深部多层坚硬顶板动−静载耦合致灾机制与监测

Dynamic-static load coupling disaster mechanism and monitoring of deep multilayer hard roofs

  • 摘要: 因地质赋存、采掘布局等存在差异,冲击地压机制需要结合矿井和工作面的具体条件进行针对性研究。以河南大有能源股份有限公司耿村煤矿12240工作面为研究对象,从微震能量事件、工作面前方动静载能量叠加致灾和坚硬顶板应力在线监测的角度确定了上覆坚硬顶板对工作面冲击地压的影响。通过微震能量事件分布特征确定了坚硬顶板失稳活动的时空规律;建立了充分采动条件下工作面超前支承压力力学模型,提出了基于能量叠加原理的动静载耦合分析方法,计算了上覆各坚硬岩层破断传递至工作面的能量叠加;建立了坚硬岩层活动在线监测方案,通过锚索监测数据,定量揭示了工作面开采过程中煤岩体应力动态演化规律。研究结果表明:低位坚硬岩层、中位坚硬岩层1和中位坚硬岩层2协同破断传递至工作面的叠加能量达1.22×104 J,显著超过耿村煤矿冲击地压临界能量;锚索监测数据显示,测点在距开切眼132~143 m区间出现显著应力增幅异常,该异常区与微震能量事件时空演化具有高度相关性,确定为冲击地压产生的主要诱因;基于锚索应力动态响应特征,将工作面推进过程中前方煤岩体活动特征划分为缓慢影响阶段、显著影响阶段和影响急速下降阶段3个典型阶段。

     

    Abstract: Due to differences in geological occurrence and mining layout, the mechanism of rock burst requires targeted research based on specific mine and working face conditions. Taking the No. 12240 working face of Gengcun Coal Mine, Henan Dayou Energy Co., Ltd. as the research object, this study investigated the influence of the overlying hard roofs on rock bursts from the perspectives of microseismic energy events, dynamic–static load superposition in front of the working face, and online stress monitoring of hard roofs. The temporal and spatial patterns of hard roof instability were identified based on the distribution characteristics of microseismic energy events. A mechanical model of the front abutment pressure under full mining conditions was established, and a dynamic–static load coupling analysis method based on the energy superposition principle was proposed to calculate the total energy transmitted from the fractured hard rock strata to the working face. An online monitoring scheme for hard rock layer activity was also developed, and the dynamic stress evolution of the coal rock mass during mining was quantitatively revealed using cable-bolt monitoring data. The results show that the combined failure of the low-position hard layer, the first middle-position hard layer, and the second middle-position hard layer transmitted a total superimposed energy of 1.22 × 104 J to the working face, which significantly exceeds the critical rock-burst energy threshold of Gengcun Coal Mine. Cable-bolt monitoring data indicated a pronounced abnormal increase in stress within the 132–143 m range ahead of the cut-hole, which strongly correlated with the spatiotemporal evolution of microseismic energy events and was identified as the main trigger of rock bursts. Based on the dynamic stress-response characteristics of the cable bolts, the coal rock mass activity in front of the working face during advancement was divided into three typical stages: the slow-influence stage, the significant-influence stage, and the rapid-decline stage.

     

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