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Stability analysis of underground space with discontinuous planes using a four-node iso-parametric element numerical manifold method with rigid body rotation

机译:具有刚体旋转的四节点等参单元数值流形方法在不连续平面地下空间稳定性分析中的应用

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u In a large-scale rock structure with discontinuous planes in a rock mass, the pattern of the discontinuous planes strongly influences the deformation and stress distribution behaviors along the structure. A jointed rock mass, however, is generally assumed to be partially and imperfectly connected rather than completely discontinuous. Earlier the authors presented an elastic-plastic analysis of a discontinuous model of a jointed rock mass using a four-node iso-parametric manifold method (Sasaki and Ohnishi, 2001). The authors adapted Drucker-Prager's elastic-plastic yield criterion, the Jaumann co-rotational derivative to determine the objectivity of stresses for rotation, and a rock-bolting element.In discontinuous models such as the original numerical manifold method (NMM), however, rigid rotation is not introduced in the degrees of freedom in the manner seen in the conventional finite element method (FEM). This paper describes the co-rotational formulation theory (Crisfield and Moita, 1996) introduced for a four-node iso-parametric NMM, along with examples of a model of rockfall activity in underground space. The results compare very well with the values obtained without a rigid body rotation analysis, especially those obtained for block shapes with large rotations.
机译:u在岩体中具有不连续平面的大型岩石结构中,不连续平面的样式强烈影响沿结构的变形和应力分布行为。然而,通常认为节理岩体是部分不完美连接的,而不是完全不连续的。早些时候,作者使用四节点等参流形方法对节理岩体的不连续模型进行了弹塑性分析(Sasaki and Ohnishi,2001)。作者采用了Drucker-Prager的弹塑性屈服准则,Jaumann同向导数来确定旋转应力的客观性以及锚杆锚固元素,但是在不连续的模型中,例如原始的数值流形方法(NMM),刚性旋转不会像传统的有限元方法(FEM)那样以自由度引入。本文介绍了针对四节点等参NMM引入的同向旋转理论(Crisfield和Moita,1996),并举例说明了地下空间中的落石活动模型。该结果与没有进行刚体旋转分析时获得的值进行了很好的比较,特别是对于具有大旋转量的块形状获得的值。

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