4.6 Article

Mechanism of Charge Transfer in Olivine-Type LiFeSiO4 and LiFe0.5M0.5SiO4 (M = Mg or Al) Cathode Materials: First-Principles Analysis

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JOURNAL OF PHYSICAL CHEMISTRY C
卷 119, 期 17, 页码 9125-9133

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AMER CHEMICAL SOC
DOI: 10.1021/acs.jpcc.5b01692

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  1. US-India Partnership to Advance Clean Energy-Research (PACE-R) for the Solar Energy Research Institute for India
  2. United States (SERIIUS) - U.S. Department of Energy (Office of Science, Office of Basic Energy Sciences, and Energy Efficiency and Renewable Energy, Solar Energy Technology Program [DE-AC36-08GO28308]
  3. Government of India, through the Department of Science and Technology under Subcontract IUSSTF/JCERDC-SERIIUS/2012

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Olivine silicates LiMSiO4 (where M = Mn, Fe, Co, and Ni) are promising candidates for the next generation of cathode materials for use in lithium ion batteries (LIB). Among these compounds, LiFeSiO4 is an attractive choice due to its low cost, environmental friendliness, high safety, and stability. In this work, we use first-principles density functional theory-based calculations to determine the structural and electrochemical properties of olivine-type LiFeSiO4 and LiFe0.5M0.5SiO4 (where M = Mg or Al). Because of the influence of stronger Si-O bonds in weakening Fe-O bonds via an inductive effect, we find that these compounds have a high lithium intercalation voltage (i.e., similar to 5 V) and undergo negligible changes in volume during lithiation and delithiation. Using the Bader scheme for topological partitioning of charge density and projected density of states (PDOS) in the electronic strucutre, we highlight the significant role of O-2p states and the relatively inert role of Fe-3d states in the charge transfer associated with delithiation. We show that 50% substitution of Fe with Al or Mg results in enhancement in the theoretical capacity of LiFeSiO4 from 173 mAhg(-1) to 191 mAhg(-1) (similar to 10%) and 193 mAhg1 (similar to 12%), respectively, while maintaining its intercalation voltage and structural stability during lithiation and delithiation.

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