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Modeling of liquefaction-induced shear deformation

机译:液化引起的剪切变形的建模

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摘要

A constitutive model is developed to reproduce salient aspects associated with seismicallyinduced soil liquefaction (medium to dense clean cohesionless soils). Attention is mainly focused on the deviatoric (shear) stress-strain response mechanism. Soil cyclic shear behavior during liquefaction is modeled to display a significant regain in stiffness nad strength with the increase in deformation during each cycle of applied load. This behavior appears to play a major role in dictating the magnitude of shear deformations as observed in laboratory tests and manifested in acceleration records from earthquakes and centrifuge experiments (clean sands and non-plastic silts). Constitutive model parameters are selected to represent medium, medium-dense and dense clean cohesionless soils. Using these parameters, the resulting model response is presented under simple-shear cyclic loading situations. Further modeling accuracy may be achieved based on a more thorough understanding of the underlying physical processes.
机译:建立了本构模型以重现与地震诱发的土壤液化有关的显着方面(中等至稠密清洁的无粘性土壤)。注意主要集中在偏斜(剪切)应力应变响应机制上。对液化过程中的土壤循环剪切行为进行了建模,以显示在施加载荷的每个周期中,随着变形量的增加,刚度和强度都得到了显着的恢复。这种行为似乎在决定剪切变形的大小方面起着主要作用,如在实验室测试中观察到的那样,并在地震和离心实验(干净的沙子和非塑料淤泥)的加速度记录中得到体现。选择本构模型参数来代表中等,中等密度和致密清洁的无粘性土壤。使用这些参数,可以在简单剪切循环荷载情况下显示模型响应。基于对基础物理过程的更透彻理解,可以实现进一步的建模精度。

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