Abstract
Herein, a method is presented to determine the kinetics of the oxygen dissociation on different metals, allowing for the determination of the oxygen reduction reaction mechanism. This analysis reveals that molecular oxygen rapidly dissociates to underpotentially deposited oxygen species on platinum and rhodium surfaces. These species' experimentally determined surface charges lead to a simple kinetic model of the ORR, which agrees well with experimental ORR activities and predicts the Volcano relationship with the oxygen reduction reaction.