“…The diffraction peaks at 23.91, 33.32, 35.71, 40.71, 49.53, 54.14, 57.72, 62.54, and 63.93° correspond to the (012), (104), (110), (113), (024), (116), (018), (214), and (030) diffractions of pure hematite (α-Fe 2 O 3 ). , The compositional (changing the Fe/O ratio from 3:4 to 2:3) and structural modifications are both involved in the phase transformation from Fe 3 O 4 to α-Fe 2 O 3 . The process is called oxygen dissociation and can occur at temperatures starting from 700 to 1000 °C, but the exact temperature varies due to composition and oxygen partial pressure.…”