李伟. 双弱层烧变岩边坡失稳模式研究[J]. 煤矿安全, 2022, 53(7): 227-234.
    引用本文: 李伟. 双弱层烧变岩边坡失稳模式研究[J]. 煤矿安全, 2022, 53(7): 227-234.
    LI Wei. Study on instability mode of double weak layer burnt rock slope[J]. Safety in Coal Mines, 2022, 53(7): 227-234.
    Citation: LI Wei. Study on instability mode of double weak layer burnt rock slope[J]. Safety in Coal Mines, 2022, 53(7): 227-234.

    双弱层烧变岩边坡失稳模式研究

    Study on instability mode of double weak layer burnt rock slope

    • 摘要: 为了研究露天煤矿双弱层烧变岩边坡失稳模式,采用FLAC3D数值模拟,分析了边坡破坏变形特征,建立边坡力学模型;全面考虑烧变岩体、地下水对边坡稳定性的影响和软弱夹层对边坡的控制作用,基于极限平衡法推导不同力学条件下边坡滑移破坏模式。模拟结果显示:上部弱层控制区域岩体及后缘烧变岩体在水平方向位移较大,变形速度较快,塑性变形明显,沿下部弱层带存在塑性区,其控制区域岩体变形速度有所增大。力学分析结果表明:边坡稳定性受上部弱层控制时,上部岩体沿上部弱层移动变形,后缘烧变岩体拉裂破碎推动岩体发生顺层剪切破坏;边坡受下部弱层控制时,岩体沿下部弱层滑移,后缘拉裂,边坡发生沿下部弱层的剪切破坏;后缘拉裂面垂直高度达到两弱层间距时,拉裂面位于上部弱层下方,边坡稳定性同时受到上下2个弱层控制;若上部弱层之上岩体被拉裂,拉裂岩体随两弱层之间岩体变形移动;上部弱层之上岩体保持稳定,则两弱层之间变形岩体滑移与上部岩体分离;上部弱层之上岩体整体失稳,则坡顶处烧变岩体拉裂破碎,两弱层之间岩体沿下部弱层剪切失稳,上部弱层之上岩体整体随下部岩体变形移动。以大南湖二矿南端帮为工程实例,代入力学参数得到上部岩体安全系数为0.942,处于失稳状态,下部岩体安全系数为1.070,处于滑移临界状态,考虑两弱层控制区域岩体之间的相互影响,坡体发生上下两弱层控制下的阶段式滑移-拉裂失稳。

       

      Abstract: In order to study the failure mode of double weak layer slope of burnt rock in opencast coal mine, the failure and deformation characteristics of the slope were analyzed by means of FLAC3D numerical simulation, and the mechanical model of the slope was established, considering the influence of burnt rock mass and groundwater on slope stability and the control of weak interlayer on slope, the failure mode of slope sliding under different mechanical conditions is deduced based on the limit equilibrium method. The simulation results show that the upper rock mass and the back edge of the burnt rock mass have larger displacement in the horizontal direction, faster deformation speed, obvious plastic deformation; plastic zone exists along the lower weak layer, and the deformation speed of the rock mass in the control area increases. The results of mechanical analysis show that when the stability of slope is controlled by the upper weak layer, the upper rock mass moves and deforms along the upper weak layer; when the slope is controlled by the lower weak layer, the rock mass slips along the lower weak layer, the back edge is split, and the slope is sheared along the lower weak layer; when the vertical height of the trailing edge crack plane reaches the distance between two weak layers, the crack plane lies below the upper weak layer, and the slope stability is controlled by two weak layers at the same time. If the upper rock mass is cracked, the cracked rock mass moves along with the deformation of the lower rock mass; if the upper rock mass remains stable, the lower rock mass slips away from the upper rock mass; and if the upper rock mass loses stability as a whole, the upper rock mass is fractured by the tensile fracture of the burnt rock mass at the back edge of the upper rock mass, the lower part of the rock mass along the lower weak shear instability, the upper rock mass as a whole with the lower rock mass deformation. Taking the southern end of the second mine of Dananhu as an engineering example, substituting mechanical parameters, the safety factor of upper rock mass is 0.942, and the safety factor of lower rock mass is 1.070, and the rock mass is in critical slip state, the slope is subject to a staged sliding-tension instability controlled by the upper and lower weak layers.

       

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