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首页> 外文期刊>International journal of geomechanics >Coupled Hydro-Mechanical Elastoplastic Constitutive Model for Unsaturated Sands and Silts. I: Formulation
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Coupled Hydro-Mechanical Elastoplastic Constitutive Model for Unsaturated Sands and Silts. I: Formulation

机译:非饱和砂土的水力-弹塑性耦合本构模型。一:配方

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摘要

Unsaturated soils are three-phase porous media consisting of a solid skeleton, pore water, and pore air. The behavior of unsaturated soils is strongly influenced by the matric suction (pore air pressure minus the pore water pressure). Soil water characteristic curves (SWCCs) describe the relationship between matric suction and water content in unsaturated soils and, therefore, capture the hydro-behavior of soils. SWCCs show hysteretic behavior that not only depends on the wetting or drying history of the soil, but also on the stress-strain history (mechanical behavior) of a soil. The hydro-behavior of unsaturated soils, on the other hand, influences the mechanical behavior through matric suction. To predict the behavior of unsaturated soils, a hysteretic SWCC model is proposed based on the bounding surface plasticity concept. The model for hysteretic SWCCs is then incorporated into a constitutive model for unsaturated sands and silts in the general stress space. The resulting model is a comprehensive constitutive model that accounts for the coupling effects between hydro-and mechanical behavior of unsaturated sands and silts in the general stress space. The numerical integration of the constitutive equations and model calibration and validation are presented in a companion paper.
机译:不饱和土壤是由固体骨架,孔隙水和孔隙空气组成的三相多孔介质。基质吸力(孔隙空气压力减去孔隙水压力)强烈影响非饱和土壤的行为。土壤水分特征曲线(SWCC)描述了基质吸力与非饱和土壤中水分含量之间的关系,因此捕获了土壤的水质行为。 SWCC的滞后行为不仅取决于土壤的湿润或干燥历史,还取决于土壤的应力应变历史(机械行为)。另一方面,非饱和土壤的水力行为会通过基质吸力影响其机械性能。为了预测非饱和土的行为,基于边界表面可塑性概念,提出了一个滞后SWCC模型。然后将迟滞SWCC的模型合并到总应力空间中非饱和砂土和粉砂的本构模型中。生成的模型是一个综合的本构模型,它考虑了总应力空间中非饱和砂土和粉土的水力和力学行为之间的耦合效应。本构方程的数值积分以及模型校准和验证在随附的论文中提供。

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