Inelastic Neutron Spectra of Uranium Tetrafluoride Hydrate, UF4(H2O)2.5

Andrew Miskowiec, K. J. Pastoor, Jonathan H. Christian, J. L. Niedziela, Bryan J. Foley, Sara Isbill, A. E. Shields, L. L. Daemen, E. Novak, E. Nykwest, T. Spano, Matthew S. Wellons, M. Jensen, J. Shafer

Research output: Contribution to journalArticlepeer-review

3 Scopus citations

Abstract

Uranium tetrafluoride hydrate (UFH) is formed by immersing anhydrous UF4 under water for 12 h. UFH is therefore clearly a chemical species of environmental concern, as anhydrous UF4 is an intermediate uranium form in the nuclear fuel cycle. We use inelastic neutron scattering (INS) to probe the full vibrational spectra of UFH and its deuterated analogue in an effort to improve the fundamental understanding of its vibrational spectra. Coupled with density functional theory (DFT) calculations, the first for this compound, and full spectral modeling, we generate the complete vibrational spectra of UFH and compare them to prior optical spectroscopic results. In particular, the combination of DFT with INS allows us to identify multiple distinct chemical environments in the water bending and OH stretching regions. Whereas the water molecules directly bound to the U atoms execute OH stretching around 3600 cm-1, a second class of H-bonded waters vibrate below 3000 cm-1, an indicator of strong H bonding. In addition, a class of librational water modes are observed between 400 and 900 cm-1, which themselves can be separated in energy according to their chemical environments. Measurements presented herein directly assist in the assignment of certain spectral features in the infrared spectrum and will inform future investigations of UFH for environmental or forensics purposes.

Original languageEnglish
Pages (from-to)25007-25021
Number of pages15
JournalJournal of Physical Chemistry C
Volume125
Issue number45
DOIs
StatePublished - Nov 18 2021

Funding

A portion of this research used resources at the Spallation Neutron Source, a U.S. Department of Energy (DOE) Office of Science User Facility operated by Oak Ridge National Laboratory. Part of this work was also produced by Battelle Savannah River Alliance, LLC under Contract no. 89303321CEM000080. This research used resources of the Compute and Data Environment for Science and the Oak Ridge Leadership Computing Facility at Oak Ridge National Laboratory, which are supported by the DOE Office of Science under Contract number DE-AC05-00OR22725. K.J.P. and J.C.S. acknowledge support from DTRA Grant No. HDTRA1-18-1-0015. S.R.N.L. thanks Kaitlin Coopersmith for XRD analysis. This manuscript has been authored by UT-Battelle LLC under Contract No. DE-AC05-00OR22725 with the U.S. Department of Energy (DOE). The U.S. government retains and the publisher, by accepting the article for publication, acknowledges that the U.S. government retains a nonexclusive, paid-up, irrevocable, worldwide license to publish or reproduce the published form of this manuscript, or allow others to do so, for the U.S. government purposes. DOE will provide public access to these results of federally sponsored research in accordance with the DOE Public Access Plan ( http://energy.gov/downloads/doe-public-access-plan ).

FundersFunder number
U.S. Department of Energy
Office of ScienceDE-AC05-00OR22725, HDTRA1-18-1-0015
Oak Ridge National Laboratory89303321CEM000080
UT-Battelle

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