The Rh(111) electrode shows superior oxygen reduction reaction (ORR) activity to Ir(111), contradicting the predicted trend based on the volcano plot. To unveil the origin for this, we investigate the interfacial structures of Rh(111) single crystalline electrode in 0.1 M HClO4 and 0.5 M H2SO4 solutions using cyclic voltammetry and potential step chronoamperometry under a hanging meniscus rotating disk electrode configuration. Our results reveal that i) in N2 saturated solution even at a potential below 0.20 V, oxygen-containing species adsorbates can be formed on the Rh(111) surface probably generated by oxidation of water; ii) Even under mild conditions, multiple cycles and current transients in O2 saturated solution at potentials where ORR taking place can cause significant surface disordering; iii) The disordering of the Rh(111) electrode induced by ORR exhibits similar base cyclic voltammograms to those of vicinal Rh(hkl) such as Rh(553) and Rh(332) etc., depending on the potentials applied during ORR, which, in turn, enhances the ORR activity in both 0.1 M HClO4 and 0.5 M H2SO4. These new findings provide valuable insights into the structure-performance relationship of ORR.
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