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Deformation Mechanism and Stability of a Rocky Slope

机译:岩质边坡的变形机理与稳定性

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摘要

A high slope is located on the side of the spillway at a hydropower station in Southwest China, which has some weak inter-layers inclining outwards. Parts of the slope show heavy weathering and unloading. There appeared deformation and tensile crack either on the surface or on the afteredge of the slope during excavation, and under a platform (elev. 488 m), two levels of slopes collapsed on the downriver side. Based on the investigation in situ and the analysis of the geological structure, the conceptual model of deformation and failure mechanism was erected for this slope. Furthermore, the deformation characteristics were studied with FLAC~(3D) numerical simulation. Comprehensive analysis shows that the whole deformation of the slope is unloading rebound in certain depth scope and the whole body does not slide along any weak interlayer. In addition, two parts with prominent local deformation in the shallow layer of the slope show the models of "creep sliding-tensile cracking" and "sliding-tensile cracking", respectively. Based on the above analysis, the corresponding project of support and reinforcement is proposed to make the slope more stable.
机译:中国西南某水电站溢洪道的一侧有一个高斜坡,斜坡中间有一些薄弱的中间层。斜坡的某些部分显示出严重的风化和卸载。在开挖过程中,在斜坡的表面或后缘上都出现了变形和拉伸裂纹,在一个平台(海拔488 m)下,两级斜坡在下游侧塌陷。在现场调查和地质结构分析的基础上,建立了该边坡变形破坏机理的概念模型。此外,利用FLAC〜(3D)数值模拟研究了变形特性。综合分析表明,该边坡的整体变形在一定深度范围内为卸载回弹,整个主体不沿任何薄弱夹层滑动。另外,在斜坡的浅层中具有明显局部变形的两个部分分别显示了“蠕变滑动拉伸裂纹”和“滑动拉伸裂纹”的模型。在以上分析的基础上,提出了相应的支护方案,使边坡更加稳定。

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