Journal of Applied Mathematics and Decision Sciences
Volume 4 (2000), Issue 2, Pages 165-173
doi:10.1155/S1173912600000122
Abstract
Since the days of Darcy, many refinements have been made to the
equations used to model single-phase fluid flow and heat transfer in a
saturated porous medium, to allow for such basic things as inertial
effects, boundary friction and viscous dissipation, and also
additional effects such as those due to rotation or a magnetic
field. These developments are reviewed.