Zhao Hongze, Lu Yan, Qin Binde, Hao Qiang, Sun Yu
School of Energy and Mining Engineering, China University of Mining and Technology (Beijing), Beijing, 100083, China.
State Key Laboratory of Deep Rock Mechanics and Underground Engineering, China University of Mining and Technology (Beijing), Beijing, 100083, China.
Heliyon. 2024 Jul 19;10(14):e34891. doi: 10.1016/j.heliyon.2024.e34891. eCollection 2024 Jul 30.
Wind-blow sand (WBS) is widely distributed in the "Desert Gobi" region. This study is aimed at exploring the mechanism of how different thicknesses of the WBS layer influence the slope movement of external dumps in open-pit mines. To achieve this aim, the slope of the external dump in the open-pit mining area of Panel 3 in Daliuta Coal Mine was taken as the research object. First, similar simulation experiments were performed for investigating the failure modes and deformation characteristics of the external dump slopes under three geo-morphological conditions: loess base, 10-m-thick WBS base, and 20-m-thick WBS base, respectively. The following results were obtained from the experiments. For the slope with a loess base, its failure is mainly caused by circular sliding from the dump to the interior of the loess layer. For the slope with a 10-m-thick WBS base, the sliding mode involves circular sliding from the dump area to the interior of the WBS layer, linear sliding along the WBS base, and shearing along the foot of the dump area. For the slope with a 20-m-thick WBS base, the sliding mode is circular sliding from the dump area to the interior of the WBS layer. Besides, the sliding area of the dump slope expands as the WBS layer thickens. Furthermore, the results of similar simulation experiments were verified by the finite difference software FLAC based on the strength reduction method, and an equation of relationship between the safety factor of the dump slope with a WBS base and the thickness of the WBS layer was derived.
风沙(WBS)广泛分布于“沙漠戈壁”地区。本研究旨在探究不同厚度的WBS层对露天矿外排土场边坡移动的影响机制。为实现这一目标,以大柳塔煤矿3盘区露天采场的外排土场边坡为研究对象。首先,分别针对黄土基底、10米厚WBS基底和20米厚WBS基底三种地貌条件下的外排土场边坡进行相似模拟试验,研究其破坏模式和变形特征。试验得到以下结果。对于黄土基底边坡,其破坏主要由从排土场向黄土地层内部的圆弧滑动引起。对于10米厚WBS基底边坡,滑动模式包括从排土场区域向WBS层内部的圆弧滑动、沿WBS基底的直线滑动以及沿排土场区域坡脚的剪切。对于20米厚WBS基底边坡,滑动模式为从排土场区域向WBS层内部的圆弧滑动。此外,排土场边坡的滑动面积随WBS层厚度增加而扩大。再者,基于强度折减法,利用有限差分软件FLAC对相似模拟试验结果进行验证,并推导了WBS基底排土场边坡安全系数与WBS层厚度之间的关系式。