端帮开采扰动下高陡逆倾复合边坡变形机制研究

    Research on the deformation mechanism of high steep reverse inclined composite slope under disturbance of end slope mining

    • 摘要: 端帮开采作为一种新型开采端帮压煤的方法,为探究其对高陡逆倾复合边坡变形的影响,以某露天矿为工程背景,分析了端帮开采后煤柱群、坡体变形破坏特征,结果表明:端帮煤开采后,重力非线性分布与两边简支、一边固支的边界条件改变了复合边坡的应力变形特征,端帮变形以水平方向为主,排土场变形以沉降为主。沿倾向,煤柱竖向位移与应力曲线先缓后陡变化,中心靠近煤壁侧,水平位移逐渐衰减,塑性破坏程度减小;沿走向,煤柱群变形呈马鞍形,永久煤柱边缘受剪切作用变形成拱形分布,单一采硐及煤柱群上方形成了稳定的岩体结构,顶板应力成拱形分布,塑性区由中心向两侧扩展。复合边坡变形分为剧烈变形区、缓慢变形区、稳定区,坡体前缘变形由与坡面平行转变为斜交,采硐顶板由圆弧剪出滑动变为沉降,变形破坏模式由重力引起的圆弧形滑移转变为煤柱破坏后沉降引起的大范围折线形滑动。由此得出结论:端帮开采使复合边坡变形以沉降为主,在排土场、端帮分区分布,加剧了开采区域坡体的变形,煤柱变形是复合边坡稳定的关键,应力、变形与采深为非线性关系,为非对称分布,破坏程度减小,竖向应力与位移峰值点靠近工作面,水平位移非线性减小,复合边坡的先陡后缓结构与煤层逆倾特征导致的坡体重力非线性分布、端帮开采造成的边界条件差异是煤柱与边坡变形破坏的主要原因。

       

      Abstract: As a new method for mining end slope coal, in order to explore its impact on the deformation of high steep reverse inclined composite slopes, taking a certain open-pit mine as the engineering background, the deformation and failure characteristics of coal pillar groups and slopes after end slope mining are analyzed. The results show that after the end slope coal mining, the nonlinear distribution of gravity and the boundary conditions of simply supported on two sides and fixed supported on one side change the stress deformation characteristics of the composite slope. The deformation of the end slope is mainly in the horizontal direction, and the deformation of the waste dump is mainly settlement. Along the dip direction, the vertical displacement and stress curves of the coal pillars change from gentle to steep. Near the coal wall side of the center, the horizontal displacement gradually attenuates, and the degree of plastic failure decreases. Along the strike direction, the deformation of the coal pillar group is saddle-shaped. The edges of the permanent coal pillars are deformed into an arch-shaped distribution under shear action. A stable rock mass structure is formed above the single mining roadway and the coal pillar group. The roof stress is distributed in an arch shape, and the plastic zone expands from the center to both sides. The deformation of the composite slope is divided into a violent deformation zone, a slow deformation zone, and a stable zone. The deformation of the slope front changes from parallel to the slope surface to oblique intersection. The roof of the mining roadway changes from arc-shaped shear-out sliding to settlement. The deformation and failure mode changes from arc-shaped sliding caused by gravity to large-scale fold-shaped sliding caused by the settlement after the failure of the coal pillars. Thus, it can be concluded that end slope mining makes the deformation of the composite slope mainly settlement, which is distributed in the waste dump and the end slope in a zoned manner, intensifying the deformation of the slope in the mining area. The deformation of the coal pillars is the key to the stability of the composite slope. The stress, deformation and mining depth have a non-linear relationship and are asymmetrically distributed. The degree of damage decreases. The peak points of vertical stress and displacement are close to the working face, and the horizontal displacement decreases non-linearly. The non-linear distribution of slope gravity caused by the steep then gentle structure of the composite slope and the reverse inclined characteristics of the coal seam, as well as the differences in boundary conditions caused by end slope mining, are the main reasons for the deformation and failure of the coal pillars and slopes.

       

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