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Numerical Simulation of Meso-mechanism of Liquefaction in Saturated Stratified Silty Sands

机译:饱和分层粉状液化中液化机理的数值模拟

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Constant volume equivalent undrained testing is performed under cyclic loading by the PFC~(2D) model, and the liquefaction behavior of saturated stratified silty sands is discussed from the viewpoint of meso-mechanism. Meso-scale parameters such as co-ordination number, distribution of contact normal and contact forces are studied under cyclic loading. Some results are obtained. The important factors which control the macro-response of saturated stratified silty sands are the average co-ordination number, distribution of contact normal and contact forces at mesomechanical level. The major characteristics of deformation are stress-induced anisotropy and fabricinduced anisotropy. And the liquefaction behavior of loose saturated stratified silty sands is mainly due to continued and cumulative loss of the co-ordination number under cyclic loading. Numerical simulation can describe the liquefaction behavior of saturated stratified silty sands. The meso-fabric evolutions including co-ordination number, distribution of contact normal and contact forces can be analyzed during liquefaction induced by cyclic loading. Numerical simulation can also be used to illustrate and verify a theoretical relationship between measures of macro- and meso-scopic parameters that describe the anisotropy in contact forces and contact orientations.
机译:通过PFC〜(2D)模型在循环加载下进行恒定体积等效的未润湿测试,从中间机构的观点来看,讨论了饱和分层粉状的液化行为。在循环载荷下,研究了诸如协调号的中间级参数,如协调号,接触正常和接触力的分布。一些结果是获得的。控制饱和分层粉末宏观响应的重要因素是平均协调数量,在脱模机械水平下接触正常和接触力的分布。变形的主要特征是应激诱导的各向异性和织物诱导的各向异性。松动饱和分层粉状砂的液化行为主要是由于循环载荷下的协调数量的持续和累积损失。数值模拟可以描述饱和分层粉状砂的液化行为。在通过循环载荷诱导的液化期间,可以分析包括协调数的中间结构演进,接触正常和接触力的分布。数值模拟也可用于说明和验证宏观和中间基调参数的措施之间的理论关系,该参数描述了接触力和接触方向的各向异性。

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