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首页> 外文期刊>International Journal of Rock Mechanics and Mining Sciences >Simulation of cracking near a large underground cavern in a discontinuous rock mass using the expanded distinct element method
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Simulation of cracking near a large underground cavern in a discontinuous rock mass using the expanded distinct element method

机译:扩展离散元法模拟不连续岩体中大型地下洞室附近的裂缝

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The rock masses in a construction site of underground cavern are generally not continuous, due to the presence of discontinuities, such as bedding, joints, faults and fractures. The performance of an underground cavern is principally ruled by the mechanical behaviors of the discontinuities in the vicinity of the cavern. A number of experimental and numerical investigations have demonstrated the significant influences of discontinuities on the mechanical, thermal and hydraulic behaviors of discontinuous rock masses, indicating that the deformation mechanism and stability of rock structures in the discontinuous rock masses depend not only on the existing discontinuities but also on the new cracks generated and thereafter keep propagating due mainly to the stress redistribution induced by excavation.In this study, an expanded distinct element method (EDEM) was developed for simulating the crack generation and propagation due to the shear and tension failures in the matrix rock blocks. Using this method, excavation simulations of deep underground caverns have been carried out on the models with differing depths of cavern and differing geometrical distributions of the existing discontinuities. Model experiments by using the base friction test apparatus were conducted to verify the proposed numerical approach. Furthermore, the support effects of rock bolts on controlling the deformations of the rock mass surrounding a cavern and movements of key blocks were evaluated by means of the EDEM approach.
机译:由于存在不连续性,例如层理,节理,断层和裂缝,地下洞穴施工现场的岩体通常不连续。地下洞室的性能主要由洞室附近不连续处的力学行为决定。大量的实验和数值研究表明,不连续性对不连续岩体的力学,热力和水力行为有重大影响,表明不连续岩体中岩石结构的变形机制和稳定性不仅取决于现有的不连续性,而且还取决于不连续性。本研究中,开发了一种扩展的离散元方法(EDEM),用于模拟由于剪切和拉伸破坏引起的裂纹的产生和扩展。矩阵岩块。使用这种方法,已经对具有不同深度的洞穴和现有不连续点的几何分布不同的模型进行了深层地下洞穴的开挖模拟。使用基础摩擦测试仪进行了模型实验,以验证所提出的数值方法。此外,通过EDEM方法评估了锚杆对控制洞室周围岩体变形和关键块体运动的支撑作用。

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