Abstract

Chemical diffusion of oxygen in calcia‐stabilized zirconia, with impurities of A12O3, SiO2, MgO, Fe2O3, and TiO2, was studied by the non‐steady‐state permeation technique at 960° to 1450°C. The apparent chemical diffusion coefficient, D, was found to decrease with increasing content of Fe2O3, and with decreasing oxygen pressure. The results were consistent with a trapping mechanism involving free and trapped electron holes or with partial control by surface processes.

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