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An endochronic approach in modeling liquefaction of sand

机译:砂土液化建模的内时方法

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Liquefaction is the transformation of cohesionless saturated soil skeleton from loose to densernstate causing reduction of shearing resistance due to increase in pore water pressure and drop in effective stress.rnUnderstanding the liquefaction behaviour is limited mainly to empirical approaches, although progress hasrnbeen made in constitutive modeling, models which could account for the volumetric changes due to variationsrnin effective stress and that could realistically capture the liquefaction phenomenon were seldom achieved. Inrnthe present study a pseudo coupled endochronic viscoplastic constitutive model is developed to study thernliquefaction behaviour of sands. Endochronic model is based on the observation of the state of stress in thernneighborhood of a point in a plastic material and rapidity of deformation of the neighborhood. The modelrnincorporated in to FLAC3D using user defined constitutive model is validated with static and cyclic triaxial testrndata and is found to predict accurately the liquefaction phenomenon.
机译:液化是指无粘性的饱和土壤骨架从松散状态转变为致密状态,由于孔隙水压力的增加和有效应力的下降而导致抗剪强度的降低。尽管本构模型已取得进展,但了解液化行为主要限于经验方法,很少能建立模型来解释有效应力变化引起的体积变化,并不能真实地捕捉到液化现象。在本研究中,建立了伪耦合的内期粘塑性本构模型来研究砂的液化行为。内时模型基于对塑料材料中某点附近的应力状态和邻域变形速度的观察。使用静态和循环三轴试验数据验证了使用用户定义的本构模型并入FLAC3D的模型,并发现该模型可准确预测液化现象。

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