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Paramagnetic Fe3+: a sensitive probe for disorder in kaolinite


Clays and Clay Minerals 45(4): 496-505
Paramagnetic Fe3+: a sensitive probe for disorder in kaolinite
The Fe3+ substituted for Al3+ at the 2 octahedral positions was one of the most common impurities in the kaolinite structure detected by electron paramagnetic resonance (EPR). Evidence was provided for a relationship between the shape of EPR spectra for structural Fe and the structural disorder in kaolinite.

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Accession: 002914981



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