“…In various types of rocks the local permeability may be correlated over considerable length-scales due to geological processes. The evidence from numerical modelling based on microscopically faithful descriptions of pore-networks seems to indicate, that multi-phase flow phenomena as imbibition in particular are much more prone for correlationinduced effects than, e.g., simple one-phase permeability [10,42,66,94,141,153,212,257,258,308,326,334]. Typical quantities where this would be visible are relative permeabilities for given saturations, and remaining saturations of the non-wetting fluid.…”