到最大值,极易导致强矿震、冲击矿压的发生。利用微震监测系统,对关键层破断诱发冲击矿压进行定位分析,证明了高能量级别的矿震大多数发生在工作面推进过程中覆岩关键层处于正“O-X”型破断位置。研究表明由关键层运动破断诱发冲击矿压前后,微震事件的时空演化规律、前兆信息显著。研究结果为利用岩层运动理论与微震监测相结合的方法预测冲击矿压奠定了基础。

     

    Abstract: The fracture and movement of overlying strata caused by the mining activities have great influence on the behaviors of violent strata such as mining shock and rock bursts. Based on the key stratum theory, the fracture rules of the key strata are studied. When the phenomenon of square “O-X” style caving occurs, the rock pressure reaches its maximum, and as a result, strong mining shock and rock burst easily occur, which is proved by mechanical mechanism. The rule that the most strong tremors with great energy occur in the zone with the overlying key strata caving as square “O-X” is validated by monitoring and analysis results using the micro-seismic observation system. The monitoring results show that the “time-space” evolvement regulation and omen information of the micro-seismic events are obvious. The research achievements establish a foundation for the rock burst forecast method on the basis of the stratum movement theory and micro-seismic observation.

     

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