Heat capacities of UO 2.017 and UO 2.254 have been measured in the range 300 to 1000 K by adiabatic calorimetry. The enthalpy and entropy increments { X o(1000 K) − X o(0)} are 66.49 kJ mol −1 and 170.2 J K −1 mol −1 for UO 2.017, and 72.91 kJ mol −1 and 185.7 J K −1 mol −1 for UO 2.254. The increments { X o(298 K) − X o(0)} are based upon literature data. In UO 2.017 the presence of the U 4O 9 phase causes slightly variable heat capacities in the range 300 to 360 K due to a partial suppression of the transition in U 4O 9 in the super-saturated solid solution of U 4O 9 in UO 2. Augmented heat capacity values are observed in the range 500 to 800 K, due to the solution of U 4O 9 in UO 2. In UO 2.254 a λ-type transition is present with maximum at 348 K and an entropy increment of 2.18 J K −1 mol −1, presumably connected with interchange of interstitial and displaced oxygen atoms. A small irregularity in the heat capacity is observed in the region 900 to 950 K with an entropy increment of 0.15 J K −1 mol −1. It is superimposed on a general increase in the heat capacity, presumably due to the onset of a transition. Attempts to resolve the various contributions to the heat capacity of UO 2 show that the electronic contribution is large. It is interpreted in terms of a doubly degenerate level of the 5f 2 electrons about 900 cm −1 above the triply degenerate ground level followed by a triply degenerate level about 1600 cm −1 above, and a singly degenerate level about 2900 cm −1, above the ground level. Further excited levels are also considered, but they are apparently not numerous enough to explain the enhanced heat capacity above 2000 K. In the region 2000 to 3000 K structural order-disorder processes, vacancy formation, and phase separation from the stoichiometric dioxide probably occur. The results for UO 2.254 also indicate a large electronic contribution. It is tentatively analyzed assuming the presence of U(IV) and U(V) in equal amounts, corresponding to the formula 2UO 2·U 2O 5. If the contribution from U(IV) remains unchanged above 300 K, the electronic entropy of U(V) is about 7.3 J K −1 mol −1 for 1 2 UO 2. 1 4 U 2O 5 at 600 K. This indicates that at least six levels of the 5f 1 configuration are of importance in the region up to 600 K. The possibility of a doubly degenerate ground level followed by a quadruply degenerate level about 500 cm −1 above it is discussed in terms of available ligand field data for U(V).
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