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Study on movement of surrounding rock and instability mechanism of rock mass structure in steeply dipping seam mining

机译:岩体结构周围岩石和不稳定机制在陡峭浸渍缝煤矿中的运动研究

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Steeply dipping seam refers to the coal seam with dipping angle in the range of 35°~55°, which is well recognized to be very hard to mine by the mining industry all the world.Based on physical simulation test, some fundamental researches focused on the rock strata breaking and moving process, Rock structure stability mechanism and control provide a theoretical basis for mining safely and efficiently in steeply dipping seam.The results indicated that time sequence and unbalance are main caving traits of main roofs, In tendency direction, the bedding separation initially emerge at the upper position (two-thirds) of roof beams, which induces tensile failure and roof caving shifting towards the upper parts of working face, which results in the critical layer zone conversion and change along inclination, forming scalar structure.Mechanics model and stability criterion of scalar structure is established and destabilization model of critical layer rock is revealed.
机译:陡峭的浸渍缝是指煤层的倾斜角度在35°〜55°的范围内,这很容易被矿业行业难以通过全球矿业造型。基于物理仿真试验,一些基本研究侧重于岩石地层破碎和移动过程,岩石结构稳定性机制和控制提供了在陡峭的浸湿接缝中安全有效地开采的理论依据。结果表明时间序列和不平衡是主屋顶的主要塌陷性状,趋势方向,床上用品分离最初在屋顶梁的上部位置(三分之二)出现,这引起拉伸失效和屋顶塌陷朝向工作面的上部换档,这导致临界层区转换和沿倾斜变化,形成标量结构。建立标量结构的模型和稳定性标准,揭示了临界层岩石的稳定化模型。

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