Molecular-scale information reveals non-classical diffusion behavior during the initial stages of uranium dioxide corrosion.
Density-functional theory and X-ray based methods sensitive to surface atomic structure and oxidation state [crystal truncation rod (CTR), X-ray diffraction, and X-ray photoelectron spectroscopy (XPS)] were used to determine the behavior of the natural cleavage surface of uraninite (UO2) in water at ambient conditions. Oxygen was found to react strongly with UO2. However, rather than following classical diffusion patterns, oxygen self-organized as interstitial atoms within the mineral lattice of every third atomic layer.
Uranium dioxide occurs naturally in anoxic sediments, is the desired product of in situ bioremediation of uranium-contaminated aquifers, and is likely to control uranium release from such sediments over the long term. These surprising insights indicate that UO2 oxidation is far more complicated that previously known and offer a new conceptual molecular-scale framework for understanding UO2 fate in the environment.
CTR X-ray diffraction measurements of a polished UO2 (111) surface exposed to atmospheric oxygen revealed a periodic, oscillatory structure of the oxidation front perpendicular to the mineral-water interface. This behavior could be explained by quantum mechanic considerations of the electron-transfer from U 5f orbitals to O 2p orbitals, assuming at least partial contribution from hemi-uranyl (resembling half of the UO22+ uranyl cation, i.e., with only a single short U-O bond) termination groups at the mineral surface, which favor the incorporation of interstitial oxygens into slab 3 of the UO2 lattice. The presence of hemi-uranyl termination groups was supported by XPS analyses revealing that both U(V) and U(VI) were present at the mineral surface, suggesting a mixed termination of the oxidized surface with hemi-uranyl, hydroxyl, and molecular water. The ordered oscillatory oxidation front with a three-layer periodicity observed is distinct from previously proposed models of oxidative corrosion under vacuum and offers important molecular-scale insights into UO2 oxidation under ambient conditions.
Contact (BER PM)
Roland F. Hirsch, SC-23.2, email@example.com, 301-903-9009
SSRL, SLAC National Accelerator Laboratory
Support was provided by the U.S. Department of Energy (DOE), Office of Science, Biological and Environmental Research (BER), Subsurface Biogeochemical Research activity, through the SLAC Scientific Focus Area program (Contract No. DE-AC02-76SF00515); and by the Geosciences Research Program at Pacific Northwest National Laboratory (PNNL), funded by DOE’s Office of Basic Energy Sciences (BES). XPS data were collected in the Radiochemistry Annex at the Environmental Molecular Sciences Laboratory, a DOE user facility located at PNNL. A portion of the DFT study was also performed using the computational resources of EMSL. GeoSoilEnviroCARS is supported by the National Science Foundation-Earth Sciences (EAR-1128799) and BES GeoSciences (DE-FG02-94ER14466). This research used resources at the Advanced Photon Source, a DOE user facility.
Stubbs, J. E.,et al. 2015. “UO2 Oxidative Corrosion by Nonclassical Diffusion,” Physical Review Letters 114, 246103. DOI: 10.1103/PhysRevLett.114.246103. (Reference link)
SC-23.1 Climate and Environmental Sciences Division, BER
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