Abstract
A low-frequency internal friction peak was observed at 200 °C for sintered bar specimens annealed at different temperatures between 400 and 650 °C. This peak is interpreted in terms of diffusional jumps of oxygen atoms in the basal planes between sublattice sites ((1/2, 0,0) and (0,(1/2,0). These two sites are not crystallographically equivalent in orthorhombic symmetry. Oxygen diffusivity for planar diffusion in the basal planes was derived on the basis of a one-dimensional random-walk process, which yields: D=((1/4)/(+)ν exp(-/kT) =exp(-/kT), where =+ΔE. The parameters , , , and are evaluated from internal friction data for the specimens of known oxygen deficiency x and ΔE, the poten- tial energy difference between sites and , from Boltzmann’s distribution law /=exp(-ΔE/kT). The preexponential factor =3.5× /sec and the activation energy of the 200 °C internal-friction peak =1.03 eV are both temperature insensitive. By contrast, ΔE is temperature dependent; it is 0.23 eV at 400 °C and decreases as the temperature is raised, vanishing at 670 °C, the temperature of the orthorhombic-to-tetragonal transition temperature at which and sites become indistinguishable. Non-Arrhenius behavior exists between the oxygen diffusivity and the diffusion temperature in this type of diffusion mechanism.
- Received 30 January 1989
DOI:https://doi.org/10.1103/PhysRevB.40.4549
©1989 American Physical Society