Macroscopic behavior of gas flow with adsorption through a fractured porous medium
Résumé
A fractured porous medium is a double-porosity medium, i.e. it consists of two interacting
porous systems whose permeabilities are very different. One of the two porous structures
is associated with the fractures and the other one with the porous matrix. Thus, when
looking for a macroscopic equivalent description, three separated scales whose characteristic
lengths are very different may be under consideration: the pore-scale, the fracture-scale and
the macroscopic scale. Modeling gas flow with adsorption through double-porosity media
is of particular interest in mining engineering. lndeed, coal is a multiple-porosity system
that naturally contains gas. Gas adsorption within coal skeleton is strongly connected to
the occurence of a coal-outburst. To prevent outbursts and also to draw up reliable safety
measures, an accurate knowledge of coal-gas system behavior is required. A three-scale homogenization
method bas been first used in [1] and (2] for the investigation of incompressible
fluid flow in a deformable fractured porous medium. The local descriptions at both porescale
and fracture-scale are expressed by Navier-Stokes equations. This upscaling method
allows to convey the influence of the local effects to the macroscopic level. This technique
bas been taken up again for modeling gas flow through a rigid fractured porous matrix
while considering the strong compressibility of the fluid [3], (4], (5], [6]. Here, the adsorption
phenomenon is implemented to gas-flow equations at both local scales through additionnai
boundary conditions. Then, the macroscopic behavior is derived via the same three-scale
homogenization method.
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