By viewing thermal and viscous diffusion in porous media as relaxation
al processes, a particularly simple, phenomenological model for sound
propagation in these materials is developed. The relaxation model para
meters (characteristic times) are chosen by comparison to three existi
ng models. Delany and Bazley's empirical equations; the Biot-Allard mi
crostructural model; and Champoux and Stinson's generalized, microstru
ctural model. It is shown that the relaxation model can effectively mi
mic the Delany-Bazley equations in their valid frequency range; yet, u
nlike the Delany-Bazley equations, the relaxation model has the advant
age providing of realistic predictions at a broad range frequencies. I
n more exacting applications the characteristic times can be selected
in a manner that makes the relaxation model predictions practically in
distinguishable from the two microstructural models. The advantage of
the relaxation model in these applications is its simple equations.