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Micro-scale modeling of saturated sandy soil behavior subjected to cyclic loading

机译:循环荷载作用下饱和砂土行为的微观模型

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摘要

Liquefaction induced damage to the built environment is one of the major causes of damage in an earthquake. Since Niigata earthquake in 1964, it has been popularly recognized that the liquefaction induced ground failures caused severe damage in various forms such as sand boiling, ground settlement, lateral spreading, landslide, etc. Since then, understanding the mechanism of liquefaction phenomena became very important to take measures against the liquefaction induced ground failures. To understand the mechanism of liquefaction, it is important to consider the soil as an assemblage of particles. A continuum approach may fail to explain some of the phenomena associated with liquefaction. Discrete approach, such as distinct/discrete element method (DEM), is an effective method that can simulate the mechanism of liquefaction and associated phenomena well at the microscopic level.In this study, a new three-dimensional DEM model is developed to study the liquefaction and its associated phenomena. The hollow cylindrical torsion test under undrained condition, which replicates the ground condition before and during the earthquake well, is simulated using the newly developed model. A vertical strip from the hollow cylindrical specimen is considered in the study and the boundaries in the tangential direction are numerically connected to simulate the continuity in tangential direction. The liquefaction study is carried out by strain control shearing at the top while keeping the bottom plate fixed. The cyclic mobility, which is observed in saturated sands when subjected to cyclic shearing, is predicted by the proposed model. The effect of particle rotation on the development of dynamic pore water pressure is also investigated using the model. Also, sand boiling is simulated using the proposed model.
机译:液化引起的对建筑环境的破坏是地震破坏的主要原因之一。自1964年新泻地震以来,人们普遍认识到,液化引起的地面破坏以各种形式造成严重破坏,例如砂沸腾,地面沉降,侧向扩展,滑坡等。从那时起,了解液化现象的机理就变得非常重要。采取措施防止液化引起的地面破坏。要了解液化的机理,重要的是将土壤视为颗粒的集合体。连续方法可能无法解释与液化有关的某些现象。离散方法(例如离散/离散元素方法(DEM))是一种可以在微观水平上很好地模拟液化机理和相关现象的有效方法。在本研究中,我们开发了一种新的三维DEM模型来研究该模型。液化及其相关现象。使用新开发的模型模拟了不排水条件下的空心圆柱扭转试验,该试验模拟了地震之前和地震期间的地面情况。在研究中考虑了空心圆柱试样的垂直条,并沿切线方向的边界进行了数值连接,以模拟切线方向的连续性。液化研究是通过在顶部保持应变板的同时进行应变控制剪切来进行的。所提出的模型预测了在周期性剪切作用下在饱和砂土中观察到的循环迁移率。使用该模型还研究了颗粒旋转对动态孔隙水压力发展的影响。此外,使用所提出的模型模拟了砂沸腾。

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