Gas-phase diffusion in porous media: Evaluation of an advective- dispersive formulation and the dusty-gas model including comparison to data for binary mixtures

Two models for gas-phase diffusion and advection in porous media, the Advective-Dispersive Model (ADM) and the Dusty-Gas Model (DGM), are reviewed. The ADM, which is more widely used, is based on a linear addition of advection calculated by Darcy`s Law and ordinary diffusion using Fick`s Law. Knudsen diffusion is often included through the use of a Klinkenberg factor for advection, while the effect of a porous medium on the diffusion process is through a porosity-tortuosity-gas saturation multiplier. Another, more comprehensive approach for gas-phase transport in porous media has been formulated by Evans and Mason, and is referred to as the Dusty- Gas Model (DGM). This model applies the kinetic theory of gases to the gaseous components and the porous media (or ``dust``) to develop an approach for combined transport due to ordinary and Knudsen diffusion and advection including porous medium effects. While these two models both consider advection and diffusion, the formulations are considerably different, especially for ordinary diffusion. The various components of flow (advection and diffusion) are compared for both models. Results from these two models are compared to isothermal experimental data for He-Ar gas diffusion in a low-permeability graphite. Air-water vapor comparisons have also been performed, although data are not available, for the low-permeability graphite system used for the helium-argon data. Radial and linear air-water heat pipes involving heat, advection, capillary transport, and diffusion under nonisothermal conditions have also been considered.

[1]  P. M. Heertjes,et al.  Analysis of diffusion in macroporous media in terms of a porosity, a tortuosity and a constrictivity factor , 1974 .

[2]  L. Klinkenberg The Permeability Of Porous Media To Liquids And Gases , 2012 .

[3]  C. Doughty,et al.  A mathematical model for two-phase water, air, and heat flow around a linear heat source emplaced in a permeable medium , 1991 .

[4]  J. Hoogschagen Equal Pressure Diffusion in Porous Substances , 1953 .

[5]  H. Hanley Experimental Verification of the ``Dusty-Gas'' Theory for Thermal Transpiration , 1965 .

[6]  R. Jackson,et al.  Transport in porous catalysts , 1977 .

[7]  J. Hoogschagen Diffusion in Porous Catalysts and Adsorbents , 1955 .

[8]  V. Denny,et al.  Diffusion, flow, and heterogeneous reaction of ternary mixtures in porous catalytic media , 1975 .

[9]  D. W. Pollock,et al.  Gas transport in unsaturated porous media: The adequacy of Fick's law , 1989 .

[10]  G. L. Hubbard,et al.  Effects of temperature and pressure gradients on catalyst pellet effectiveness factors—I , 1976 .

[11]  E. Hopfinger,et al.  Experimental Verification of the Dusty‐Gas Theory for Thermal Transpiration through Porous Media , 1969 .

[12]  S. Finsterle,et al.  Exploratory simulations of multiphase effects in gas injection and ventilation tests in an underground rock laboratory , 1990 .

[13]  George F. Pinder,et al.  A Multiphase Approach to the Modeling of Porous Media Contamination by Organic Compounds: 1. Equation Development , 1985 .