During further charging, the Fe3+ doublet successively disappears and is replaced by a new narrow doublet with isomer shift of -0.134(6) mm/s. This negative value clearly reveals that Fe4+ is formed. Further cycling between 5.3 V and 4.3 V reveals that this oxidation is highly reversible.
The XAS spectra acquired during charging of LiCo0.8Fe0.2MnO4 vs. Li+|Li clearly show a shift of the Fe K absorption edge towards higher binding energies and thus an oxidation of Fe3+ to Fe4+. The XAS spectra acquired during discharging show again that this process is fully reversible.
In summary, the reversible formation Fe4+ was clearly observed by both methods, hence proving the electrochemical activity of Fe at voltages above 5 V vs. Li+/Li. This enables future research on new environmentally benign and inexpensive electrode materials with operating voltages above 5 V and thus an increased energy density.
[1] Observation of Electrochemically Active Fe3+/Fe4+ in LiCo0.8Fe0.2MnO4 by in situ Mössbauer Spectroscopy and X-Ray Absorption Spectroscopy,
C. Dräger, F. Sigel, R. Witte, R. Kruk, L. Pfaffmann, V. Mereacre, M. Knapp, H. Ehrenberg, S. Indris, Phys. Chem. Chem. Phys. 21, 89-95 (2019).
