Abstract
The oxygen permeability of undoped and lutetia-doped polycrystalline alumina wafers that were exposed to oxygen potential gradients was evaluated at temperatures up to 1973 K. The main diffusion species during oxygen permeation through the alumina grain boundaries were found to depend on oxygen partial O 2 pressures ( P O 2 ), which created oxygen potential gradients. Under oxygen potential gradients generated by P O 2 values below 10 −3 Pa, where oxygen permeation occurred by oxygen diffusion from regions of higher to lower P O 2 , segregated lutetium at the grain boundaries suppressed only the mobility of oxygen in the wafers, without affecting the oxygen permeation mechanism. By contrast, under oxygen potential gradients generated by P O 2 values above 10 3 Pa, where oxygen permeation proceeded by aluminum diffusion from regions of lower to higher P O 2 , lutetium had little effect on aluminum diffusion and migrated together with aluminum, resulting in precipitation and growth of Al 5Lu 3O 12 particles on the higher P O 2 surface.
Published Version
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