Smoothed particle hydrodynamics (SPH) is a versatile technique which can be
applied to single and multiphase flow through porous media. The Versatilit
y of SPH is offset by its computational expense which limits the practicabi
lity of SPH for large problems involving low Reynolds number flow. A parall
el pore-scale numerical model based on SPH is described for modeling flow p
henomena in porous media. Aspects of SPH which complicate parallelization a
re emphasized. The speed of the method is demonstrated to be proportional t
o the number of processors for test cases where load balance was achieved.
The parallel algorithm permits the application of SPH to more complicated p
orous media problems than previously considered. For such problems, best pe
rformance is achieved when several soil grains are simulated by each proces
sor. Finally, future applications of the method and possible extensions are
discussed. (C) 1999 Elsevier Science Ltd. All rights reserved.