Understanding the
alteration mechanisms of UO2-based
nuclear fuel has a range of practical implications for both short-
and long-term storage of spent fuel rods and environmental ramifications
for the mobility of radioactive material at the Chernobyl and Fukushima
sites. The major identified alteration phases on the surface of nuclear
waste are analogues of schoepite UO3·2H2O, studtite UO2(O2)·4H2O, rutherfordine
UO2CO3, and čejkaite Na4UO2(CO3)3. While α-radiolysis has
been shown to cause the ingrowth of uranyl peroxide alteration phases,
the prevalence of uranyl carbonate phases on solid waste forms has
not been mechanistically explained to date, especially since the alteration
chemistry is largely affected by the high temperatures of the spent
nuclear material. Herein, we demonstrate the first mechanistic link
between the formation of the uranyl superoxide (KUPS-1) phase, its reactivity at temperature ranges relevant to the spent
nuclear fuel (40–350 °C), and its thermodynamic transformation
into a potassium uranyl carbonate mineral phase, agricolaite K4[UO2(CO3)3], using thermogravimetric
analysis, calorimetry, vibrational spectroscopy, and powder X-ray
diffraction techniques. The thermodynamics data reveal the metastability
of the uranyl superoxide KUPS-1 phase through decomposition
of the hydrogen peroxide within the solid-state lattice. Increasing
the temperature does not result in the breakdown of the superoxide
anion bound to the uranyl cation but instead enhances its reactivity
in the presence of CO2 gas, resulting in potassium carbonate
phases at intermediate temperatures (150 °C) and in uranyl carbonate
phases at higher temperatures (350 °C).