We treat the infiltration of an initially dry deformable porous medium
by a pressurized liquid, taking into account the influence of variati
ons in permeability within the deformed porous medium. Chief assumptio
ns of our analysis are neglect of gravity, of inertial forces, and of
partial saturation in the porous medium. We focus on unidirectional in
filtration under constant liquid pressure, and present data from the i
nfiltration of polyurethane sponge by ethylene glycol in a configurati
on of nearly unidirectional infiltration with reflief from friction ef
fects along sample sides. We find excellent agreement between theory a
nd experiment at longer infiltration times. We examine an additional a
ssumption, namely the neglect of solid-phase velocity compared with av
erage local liquid velicity at lower porous-medium strains. Agreement
of this simplified model with experimental data, albeit less good, rem
ains quite acceptable given the considerable computational simplicity
it produces.