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过渡金属迁移和氧的形成是氧氧化还原无序岩盐阴极中电压滞后现象的基础。

Transition metal migration and O formation underpin voltage hysteresis in oxygen-redox disordered rocksalt cathodes.

作者信息

McColl Kit, House Robert A, Rees Gregory J, Squires Alexander G, Coles Samuel W, Bruce Peter G, Morgan Benjamin J, Islam M Saiful

机构信息

Department of Chemistry, University of Bath, Bath, UK.

The Faraday Institution, Harwell Science and Innovation Campus, Didcot, UK.

出版信息

Nat Commun. 2022 Sep 7;13(1):5275. doi: 10.1038/s41467-022-32983-w.

Abstract

Lithium-rich disordered rocksalt cathodes display high capacities arising from redox chemistry on both transition-metal ions (TM-redox) and oxygen ions (O-redox), making them promising candidates for next-generation lithium-ion batteries. However, the atomic-scale mechanisms governing O-redox behaviour in disordered structures are not fully understood. Here we show that, at high states of charge in the disordered rocksalt LiMnOF, transition metal migration is necessary for the formation of molecular O trapped in the bulk. Density functional theory calculations reveal that O is thermodynamically favoured over other oxidised O species, which is confirmed by resonant inelastic X-ray scattering data showing only O forms. When O-redox involves irreversible Mn migration, this mechanism results in a path-dependent voltage hysteresis between charge and discharge, commensurate with the hysteresis observed electrochemically. The implications are that irreversible transition metal migration should be suppressed to reduce the voltage hysteresis that afflicts O-redox disordered rocksalt cathodes.

摘要

富锂无序岩盐阴极由于过渡金属离子(TM-氧化还原)和氧离子(O-氧化还原)上的氧化还原化学作用而展现出高容量,这使其成为下一代锂离子电池的有潜力候选材料。然而,无序结构中控制O-氧化还原行为的原子尺度机制尚未完全被理解。在此我们表明,在无序岩盐LiMnOF的高充电状态下,过渡金属迁移对于形成被困在体相中的分子氧是必要的。密度泛函理论计算表明,相比于其他氧化态的氧物种,O在热力学上更受青睐,这一点通过仅显示O形式的共振非弹性X射线散射数据得到证实。当O-氧化还原涉及不可逆的Mn迁移时,这种机制会导致充电和放电之间与电化学观测到的滞后现象相当的路径依赖电压滞后。这意味着应抑制不可逆的过渡金属迁移以减少困扰O-氧化还原无序岩盐阴极的电压滞后。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/672d/9452515/329a55e2c080/41467_2022_32983_Fig1_HTML.jpg

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