In this paper, a length scale included in multiphase materials such as satu
rated and partially saturated porous media is discussed, where the viscous
terms are introduced naturally by the fluid mass balance equations. The dis
cussion is limited to the dynamic case. The characteristic stability equati
on is given in explicit form for one-dimensional wave propagation. It is sh
own that for axial waves a wave number domain exists for which the material
model is dispersive when softening behaviour occurs for solid skeleton and
that an internal length scale can be derived, while for ideal shear propag
ation this is not the case. Numerical examples are given to corroborate the
validity of the expressions derived. Copyright (C) 1999 John Wiley & Sons,
Ltd.