The O/U ratios of UO
2+x (0 ?? x ?? 0.1) were determined at 1, 000 and 1, 200°C, using a thermobalance in atmospheres of controlled oxygen pressures set by CO/CO
2 gases. The oxygen potentials corresponding to the x values were measured in situ with a solid elec-trolyte oxygen sensor. For x ?? 0.015 the present
ΔGO2 data agree well with the previously published data. In the range of 0<x ?? 0.015, the increasing disagreement at smaller values of x was indicated ; the present
ΔGO2 values are 2 to 15 kcal/mol more negative than the prior thermogravimetric data. The results also showed that a reverse in
ΔGO2 at 1, 000 and 1, 200°C occurs in the range of 2.003<O/U<2.015. The maximum in the plot of the partial molar entropy
ΔSO2 vs. O/U ratio has consequently been found near
ΔSO2=11 e.u. for O/U=2.007. This
ΔSO2 value is considerably high in comparison with Markin & Bones' EMF data, suggesting a characteristic configuration of oxygen in the lattice near UO
2.007.
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