This paper is devoted to the modelling of isothermal low Reynolds and Mach
numbers transient compressible flow through porous media. Traditionally, th
is type of flow at the macroscopic level is described by the classical Darc
y's law combined with a mass balance that includes the transient term. This
model is called the 'classic model'. The aim of this paper is to explore t
he validity of this classic model. To this end, the flow of an ideal gas is
considered within two-dimensional model porous media. The flow is due to t
he imposed pressure variations at the outlet of the fluid domain. At the mi
croscopic level, the flow is computed by solving the full compressible Navi
er-Stokes equations in two dimensions. Special attention is given to the ou
tlet boundary conditions. The analysis is based on the comparison between t
he macroscopic data, obtained on the one hand by spatially averaging the mi
croscopic results, and on the other hand by solving the problem directly at
the macroscopic level. Situations for which a good agreement is found betw
een the two series of data and situations for which discrepancies are obser
ved are exhibited. These various behaviours are discussed in terms of the v
arious time scales controlling the flow and are explained by analysing the
flow structure at pore level. Copyright (C) 1999 John Wiley & Sons, Ltd.