“…In fact, the site occupation mainly depends on the electrostatic contribution to the lattice energy, the cation radii, cation charges, and crystal eld effects. In a typical spinel ferrite structure, the A 2+ cations are located at tetrahedral sites, while Fe 3+ cations are found at octahedral sites, for example in ZnFe 2 O 4 , which is similar to some other spinel crystalline structures such as CoAl 2 O 4 , 18 MgAl 2 O 4 , and Mn 3 O 4 . 19 For the inverse spinel structure, Fe 3+ cations are equally distributed between tetrahedral and octahedral sites while A 2+ cations only occupy octahedral sites, for example in NiFe 2 O 4 , CoFe 2 O 4 , 20,21 In 1945, L. Néel et al 16 investigated the exchange interactions and cationic distributions in spinel ferrite nanostructures to evaluate their magnetic properties.…”