Metal oxide surface properties, including surface reactivity, deconstruction, and electrostatics, all impact catalytic activity, but characterization of the metal oxide surface under hydrated conditions is notoriously challenging. Here, we modify a spinel cobalt oxide (Co3O4) lattice with La3+, systematically varying both the catalyst composition and the water vapor pressure to reveal how the ancillary cation changes the catalyst–water interface with ambient-pressure X-ray photoelectron spectroscopy (APXPS). Together with impedance spectroscopy and titrations, characterization of the interfacial surface reveals that increased La3+ incorporation increases metal oxide surface hydroxylation with higher water pressures (from 0 to 10 to 17 Torr). This increased hydroxylation of the unbiased metal oxide surface increases the formation of active sites that promote the oxygen evolution reaction (OER) by proton-coupled electron transfer. The correlation of increased hydroxylated active sites with La3+ ion incorporation is consistent with the previously established role of rare-earth cations in deconstructing Co3O4 to result in higher OER activity arising from more hydroxylated active sites in the amorphous overlayer of the Co3O4 spinel oxide lattice.
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Hartnett et al. (2026) studied this question.
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