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Diffusion measurements were made between 1000 and 1300 K on films of In 2 O 3 by electrochemical techniques using an yttria‐stabilized zirconia solid electrolyte. At atmospheric oxygen pressures, diffusion invariably occurred via an oxygen interstitial mechanism. The diffusion coefficient decreased with decreasing oxygen pressure with a P O2 1/2 dependence. Near 1.0 Pa P O2 the mechanism began to change to a vacancy mechanism which dominated at P O2 <10 −3 Pa, where diffusivity increased with further decrease in oxygen pressure according to a P O2 −1/2 dependence. Activation energies for interstitial and vacancy diffusion were 166 and 190 kJ/mol, respectively.
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WIRTZ et al. (1981) studied this question.
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