The
oxygen (O2) evolution reaction (OER) is accepted
as the bottleneck in the overall water splitting and has seen intense
interest. In this work, we prepared rutile TiO2 modified
with nanoclusters of alkaline-earth metal oxides for the OER. Photocatalytic
OER was performed over rutile TiO2 surface-modified with
alkaline-earth oxide nanoclusters, namely, CaO and MgO. The O2 evolution activity is notably enhanced for MgO-modified systems
at low loadings and a combination of characterization and first-principles
simulations allows interpretation of the role of the nanocluster modification
in improving the photocatalytic performance of alkaline-earth-modified
rutile TiO2. At such low loadings, the nanocluster modifiers
would be small, and this facilitates a close correlation with theoretical
models. Structural and surface characterizations of the modified systems
indicate that the integrity of the rutile phase is maintained after
modification. However, charge-carrier separation is strongly affected
by the presence of surface nanoclusters. This improved performance
is related to surface features such as higher ion dispersion and surface
hydroxylation, which are also discussed with first-principles simulations.
The modified systems are reducible so that Ti3+ ions will
be present. Water dissociation is favorable at cluster and interfacial
sites of the stoichiometric and reduced modified surfaces. Pathways
to water oxidation at interfacial sites of reduced MgO-modified rutile
TiO2 are identified, requiring an overpotential of 0.68
V. In contrast, CaO-modified systems required overpotentials in excess
of 0.85 V for the reaction to proceed.