露天矿下伏采空区群影响下边坡稳定性研究

Slope stability under influence of underlying goaf groups in open-pit mines

  • 摘要: 为探究露天−地下联合开采模式下,下伏采空区群对边坡稳定性的影响,以大煤沟露天矿采场西帮排土场−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UDEC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、剪应变变化规律,探明采空区群形成的垮落带、断裂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”影响下的边坡稳定性系数;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,且随着采空区数量增加,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”效应时W1,W2剖面边坡稳定性系数一致,分别为2.038和2.634,考虑“三带”效应后分别降至1.637和1.685,验证了采空区群形成的“三带”效应是影响边坡稳定性的关键。

     

    Abstract: This study aims to investigate the influence of underlying goaf groups on slope stability under the open-pit–underground combined mining mode. Taking the composite slope of the west dump and pit of the Dameigou Open-pit Coal Mine as the research object, six underlying goafs of working faces beneath the W1 section and four underlying goafs beneath the W2 section were selected as calculation sections. UDEC numerical simulation software was used to sequentially simulate and analyze the displacement and shear strain evolution of overburden after the formation of each working face goaf, and the development characteristics of the caving zone, fracture zone, and bending subsidence zone formed by the goaf group were identified. Based on the distribution characteristics of the "three zones" an engineering geological model of the slope was established, and the slope stability coefficients with and without considering the influence of the "three zones" were calculated using the limit equilibrium method. Based on the Mohr–Coulomb criterion, numerical simulations of slope stability were conducted to reveal the landslide mechanism under the influence of goaf groups. The results indicated that the overlying strata above the goafs exhibited trapezoidal caving, and with an increase in the number of goafs, a superposition effect occurred, significantly expanding the caving range of the overlying strata. The potential landslide modes of the slopes along the W1 and W2 sections were circular sliding. The calculated slope stability coefficients of the W1 and W2 sections were identical when goaf groups were not present and when goaf groups were present but the "three zones" effect was not considered, with values of 2.038 and 2.634, respectively. After considering the "three zones" effect, the stability coefficients decreased to 1.637 and 1.685, respectively, confirming that the "three zones" effect formed by goaf groups was a key factor affecting slope stability.

     

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