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DEM simulation of small strain and large strain behaviors of granular soils with a coherent contact model

机译:基于相干接触模型的颗粒土小应变和大应变行为的DEM模拟

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摘要

Abstract Discrete element method is widely used to study the macroscopic behaviors of granular soils subjected to various loading conditions at a particulate level. However, most of previous studies used different contact models to simulate soil behaviors at different strain levels. To reconcile the disparities between different contact models in DEM simulation, a modified rolling resistance Hertz-Mindlin model is proposed for simultaneously emulating distinct behaviors of granular soils at both small strain and large strain. The Hertz-Mindlin contact model is used to capture the stress-dependent small strain stiffness, while the rolling resistance model is adopted to capture the main effect of particle shape. Contact stiffness degradation is also taken into consideration in the simulation. The comparisons with experimental data show that the model used in this paper can effectively capture the essential features of soil behaviors at both small and large strains in drained and undrained triaxial shear tests. The results indicate that contact stiffness degradation during shearing should be considered for avoiding irrationally high negative excess pore water pressure in undrained triaxial shearing. Incorporation of rolling resistance into the contact model is necessary for reaching a reasonably high critical state stress ratio arising from particle shape.Graphical abstract
机译:摘要 离散元法被广泛用于研究颗粒土在颗粒水平上不同荷载条件下的宏观行为。然而,以前的大多数研究都使用不同的接触模型来模拟不同应变水平下的土壤行为。为了调和DEM模拟中不同接触模型之间的差异,该文提出一种改进的滚动阻力Hertz-Mindlin模型,用于同时模拟粒状土在小应变和大应变下的不同行为。采用Hertz-Mindlin接触模型捕捉应力相关的小应变刚度,采用滚动阻力模型捕捉颗粒形状的主要效应。在仿真中还考虑了接触刚度退化。与实验数据的对比表明,本文采用的模型能够有效地捕捉排水和不排水三轴剪切试验中小应变和大应变下土体行为的本质特征。结果表明,为了避免不排水三轴剪切过程中出现不合理的负过孔隙水压力,应考虑剪切过程中接触刚度的退化。将滚动阻力纳入接触模型对于达到由颗粒形状引起的合理高临界状态应力比是必要的。图形摘要

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