The structures, properties, and spectroscopic
signatures of oxidized
water clusters,(H2O)+
n=6–21, are examined
in this work, to provide fundamental insight into renewable energy
and radiological processes. Computational quantum chemistry approaches
are employed to sample cluster morphologies, yielding hundreds of
low-lying isomers with low barriers to interconversion. The ion–radical
pair-separation trend, however, which was observed in previous computational
studies and in small-cluster spectroscopy experiments, is shown to
continue in this larger cluster size regime. The source of this trend
is preferential solvation of the hydronium ion by water, including
effects beyond the first solvation shell. The fundamental conclusion
of this work, therefore, is that the initially formed ion–radical
dimer, which has served as a prototypical model of oxidized water,
is a nascent species in large, oxidized water clusters and, very likely,
bulk water.