We investigate the reversible and irreversible transformations, the Li, Mn spinel undergoes under different atmospheres (air, O2, and N2) when heated up to 1050 °C. In air and O2, a substantial reversible cation exchange occurs. For T≥800 °C, Mn2+ ions substitute Li+ at the tetrahedral (8a) position, and Li+ shifts to interstitial octahedral (16c) site. Charge balance is achieved by a decrease in
... [Show full abstract] the Mn3+ fraction, which is partially reduced to Mn2+ in the regular octahedral (16d) site, according to the charge distribution (Li1−2y+Mn2y2+)8a[Li3y+]16c[Mn5y2+Mn1−5y3+Mn14+]16dO4 (y increases with T). Under N2 flow, a first decomposition occurs between 600 and 800 °C and yields Mn3O4, orthorhombic LiMnO2 and O2. A minor O2 release occurs when heating above 900 °C, which is accompanied by the transformation of o-LiMnO2 into a cubic LixMn1−xO solid solution (x≤0.5), consistent with a decrease in the average oxidation state of Mn ions. This cubic phase is stable at high temperature and decomposes upon cooling leaving just the Mn3O4 and o-LiMnO2 phases.