Many important technological and natural processes involving flow through p
orous media are characterized by large filtration velocity It is important
to know when the transition from the linear flow regime to the quadratic fl
ow regime actually occurs to obtain accurate models for these processes. By
interpreting the quadratic extension of the original Darcy equation as a m
odel of the macroscopic form drag, we suggest a physically consistent param
eter to characterize the transition to quadratic flow regime in place of th
e Reynolds number, Re. We demonstrate that an additional data set obtained
by Darcy, and so far ignored by the community, indeed supports the Darc equ
ation. Finally, we emphasize that the cubic extension proposed in the liter
ature, proportional to Re-3 and mathematically valid only for Re much less
than1, is irrelevant in practice. Hence, it should not be compared to the q
uadratic extension experimentally observed when Re greater than or equal to
O(1). [S0098-2202(00)01703-X].