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Numerical simulation on slope stability analysis considering anisotropic properties of layered fractured rocks: a case study

机译:考虑层状裂隙岩各向异性特性的边坡稳定性数值模拟研究

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摘要

Anisotropy is one of the natural properties of layered fractured rock, and it plays an important role in slope stability analysis, which is a vital problem in the geotechnical engineering. However, in the present engineering design, rock mass is simply treated as isotropic material, which fails to take into account the anisotropic properties. This work begins with formulizations of the anisotropic seepage-stress coupled model for the layered fractured rock slope stability analysis based on the equivalent continuum theory. Next, the model is applied in the numerical simulation of the southern slope of an open-pit mine in China to understand the mechanism of the existing failure strain as well as the failure mechanism of the potential landslide. The computed water table and damage zone have been compared with the field measurements and found to be in good agreement with field observations. Finally, the effective measures to prevent the slope failure and strengthen the slope stability have been suggested. The proposed model successfully applied in the case study indicated that it is much more feasible and efficient comparing with using the traditional isotropic coupled model in such layered fractured rock slopes stability problems.
机译:各向异性是层状裂隙岩的自然属性之一,它在边坡稳定性分析中起着重要的作用,这是岩土工程中一个至关重要的问题。然而,在当前的工程设计中,岩体仅被视为各向同性的材料,这没有考虑到各向异性的特性。这项工作从基于等效连续体理论的层状裂隙岩体边坡稳定性分析的各向异性渗流-应力耦合模型的建立开始。接下来,将该模型应用于中国露天矿南坡的数值模拟中,以了解现有破坏应变的机理以及潜在滑坡的破坏机理。计算出的水位和破坏区已与现场测量结果进行了比较,发现与现场观察结果非常吻合。最后,提出了防止边坡破坏和加强边坡稳定性的有效措施。在案例研究中成功应用的拟议模型表明,在这种层状裂隙岩体边坡稳定性问题中,与使用传统的各向同性耦合模型相比,该模型更加可行和有效。

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