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深部开采强动载波形分类特征及震源参量响应规律

Classification characteristics of strong motion-carrying waveforms for deep mining and seismic source parametric response law

  • 摘要: 为了揭示深部开采过程中强动载震源机制及震源参量响应规律, 以古城煤矿3105工作面为工程背景, 分析了开采期间强动载事件分布特征与震源机制, 并采用HHT方法对不同类型的强动载波进行了时频特征分析, 定量计算了3类动载的震源参量, 揭示了不同类型动载的能量释放特征与破裂模式。研究结果表明: 强动载可分为顶板运动型、煤柱失稳型和断层错动型。断层区域动载断层两侧应力出现变化, 发生压缩破坏; 顶板区域动载受顶板破坏机制影响, 主要发生压缩破坏和剪切破坏; 煤柱区域动载主要发生压缩破坏。断层型强动载倾向角范围主要为30°~45°, 顶板型强动载为10°~65°, 煤柱型强动载为40°~50°。3类动载波在频率分布、能量分布上存在较大差异, 其震源破裂时能量释放特征各不相同。顶板型强动载波边际谱呈单峰分布, 频率主要集中在50~90 Hz; 断层型强动载波边际谱呈双峰分布, 频率主要集中在0~50 Hz; 煤柱型强动载波边际谱呈宽频谱分布, 频率主要集中在10~100 Hz。煤柱型强动载的地震矩最大, 其次为顶板型, 断层型最小。在震源半径相同的情况下, 断层型动载的非弹性变形导致体积增大程度最大, 煤柱型强动载次之, 顶板型强动载最小。研究结果可为冲击地压矿井分源防控提供一定的理论参考。

     

    Abstract: To reveal the seismic source mechanism of strong dynamic loads and the corresponding law of seismic source parameter in the deep mining, the distribution characteristics of strong dynamic loads and the seismic source mechanism during the mining period were analyzed by taking the working face of Gucheng Mine 3105 as the engineering background. The time-frequency characterization of different types of strong dynamic loads was carried out with the method of HHT, and the seismic source parameter of the three types of dynamic loads was quantitatively calculated, which reveals the energy release characteristics and rupture patterns of different types of dynamic loads. The energy release characteristics and rupture modes of different types of dynamic loads are revealed. The results show that the strong dynamic loads can be divided into roof motion type, coal column instability type and fault misalignment type. It is found that the dynamic load in the fault area changes the stresses on both sides of the fault and causes compression damage; the dynamic load in the roof area is affected by the roof damage mechanism and mainly causes compression damage and shear damage; and the dynamic load in the coal pillar area mainly causes compression damage. The inclination angle of fault-type strong dynamic load mainly ranges from 30° to 45°, that of roof-type strong dynamic load from 10° to 65°, and that of coal pillar-type strong dynamic load from 40° to 50°, respectively. The three types of dynamic load waves differ greatly in frequency distribution and energy distribution, and the energy release characteristics of the rupture of their seismic sources are also different. The marginal spectrum of the roof-type strong dynamic wave shows a single-peak distribution, and the frequency is mainly concentrated in 50−90 Hz; the marginal spectrum of the fault-type strong dynamic wave shows a double-peak distribution, and the frequency is mainly concentrated in 0−50 Hz; and the marginal spectrum of the coal-pillar-type strong dynamic wave shows a broadband spectrum distribution, and the frequency is mainly concentrated in 10−100 Hz. The coal-pillar type strong dynamic wave has the largest seismic moment, followed by roof type, and the smallest one of the fault-type. In the case of the same radius of the seismic source, the inelastic deformation of the fault-type dynamic load leads to the largest volume increase, followed by the coal-pillar-type strong dynamic load, and the roof-type strong dynamic load has the smallest scale. The findings can provide some theoretical references for the prevention and control of sub-sources in mines of rockburst tendency.

     

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