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Mechanism of Coal Bump among Mine Group under the Control of Large Geological Body: A Case Study of Yima Mining Area, China

机译:大型地质机构控制下矿区煤撞击机制 - 以中国伊马矿区为例

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Coal bump often occurs in coal mining among many working faces in mine group under the control of large geological bodies. In order to study the coal bump mechanism between adjacent working faces under the conditions of large fault and huge thick overburden conglomerate, this paper regards Yima mining area as a practical engineering background and theoretically analyzes the mechanical behavior of overlying rock in the spatial structure. Then, the deep-ground and whole-space measurement is carried out in the 13230 working face of Gengcun mine and 21121 working face of Qianqiu mine. The results show that the basic structural unit in Yima mining area is composed of two goafs, middle coal pillar, and overlying conglomerate. Under the condition of nonsynchronous mining in adjacent working faces, there is a comovement effect similar to lever’s “prying” phenomenon in thick conglomerate beam—the conglomerate strata above larger goaf side induce an overall uplift movement of the corresponding strata above smaller goaf side, and uplift length of the conglomerate strata is related to the mining length, coal pillar width, caving angle, and coal-conglomerate distance. The results of surface subsidence, microseism, and stress in the two working faces verify the conglomerate’s phenomenon of comovement effect and disturbance range and further explain the role of active movement of F16 fault and overall causes of huge thick conglomerate on the coal bump. The vertical stress of the 13230 face is relatively low at the beginning, and high horizontal stress by fault activation causes typical bump accident with the horizontal sliding of coal body. With the increasing development of 13230 face, the intensity and frequency of coal bump in horizontal direction decrease obviously, but with high proportion in vertical direction. The results provide a theoretical basis for the study on the mechanism of coal bump between two adjacent working faces under the conditions of huge thick conglomerate and large thrust fault.
机译:冲击地压往往较大地质体的控制下矿集团的众多工作中的面孔出现在煤矿。为了研究大故障和巨大的厚覆盖砾岩的条件下工作的相邻面之间的煤凸块机构,本文关于义马矿区作为实际工程背景和理论上分析在空间结构上覆岩石的力学性能。随后,深地面和整体空间的测量是在耿村煤矿和矿山千秋的21121工作面的13230工作面进行。结果表明,在义马矿区的基本结构单元是由两个采空区,中煤柱和上覆砾岩。下在相邻的工作面非同步采矿的情况下,有类似于厚砾岩束砾岩地层杠杆的“撬”的现象一联动效果上方的具有较大充填侧诱导上述小充填侧对应的阶层的整体隆起运动,并且砾岩地层的隆起长度是关系到采矿长度,煤柱宽度,崩落角,和煤砾岩距离。地面沉降,微震,并强调在这两个工作面的结果验证了联动效应,干扰范围砾岩的现象,并进一步解释F16断层和对冲击地压巨厚砾岩的总体原因主动运动的角色。在13230面的垂直应力是相对低的开头,并通过故障激活高水平应力导致典型凸点事故与水平滑动煤体。用13230面,强度和在水平方向上减小煤凸点的频率明显,的日益发展,但在垂直方向的高比例。结果提供了对煤凸块的两个相邻的工作表面之间的巨大厚砾岩和大推力故障的条件下的机理研究了理论基础。

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