The increased energy
density in Li-ion batteries is particularly
dependent on the cathode materials that so far have been limiting
the overall battery performance. A new class of materials, Li-rich
disordered rock salts, has recently been brought forward as promising
candidates for next-generation cathodes because of their ability to
reversibly cycle more than one Li-ion per transition metal. Several
variants of these Li-rich cathode materials have been developed recently
and show promising initial capacities, but challenges concerning capacity
fade and voltage decay during cycling are yet to be overcome. Mechanisms
behind the significant capacity fade of some materials must be understood
to allow for the design of new materials in which detrimental reactions
can be mitigated. In this study, the origin of the capacity fade in
the Li-rich material Li2VO2F is investigated,
and it is shown to begin with degradation of the particle surface
that spreads inward with continued cycling.
Lithium-rich transition metal disordered rock salt (DRS) oxyfluorides have the potential to lessen one large bottleneck for lithium ion batteries by improving the cathode capacity. However, irreversible reactions at the electrode/electrolyte interface have so far led to fast capacity fading during electrochemical cycling. Here, we report the synthesis of two new Li-rich transition metal oxyfluorides Li 2 V 0.5 Ti 0.5 O 2 F and Li 2 V 0.5 Fe 0.5 O 2 F using the mechanochemical ball milling procedure. Both materials show substantially improved cycling stability compared to Li 2 VO 2 F. Rietveld refinements of synchrotron X-ray diffraction patterns reveal the DRS structure of the materials. Based on density functional theory (DFT) calculations, we demonstrate that substitution of V 3+ with Ti 3+ and Fe 3+ favors disordering of the mixed metastable DRS oxyfluoride phase. Hard X-ray photoelectron spectroscopy shows that the substitution stabilizes the active material electrode particle surface and increases the reversibility of the V 3+ /V 5+ redox couple. This work presents a strategy for stabilization of the DRS structure leading to improved electrochemical cyclability of the materials. † Electronic supplementary information (ESI) available: PXRD pattern of ceramic synthesis attempts; structural parameters of the Rietveld renements; PXRD pattern of Li 2 VO 2 F with Rietveld renement; Williamson-Hall-plots; TEM and EDX analysis; SQS of Li 2 TMO 2 F and Li 2 TM1 0.5 TM2 0.5 O 2 F; ordered structures of Li 2 TM1 0.5 TM2 0.5 O 2 F; table of energy difference between the ordered/decomposed state and disordered state; table of oxidation states of TMs; voltage proles of Li 2 VO 2 F, Li 2 V 0.5 Ti 0.5 O 2 F and Li 2 V 0.5 Fe 0.5 O 2 F half-cells cycled up to 4.1 V; PXRD pattern of cycled electrodes; HAXPES Fe 2p peak tting; HAXPES survey of Li 2 V 0.5 Fe 0.5 O 2 F and Li 2 VO 2 F and uorine plasmon overlaps with the Fe 2p 3/2 peak; core level photoelectron spectra of Fe 2p and Ti 2p; cycling performance of Li 2 VO 2 F, Li 2 V 0.5 Ti 0.5 O 2 F and Li 2 V 0.5 Fe 0.5 O 2 F half-cells cycled up to 4.5 V. See
Disordered rock salt Li 2 VO 2 F cathode material for lithium-ion batteries was investigated using operando X-ray diffraction and total scattering to gain insight into the structural changes of the short-range and long-range orders during electrochemical cycling. The X-ray powder diffraction data show the well-known pattern of the disordered rock salt cubic structure, whereas the pair distribution function (PDF) analysis reveals significant deviations from the ideal cubic structure. During battery operation, a reversible rock salt-toamorphous phase transformation is observed, upon Li extraction and reinsertion. The X-ray total scattering data show strong indications of the formation of tetrahedrally coordinated V in a nondisordered rock salt phase of the charged electrode material. The results show that the disordered rock salt Li 2 VO 2 F material undergoes a hidden structural rearrangement during battery operation.
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