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Phase stability of some actinides with brannerite structure at high pressures
Authors:F.X. Zhang  M. Lang  Zhenxian Liu  R.C. Ewing
Affiliation:aDepartment of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, United States;bGeophysical Laboratory, Carnegie Institute of Washington, DC 200015, United States
Abstract:Structure behavior of actinide brannerites ThTi2O6, Y0.5U0.5Ti1.5Nb0.5O6 and their analog oxide CeTi2O6 was studied at high pressure by using in situ x-ray diffraction, Raman scattering and infra-red absorption techniques, respectively. Brannerite structure was found to be not stable and started to become amorphous at pressures above 20 GPa. Some minor crystalline phase(s) due to phase decomposition was observed in all the three samples during pressurization. In addition, the observed bulk modulus indicated that the actinide-bearing brannerites are more compressible than their analog compound CeTi2O6, which may be related to the asymmetric 5f electron orbits of actinide elements.
Keywords:Brannerite   Actinide   High pressure   Amorphization
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