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Interpretation of unsaturated soil behaviour in the stress - Saturation space,I: Volume change and water retention behaviour

机译:应力中非饱和土行为的解释-饱和空间,I:体积变化和保水行为

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Unsaturated soil behaviour, such as volume change, shear strength and yield stress, is usually interpreted and modelled in terms of stress and suction. This approach is consistent with laboratory tests where suction is a controllable variable. However, it also suffers some limitations. This paper (Parts I and II) presents an alternative approach for interpreting unsaturated soil behaviour, which is built in the space of stress versus degree of saturation. In Part I, a new volume change equation is proposed in terms of stress and degree of saturation, to give a better explanation to the non-linear change of soil compressibility under constant suctions. The soil compression index is assumed to be a function of the effective degree of saturation and is interpolated from the known compressibility at the fully saturated state and that at a dry state. An alternative approach to simulate hydraulic hysteresis and hydro-mechanical interaction is then introduced, which enables the calculation of the effective degree of saturation under complex stress and suction paths. The proposed volume change equation and the approach to describe saturation variation, which are two fundamental aspects to establish constitutive laws for unsaturated soils, are validated against a variety of experimental data in literature.
机译:通常根据应力和吸力来解释和建模不饱和的土壤行为,例如体积变化,剪切强度和屈服应力。这种方法与实验室测试一致,在实验室测试中吸力是可控制的。但是,它也有一些局限性。本文(第一部分和第二部分)提出了一种解释非饱和土壤特性的替代方法,该方法建立在应力与饱和度之间的空间内。在第一部分中,根据应力和饱和度提出了一个新的体积变化方程,以更好地解释恒定吸力下土壤可压缩性的非线性变化。假定土壤压缩指数是有效饱和度的函数,并根据完全饱和状态和干燥状态下的已知压缩率进行内插。然后介绍了一种模拟水力滞后和水力-机械相互作用的替代方法,该方法可以计算复杂应力和吸力路径下的有效饱和度。拟议的体积变化方程和描述饱和度变化的方法是建立非饱和土本构律的两个基本方面,已针对各种实验数据进行了验证。

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