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Spreading of Ground Pressure Fluctuation in the Gob

机译:GOB中地压波动的传播

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We address the problem of the stochastic nature of ground pressure manifestation. Stress distribution in a rock mass and ground irreversible movement are governed with a set of random factors that affect the over-peak strength of the rocks, making them extremely sensitive to any perturbation of the external environment and to internal fluctuations of the thermodynamic state of the rock. We investigate the fluctuation evolution during a longwall face movement to find out whether the fluctuation dissipates or builds up. Five adjacent powered support failures simulate the ground pressure fluctuation. The main roof has been presented as a plate that reposed on the rigid base. The stiffness of the base depends on the thickness of the extracted coal seam and on the dilation of the caving roof. Maximum stiffness occurs in situ, and minimum stiffness is in the gob when the roof is highly flexible and subsides elastically, without caving. The more stress acts in the roof, the higher the cavity that occurs and the larger increment of the base stiffness. The wave of the fluctuation has extended both to the direction of the longwall advance and along the face from the point of the fluctuation agitation. There was an incubation period when the fluctuation was negligible, and the process of the main roof caving remained unaffected. The distance of the longwall advance during the incubation period was twice the longwall length when the fluctuation magnitude was 1% relative to the maximum possible disturbance and 0.76 of the longwall length for the magnitude of 24%. However, the pattern of the roof caving has dramatically changed during further movement of the longwall. All caving parameters have changed: step of the caving, ground pressure distribution, and the manifestation in the longwall and entries. A histogram of the fluctuation magnitude is symmetric in accordance with normal distribution. However, the distribution has abnormal excess. These findings are the first step toward answering the question whether it is possible to forecast the process of main roof caving and weighting consistently. Our preliminary conclusion is that the space and time intervals where this prediction can be made with certain reliability are limited, so further investigation is needed.
机译:我们解决了地面压力表现的随机性质问题。岩体中的应力分布与地面不可逆运动受到一组随机因素,影响岩石的过峰强度,使它们对外部环境的任何扰动非常敏感,以及热力学状态的内部波动岩石。我们在长墙面运动期间调查波动演变,以了解波动是否耗尽或建立起来。五个相邻的动力支持故障模拟地压波动。主屋顶已作为刚性底座置于刚性底座的板上。碱的刚度取决于提取的煤层的厚度和凹坑屋顶的扩张。当屋顶高度柔韧并弹性地,在GOB中,最大刚度发生在原位上,并且在没有洞穴的情况下弹性柔韧性并且在没有洞穴的情况下消退。屋顶的压力越多,腔的腔腔越高,并且基础刚度的较大增量越大。波动的波浪从波动搅动的点延伸到长壁前进的方向和沿着面部的方向。当波动可忽略不计时,存在潜伏期,并且主屋顶洞的过程保持不受影响。当波动幅度相对于最大可能的干扰和0.76的长壁长度为24%时,长壁前进期在孵育期间的距离是长壁长度的两倍。然而,在长壁的进一步运动期间,屋顶腔的图案显着改变。所有洞穴参数都发生了变化:洞穴,地面压力分布和长墙和条目中的表现。根据正态分布,波动幅度的直方图是对称的。但是,分布过剩异常。这些发现是回答问题的第一步,无论是否可以持续地预测主屋顶洞穴和加权的过程。我们的初步结论是,可以通过某种可靠性进行该预测的空间和时间间隔是有限的,因此需要进一步调查。

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