Oxygen stable isotopes
in uranium oxides processed through the
nuclear fuel cycle may have the potential to provide information about
a material’s origin and processing history. However, a more
thorough understanding of the fractionating processes governing the
formation of signatures in real-world samples is still needed. In
this study, laboratory synthesis of uranium oxides modeled after industrial
nuclear fuel fabrication was performed to follow the isotope fractionation
during thermal decomposition and reduction of ammonium diuranate (ADU).
Synthesis of ADU occurred using a gaseous NH3 route, followed
by thermal decomposition in a dry nitrogen atmosphere at 400, 600,
and 800 °C. The kinetic impact of heating ramp rates on isotope
effects was explored by ramping to each decomposition temperature
at 2, 20, and 200 °C min–1. In addition, ADU
was reduced using direct (ramped to 600 °C in a hydrogen atmosphere)
and indirect (thermally decomposed to U3O8 at
600 °C, then exposed to a hydrogen atmosphere) routes. The bulk
oxygen isotope composition of ADU (δ18O = −16
± 1‰) was very closely related to precipitation water
(δ18O = −15.6‰). The solid products
of thermal decomposition using ramp rates of 2 and 20 °C min–1 had statistically indistinguishable oxygen isotope
compositions at each decomposition temperature, with increasing δ18O values in the transition from ADU to UO3 at
400 °C (δ18OUO3 – δ18OADU = 12.3‰) and the transition from UO3 to U3O8 at 600 °C (δ18OU3O8 – δ18OUO3 = 2.8‰). An enrichment of 18O attributable to
water volatilization was observed in the low temperature (400 °C)
product of thermal decomposition using a 200 °C min–1 ramp rate (δ18OUO3 – δ18OADU = 9.2‰). Above 400 °C, no additional
fractionation was observed as UO3 decomposed to U3O8 with the rapid heating rate. Indirect reduction of
ADU produced UO2 with a δ18O value 19.1‰
greater than the precipitate and 4.0‰ greater than the intermediate
U3O8. Direct reduction of ADU at 600 °C
in a hydrogen atmosphere resulted in the production of U4O9 with a δ18O value 17.1‰ greater
than the precipitate. Except when a 200 °C min–1 ramp rate is employed, the results of both thermal decomposition
and reduction show a consistent preferential enrichment of 18O as oxygen is removed from the original precipitate. Hence, the
calcination and reduction reactions leading to the production of UO2 will yield unique oxygen isotope fractionations based on
process parameters including heating rate and decomposition temperature.