TY - JOUR
T1 - Thermochemistry of rare earth doped uranium oxides LnxU1-xO2-0.5x+y (Ln = La, Y, Nd)
AU - Zhang, Lei
AU - Navrotsky, Alexandra
N1 - Funding Information:
This work was supported as part of the Materials Science of Actinides, an Energy Frontier Research Center funded by the U.S. Department of Energy, Office of Science, Basic Energy Sciences under Award # DE–SC0001089 . L. Zhang thanks T.Y. Shvareva for help on the preparation of lanthanum doped uranium oxide samples. The authors thank Sarah Roeske and Nicholas Botto for help with the electron probe microanalysis.
Publisher Copyright:
© 2015 Published by Elsevier B.V.
PY - 2015/7/15
Y1 - 2015/7/15
N2 - Abstract Lanthanum, yttrium, and neodymium doped uranium dioxide samples in the fluorite structure have been synthesized, characterized in terms of metal ratio and oxygen content, and their enthalpies of formation measured by high temperature oxide melt solution calorimetry. For oxides doped with 10-50 mol % rare earth (Ln) cations, the formation enthalpies from constituent oxides (LnO1.5, UO2 and UO3 in a reaction not involving oxidation or reduction) become increasingly exothermic with increasing rare earth content, while showing no significant dependence on the varying uranium oxidation state. The oxidation enthalpy of LnxU1-xO2-0.5x+y is similar to that of UO2 to UO3 for all three rare earth doped systems. Though this may suggest that the oxidized uranium in these systems is energetically similar to that in the hexavalent state, thermochemical data alone can not constrain whether the uranium is present as U5+, U6+, or a mixture of oxidation states. The formation enthalpies from elements calculated from the calorimetric data are generally consistent with those from free energy measurements.
AB - Abstract Lanthanum, yttrium, and neodymium doped uranium dioxide samples in the fluorite structure have been synthesized, characterized in terms of metal ratio and oxygen content, and their enthalpies of formation measured by high temperature oxide melt solution calorimetry. For oxides doped with 10-50 mol % rare earth (Ln) cations, the formation enthalpies from constituent oxides (LnO1.5, UO2 and UO3 in a reaction not involving oxidation or reduction) become increasingly exothermic with increasing rare earth content, while showing no significant dependence on the varying uranium oxidation state. The oxidation enthalpy of LnxU1-xO2-0.5x+y is similar to that of UO2 to UO3 for all three rare earth doped systems. Though this may suggest that the oxidized uranium in these systems is energetically similar to that in the hexavalent state, thermochemical data alone can not constrain whether the uranium is present as U5+, U6+, or a mixture of oxidation states. The formation enthalpies from elements calculated from the calorimetric data are generally consistent with those from free energy measurements.
KW - Doped uranium oxide
KW - Formation enthalpy
KW - Thermochemistry
UR - http://www.scopus.com/inward/record.url?scp=84937539055&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84937539055&partnerID=8YFLogxK
U2 - 10.1016/j.jnucmat.2015.06.059
DO - 10.1016/j.jnucmat.2015.06.059
M3 - Article
AN - SCOPUS:84937539055
SN - 0022-3115
VL - 465
SP - 682
EP - 691
JO - Journal of Nuclear Materials
JF - Journal of Nuclear Materials
M1 - 49197
ER -