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|Title:||Incorporation of uranium in pyrochlore oxides and pressure-induced phase transitions.|
|Publisher:||Elsevier - ScienceDirect|
|Citation:||Zhang, F. X., Lang, M., Tracy, C., Ewing, R. C., Gregg, D. J., & Lumpkin, G. R. (2014). Incorporation of uranium in pyrochlore oxides and pressure-induced phase transitions. Journal of Solid State Chemistry, 219(0), 49-54. doi:10.1016/j.jssc.2014.07.011|
|Abstract:||Uranium-doped gadolinium zirconates with pyrochlore structure were studied at ambient and high-pressure conditions up to 40 GPa. The bonding environment of uranium in the structure was determined by x-ray photoelectron and Raman spectroscopies and x-ray diffraction. The uranium valence for samples prepared in air is mainly U6+, but U4+ is present in pyrochlores fabricated in an argon atmosphere. Rietveld refinement of the XRD pattern suggests that uranium ions in pyrochlores are on the 16d site in 6-fold coordination with oxygen. At pressures greater than 22 GPa, the pyrochlore structure transformed to a cotunnite-type phase. The cotunnite high-pressure phase transformed to a defect fluorite structure on the release of pressure. © 2014 Elsevier Inc.|
|Gov't Doc #:||7579|
|Appears in Collections:||Journal Articles|
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