“…Digital rock models [Andrä et al, 2013] have allowed for about a decade, computation of these average parameters from pore-scale models. Pore network models in which both pore space and flow are simplified to a substantial degree, and more direct pore scale approaches using lattice Boltzmann [Coles et al, 1998;Ramstad et al, 2009], direct Navier-Stokes [Raeini et al, 2014], and other methods [Armstrong et al, 2013] have, for coarse grained rocks, produced results which compare well with bulk measurements [Andrä et al, 2013]. Here fluid flow is modeled in the pore space, which is quantified by, e.g., micro X-ray computed tomography (micro-CT) [Coles et al, 1998].…”