断层煤柱耦合型冲击失稳机理及防治

    Mechanism and prevention of coupling rock burst instability of fault coal pillar

    • 摘要: 断层构造是冲击地压的重要诱因之一,破坏性最强,易引起煤矿覆岩破坏及地表沉陷等一系列问题,严重制约了煤矿断层构造区的安全生产。为解决断层构造区断层煤柱耦合造成冲击失稳的问题,采用微震监测技术,搜集实际现场数据结合理论力学模型分析了断层活化失稳致冲机制,揭示了两类活化失稳致灾类型(分别为断层失稳型及煤柱失稳型),以此为基础建立了数值模型分析了地质构造区域工作面回采至不同阶段时,断层情况对工作面回采应力分布特征的影响,结合现场微震事件分布情况,制定了断层构造区冲击地压防治方案。研究结果表明,工作面回采至断层区域时,与断层之间易形成断层煤柱区,同时受到采动应力及坚硬顶底板破裂的影响,动应力在水平方向上呈现卸载,在垂直方向上体现为加载,断层的最大主应力减小导致失稳临界值降低,工作面应力集中程度升高,因此,在接近断层时易发生断层活化失稳,增加断层构造区冲击风险,多断层交叉区域应力集中程度较单一断层影响区域更大;根据现场实际地质开采条件制定断层构造区顶板深孔爆破、大直径钻孔卸压及煤层爆破卸压的降载释能防冲方案,基于微震监测及震动波CT反演结果发现同时段同区域微震频次及能量均下降了67%,断层构造区煤岩体应力集中区域明显减小,有效避免了断层构造区冲击地压的发生。

       

      Abstract: Fault structure is one of the important causes of rock burst, with the strongest destructive power, which can easily cause a series of problems such as coal mine overburden damage and surface subsidence, seriously restricting the safe production of fault structure areas of coal mine. To solve the problem of instability caused by the coupling of fault coal pillars in the fault structure area, microseismic monitoring technology is used to collect actual field data and analyze the mechanism of fault activation instability and rock burst using theoretical mechanical models. Two types of activation instability and disaster causing types are revealed (namely fault instability and coal pillar instability). Based on this, a numerical model is established to analyze the influence of fault conditions on the stress distribution characteristics of the working face during different stages of mining in the geological structure area. Combined with the distribution of microseismic events on site, a plan for preventing and controlling rock burst in the fault structure area is formulated. Research has shown that when the working face is mined to the fault area, a fault coal pillar area is easily formed between the working face and the faults. At the same time, it is affected by mining stress and the rupture of the hard roof and floor. The dynamic stress is unloaded in the horizontal direction and reflected as loading in the vertical direction. The decrease in the maximum principal stress of the fault leads to a decrease in the critical value of instability, and the degree of stress concentration in the working face increases. Therefore, when approaching the fault, fault activation instability is prone to occur, increasing the risk of rock burst in the fault structure area. The stress concentration in the intersection area of multiple faults is greater than that in the impact area of a single fault. Based on the actual geological mining conditions on site, a load reduction and energy release anti erosion plan is developed for deep hole blasting, large-diameter drilling pressure relief, and coal seam blasting pressure relief in the fault structure area. Based on microseismic monitoring and seismic wave CT inversion results, it is found that the microseismic frequency and energy in the same period and area decrease by 67%, and the stress concentration area of the coal rock mass in the fault structure area is significantly reduced, effectively avoiding the occurrence of rock burst in the fault structure area.

       

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