A new computational model is presented to analyze intergranular creep crack
growth in a polycrystalline aggregate in a discrete manner and based direc
tly on the underlying physical micromechanisms. A crack tip process zone is
introduced in which grains and their grain boundaries are represented disc
retely, while the surrounding undamaged material is described as a continuu
m. Special-purpose finite elements are used to represent individual grains
and grain boundary facets. The constitutive description of the grain bounda
ry elements accounts for the relevant physical fracture mechanisms, i.e. vi
scous grain boundary sliding, the nucleation of grain boundary cavities, th
eir growth by grain boundary diffusion and local creep, until coalescence o
f cavities leads to microcracks. Discrete propagation of the main crack occ
urs by linking up of neighbouring facet microcracks. Assuming small-scale d
amage conditions, the model is used to simulate the initial stages of growt
h of an initially sharp crack under C* controlled, mode I loading condition
s. Material parameters are varied so as to lead to either ductile or brittl
e fracture, thus elucidating creep constrained cavitation near cracks. The
role of the stress state dependence of cavity nucleation on the crack growt
h direction is emphasized. (C) 1998 Elsevier Science Ltd. All rights reserv
ed.