Journal Article PUBDB-2025-01918

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Site-Resolved Near-Surface Cation Diffusion in Magnetite

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2025
APS College Park, Md.

Physical review letters 134(23), 236203 () [10.1103/PhysRevLett.134.236203]
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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.

Classification:

Contributing Institute(s):
  1. Nanolab (FS-NL)
  2. PETRA-S (FS-PETRA-S)
Research Program(s):
  1. 632 - Materials – Quantum, Complex and Functional Materials (POF4-632) (POF4-632)
  2. SFB 986 C07 - Deposition und Stabilität von hochtemperaturfesten geschichteten Metamaterialien (C07) (318029273) (318029273)
  3. DFG project G:(GEPRIS)192346071 - SFB 986: Maßgeschneiderte Multiskalige Materialsysteme - M3 (192346071) (192346071)
Experiment(s):
  1. DESY NanoLab: Sample Preparation
  2. DESY NanoLab: Surface Spectroscopy
  3. DESY NanoLab: X-Ray Diffraction
  4. PETRA Beamline P01 (PETRA III)

Appears in the scientific report 2025
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 Record created 2025-06-19, last modified 2025-07-15


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