“…Since there is a significant difference between the proposed phase regions, and Aitken and Joseph [7] only determined the presence of the fluorite and rhombohedral phases, the phase equilibria of Bartram et al [6] were used in the current assessment. A limitation in the work of Bartram et al [6] however, is that no three-phase regions appear in their proposed diagram, whereas that would be expected based on observations in similar systems containing rare earths (RE) [8]. The only other thermodynamic data for this system are from thermogravimetric determinations of oxygen potential vs O/M of Hagemark and Broli [9] and partial pressure determinations of U, UO, and UO 2 species from the Knudsen effusion mass spectrometry (KEMS) of Nakajima et al [10].…”