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 language | English |
|---|---|
| Pages (from-to) | 139-142 |
| Number of pages | 4 |
| Journal | Materials Letters |
| Volume | 84 |
| DOIs | |
| State | Published - 1 Oct 2012 |
Keywords
- Defects
- Energy storage and conversion
- Fe excess
- Hydrothermal
- Lithium iron phosphate
- Surfaces