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Constitutive model with double yield surfaces of freeze-thaw soil considering moisture migration

机译:考虑水分迁移的冻融土双屈服表面的本构模型

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In cold regions, the effects of moisture migration will destroy the original structure of the soil and cause the redistribution of moisture inside the soil. In order to research the effects of moisture migration on soil's mechanics behaviors under freeze-thaw cycles, an elastoplastic constitutive model with double yield surfaces considering moisture migration was proposed based on the internal state variables (ISV) theory. The amount of moisture migration was obtained by the segregation potential model and used as an intrinsic variable to obtain the Helmholtz free energy function coupled with the amount of moisture migration. Two kinds of plastic deformation mechanisms, including plastic volumetric compression and plastic shear, were considered to develop the coupled model based on the ISV theory with moisture migration. This model was given in incremental form, and detailed numerical calculation processes were described. The proposed model was concretized with elliptic-parabolic yield surfaces and validated by tests under different freeze-thaw cycles and different confining pressure. Desirably, the calculated deviatoric stress-axial strain curves and volumetric strain-axial strain curves agreed well with the test results.
机译:在寒冷的地区,水分迁移的影响将破坏土壤的原始结构,并导致土壤内部的湿润再分布。为了研究水分迁移对冻融循环下的土壤力学行为的影响,基于内部状态变量(ISV)理论,提出了一种考虑水分迁移的双屈服表面的弹塑性本构模型。通过分离电位模型获得水分迁移量,并用作固有变量,以获得与水分迁移量相连的Helmholtz自由能功能。认为两种塑料变形机构包括塑料容积压缩和塑料剪切,以基于ISV理论的含量迁移来开发耦合模型。该模型以增量形式给出,并描述了详细的数值计算过程。所提出的模型用椭圆抛物线屈服表面混合,并通过不同的冻融循环和不同的限制压力进行验证。理想地,计算的脱极应力 - 轴向应变曲线和体积应变轴向应变曲线与测试结果很好。

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