Publication

A combination of the Hashin-Shtrikman bounds aimed at modelling electrical conductivity and permittivity of variably saturated porous media

Alessandro Brovelli
2010
Journal paper
Abstract

In this paper we propose a novel theoretical model for the dielectric response of variably saturated porous media. A model is constructed for fully saturated porous media as a combination of the well established Hashin and Shtrikman [1962] bounds and Archie’s [1942] law, the latter usually adopted for electrical conductivity of multiphase porous media. One of the key advantages of the new constitutive model is that it explains both electrical conductivity and permittivity using the same parameterization, so that the measurements made on one such physical quantity can be used to predict the other. The model for partially saturated media is derived as an extension of the fully saturated model, where the permittivity of the pore space is in turn obtained as a combination of the permittivity of the aqueous and non aqueous phases. Both fully saturated and unsaturated models are successfully tested against both synthetic data from pore-scale digital modeling and laboratory data from the literature, proving effective for a wide range of different porous media. As opposite to most of existing constitutive laws for the water saturation – dielectric constant relationship, model parameters are related to the micro-geometrical and chemical-physical properties of the porous medium.

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Related concepts (32)
Porosity
Porosity or void fraction is a measure of the void (i.e. "empty") spaces in a material, and is a fraction of the volume of voids over the total volume, between 0 and 1, or as a percentage between 0% and 100%. Strictly speaking, some tests measure the "accessible void", the total amount of void space accessible from the surface (cf. closed-cell foam). There are many ways to test porosity in a substance or part, such as industrial CT scanning.
Porous medium
In materials science, a porous medium or a porous material is a material containing pores (voids). The skeletal portion of the material is often called the "matrix" or "frame". The pores are typically filled with a fluid (liquid or gas). The skeletal material is usually a solid, but structures like foams are often also usefully analyzed using concept of porous media. A porous medium is most often characterised by its porosity. Other properties of the medium (e.g.
Water content
Water content or moisture content is the quantity of water contained in a material, such as soil (called soil moisture), rock, ceramics, crops, or wood. Water content is used in a wide range of scientific and technical areas, and is expressed as a ratio, which can range from 0 (completely dry) to the value of the materials' porosity at saturation. It can be given on a volumetric or mass (gravimetric) basis. Volumetric water content, θ, is defined mathematically as: where is the volume of water and is equal to the total volume of the wet material, i.
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