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A constitutive model for hydromechanically coupled behavior of unsaturated soils with hydraulic hysteresis

机译:液压滞后的不饱和土的流体力学耦合行为的组成模型

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摘要

There are several constitutive models developed for understanding coupled hydromechanical behavior of three phase medium of unsaturated soils as well as models for explaining hydraulic hysteresis in water retention. However, very few attempts that merge the two aspects of behavior are available. This study develops a one-way coupled model for understanding the hydromechanical behavior of unsaturated soils. In addition to the hysteresis between main drying and wetting retention curves, the model considers non-uniqueness of retention behavior resulting from void ratio changes due to compression under the stress application. As for the elastoplastic stress strain relationship of soil skeleton, the model is based on the formulation of classical plasticity relying on the critical state concept. Consequently, volumetric deformation due to wetting-drying cycles and its effect on elastoplastic behavior through simultaneously changing matric suction is modeled. Model results are calibrated with the results of isotropic compression stages of triaxial tests at both constant suction and constant water content conditions.
机译:有几个组成型模型,用于了解不饱和土的三相介质的耦合流体力学行为以及用于解释水保留中水力滞后的模型。但是,很少几次合并行为的两个方面的尝试。该研究开发了一种用于理解不饱和土的流体机械行为的单向耦合模型。除了主干和润湿保留曲线之间的滞后之外,该模型还考虑了由于压缩在应力施加下的压缩而导致的保留行为的非唯一性。至于土壤骨架的弹塑性应力应变关系,该模型基于依赖于临界状态概念的古典塑性的配方。因此,建模了由于润湿干燥循环引起的体积变形及其对弹性塑性行为通过同时改变测力抽吸的影响。模型结果校准了在恒定抽吸和恒定水含量条件下三轴试验的各向同性压缩阶段的结果。

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