The reactions in the U-Cs-Mo-I-O system at 1073 K have been studied as
a function of oxygen potential. The chemical constitution and the mor
phology of the phases formed were examined by electron-probe microanal
yzer and X-ray diffractometer. The existence of a two-phase field UO2x + Cs2UO4 was confirmed in the U-Cs-O system, The threshold oxygen po
tential was determined for the decomposition of CsI by UO2+x to form C
s2U4O12 and gaseous iodine. The effect of molybdenum on the UO2+x-CsI
reaction was also investigated. Predominance of Cs2MoO4 over Cs2UO4 wa
s verified in a certain range of oxygen potentials. Some assessments a
nd interpretations of the experimental results were made with the aid
of thermodynamic calculations.