While Fe–N–C materials exhibit great potential
for
catalyzing the oxygen reduction reaction (ORR), their activity origin,
especially the significant activity difference in acidic and alkaline
media, remains a long-standing conundrum hindering the development
of such catalysts. Here, we show an unanticipated pH-dependent regulation
mechanism in Fe–N–C materials via first-principles microkinetic
computations that explicitly consider the pH, solvation, and electrode
potential effects. We find that, under typical operating potentials,
the well-established FeN4 centers of Fe −N–C
catalysts, regardless of the pyridinic and pyrrolic-type N-coordination
environments, are not adsorbate-free but covered by an intrinsic intermediate
*OH at pH = 1 and *O at pH = 13, resulting in FeN4–OH
and FeN4–O centers formed in situ. We evaluate the
pH- and potential-dependent kinetics and thermodynamics of the real
active Fe centers of Fe–N–C catalysts against experimental
measurements. We demonstrate that the activity difference of Fe–N–C
catalysts is attributed to the *O coordination-induced optimization
of the electronic structure and intermediate adsorption over the *OH
case. Our work provides the mechanistic insight into the pH effects
and paves the way toward a more effective catalyst design.