4.8 Article

Structure Stabilization by Mixed Anions in Oxyfluoride Cathodes for High-Energy Lithium Batteries

Journal

ACS NANO
Volume 9, Issue 10, Pages 10076-10084

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/acsnano.5b03643

Keywords

lithium batteries mixed-anion cathodes; iron oxyfluoride; scanning transmission electron microscopy (STEM); electron energy loss spectroscopy (EELS)

Funding

  1. NorthEast Center for Chemical Energy Storage, an Energy Frontier Research Center - U.S. Department of Energy, Office of Science [DE-SC0001294, DE-SC0012583]
  2. U.S. Department of Energy, Office of Basic Energy Sciences [DE-SC0012704]
  3. Laboratory Directly Research and Development at Brookhaven
  4. U.S. Department of Energy (DOE) Office of Energy Efficiency and Renewable Energy under the Advanced Battery Materials Research (BMR) program [DE-SC0012704]
  5. National Research Foundation (NRF) - Korea Government (MSIP) [2012M2A8A5025697]
  6. National Research Foundation of Korea [2012M2A8A5025697] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)

Ask authors/readers for more resources

Mixed-anion oxyfluorides (i.e., FeOxF2-x) are an appealing alternative to pure fluorides as high-capacity cathodes in lithium batteries, with enhanced cyclability via oxygen substitution. However, it is still unclear how the mixed anions impact the local phase transformation and structural stability of oxyfluorides during cycling due to the complexity of electrochemical reactions, involving both lithium intercalation and conversion. Herein, we investigated the local chemical and structural ordering in FeO0.7F1.3 at length scales spanning from single particles to the bulk electrode, via a combination of electron spectrum-imaging, magnetization, electrochemistry, and synchrotron X-ray measurements. The FeO0.7F1.3 nanoparticles retain a FeF2-like rutile structure but chemically heterogeneous, with an F-rich core covered by thin O-rich shell. Upon lithiation the O-rich rutile phase is transformed into Li-Fe-O(-F) rocksalt that has high lattice coherency with converted metallic Fe, a feature that may facilitate the local electronic and ionic transport. The O-rich rocksalt is highly stable over lithiation/delithiation and thus advantageous to maintain the integrity of the particle, and due to its predominant distribution on the surface, it is expected to prevent the catalytic interaction of Fe with electrolyte. Our findings of the structural origin of cycling stability in oxyfluorides may provide insights into developing viable high-energy electrodes for lithium batteries.

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