Fe excess in hydrothermally synthesized LiFePO 4

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Abstract

Olivine lithium iron phosphate (LiFePO 4 ) is synthesized by a typical hydrothermal route. Although X-ray diffraction (XRD) shows no detectable impurities, inductively coupled plasma-atomic emission spectroscopy (ICP-AES) demonstrates extra iron (Fe) in the sample which is further indicated as crystallographic defects occupying lithium sites and a small amount of surface amorphous Fe 3 impurities by Rietveld refinement of high resolution synchrotron XRD and Raman spectroscopy, respectively. The latter possibility is also verified by high resolution transmission electron microscopy (HRTEM) and galvanostatic discharge/charge measurements between 2.0 and 3.2 V (vs. Li/Li). In addition, the influence of Fe excess on the electrochemical performance of LiFePO 4 as a cathode material for lithium ion batteries (LIBs) is discussed.

Original languageEnglish
Pages (from-to)139-142
Number of pages4
JournalMaterials Letters
Volume84
DOIs
StatePublished - 1 Oct 2012

Keywords

  • Defects
  • Energy storage and conversion
  • Fe excess
  • Hydrothermal
  • Lithium iron phosphate
  • Surfaces

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