Abstract:
The valency state and local coordination of Fe ions of four industrial samples and a sample of cathodic materials for recharcheable lithium ion batteries obtained using an original technology of St. Petersburg State Technological Institute (Technological University) were studied using the Mössbauer effect on the $^{57}$Fe isotope. It was found that the main valency state for more than 90% of iron ions was Fe$^{2+}$. The values of isomer shift $\delta$ = 0.96–0.98 mm/s and quadrupole splitting $\sigma$ = 2.88–2.93 mm/s for Fe$^{2+}$ ions coincide with the values for compounds with the structure of olivine LiFePO$_4$ and occupy positions in highly distorted FeO$_6$ octahedrons. Fe$^{3+}$ ions are in octahedral and/or tetrahedral local positions.