浅埋煤层开采触发岩溶坡体崩滑机制研究

Mechanism of karst slope slide and slip triggered by shallow buried coal seam mining

  • 摘要: 以贵州省纳雍县张家湾镇普洒村发生特大型滑坡事件为例,经过地质调查,可知滑坡的主滑动方向为310°,长720 m,宽360~380 m,整体体积约82.3×104 m3,认定为中型滑坡。坡体地层岩性由上二叠统龙潭组、长兴-大隆组和下三叠统夜郎组构成,显示出古气候变化与沉积环境的演变。坡体稳定性受多种因素影响,包括微地貌、岩性组合、坡体构造与风化作用等主导因素,以及采空区、强降雨和采掘爆破振动等触发因素。为研究坡体崩滑,采用二维离散元数值方法构建了数值模型,考虑了多层采煤层的相互作用,模拟了不同荷载下的变形与破坏特征。研究表明,煤层开采、强降雨和爆破振动对坡体稳定性有显著影响,为进一步的滑坡防治提供了科学依据。

     

    Abstract: A mega landslide incidence occurred in Pusa Village, Zhangjiawan Town, Nayong County of Guizhou Province was taken as an example.After geological investigation, we found the main sliding direction of the landslide was 310°,with a length of 720 m, a width of 360~380 m, and an overall volume of about 82.3×104 m3,which was recognized as a medium-sized landslide.The stratigraphic lithology of the slope body consists of the upper permian longtan formation, changxing-dalong formation, and the lower triassic yelang formation, showing the evolution of paleoclimate changes and depositional environment.Slope stability is affected by a variety of factors, including dominant factors such as microgeomorphology, lithologic assemblage, slope structure and weathering, as well as triggering factors such as goaf, strong rainfall and vibration of mining and blasting.In order to study the slope failure and slide, a numerical model was constructed using a two-dimensional discrete element numerical method, which considered the interaction of multi-layer coal mining seams and simulated the deformation and failure characteristics under different loads.The study shows that coal seam mining, heavy rainfall and blasting vibration have a significant effect on slope stability.

     

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