“…Moreover, differences in j p ORR values at different ω but constant v , as in Figure A,B, can only be explained by considering the existence of, at least, two soluble species with different diffusion coefficients. Different studies have shown currents larger than those expected in LSVs owing to the coupling of the diffusional pathways by very fast reactions of species in the diffusion layer with different diffusion coefficients, as in the case of homogeneously catalyzed reactions. − In our case, the thickness of the diffusion layer of one of the species is being determined by ω (eq ) and that of the other species by v . Then, changing ω at constant v would modify the flux of the soluble species whose diffusion layer is controlled by ω, giving rise to changes in j p ORR . ,, If only one soluble species were present, or several species with equal D , identical j p ORR values would have been observed at constant v , regardless of ω, since the concentration profiles close to the surface are only controlled by the magnitude of D . − , …”