Magnetic Anomaly in FeTi- System by Mössbauer Effect
- 15 August 1961
- journal article
- research article
- Published by American Physical Society (APS) in Physical Review B
- Vol. 123 (4), 1239-1240
- https://doi.org/10.1103/physrev.123.1239
Abstract
The solid solutions exhibit strong ferrimagnetic moments for the compositions , where the Fe and Ti ions are ordered in the alternate (111) layers. The anomaly revealed by the Mössbauer measurements is that the ferrimagnetic phase consists of ferrimagnetic clusters surrounded by paramagnetic media. The size of these clusters decreases with increasing temperature or increasing local concentration of Ti. The isomer shift of FeTi is 1.2 mm/sec at room temperature as expected for , although the quadrupole splitting of 0.62 mm/sec is smaller than that observed in other ferrous environments.
Keywords
This publication has 11 references indexed in Scilit:
- Interpretation of theIsomer ShiftPhysical Review Letters, 1961
- Acoustically ModulatedRays FromPhysical Review Letters, 1960
- Evidence for Quadrupole Interaction of, and Influence of Chemical Binding on Nuclear Gamma-Ray EnergyPhysical Review Letters, 1960
- Neutron-diffraction study of antiferromagnetic FeTi03 and its solid solutions with α-Fe2O3Journal of Physics and Chemistry of Solids, 1959
- Kernresonanzfluoreszenz von Gammastrahlung in Ir191The European Physical Journal A, 1958
- Magnetization of Ilmenite-Hematite System at Low TemperaturesPhysical Review B, 1957
- Effect of Heat Treatments on the Magnetic Properties of the FeTiO3–Fe2O3 Solid Solution SeriesJournal of the Physics Society Japan, 1957
- Molecular Field Fluctuation Effects in Mixed Nickel-Zinc FerritesPhysical Review B, 1957
- Magnetic properties of ferromagnetic ilmenitesPure and Applied Geophysics, 1956
- Neutron Diffraction by Paramagnetic and Antiferromagnetic SubstancesPhysical Review B, 1951