“…Fe 2p core-level spectra is shown in Figure b. The peaks at 710.2 and 724.6 eV correspond to Fe 3+ 2p 3/2 and Fe 3+ 2p confirming the presence of Fe in its 3+ state present at the O h sites. ,,, Alongside this, peaks at 713.3 and 726.4 eV correspond to the presence of Fe 3+ 2p 3/2 and Fe 3+ 2p, confirming the presence of Fe in its 3+ state present at the tetrahedral sites, thereby showing that successful spinel inversion has occurred, because Fe is present in both octahedral and tetrahedral sites. ,,,,, The δ parameter can be calculated from the area ratio of the octahedral and tetrahedral site peaks of Fe 2p and Cu 2p, according to Fantauzzi et al The ratio of Fe:Cu in the analyzed sample CuFeM was observed to be 1.9. The general formula for CuFe 2 O 4 spinel is [Fe δ Cu 1−δ ]( T d )[Cu δ Fe 2−δ ](O h )O 4 .…”