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Evolution Law of Coal Seam Abutment Pressure under the Influence of Shallow Buried Complex Strata: A Case Study

机译:浅埋复合地层影响下的煤层邻接压力的演化法 - 以案例研究

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The evolution law of lateral abutment pressure under the condition of fully mechanized mining in shallow coal seam is studied using the change process of coal pillar stress in disturbed section as the research object. The results of physical simulation experiment show that, after coal mining, due to the collapse of coal seam roof, the overlying strata of key layer will disturb the section coal pillar to different degrees, and the sudden change of degrees of abutment pressure near the coal wall reaches the maximum. Affected by the energy released by the fracture of key stratum, the stress mutation area shifts to the coal wall at a deeper level and the range of plastic zone increases. From the perspective of the numerical simulation, according to the change characteristics of coal pillar abutment pressure in the mining process, the dynamic load process of complex roof strata is divided into three stages: the stage not affected by mining, the stage of dynamic load action, and the stage of static load. In the first stage, the lateral abutment pressure is only affected by the roadway mining, causing stress concentration in the coal body. The stress concentration coefficient is small, and the supporting stress is stable. In the second stage, with the advance of the working face, the coal seam load changes continuously owing to the movement of overlying rock in the goaf, and the lateral abutment pressure changes evidently under the influence of dynamic load. In the third stage, the overlying load forms stress concentration in the coal seam and continuously transfers to the coal wall at a deeper level, which increases the limit equilibrium area of coal body. During this period, the range of plastic zone still increases at a certain rate for a period of time and finally tends to be stable.
机译:用煤柱应力造成良好煤层综合煤矿综采采矿条件下的横向邻接压力的演化定律。物理仿真实验结果表明,在煤矿煤矿后,由于煤层屋顶的崩溃,关键层的覆盖层将扰乱煤柱的不同程度,以及煤层附近的邻接压力突然变化墙壁达到最大值。受关键地层断裂释放的能量影响,应力突变面积在更深层次的煤墙上变化,塑料区的范围增加。从数值模拟的角度来看,根据煤柱邻接压力的变化特性,复杂屋顶地层的动态载荷过程分为三个阶段:舞台不受采矿的影响,动态负荷动态阶段和静载荷的阶段。在第一阶段,横向邻接压力仅受道路挖掘的影响,导致煤体中的应力浓度。应力浓度系数小,并且支撑应力稳定。在第二阶段,随着工作面的前进,煤缝负荷由于覆盖岩石中的覆盖岩体的运动而连续变化,并且在动态载荷的影响下,横向邻接压力显着变化。在第三阶段,覆盖载荷在煤层中的应力浓度形成压力浓度,并在更深的水平下连续转移到煤壁,这增加了煤体的极限平衡面积。在此期间,塑料区的范围仍然在一段时间内以一定的速度增加,最后趋于稳定。

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