RuO2 and IrO2 are among the most
active catalysts
for the Oxygen Evolution Reaction (OER). Recently, it was demonstrated
that the catalytic surface of these oxides plays a role in the reaction,
where a hydrogen bond with a neighbor OH group stabilizes an unconventional
−OO intermediate (−OO–H), prior to O2 evolution. Quantum chemical calculations neglecting solvation effects
indicated that this intermediate is more stable than the conventional
−OOH, and that deprotonation of the stabilizing −OH
is the rate limiting step for OER on RuO2(110) and RuO2(100). In this work, we investigate the role of water molecules
on the relative stability of −OOH and −OO–H oxygenates
on RuO2 (110) by means of density functional theory calculations
combined with ab initio Molecular Dynamics simulations (AIMD). We
show that the two intermediates participate in a hydrogen bonding
network with water to a similar extent, but leading to different interfacial
water structures, with possible implications on interfacial proton
dynamics and reaction kinetics. Moreover, −OOH can spontaneously
convert to −OO–H through a process mediated by water,
demonstrating the critical role of explicitly including water in the
model. This study provides further mechanistic insights on the role
of the oxide surface chemistry in the OER mechanism and highlights
the importance of explicitly treating the catalyst/water interfaces
including dynamical aspects to assess the stability and the interconversion
mechanism of key surface species, since the adoption of static solvation
approaches tends to overestimate the energetic difference between
−OOH and −OO–H reaction intermediates.