“…The XPS N 1s patterns had four sub-peaks, namely, the pyridinic N group, pyrrolic N group, graphitic N group, and oxidized N group, which corresponded to 398.9, 400.2, 401.7, and 405.3 eV, respectively. ,,,− Table lists the corresponding deconvolution results of the two samples. Several studies have reported that, except for oxidized N, the other N-containing groups (i.e., pyridinic N and graphitic N) play crucial roles in the ORR process. ,,, Pyridinic N exerts a conjugation effect on its lone pair of electrons and the π system, facilitating O 2 adsorption and therefore improving ORR activity. ,− Graphitic N makes neighboring carbons display more positive spin and charge densities, which produce active sites for ORR . The total contents of pyridinic N and graphitic N in Fe–N–Co@C-800-AL are higher than those in Co@C-800-AL, which is consistent with the trends of ORR activity.…”