We consider a weakly compressible single phase fluid flow through a ra
ndomly fissured porous medium. Under standard assumptions of the stoch
astic homogenization theory we obtain the stochastic version of the pe
riodic case. The basic tool is the stochastic two-scale convergence. T
he source-like terms are given by the coupling with a newly introduced
stochastic auxiliary problem. (C) Academie des Sciences/Elsevier, Par
is.