An analytical three-dimensional solution to the fluid flow problem thr
ough heterogeneous porous media in a rotating square channel is presen
ted. The permeability of the fluid saturated porous domain varies in t
he vertical direction, thus affecting the imposed main flow in the cha
nnel. As a result of Coriolis acceleration, secondary circulation in a
plane perpendicular to the main flow direction is created. A particul
ar example of a monotonic distribution of the permeability function is
analyzed leading to a single vortex secondary circulation. Neverthele
ss, multiple vortex secondary flow solutions are possible depending on
the particular variation of the permeability in the vertical directio
n. No secondary motion is expected for isothermal flows in homogeneous
porous media.