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Numerical simulations of pattern evolution of shear bands during pure shear of geomaterials

机译:岩土材料纯剪切过程中剪切带模式演化的数值模拟

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Numerical simulations with finite element method were carried out and five types of patterns of shear bands and their process of self-organization were obtained. The elasto-plastic theory of constitutive relationship with the non-associated flow rule, vertex-like yielding surfaces and strain softening of strength were adopted to describe the mechanical behavior of geomaterials of rock or soil. The non-symmetrical matrix due to the adoption of the non-associated flow rule was solved with the algorithm of dynamical relaxation of finite element method. The discrete or banded patterns of shear strain in the form of superlattice, parallel strips, super lattice turned parallel strips, rhomboid net and concentric rhomboid loops, were gradually formed as the loading increased. The mechanism of the structural pattern generation and the process of pattern self-organization in geomaterials of rock and soil were a process of mechanical equilibrium of stresses and the allocation of material deformation between the elastic sites and plastic sites. The approach provided a way for researching mechanical origin of shear band pattern. (C) 2015 Elsevier B.V. All rights reserved.
机译:进行了有限元数值模拟,得到了五种剪切带模式及其自组织过程。采用弹塑性本构关系和非关联流动规律,顶点状屈服面和强度应变软化理论来描述岩石或土壤土工材料的力学行为。通过有限元方法的动态松弛算法解决了由于采用非关联流规则而引起的非对称矩阵。随着载荷的增加,剪切应变的离散或带状形式逐渐形成,包括超晶格,平行带,超晶格转向平行带,菱形网和同心菱形环。在岩石和土壤的土工材料中,结构模式产生的机理和模式自组织的过程是应力的机械平衡过程以及弹性部位和塑性部位之间材料变形分配的过程。该方法为研究剪切带模式的机械起源提供了一种方法。 (C)2015 Elsevier B.V.保留所有权利。

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