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An Elastoplastic Constitutive Model of Unsaturated Soils with Coupling of Capillary Hysteresis and Skeletal Deformation

机译:毛细滞回与骨架变形耦合的非饱和土弹塑性本构模型

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摘要

A constitutive model of unsaturated soils coupling skeletal deformation and capillary hysteresis is developed based on the modified Cam-clay model.To describe the effect of capillary hysteresis on skeletal deformation,an evolution equation is first developed for the degree of saturation to characterize the soil-water states under arbitrary drying/wetting conditions,and then a new hardening function is proposed,in which the matric suction and the degree of saturation as well as the plastic volumetric strain are simultaneously introduced to represent the hardening effect.It is shown that the proposed hardening function can properly capture the difference of preconsolidation pressure under different soil-water states and effectively describe the effect of drying/wetting history on the skeletal deformation.Theoretical simulations are compared to the experimental data available in the literature,showing that the new model captures very well the main features of unsaturated soil behavior.Unlike other unsaturated soil models,the new model treats the degree of saturation as an internal variable,whose evolution equation explicitly accounts for the capillary hysteresis.The new model can smoothly transit to the modified cam-clay model of saturated soils when the degree of saturation becomes one.The new constitutive model is implemented into a finite element code,U-DYSAC2,in which the displacement of solid skeleton,pore pressure and air pressure are primary nodal unknowns.An implicit algorithm is developed to integrate the constitutive relation at the Gaussian-point level.The proposed numerical procedure is used to simulate a typical two-dimensional unsaturated soil problem,illustrating the applicability and capabilities of the new numerical procedure.
机译:在修正的Cam-clay模型的基础上,建立了一个非饱和土的本构模型,其耦合了骨架变形和毛细滞后作用。为了描述毛细滞后作用对骨架变形的影响,首先针对饱和度建立了一个演化方程,以表征土壤-在任意干燥/湿润条件下保持水状态,然后提出了一种新的硬化功能,其中同时引入了基质吸力和饱和度以及塑性体积应变来表示硬化效果。硬化函数可以正确捕捉不同土壤-水状态下预固结压力的差异,并有效地描述干燥/润湿历史对骨骼变形的影响。将理论模拟与文献中的实验数据进行比较,表明新模型可以捕捉到非常好的非饱和土行为的主要特征。与其他非饱和土模型一样,新模型将饱和度视为一个内部变量,其演化方程明确考虑了毛细管滞后现象。当饱和度达到饱和度时,新模型可以平滑地过渡到改进的饱和黏土模型新的本构模型被实现为有限元代码U-DYSAC2,其中固体骨架的位移,孔隙压力和气压是主要的节点未知数。开发了一种隐式算法,以对高斯本构关系进行积分本文提出的数值程序用于模拟一个典型的二维非饱和土问题,说明了新数值程序的适用性和功能。

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  • 会议地点 Beijing(CN)
  • 作者单位

    State Key Laboratory of Geomechanics and Geotechnical Engineering,Institute of Rock and Soil Mechanics,Chinese Academy of Sciences,Wuhan 430071,China;

    State Key Laboratory of Geomechanics and Geotechnical Engineering,Institute of Rock and Soil Mechanics,Chinese Academy of Sciences,Wuhan 430071,China;

    Gulin University of Technology,Guilin 541004,China;

    State Key Laboratory of Geomechanics and Geotechnical Engineering,Institute of Rock and Soil Mechanics,Chinese Academy of Sciences,Wuhan 430071,China;

    State Key Laboratory of Geomechanics and Geotechnical Engineering,Institute of Rock and Soil Mechanics,Chinese Academy of Sciences,Wuhan 430071,China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 土力学、地基基础工程;
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