An assessment of fracture origins is conducted in yttria-stabilized zirconi
a ceramics containing different grain sizes. As the microstructure coarsens
due to the application of heat treatments, fracture origins change from si
ngle pores to transformed regions at the free surface which are induced by
the applied stress. The observation of an increasing size of failure origin
s with microstructural coarsening lies as the underlying reason for the fin
ding that specimens containing coarser microstructures and a more pronounce
d R-curve behavior do not fail at larger stresses. A fracture model is used
to link the strength variability of a fully tetragonal zirconia containing
a small grain size to its pore size distribution. The increased transforma
bility of zirconia ceramics with coarser tetragonal grains is evaluated by
means of quantitative phase analysis, characterizations of fracture surface
morphology, and R-curve assessments. It is confirmed that tetragonal grain
s of up to 4 mum may not necessarily undergo a spontaneous t-m transformati
on upon cooling from sintering. (C) 2001 Kluwer Academic Publishers.