In this theoretical paper we show how to solve a time-dependent diffusion e
quation by means of a perturbation series. This technique is applied to the
case of diffusion of a liquid through a time-dependent porous matrix. We c
ompute to first order the phase and amplitude relations between the small d
eformation of the transporting matrix and the corresponding variation of th
e saturation at the surface. In particular we show that, for a large freque
ncy range, there is a constant phase shift of pi/2 between the matrix and t
he surface saturation variations. Since the conductivity is to first approx
imation proportional to the saturation at the surface, this might explain t
he observed phase relations observed in an experiment in a cave near Abarat
subo (Japan).