坑壁稳定性分析-案例研究*

M. Affam, K. Allen
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摘要

长期以来,露天矿围岩稳定性在设计和经济上的重要性一直是岩石力学研究的热点问题。难以察觉的缓慢群众运动是导致重大坑壁失效的一个秘密因素。该问题与具体地点有关,并与应力发展、剪切强度、不连续面方向和地下水状况有关。因此,本文着手介绍了在加纳Birimian环境中一些选定的坑壁稳定性分析。特别是在下盘和沿着斜坡面的氧化岩、过渡岩和新鲜(硫化物)岩石材料进行了一些姿态测量。地质数据采用罗曼纳边坡质量等级(SMR)分析程序,并通过安装的棱镜监测坑壁。氧化/过渡区下盘的SMR定量值为43.1,上盘的SMR定量值为44,表明在500o处部分稳定。新鲜岩石(硫化物)在下盘的值为64,表明稳定在55度。与往常一样,根据SMR评估,与氧化物和过渡材料相比,新鲜岩石的问题较少。观察到蠕变运动占主导地位,在氧化带内接近250毫米/天,但在过渡和新鲜岩石中较小。Birimian内部的诱导坑壁破坏模式更多的是复合破坏(即;如果不加以控制,可能会破坏几个坑的稳定。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Pitwall Stability Analysis-Case Studies*
The importance of pitwall stability in design and economy of open pits has been a subject of considerable research in rock mechanics for some time now. Imperceptible slow mass movement has been a secret agent in inducing major pitwall failure. The problem is location specific and is associated with stress development, shear strength, discontinuity orientations and groundwater regimes. This paper therefore sets out to present pitwwall stability analysis in some selected pits within the Birimian environment in Ghana. Several attitude measurements were taken particularly on the footwall and along the slope face of the oxide, transition and fresh (sulphide) rock materials from some selected pits. The geologic data was subjected to the Romana’s Slope Mass Rating (SMR) analytical procedure and the pitwalls monitored through installed prisms. The oxide/ transition zones gave an SMR quantitative value of 43.1 in the footwall and 44 within the hangingwall, indicating a partial stability at 50o. The fresh rock (sulphide) gave a value of 64 in the footwall showing stability at 55o. As usual, the fresh rock was less problematic as indicated by the SMR assessment compared to the oxide and the transition materials. Creep movement was observed to predominate, being nearly 250 mm/day within the oxidised zone but lesser in the transition and fresh rocks. Induced pitwall failure pattern within the Birimian was more of composite failure (ie.,planar and toppling) capable of destabilising several pits if unchecked.
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