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Stacking-Fault Enhanced Oxygen Redox in Li_2MnO_3

机译:堆叠故障增强氧氧化还原在Li_2MnO_3中的应用

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摘要

Lattice oxygen redox yields anomalous capacity and can significantly increase the energy density of layered Li-rich transition metal oxide cathodes, garnering tremendous interest. However, the mechanism behind O redox in these cathode materials is still under debate, in part due to the challenges in directly observing O and following associated changes upon electrochemical cycling. Here, with O-17 NMR as a direct probe of O activities, it is demonstrated that stacking faults enhance O redox participation compared with Li2MnO3 domains without stacking faults. This work is concluded by combining both ex situ and in situ O-17 NMR to investigate the evolution of O at 4i, 8j sites from monoclinic C2/m and 6c(1), 6c(2), 6c(3) sites from the stacking faults (P3(1)12). These measurements are further corroborated and explained by first-principles calculations finding a stabilization effect of stacking faults in delithiated Li2MnO3. In situ O-17 NMR tracks O activities with temporal resolution and provides a quantitative determination of reversible O redox versus irreversible processes that form short covalent O-O bonds. This work provides valuable insights into the O redox reactions in Li-excess layered cathodes, which may inspire new material design for cathodes with high specific capacity.
机译:晶格氧氧化还原产生异常容量,可以显着提高层状富锂过渡金属氧化物阴极的能量密度,引起了极大的兴趣。然而,这些阴极材料中O氧化还原背后的机制仍在争论中,部分原因是直接观察O和跟踪电化学循环相关变化的挑战。在这里,以O-17 NMR作为O活性的直接探针,证明了与没有堆叠故障的Li2MnO3结构域相比,堆叠断层增强了O氧化还原的参与。结合非原位和原位O-17核磁共振,研究了单斜晶系C2/m和6c(1)、6c(2)、6c(3)位点O在4i、8j位点的演化(P3(1)12)。第一性原理计算进一步证实了这些测量结果,并解释了叠层Li2MnO3中堆积断层的稳定效应。原位 O-17 NMR 以时间分辨率跟踪 O 活性,并定量测定可逆 O 氧化还原与形成短共价 O-O 键的不可逆过程。这项工作为锂过量层状阴极中的O氧化还原反应提供了有价值的见解,这可能为高比容量阴极的新材料设计提供灵感。

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