Creep fracture behaviour of pure aluminium-matrix composites with 10-3
0 vol% SiC particulates at 623 K is reported. A comparison of tensile
and compression creep data shows the existence of a ''transition stres
s''. Above this transition stress no steady state creep is observed in
tension. This transition stress is related to a transition from inter
granular to transgranular fracture. The origin of transition stress is
perhaps associated with the diffusional relaxation of stress concentr
ation at the matrix/particle interface by lattice diffusion. The inter
granular creep fracture of composites appears to be similar to that of
unreinforced aluminium and it is power-law creep controlled. The tran
sgranular creep fracture occurs by void nucleation and growth. The nuc
leation strain for voids is quite small and hence the tertiary stage s
tarts before the end of the primary stage. The ductile fracture models
overestimate the strain to fracture and do not predict the observed s
tress dependence of strain to fracture.