Hydrogen peroxide
is produced upon radiolysis of water and has
been shown to be the main oxidant driving oxidative dissolution of
UO
2
-based nuclear fuel under geological repository conditions.
While the overall mechanism and speciation are well known for granitic
groundwaters, considerably less is known for saline waters of relevance
in rock salt or during emergency cooling of reactors using seawater.
In this work, the ternary uranyl–peroxo–chloro and uranyl–peroxo–bromo
complexes were identified using IR, Raman, and nuclear magnetic resonance
(NMR) spectroscopy. Based on Raman spectra, the estimated stability
constants for the identified uranyl–peroxo–chloro ((UO
2
)(O
2
)(Cl)(H
2
O)
2
–
) and uranyl–peroxo–bromo ((UO
2
)(O
2
)(Br)(H
2
O)
2
–
) complexes are
0.17 and 0.04, respectively, at ionic strength ≈5 mol/L. It
was found that the uranyl–peroxo–chloro complex is more
stable than the uranyl–peroxo–bromo complex, which transforms
into studtite at high uranyl and H
2
O
2
concentrations.
Studtite is also found to be dissolved at a high ionic strength, implying
that this may not be a stable solid phase under very saline conditions.
The uranyl–peroxo–bromo complex was shown to facilitate
H
2
O
2
decomposition via a mechanism involving
reactive intermediates.