Clay Minerals · 1974 · 118 citations · 15 references
Natural SciencesMaterials EngineeringMaterials ScienceInorganic ChemistryMaterials ChemistrySpectroscopyDefects In CeramicsMineral ChemistrySilicate MineralsLattice Vacancies
Abstract Synthetic kaolinites of varying crystallinity, and in some instances with ideal morphology, have been produced by hydrothermal reaction of aluminiosilicate gels. Synthetic kaolinites doped with Mg 2+ and Fe 3+ were also obtained. Synthetic kaolinite doped with Fe 3+ produced an ESR spectrum at g = 4 identical to spectra observed in natural kaolinites. Following X-irradiation and annealing at ~200°C, synthetic kaolinite doped with Mg 2+ exhibited an ESR signal at g = 2·0 identical to a resonance observed in natural kaolinites. It is concluded that the g = 2·0 signal in kaolinite is due to a defect centre stabilized by Mg 2+ substitution. All synthetic and natural kaolinites exhibit an additional resonance at g = 2·0 following X-irradiation which can be repeatedly created and destroyed by irradiation and annealing. This resonance is attributed to defects possibly associated either with the substitution of Al 3+ for Si 4+ in kaolinite or with lattice vacancies.
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Note on the Paramagnetic Resonance of Iron in Glass
T. G. Castner, G.S. Newell, W. C. Holton et al. · The Journal of Chemical Physics · 1960 · 564 citations