...
首页> 外文期刊>Chemistry of Materials: A Publication of the American Chemistry Society >First-Principles Simulation of the (Li-Ni-Vacancy)O Phase Diagram and Its Relevance for the Surface Phases in Ni-Rich Li-Ion Cathode Materials
【24h】

First-Principles Simulation of the (Li-Ni-Vacancy)O Phase Diagram and Its Relevance for the Surface Phases in Ni-Rich Li-Ion Cathode Materials

机译:(Li-Ni-空位)O相图的第一原理模拟及其对富锂离子阴极材料表面相的相关性

获取原文
获取原文并翻译 | 示例

摘要

Despite several reports on the surface phase transformations from a layered to a disordered spinel and a rock-salt structure at the surface of the Ni-rich cathodes, the precise structures and compositions of these surface phases are unknown. The phenomenon, in itself, is complex and involves the participation of several contributing factors. Of these factors, transition metal (TM) ion migration toward the interior of the particle and hence formation of TM-densified surface layers, triggered by oxygen loss, is thermodynamically probable. Here, we simulate the thermodynamic phase equilibria as a function of TM ion content in the cathode material in the context of lithium nickel oxides, using a combined approach of first-principles density functional calculations, the cluster expansion method, and grand canonical Monte Carlo simulations. We developed a unified lattice Hamiltonian that accommodates not only rock-salt like structures but also topologically different spinel-like structures. Also, our model provides a foundation to investigate metastable cation compositions and kinetics of the phase transformations. Our investigations predict the existence of several Ni-rich phases that were, to date, unknown in the scientific literature. Our simulated phase diagrams at finite temperature show a very low solubility range of the prototype spinel phase. We find a partially disordered spinel-like phase with far greater solubility that is expected to show very different Li diffusivity compared to that of the prototype spinel structure.
机译:尽管从分层到无序尖晶石的表面相变有几个报告,但富含Ni的阴极表面的岩盐结构,但这些表面相的精确结构和组成是未知的。本身就是复杂的现象,涉及几种贡献因素的参与。在这些因素中,过渡金属(TM)离​​子迁移到颗粒的内部并因此形成由氧气损失引发的TM致密的表面层,是热力学上可能的。在这里,我们在锂镍氧化物的背景下模拟了热力相平的阴极材料中Tm离子含量的函数,使用一致性密度函数计算,集群扩展方法和大规范蒙特卡罗模拟的组合方法。我们开发了一个统一的格子哈密顿,不仅可以容纳岩盐,如结构,而且是拓扑上不同的尖晶石状结构。此外,我们的模型提供了研究亚稳阳离子组合物和相变的动力学的基础。我们的调查预测了在科学文献中迄今为止未知的几个富国阶段的存在。我们有限温度的模拟相图显示了原型尖晶石相的非常低的溶解度范围。我们发现与原型尖晶石结构相比,预期的溶解度远远较大的溶解度。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号