Journal
SCIENTIFIC REPORTS
Volume 12, Issue 1, Pages -Publisher
NATURE PORTFOLIO
DOI: 10.1038/s41598-022-07834-9
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Funding
- Laboratory Directed Research and Development (LDRD) [20-SI-006]
- Consortium for Monitoring, Verification, and Technology [DE-NE000863]
- National Science Foundation Graduate Research Fellowship Program [DGE 1256260]
- Department of the Defense, Defense Threat Reduction Agency under the Materials Science in Extreme Environments University Research Alliance [HDTRA1-20-2-0001]
- U.S. Department of Energy by Lawrence Livermore National Laboratory [DEAC52-07NA27344]
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In this study, the influence of oxygen on rapidly cooling uranium was investigated through laser ablation of uranium metal in different concentrations of oxygen gas. The analysis of recovered particulates revealed that the micrometer-sized particulates are mainly amorphous UOx and UO2, and they convert to alpha-U3O8 when heated. It was also found that cooling timescales can affect the structural composition of uranium oxides.
In order to model the fate and transport of particles following a nuclear explosion, there must first be an understanding of individual physical and chemical processes that affect particle formation. One interaction pertinent to fireball chemistry and resultant debris formation is that between uranium and oxygen. In this study, we use laser ablation of uranium metal in different concentrations of oxygen gas, either O-16(2) or O-18(2), to determine the influence of oxygen on rapidly cooling uranium. Analysis of recovered particulates using infrared absorption and Raman spectroscopies indicate that the micrometer-sized particulates are predominantly amorphous UOx (am-UOx, where 3 <= x <= 4) and UO 2 after ablation in 1 atm of pure O-2 and a 1% O-2/Ar mixture, respectively. Energy dispersive X-ray spectroscopy (EDS) of particulates formed in pure O-2 suggest an O/U ratio of similar to 3.7, consistent with the vibrational spectroscopy analysis. Both am-UOx and UO 2 particulates convert to alpha-U3O8 when heated. Lastly, experiments performed in O-18(2) environments show the formation of O-18-substituted uranium oxides; vibrational frequencies for am-(UOx)-O-18 are reported for the first time. When compared to literature, this work shows that cooling timesca les can affect the structural composition of uranium oxides (i.e., crystalline vs. amorphous). This indicator can be used in current models of nuclear explosions to improve our predicative capabilities of chemical speciation.
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