Crenulative turbulence is a nonlinear extension of the Bell-Plesset instabi
lity, usually observed in a converging system in which there is a nonhomoge
neous response of stress to strain and/or strain rate. In general, crenulat
ion occurs in any circumstance in which the mean flow streamlines converge
the material more strongly than the compressibility can accommodate. Elemen
ts of the material slip past each ether, resulting in local fluctuations in
velocity from that of the mean flow, producing a type of turbulence that i
s more kinematic than inertial. For a homogeneous material, crenulation occ
urs at the atomic or molecular scale. With nonhomogeneous stress response a
t larger scales, the crenulative process can also occur at those larger sca
les. The results are manifested by a decrease in the rate of dissipation to
heat, and by the configurationally irreversible mixing of nonhomogeneities
across any mean-flow-transported interface. A mathematical description of
the crenulative process is obtained by means of Reynolds decomposition of t
he appropriate variables, and the derivation of transport equations for the
second-order moments that arise in the mean-flow momentum and energy equat
ions. The theory is illustrated by application to the spherical convergence
of an incompressible fluid with nonhomogeneous distribution of kinematic v
iscosity. (C) 1999 American Institute of Physics. [S1070-6631(99)01208-8].