We study an invasion percolation model for drainage where the disorder come
s partly from capillary thresholds and partly from height differences in a
rough self-affine landscape. As a function of the buoyancy, the geometry of
the invaded clusters changes dramatically. Long-range correlations from th
e fracture topography induce a double cluster structure with strings and co
mpact blobs. A characteristic length is introduced comparing the width of t
he capillary threshold distribution and gravity effects at the pore scale.
We study electrical properties of percolating clusters. Current distributio
ns along percolating clusters are shown to be multifractal and sensitive to
the buoyancy.