“…The C 1s spectra can be divided into four peaks of 284.8 eV (C–C), 286.0 eV (C–O), 286.0 eV (CO), and 293.72 eV (O–CO) as shown in Figure a . In the Fe 2p spectra (Figure b), the Fe 0 2p 3/2 and Fe 0 2p 1/2 peaks appear at 706.8 and 720.4 eV, respectively, originating from Fe 3 C. The existence of nonzero valence iron including Fe 2+ 2p 3/2 (710.8 eV), Fe 2+ 2p 1/2 (724.1 eV), Fe 3+ 2p 3/2 (712.8 eV), and Fe 3+ 2p 1/2 (725.8 eV) indicates the formation of a passivating layer, and the satellite peaks (716 and 719 eV) originate from the high spin–orbit of Fe 2+ and Fe 3+ . , In addition, the increasing temperature led to the enhancement of the Fe 2p signal intensity, which indicates that more Fe elements are present on the surface of the composite material. This can attributed to the high temperature, which gives rise to significant consumption of the organic carbon resource during the carbothermal process resulting in the feature of nanosized magnetic metallic alloys wrapped by a thinner carbon layer, and the Fe-based alloys were easily oxidized.…”