57Fe Hyperfine Fields in Magnetite (Fe3O4)
- 1 March 1969
- journal article
- research article
- Published by AIP Publishing in Journal of Applied Physics
- Vol. 40 (3), 1411-1413
- https://doi.org/10.1063/1.1657696
Abstract
The 57Fe Mössbauer spectrum in an applied 37 kOe field is interpreted in terms of three superimposed six‐line patterns corresponding to at least three distinct species of Fe ions. While the observed hyperfine fields and isomer shifts of Fe3+ at A and B are consistent with the trends in ferrite spinels, the apparent Fe2+ values are rather unusual.Keywords
This publication has 6 references indexed in Scilit:
- Mössbauer Study of the Electronic and Magnetic Properties of Fe2+ Ions in Some Spinel-Type CompoundsJournal of Applied Physics, 1968
- Mössbauer-Effect Measurements in FeTi Spinels with Local DisorderJournal of Applied Physics, 1967
- A Mössbauer Study of the Internal Field at Fe57 in α-Fe2O3Journal of the Physics Society Japan, 1962
- Study of the Low-Temperature Transition in Magnetite and the Internal Fields Acting on Iron Nuclei in Some Spinel Ferrites, Using Mössbauer AbsorptionPhysical Review B, 1961
- Neutron Diffraction Investigation of the 119°K Transition in MagnetitePhysical Review B, 1958
- Electronic conductivity and transition point of magnetite (“Fe3O4”)Physica, 1941