露天矿下伏采空区群影响下边坡稳定性研究

Research on the stability of lower slopes affected by underground goaf groups in open-pit mines

  • 摘要: 为探究露天-井工矿复合开采模式下,下伏采空区群对边坡稳定性的影响,以大煤沟采场西帮排土场-采场复合边坡为研究对象,选取W1剖面下伏6个工作面采空区和W2剖面下伏4个工作面采空区为计算剖面,采用数值模拟软件依次模拟分析各工作面采空区形成后覆岩的位移、剪切应变变化规律,探明采空区群形成的垮落带、裂隙带和弯曲下沉带发育特征;基于“三带”分布特征构建了边坡工程地质模型,采用极限平衡法计算了考虑与未考虑“三带”影响下的边坡稳定系数;结合Mohr-Coulomb准则进行边坡稳定性数值模拟分析,揭示了采空区群影响下的滑坡机理。研究结果表明,采空区上覆岩层呈梯形垮落,且随采空区数量增加,产生叠加效应,上覆岩层垮落范围显著增大;W1、W2剖面边坡潜在滑坡模式为圆弧滑动,计算得到的无采空区群和含采空区群但未考虑“三带”效应的边坡稳定系数一致,为2.038和2.634,考虑“三带”效应后W1、W2剖面稳定系数分别降至1.637和1.685,采空区群形成的“三带”效应是影响边坡稳定性的关键。

     

    Abstract: To explore the influence of underground goaf groups on slope stability under the open-pit and underground composite mining mode, the composite slope of the Dameigou west side of the dump and quarry was taken as the research object. Six underground goaf areas of the W1 section and four underground goaf areas of the W2 section were selected as the calculation sections. The displacement and shear strain variation laws of overlying rocks after the formation of goaf areas in each working face were successively simulated and analyzed by using numerical simulation software to clarify the development characteristics of the collapse zone, fracture zone and bending subsidence zone formed by the goaf area group. Based on the distribution characteristics of the "three zones", the slope engineering geological model was constructed, and the slope stability coefficients considering and not considering the influence of the "three zones" were calculated by the limit equilibrium method. The numerical simulation analysis of slope stability was carried out in combination with the Mohr-Coulomb criterion, revealing the landslide mechanism under the influence of the goaf group. The research results show that the overlying strata in the goaf fall in a trapezoidal pattern. Moreover, with the increase in the number of goaf areas, a superimposed effect occurs, and the range of overlying strata collapse significantly expands. The potential landslide pattern of the slopes in the W1 and W2 sections is circular arc sliding. The calculated stability coefficients of the slopes without mined-out area groups and those with mined-out area groups but without considering the "three zones" effect are consistent, which are 2.038 and 2.634 respectively. After considering the "three zones" effect, the stability coefficients of the W1 and W2 sections drop to 1.637 and 1.685 respectively. The "three zones" effect formed by the mined-out area cluster is the key factor affecting the stability of the slope.

     

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