Cation distribution in manganese cobaltite spinels Co_3−x Mn _x O₄ (0 ≤ x ≤ 1) determined by thermal analysis

Abstract

Thermogravimetric analysis was used in order to study the reduction in air of submicronic powders of Co_3−x Mn _x O₄ spinels, with 0 ≤ x ≤ 1. For x = 0 (i.e. Co₃O₄), cation reduction occurred in a single step. It involved the Co^III ions at the octahedral sites, which were reduced to Co²⁺ on producing CoO. For 0 < x ≤ 1, the reduction occurred in two stages at increasing temperature with increasing amounts of manganese. The first step corresponded to the reduction of octahedral Co^III ions and the second was attributed to the reduction of octahedral Mn⁴⁺ ions to Mn³⁺. From the individual weight losses and the electrical neutrality of the lattice, the Co^III and Mn⁴⁺ ion concentrations were calculated. The distribution of cobalt and manganese ions present on each crystallographic site of the spinel was determined. In contrast to most previous studies that took into account either Co^III and Mn³⁺ or Co²⁺, Co^III and Mn⁴⁺ only, our thermal analysis study showed that Co²⁺/Co^III and Mn³⁺/Mn⁴⁺ pairs occupy the octahedral sites. These results were used to explain the resistivity measurements carried out on dense ceramics prepared from our powders sintered at low temperature (700–750 °C) in a Spark Plasma Sintering apparatus.