X-ray photoelectron spectroscopy (XPS) measurements also demonstrated that both of PCN-224(Fe)-900 and PANI@PCN-224(Fe)-900 samples contain Fe, N, and C elements (Figure S10). The high-resolution N 1s spectra can be deconvoluted into pyridinic N (398.2 eV), Fe-Nx (399.4 ± 0.2 eV), pyrrolic N (400.5 ± 0.1 eV), graphitic N (401.4 ± 0.2 eV), and oxidized N (403.2 ± 0.2 eV) (Figure
5(a) and Figures S11(a) and S11(b)) [
57]. Notably, the relative ratio of Fe-Nx with other nitrogen species in PANI@PCN-224(Fe)-900 is much higher than that of PCN-224(Fe)-900 (Figure
5(b)). For iron species, two peaks at 710 and 721.9 eV in the high-resolution Fe 2p spectrum of PANI@PCN-224(Fe)-900 suggested that Fe
2+ species was dominated in this sample, which may be coordinated with nitrogen that inherited from Fe-TCPP (Figure S11(c)) [
27,
28,
58]. Furthermore, according to the elemental analysis (EA, Table S1) and inductively coupled plasma atomic emission spectroscopy (ICP-AES, Table S2) results, both of the N and Fe element contents in
X-PANI@PCN-224(Fe)-900 increase along with the increasing of the inserted PANI content. It is also worth mentioning that PANI@PCN-224(Fe)-900 has much higher amounts of N and Fe element than those of PCN-224(Fe)-900 (Tables S1 and S2 and Figure S11). The results benefit from the fact that the PANI in PANI@PCN-224(Fe)-900 could provide effective protective layers and prevent the Fe species migrating and aggregating to form particles during pyrolysis. Moreover, the escaped iron element from Fe-TCPP units during annealing could be captured by the inserted PANI-derived N-doped carbon to stabilize atomic Fe-
species [
25,
38,
59–
61]. Thus, PANI@PCN-224(Fe)-900 has a higher Fe amount of 1.89 wt%, while only 0.27 wt% Fe content comprising part of Fe
3C/Fe was detected in PCN-224(Fe)-900 (Figure S5 and Figure
4(b)). The very low Fe amount in PCN-224(Fe)-900 is due to the Fe ions which were lack of protection and easy formed aggregated Fe-based NPs, which were leached by acid etching. In addition, the inserted PANI could also act as nitrogen sources to increase the nitrogen content and nitrogen-containing carbon active-site density of PANI@PCN-224(Fe)-900 (Figures S11(d) and S12), which could enhance synergistically for ORR in combination with Fe-
sites [
38,
62,
63]. To further identify the electronic and structural status of iron species in PANI@PCN-224(Fe)-900 and PCN-224(Fe)-900, X-ray absorption near-edge structure (XANES) and X-ray absorption fine structure (EXAFS) were performed (Figures
5(c) and
5(d)). The absorption edge energy of Fe K-edge in PANI@PCN-224(Fe)-900 and PCN-224(Fe)-900 located between Fe foil and 5,10,15,20-tetrakis(4-cyanophenyl)porphyrinato]-Fe(III) chloride (Fe-TPPCN), implying the positively charged iron species in both of the two samples, which are consistent with the XPS results. Furthermore, a weak pre-edge peak at 7112 eV was observed in both of PANI@PCN-224(Fe)-900 and PCN-224(Fe)-900, which is recognized as a fingerprint of
symmetry and suggested the existence of Fe-N
4 square-planar structure [
25,
33,
64]. The analysis of Fe K-edge of EXAFS further revealed that atomic Fe-
species was predominated in PANI@PCN-224(Fe)-900, while PCN-224(Fe)-900 contains the N-coordinated Fe and a large amount of Fe-based NPs including Fe
3C and Fe. As shown in Figure
5(d), the main signal at 1.47 Å that assigned to the Fe-N scattering path further revealed that the Fe species in PANI@PCN-224(Fe)-900 was predominant Fe-
configuration [
32,
65]. Notably, compared with the R value (1.47 Å) in PANI@PCN-224(Fe)-900, the corresponding value of Fe(Cl)-N
4 peak in Fe-TPPCN molecule shifts to 1.59 Å, which is ascribed to that the axial chlorine atom perpendicular to the Fe-N
4 plane elongates the Fe-N bond distance [
25,
26,
31,
66–
68]. Nevertheless, the partial R values overlap between PANI@PCN-224(Fe)-900 and Fe-TPPCN suggests the existence of Fe-N
4 and Fe-N
5 species, which is difficult to use suitable coordination model to fit. The emergence of Fe-N
5, in which one axial nitrogen atom is perpendicular to the Fe-N
4 plane, was attributed to the nitrogen of the inserted PANI-derived carbon. More importantly, no obvious signals ascribed to Fe-Fe (2.2 Å) can be detected, manifesting the atomic dispersion of iron in PANI@PCN-224(Fe)-900. By contrast, the EXAFS curves of PCN-224(Fe)-900 exhibited a strong peak at 1.94 Å, which is more like the Fe-Fe distance in Fe
3C and metallic Fe [
27,
30]. These results confirmed that Fe-based NPs were presented in PCN-224(Fe)-900, which is consistent with the high-resolution TEM observation (Figure
4(b)). Taken together, the highly porous PANI@PCN-224(Fe)-900 with graphitic structure contains abundant single-atom Fe-
sites, which is believed to show highly active in electrocatalysis for ORR.