“…The satellite peaks, energy difference (ΔE) between the first lines of the Fe 2p 3/2 and Fe 2p 1/2 doublets (range 13.12-13.94 eV), and the energy difference between subcomponents (Δε) in each doublet (range of 0.50-1.72 eV) confirm Fe ions mostly in the trivalent (+3) charge state. 30,36,50,51 The depressed satellites in Ca-doped sample suggest a large chemical disorder at the Fe sites, which may arise due to the multi-valence (+3, +2) states of Fe ions or fractional charge transfer between Fe ions via Fe +(3−δ) -O 2− -Fe +(2+δ) (0 ≤ δ ≤1) superexchange paths that lead to partially covalence character between Fe 3+ and O 2− orbitals. 53 Theoretically, Fe 2p 3/2 and 2p 1/2 bands can form 4 and 2 multiplets.…”