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Closed-Form Models for Nonisothermal Effective Stress of Unsaturated Soils

机译:非饱和土非等温有效应力的封闭形式模型

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摘要

Effective stress is a critical factor controlling the mechanical behavior of unsaturated soils. There has been an increasing interest toward fundamental and applied research on emerging applications that involve unsaturated soils subjected to elevated temperatures. However, major gaps remain in the development of a unified model that can properly represent temperature dependency of effective stress in unsaturated soils. The main objective of this study is to develop closed-form equations to describe the effective stress of unsaturated soils under nonisothermal conditions. For this purpose, suction stress-based formulations are developed for representing temperature-dependent suction stress and effective stress of unsaturated soils. The formulations incorporate temperature-dependent moist air pressure and matric suction into a skeleton stress equation originally developed using volume averaging. A nonisothermal soil water retention curve (SWRC) is used to account for thermal effects on the adsorbed water, surface tension, contact angle, and enthalpy of immersion per unit area. The validity of the model is examined by comparing predicted suction stress values against experimental data reported in the literature for various soils ranging from clay to sand. The effective stress equations developed in this study can provide further insight into the behavior of unsaturated soils under nonisothermal conditions. The models can be readily incorporated in numerical and analytical methods, leading to more accurate modeling of unsaturated soils subjected to nonisothermal loading conditions.
机译:有效应力是控制非饱和土壤力学行为的关键因素。对于涉及高温下的非饱和土壤的新兴应用的基础研究和应用研究越来越引起人们的兴趣。但是,在统一模型的开发中仍存在较大差距,该模型可以正确表示非饱和土壤中有效应力的温度依赖性。这项研究的主要目的是建立封闭形式的方程来描述非等温条件下非饱和土的有效应力。为此,开发了基于吸力应力的配方,用于表示温度依赖的吸力应力和非饱和土壤的有效应力。这些公式将取决于温度的湿空气压力和基质吸力纳入最初使用体积平均法得出的骨架应力方程式中。非等温土壤保水曲线(SWRC)用于说明对吸附水的热效应,表面张力,接触角和每单位面积的浸入焓。通过将预测的吸力应力值与文献中报道的从粘土到沙子的各种土壤的实验数据进行比较,检验了模型的有效性。在这项研究中开发的有效应力方程可以进一步了解非等温条件下非饱和土的行为。该模型可以很容易地纳入数值和分析方法中,从而可以更精确地模拟非等温荷载条件下的非饱和土壤。

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