“…The spectra were deconvoluted into several main component peaks located at 710.8, 713.2, 717.5, 724.7, and 731.7 eV. Previous studies showed that the peaks at 710.8 (Fe 3+ oct 2p 3/2), 713.2 (Fe 3+ tet 2p 3/2), and 724.7 eV (Fe 3+ 2p 1/2) were related to Fe 3+ –O , and that satellite peaks at 717.5 and 731.7 eV attributed to Fe 3+ in γ-Fe 2 O 3 were observed in the Fe 2p spectra. , In the O 1s region, the peak related to Fe–O appeared at 533.2 eV. This indicates that the material is based on γ-Fe 2 O 3 .…”