LAUSR

Abstract The co-precipitation method was used to prepare silver ferrite AgFeO 2 . The resulting powders were brick brown flakes. X-ray diffraction and Mossbauer spectroscopy were used as complementary methods to study structure and hyperfine interactions of silver ferrite. It was found that AgFeO 2 has delafossite structure with two polytypes, i.e., rhombohedral 3 R and hexagonal 2 H , wherein the 2 H polytype is dominant. The average crystallite sizes, estimated using Scherrer formula, were in the range of 15–35 nm. The Mossbauer spectrum registered at room temperature is one paramagnetic doublet with isomer shift characteristic for high-spin Fe 3+ ions in an octahedral oxygen environment. In the temperature range of 3.7 K ≤ T ≤ 16 K Mossbauer spectroscopy revealed a distribution of the hyperfine magnetic fields at 57 Fe nuclei connected with complicated collinear and non-collinear magnetic structure of AgFeO 2 . It was found that the value of the average hyperfine magnetic field monotonically decreases with an increase of temperature.