College of Geoscience and Surveying Engineering, China University of Mining and Technology-Beijing, Beijing 100083, China.
School of Mining Engineering, Taiyuan University of Technology, Taiyuan 030024, China.
Comput Intell Neurosci. 2022 May 13;2022:1698220. doi: 10.1155/2022/1698220. eCollection 2022.
Due to unique landform and lithological features of the loess gully area, the geological disasters caused by coal mining have become more complex. Moreover, the advancing direction of the working face has an important influence on the deformation of the slope on both sides of the gully. In this paper, combined with the specific conditions of a coal mine working face in western China, we use the method of particle flow numerical simulation and theoretical analysis to examine and observe the deformation, as well as characteristics of failures in the loess gully area under different mining directions of the working face. The deformation process of the gully area can be obtained by combining the numerical simulation results. According to different mining directions of the working face, the failure mode of mining in the loess gully area was divided into the back slope and along slope advancing failure modes. Through empirical evaluation, our investigation demonstrates that the bottom of the gully was damaged seriously by both along slope mining and back slope mining. Albeit the influence of coal seam excavation on the slope surface was relatively small; however, it is greater on the flat ground of the upper slope. Under the same mining conditions, the advancing direction of the working face affected the horizontal movement of the loess gully area but had less effect on the subsidence. Furthermore, we observed that the failure mode of the mining slope is highly correlated with the mining direction and relative position of the working face. The results obtained from this research can provide useful information for deformation and failure prediction, working face mining method, and geological disaster assessment in the loess gully area.
由于黄土沟壑区独特的地形地貌和岩土特征,采煤引发的地质灾害变得更加复杂。此外,工作面的推进方向对沟谷两侧边坡的变形有重要影响。本文结合中国西部某煤矿工作面的具体条件,采用颗粒流数值模拟和理论分析的方法,考察和观测了不同工作面推进方向下黄土沟壑区的变形及失稳特征。通过数值模拟结果的结合,得到了沟谷区的变形过程。根据工作面的不同推进方向,将黄土沟壑区采煤的失稳模式分为顺坡推进和沿坡推进两种模式。通过经验评价,研究表明,顺坡开采和逆坡开采都对沟底造成了严重的破坏,尽管煤层开采对坡面的影响相对较小,但对坡顶平地的影响较大。在相同的开采条件下,工作面的推进方向影响黄土沟壑区的水平移动,但对沉降的影响较小。此外,我们还观察到,采煤边坡的失稳模式与工作面的开采方向和相对位置密切相关。本研究的结果可为黄土沟壑区变形和失稳预测、工作面开采方法和地质灾害评价提供有用信息。