基于热力学的饱和和非饱和土壤混合模型

K. Hutter, L. Laloui, L. Vulliet
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引用次数: 122

摘要

许多岩土工程问题都受到固体基质和流体输送之间的耦合效应的制约,特别是在非饱和区:路堤施工、路基循环荷载、环境工程等。因此,了解饱和/非饱和土的特性对于这些地质结构的设计和分析很重要。本文总结了各向同性粘弹性材料混合物的Svendsen–Hutter热力学理论,并将其应用于饱和/非饱和、可压缩/不可压缩土壤的场方程组。重点介绍了配方中的差异、热力学和构型以及饱和压力的作用。该理论通过研究(1)粘性混合物(饱和二元/三元混合物和非饱和二元混合物)和(2)弹性土的静力学来说明。提出了这一现代热力学理论的几种变体。我们为饱和和非饱和土壤中有效应力的众所周知的概念建立了热力学基础。版权所有©1999 John Wiley&;有限公司。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Thermodynamically based mixture models of saturated and unsaturated soils

Many geotechnical problems are conditioned by the coupling effects between the solid matrix and fluid transport, in particular in unsaturated zones: construction of embankments, cyclic loading of road foundations, environmental engineering, etc. An understanding of the behaviour of saturated/unsaturated soils is therefore important for the design and analysis of those geostructures. In this paper, the Svendsen–Hutter thermodynamic theory of a mixture of isotropic visco-elastic materials is summarized and applied to the formulation of field equations for saturated/unsaturated, compressible/incompressible soils. Emphasis is on the presentation of differences in the formulation, the roles of thermodynamics and configurational as well as saturation pressures. The theory is illustrated by studying (1) viscous mixtures (saturated binary/ternary mixtures and unsaturated binary mixtures) and (2) the statics of elastic soils. Several variants of this modern thermodynamic theory are presented. We establish a thermodynamic basis for well-known concepts of effective stress in saturated and unsaturated soils. Copyright © 1999 John Wiley & Sons, Ltd.

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