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Journal Article | PUBDB-2025-01918 |
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2025
APS
College Park, Md.
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Please use a persistent id in citations: doi:10.1103/PhysRevLett.134.236203 doi:10.3204/PUBDB-2025-01918
Abstract: In situ nuclear forward scattering shows a thermally induced cation exchange between a 57 Fe3 O4 thin-film and a Fe3 O4 (001) substrate predominantly in the octahedral sublattice for a temperature range between 470 and 710 K. The overall activation barrier in this temperature range is found to be 19±32 kJ/mol, which is significantly lower than expected from extrapolating a bulk diffusion model. This observation can be attributed to the large out-of-equilibrium cation deficit as determined by surface x-ray diffraction. Despite the relatively low hopping barrier, the diffusion constant is about 5 orders of magnitude lower than expected for magnetite having an equilibrium cation stoichiometry. The results are relevant for applications relying on the near-surface structure and stoichiometry of magnetite, and we argue that the correlation between cation diffusion and stoichiometry may play a role for a wider range of oxide materials.
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