This paper shows how a unified model with a single set of equations and mat
erial constants can be used for describing inelastic flow of rocksalt submi
tted to a variety of loading conditions associated with plasticity, creep a
nd relaxation. After introducing the complete model in its full expanded ve
rsion, the authors demonstrate that these different observed material respo
nses are specific manifestations of a unique (unified) inelastic behavior,
each corresponding to an imposed load path. The unified model relies on the
use of internal state variables (ISV) attached to specific phenomena, incl
uding isotropic and kinematic hardening. Each ISV appears in the kinetic (f
low) law and evolves according to a growth rule as a function of the inelas
tic strain tensor until it reaches saturation. The flow law, which relates
the deviatoric stress to the inelastic strain rate, takes into account the
evolution of these ISV as well as the external (observable) variables. Toge
ther, they represent a complete description of inelastic flow. These concep
ts are illustrated by results obtained on rocksalt samples submitted to dif
ferent loading conditions, including constant strain rate (CSR) tests, cree
p (constant stress) tests, and relaxation (constant strain) tests. (C) 2000
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