Structural features of solid-solid phase transitions and lattice dynamics in U3 O8

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Abstract

Triuranium octoxide (U3O8) undergoes an orthorhombic to hexagonal structural phase transition near Ts=305?C, and a separate nonstructural phase transition at Tc=210?C. The later transition has previously been associated with temperature-induced fluctuations in the uranium oxidation state. A discontinuity in the slope of electrical conductivity versus temperature measurement at 210?C has supported this idea. The orthorhombic phase has three crystallographic sites in two distinct oxidation configurations [2 U(V) and 1 U(VI)], whereas the hexagonal phase has one distinct uranium site. High-resolution x-ray diffraction measurements eliminate the possibility of superlattice Bragg reflections to less than 0.2 e- scattering power and U3O8 is not metallic; consequently, the presence of oxidation fluctuations is required for charge balancing. Interestingly, the order-to-disorder transition occurs at a much lower temperature than the structural transition. Using temperature-dependent x-ray diffraction and Raman spectroscopy, we show anisotropic lattice expansion in the in-plane b and c lattice constants. A specific discontinuity in the temperature derivatives of the b and c lattice constants are the first reported structural signatures of the order-to-disorder transition, suggestive of a change in local U-O coordination. Phonon frequencies of U3O8 measured by Raman spectroscopy show significant temperature-dependent dynamics. Redshifting of several modes between 40 and 300?C cannot be explained by unit cell expansion alone because the unit cell volume decreases in this region. Instead, we show that phonon frequencies are highly correlated with the anisotropic lattice expansion/contraction along specific crystallographic directions.

Original languageEnglish
Article number093610
JournalPhysical Review Materials
Volume4
Issue number9
DOIs
StatePublished - Sep 2020

Funding

The Department of Energy will provide public access to these results of federally sponsored research in accordance with the DOE Public Access Plan in Ref. . A portion of this work was supported by the US Department of Energy National Nuclear Security Administration. ACKNOWLEDGMENTS The authors would like to thank Z. Brubaker (ORNL) and D. Duckworth (ORNL) for a critical reading of the manuscript. This manuscript has been authored by UT-Battelle, LLC under Contract No. DE-AC05-00OR22725 with the U.S. Department of Energy. The United States Government retains and the publisher, by accepting the article for publication, acknowledges that the United States Government retains a nonexclusive, paid-up, irrevocable, world-wide license to publish or reproduce the published form of this manuscript, or allow others to do so, for United States Government purposes.

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