4.8 Article

UO2 Oxidative Corrosion by Nonclassical Diffusion

期刊

PHYSICAL REVIEW LETTERS
卷 114, 期 24, 页码 -

出版社

AMER PHYSICAL SOC
DOI: 10.1103/PhysRevLett.114.246103

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资金

  1. DOE Office of Science [DE-AC02-06H11357]
  2. NSF-Earth Sciences [EAR-1128799]
  3. DOE-BES-GeoSciences [DE-FG02-94ER14466]
  4. DOE-BER, Subsurface Biogeochemical Research, through the SLAC SFA program (DOE) [DE-AC02-76SF00515]
  5. DOE-BER
  6. Geosciences Research Program at PNNL, US DOE Office of Science, Office of Basic Energy Sciences, Division of Chemical Sciences, Geosciences and Biosciences

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Using x-ray scattering, spectroscopy, and density-functional theory, we determine the structure of the oxidation front when a UO2 (111) surface is exposed to oxygen at ambient conditions. In contrast to classical diffusion and previously reported bulk UO2+x structures, we find oxygen interstitials order into a nanoscale superlattice with three-layer periodicity and uranium in three oxidation states: IV, V, and VI. This oscillatory diffusion profile is driven by the nature of the electron transfer process, and has implications for understanding the initial stages of oxidative corrosion in materials at the atomistic level.

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