The modelling of viscous dissipation in a porous medium saturated by an inc
ompressible fluid is discussed, for the case of Darcy, Forchheimer and Brin
kman models. An apparent paradox relating to the effect of inertial effects
on viscous dissipation is resolved, and some wider aspects of resistance t
o flow (concerning quadratic drag and cubic drag) in a porous medium are di
scussed. Criteria are given for the importance or otherwise of viscous diss
ipation in various situations.