“…The peaks with binding energies of 284.3, 284.8, 285.2, 286.5, and 289.6 eV could be attributed to the presence of carbon–iron bonds (C–Fe), carbon–carbon bonds (C–C), carbon–nitrogen bonds (C–N), carbon–oxygen bonds (C–O), and the carbonyl carbon (CO), respectively. , In the high-resolution XPS pattern of the O 1s (Figure b), it could be fitted into three peaks centered at 530.45, 532.09, and 533.38 eV, corresponding to three kinds of the O species. Based on the microcrystalline binding energy of magnetite, the peaks at 530.45 might be assigned to lattice oxygen (O latt ) related to metal oxide. , The peaks centered at 532.09 and 533.38 eV were ascribed to the oxygen species adsorbed on the surface (O ads ) and the surface-absorbed molecular H 2 O (O surf ), respectively. − As illustrated in the high-resolution XPS spectrum of Fe 2p (Figure c), it had two broad peaks at 711.6 and 724.3 eV, corresponding to the Fe 2p 3/2 and Fe 2p 1/2 spin orbitals, respectively. Six peaks could be deconvoluted.…”