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首页> 外文期刊>Chemistry of Materials: A Publication of the American Chemistry Society >Direct Evidence of Charge Transfer upon Anion Intercalation in Graphite Cathodes through New Electronic States: An Experimental and Theoretical Study of Hexafluorophosphate
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Direct Evidence of Charge Transfer upon Anion Intercalation in Graphite Cathodes through New Electronic States: An Experimental and Theoretical Study of Hexafluorophosphate

机译:通过新电子国家在石墨阴极中的阴离子嵌入时电荷转移的直接证据:六氟磷酸盐的实验与理论研究

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Graphite intercalation compounds continue to be central to technologies for electrochemical energy storage from anodes in established Li-ion batteries to cathodes in beyond Li-ion concepts paired with multivalent anodes. When used as a cathode, graphite intercalates a variety of anions with PF6- being among the most common. Paired with Li intercalation at the anode, the corresponding dual carbon battery yields high energy and power densities. Given the available choice of anions as intercalants, it is important to elucidate how the graphite structure accommodates them in order to tailor the molecular species to maximize charge and reversibility. However, the changes in electronic structure of the host graphite lattice upon anion intercalation are poorly understood compared to cations, which represent a fundamentally different reaction. In this work, PF6-intercalated graphite has been studied using techniques sensitive to electronic structure, namely, X-ray Raman spectroscopy (XRS), X-ray absorption near-edge spectroscopy (XANES), and X-ray emission spectroscopy (XES). Complementary full-potential, all-electron density functional theory calculations yielded excellent agreement with the spectra, thus providing insight into charge compensation in the graphite lattice. In particular, a pre-pi* feature emerged in XRS/XANES, which is direct evidence of the removal of charge from the host lattice to compensate the intercalated anions, leading to an overall lowering of the Fermi energy level. This is expected to be characteristic of many intercalants in anion-intercalated graphite. The unambiguous identification of the origin of the pre-pi* spectral feature, which is frequently seen in graphitic systems, is of broad interest to the spectroscopy of graphitic systems beyond the practical implications of anion-induced changes in the electronic properties for real devices.
机译:石墨嵌入化合物继续是从建立的锂离子电池中的阳极到与多价阳极配对的锂离子概念的阴极中的电化学能量存储技术的核心。当用作阴极时,石墨将各种阴离子插入,PF6是最常见的。与阳极的LI插入配对,相应的双碳电池产生高能量和功率密度。鉴于阴离子的可用选择作为插入物,重要的是要阐明石墨结构如何容纳它们,以便定制分子种类以最大限度地提高电荷和可逆性。然而,与阴离子插入对阴离子插入时的电子结构的变化与阳离子相比,理解差不多,这代表着基本不同的反应。在这项工作中,使用对电子结构敏感的技术研究了PF6嵌入的石墨,即X射线拉曼光谱(XRS),X射线吸收近边光谱(XANES)和X射线发射光谱(XES) 。互补的全潜能,全电子密度泛函理论计算与光谱产生非常良好的一致性,从而在石墨晶格中提供了对电荷补偿的洞察力。特别地,在XRS / XANE中出现的PIE *特征,其是从宿主格子去除电荷以补偿插入阴离子的直接证据,导致费米能量水平的总体降低。这预计将成为阴离子插入石墨中许多插入物的特征。在石墨系统中经常看到的PI PI *光谱特征的起源的明确识别对于超出实际设备的电子特性的阴离子诱导的变化的实际意义,它是广泛的兴趣。

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