RESUMEN
We study an invasion percolation model for drainage where the disorder comes 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 the fracture topography induce a double cluster structure with strings and compact blobs. A characteristic length is introduced comparing the width of the capillary threshold distribution and gravity effects at the pore scale. We study electrical properties of percolating clusters. Current distributions along percolating clusters are shown to be multifractal and sensitive to the buoyancy.
RESUMEN
We introduce a simple model for granular flows with hydrodynamic interactions. The hydrodynamic part of the model relies on a coarse grained picture of the granular medium, and is described in terms of the pressure by a local Darcy law. The model thus avoids the large computational cost of solving for detailed hydrodynamic flow fields between grains. The solid phase is described explicitly in terms of grains by event driven molecular dynamics. In the first two test cases, the model is employed to simulate a sedimenting and a fluidized particle bed. It is shown that the qualitative aspects of both phenomena are correctly captured: The sedimenting particles form a sharp upper front and move according to the theoretical prediction, which is also given. When external pressure gradients are applied the bed fluidizes, and spontaneously produces bubbles of the shape observed experimentally. Moreover, these bubbles are seen to merge, as is experimentally observed.