The wet erosive wear of a set of 100% polycrystalline alumina material
s of tailored grain sizes in the range 1-12 mum has been studied using
a slurry of coarse alumina grit in water. Detailed observations of wo
rn surfaces identify two wear mechanisms: microfracture and grain deta
chment, and tribochemical wear. Measured wear rates are a function of
(grain size)-1/2. and a linear relationship between wear rate and four
-point bend strength is also seen. Grain detachment is the dominant we
ar mechanism for grain sizes >2 mum.