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Stability analysis of the sliding process of the west slope in Buzhaoba Open-Pit Mine

机译:布扎巴露天矿西斜坡滑坡过程稳定性分析

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To study the stability of the west slope in Buzhaoba Open-Pit Mine and determine the aging stability coefficient during slide mass development, the deformation band of the west slope and the slide mass structure of the 34,600 profile are obtained on the basis of hydrology, geology, and monitoring data.The residual thrust method is utilized to calculate the stability coefficients, which are 1.225 and 1.00 under sound and transfixion conditions, respectively. According to the rock damage and fragmentation and the principle of mechanical parameter degradation, the mechanical models of the slide mass development of the hard and soft rock slopes are established. An integrated model for calculating the slope stability coefficient is built considering water, vibration, and other external factors that pertain to the structural plane damage mechanism and the generating mechanism of the sliding mass. The change curve of the stability coefficient in the slide mass development is obtained from the relevant analyses,and afterwards, the stability control measures are proposed. The analysis results indicate that in the cracking stage of the hard rock, the slope stability coefficient decreases linearly with the increase in the length Lbof the hard rock crack zone. The linear slope is positively correlated to rock cohesion c. In the transfixion stage of the soft rock, the decrease speed of the stability coefficient is positively correlated to the residual strength of the soft rock. When the slope is stable, the stability coefficient is in a quadratic-linear relationship with the decreased height Dh of the side slope and in a linear relationship with anchoring force P.
机译:为了研究布扎坝露天矿西斜坡的稳定性并确定滑坡体发育过程中的时效稳定系数,在水文,地质的基础上,获得了西坡的变形带和34,600剖面的滑坡体结构。残余推力法用于计算稳定系数,在声音和穿透条件下的稳定系数分别为1.225和1.00。根据岩石的破坏和破碎以及力学参数退化的原理,建立了软,硬岩质边坡滑动体发育的力学模型。考虑水,振动和其他与结构面破坏机理和滑动质量产生机理有关的外部因素,建立了计算边坡稳定系数的综合模型。通过相关分析,得出滑坡体发育过程中稳定系数的变化曲线,并提出了稳定控制措施。分析结果表明,在硬岩开裂阶段,边坡稳定系数随硬岩裂缝带长度Lb的增加而线性减小。线性斜率与岩石内聚力c正相关。在软岩的渗透阶段,稳定系数的下降速度与软岩的残余强度成正相关。当坡度稳定时,稳定系数与边坡高度Dh的降低呈二次线性关系,与锚固力P呈线性关系。

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