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关键层对特厚煤层综放开采地表沉陷规律的影响研究

Study on influence of key strata on surface subsidence law offully-mechanized caving mining in extra-thick coal seam

  • 摘要: 特厚煤层综放开采一次性采全高,其采放煤层厚度大,垮落带和裂隙带高度亦相应增大,使得覆岩“两带”发育直接波及到覆岩上部、对地表沉陷起重要控制的厚硬关键层,其移动变形与地表沉陷特征密切相关。为从覆岩内部岩层移动变形角度探究关键层对特厚煤层综放开采地表沉陷的控制影响作用,应用工程类比法与数值模拟综合确定了东坡煤矿914工作面“两带”高度发育情况,通过关键层理论计算了各亚关键层和主关键层破断距与层位,应用3DEC模拟了关键层对地表沉陷规律的控制影响作用。研究结果表明:应用工程类比法结合数值模拟塑性分区法可综合确定“两带”高度发育情况;上覆岩层及地表的移动变形受厚硬岩层的影响控制,表现为上覆岩层破断特征具有组合移动性、传播至地表呈突陷性;关键层内岩梁破断长度越短,地表沉陷盆地边缘越平缓、地表沉陷影响范围越大;受关键层破断距与破断形式差异的影响,地表下沉盆地开切眼侧较陡、终采线侧相对较缓。

     

    Abstract: The thickness of one-time mining and coal seam produced in the fully-mechanized caving in extra-thick coal seam is large and the height of caving zone and fracture zone increase correspondingly so that the development of the "two zones" directly affects the upper part of the overburden and the thick and hard strata that plays an important role in controlling surface subsidence. The movement and deformation of key strata which plays a role in controlling subsidence is closely related to the surface subsidence law. In order to explore the influence of key strata on the control of surface subsidence of extra-thick coal seam using fully-mechanized top coal caving method from the perspective of rock movement and deformation inside the overburden rock, Engineering Analogy and Numerical Simulation Method were applied to determine the height development of the "two zones" for the No.914 working face of Dongpo Mine. In this case, key strata theory was used to calculate the fracture spacing and position of each sub-key strata and key strata. The 3DEC Simulation was used to study the influence of key strata on the surface subsidence law. The results show that the application engineering analogy method combined with the numerical simulation plastic zoning method can comprehensively determine the high development of the "two zones". The movement and deformation of the overlying strata and surface is controlled by the thick and hard rock strata, which is characterized by the combination of the overburden strata fracture characteristics. The shorter the fracture length of rock beam in key strata, the gentler the edge of the subsidence basin and the larger the influence range of the subsidence basin. Due to the difference of the fracture spacing and form in key strata, the open-off cut side of the subsidence basin is steep and the stopping line side is relatively gentle.

     

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