The
3d transition metal oxides with a spinel structure are among
the most promising cathode materials for magnesium batteries. In this
study, we investigated the reaction mechanism of magnesium ion insertion
for magnesium spinel oxides, MgMn2O4, by electrochemical
measurements, X-ray absorption spectroscopy (XAS), and synchrotron
X-ray diffraction (XRD) with Rietveld analysis. Open-circuit-potential
and XAS measurements showed that Mg2+ insertion into MgMn2O4 does not proceed via a simple two-phase coexistence
reaction between the spinel and rock-salt phases. Synchrotron XRD
measurements showed that Mg2+ insertion into MgMn2O4 involves crystal structural changes in three stages.
In the early stage of the Mg2+ insertion process (0 < x < 0.2), Mg2+ is inserted into the spinel
(MgMn2O4) phase and rock-salt (Mg1.2Mn2O4) phases, which are included in the pristine
samples, without significant volume changes. In the middle stage of
the Mg2+ insertion process (0.2 < x < 0.4), Mg2+ is inserted into the Mg1+αMn2O4 spinel phase and the Mg2−βMn2O4 rock-salt phases with a large volume
change. In the last stage of Mg2+ insertion process (0.4
< x < 0.56), Mg2+ insertion proceeds
via a two-phase coexistence reaction between Mg1.4Mn2O4 spinel and Mg1.6Mn2O4 rock-salt phases without Mg content changes in either phase.
The phase transition from the Mg1+αMn2O4 spinel phase to the Mg2−βMn2O4 rock-salt phase with a large volume change resulted
in significant polarization during the Mg2+ insertion process.
Suppressing the phase transition, accompanied by a large volume change,
is important in designing a spinel oxide cathode with a high rate
performance.