Anisotropy of oxygen tracer diffusion in single-crystal
- 1 August 1991
- journal article
- research article
- Published by American Physical Society (APS) in Physical Review B
- Vol. 44 (5) , 2326-2333
- https://doi.org/10.1103/physrevb.44.2326
Abstract
Oxygen tracer diffusion has been measured in single-crystalline from 300 to 650 °C in the c direction, at a few temperatures in the ab plane of twinned crystals, and in the b direction of an untwinned crystal. The diffusion coefficient in the c direction, , is ≊ lower than the diffusion coefficient in polycrystals at 400 °C and diffusion in the b direction is at least 100 times faster than diffusion in the a direction at 300 °C. The oxygen diffusion coefficient in polycrystals is, within an experimental uncertainty of a factor of 2, independent of oxygen partial pressure at 400 °C, in agreement with previous results measured at 600 °C. Some suggestions are presented on the mechanism of diffusion, the relation of diffusion and internal friction in , and on the meaning of the activation energy.
Keywords
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