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A physical-chemical model for the static water retention characteristic of unsaturated porous media

机译:不饱和多孔介质静态保水特性的物理化学模型

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摘要

Water retention characteristic or water retention curve (WRC) is an important constitutive feature of porous media, and also meanwhile is an indispensable requirement in hydraulic transport modelling. Previous experiments have indicated that the specific surface area of porous media has effects on the WRC. It has also been observed that a linear relationship generally exists between the air-water interface area and the water saturation within unsaturated porous media. However it seems that no detailed study on their internal linkage with the WRC has been reported yet. This paper, at first gives a review of the development of WRC modelling, then it tries to explain the water retention characteristic according to the physical and chemical behaviours of the phases involved in unsaturated porous media. Using the traditional capillary theory, the volume averaging theorem and the advances in physical chemistry of interfacial surfaces, this paper then derives out a formula which represents the water retention characteristic of porous media. This formula demonstrates the internal linkage of the WRC to the specific surface area of porosities. It also shows agreements with the experimental observations mathematically. Based on this formula, a fitting model is proposed for the static WRC of porous media. Finally, this model is tested to fit the WRC measurements of a wide range of porous materials. Comparison with other main models is presented.
机译:保水特性或保水曲线(WRC)是多孔介质的重要本构特征,同时也是水力运输建模中必不可少的要求。先前的实验表明,多孔介质的比表面积会对WRC产生影响。还已经观察到,空气-水界面面积与不饱和多孔介质内的水饱和度之间通常存在线性关系。但是,似乎还没有关于它们与WRC内部联系的详细报道。本文首先回顾了WRC建模的发展,然后试图根据不饱和多孔介质中各相的物理和化学行为来解释保水特性。利用传统的毛细管理论,体积平均定理和界面物理化学的进展,本文推导了代表多孔介质保水特性的公式。该公式证明了WRC与孔隙比表面积的内部联系。它还在数学上显示了与实验观察结果的一致性。基于该公式,提出了多孔介质静态WRC的拟合模型。最后,对该模型进行了测试,以适合各种多孔材料的WRC测量。介绍了与其他主要模型的比较。

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