Electronic Origin and Kinetic Feasibility of the Lattice Oxygen Participation During the Oxygen Evolution Reaction on Perovskites

Density functional theory is employed to investigate the electronic origin and feasibility of surface lattice oxygen (O surf ) participation during the oxygen evolution reaction (OER) on perovskites. O surf participation occurs via the nonelectrochemical pathway in which adsorbed atomic oxygen (O*) diffuses from the transition-metal site to the oxygen site, and then O surf shifts out of the surface plane to react with O* to form O surf –O* and a surface oxygen vacancy. The different thermodynamic driving forces of O surf participation on LaMO 3−δ (M = Ni, Co, and Cu) are explained by the changes in the oxidation state of the transition-metal site throughout the reaction. We show that O surf participation on LaNiO 3 cannot be hindered by O surf protonation in the OER potential range. By including the coverage effect and utilizing the implicit solvent model, we finally show that lattice oxygen mechanism is more feasible than the conventional mechanism for OER on LaNiO 3 .