We present a statistical analysis of the acoustic emissions induced by disl
ocation motion during the creep of ice single crystals. The recorded acoust
ic waves provide an indirect measure of the inelastic energy dissipated dur
ing dislocation motion. Compression and torsion creep experiments indicate
that viscoplastic deformation, even in the steady-state (secondary creep),
is a complex and inhomogeneous process characterized by avalanches in the m
otion of dislocations. The distribution of avalanche sizes, identified with
the acoustic wave amplitude (or the acoustic wave energy), is found to fol
low a power law with a cutoff at large amplitudes which depends on the cree
p stage (primary, secondary, tertiary). These results suggest that viscopla
stic deformation in ice and possibly in other materials could be described
in the framework of non-equilibrium critical phenomena. (C) 2001 Elsevier S
cience B.V. All rights reserved.