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Coupled disaster-causing mechanisms of strata pressure behavior and abnormal gas emissions in underground coal extraction

机译:地下采煤中地层压力行为与异常瓦斯排放的耦合致灾机制

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The generalization and application of fully mechanized caving with super great mining height (SGMH) face a series of new issues, of which strata pressure behavior and abnormal gas emissions are the most prominent disasters and display a close relationship. The Tashan coalmine was chosen as the experiment base because of its SGMH and the overlying hard and thick main roof (HTMR). This coalmine had experienced many damaging hydraulic support and abnormal gas emission accidents induced by strata pressure behavior. The "Key Strata Theory" and the fracture failure process analysis model established by 3DEC were used to analyze the structural characteristics and fracture failure process of the HTMR. The geostress reduction and permeability enhancement redistribution of the adjacent coal measure strata were studied by the geostress and permeability distribution model established by FLAC 3D. The HTMR controlled the failure extent and the movement evolution of the entire overburden stratum. The HTMR acted as a large double-sided embedded rock beam during primary fracturing and a cantilever-articulated rock beam during periodic fracturing, and it generated a huge hanging space above the gob. The fully mechanized caving with SGMH caused large-scale disturbances and permeability enhancements in the adjacent rock and coal strata. Then, the substantial amounts of gas stored in the remaining coal, surrounding rock strata and adjacent coal seam rushed out and aggregated in the caved and fissured zones of the gob, forming a huge gas warehouse. The strata pressure behavior and abnormal gas emission disasters primarily occurred after the primary and periodic fracturing of the HTMR. These disasters are predominantly caused by the escaping of the abundant gas that existed in the gob during mine pressure behavior processes. When the ultimate broken span was reached, as the HTMR rotated and collapsed, the substantial amounts of gas that accumulated in the gob escaped into the working face, which easily caused abnormal gas emissions. Hydraulic presplitting and gas drainage technologies are proposed to solve these disasters.
机译:超大采高综放开采的推广应用面临一系列新问题,其中地层压力行为和异常瓦斯涌出是最突出的灾害,并具有密切的关系。塔山煤矿因其SGMH和上覆坚硬的厚主顶板(HTMR)而被选为实验基地。该煤矿经历了许多破坏性的水力支撑以及由于地层压力行为引起的异常气体排放事故。利用3DEC建立的“关键层理论”和断裂破坏过程分析模型对HTMR的结构特征和断裂破坏过程进行了分析。利用FLAC 3D建立的地应力和渗透率分布模型,研究了邻近煤系地层的地应力降低和渗透率增强分布。 HTMR控制了整个覆岩层的破坏程度和运动演化。 HTMR在一次压裂过程中起着巨大的双面埋入式岩石梁的作用,而在周期性压裂过程中起了悬臂式铰接的岩石束的作用,并在采空区上方产生了巨大的悬挂空间。 SGMH的综放开采引起了邻近岩石和煤层的大规模扰动和渗透率的提高。然后,剩余的煤,周围的岩层和相邻煤层中储存的大量气体被冲出并聚集在采空区的陷落裂隙区中,从而形成了一个巨大的储气库。地层压力行为和异常气体排放灾害主要发生在HTMR的一次和定期压裂之后。这些灾害主要是由于矿井压力行为过程中采空区中存在的大量瓦斯逸出造成的。当达到最大破裂跨度时,随着HTMR旋转和塌陷,积聚在料滴中的大量气体会逸入工作面,这很容易引起异常的气体排放。为解决这些灾害,提出了液压预裂和瓦斯抽放技术。

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