The behaviour of a synthetic57Fe-doped kaolin: Mössbauer and electron paramagnetic resonance studies
- 1 December 1980
- journal article
- Published by Mineralogical Society in Clay Minerals
- Vol. 15 (4) , 429-444
- https://doi.org/10.1180/claymin.1980.015.4.10
Abstract
The thermal behaviour of a ferrous doped kaolin has been studied by Mössbauer spectroscopy and electron paramagnetic resonance spectroscopy. From the observations it is concluded that the iron substitutes trioctahedrally as Fe2+in the ‘gibbsite-like’ sheet in place of dioctahedral aluminium. The g = 2 EPR signal is shown to be associated with these ferrous ‘cells’ which appear to occur in clusters. It is suggested that these ferrous cells are trapped within the normal dioctahedral aluminium structure. Dehydroxylation of the ferrous iron cells takes place between 623 and 673 K leading to the formation of an iron-rich pyroxene and, by 723 K, a ferric oxide. At temperatures > 723 K the pyroxene itself oxidizes to a second ferric oxide. The EPR signal changes at 623 K and disappears at 723 K. The signal is attributed to a trapped hole induced by X-irradiation, located near a silicon atom on the boundary between normal dioctahedral cells and trioctahedral Fe2+cells. It is possible to extend the model to explain some puzzling features concerning the g = 2 EPR signals reported by other authors and to propose other effects which might result from the presence of these cells.Keywords
This publication has 13 references indexed in Scilit:
- Further studies of a ferrous iron doped synthetic kaolin: dosimetry of X-ray induced defectsClay Minerals, 1981
- Synthetic Kaolinites Doped with Fe2+ and Fe3+ IonsClays and Clay Minerals, 1977
- Electron spin resonance in natural kaolinites containing Fe3+ and other transition metal ionsClay Minerals, 1975
- A Mössbauer study of thermal decomposition of biotitesMineralogical Magazine, 1975
- Electron spin resonance studies of doped synthetic kaolinite. IClay Minerals, 1974
- Electron spin resonance studies of doped synthetic kaolinite. IIClay Minerals, 1974
- A precision velocity generator suitable for M ssbauer experimentsJournal of Scientific Instruments, 1967
- Substitution by Iron in KaoliniteNature, 1967
- Mössbauer study of Fe2+ in some normal spinelsPhysics Letters, 1966
- Studies of the system iron oxide-silicawater at low oxygen partial pressuresEconomic Geology, 1957