Abstract
The dehydroxylation of kaolinite has been investigated by Fourier-transform in situ infrared emission spectroscopy from 100 to 800 °C at 5 degree intervals. The major advantage lies in the ability to obtain vibrational spectroscopic information in situ at the elevated temperature. Dehydroxylation was determined by the loss of intensity of the hydroxyl bands in the 3550–3750 cm-1 emission spectra. No clay phase changes occur until after dehydroxylation takes place. The kaolinite layers lose their outer and inner hydroxyl groups simultaneously. It is proposed that the kaolinite dehydroxylation process takes place homogeneously and involves two mechanisms.
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© 1997 Springer-Verlag Wien
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Frost, R.L., Vassallo, A.M. (1997). Fourier-transform Infrared Emission Spectroscopy of Kaolinite Dehydroxylation. In: Mink, J., Keresztury, G., Kellner, R. (eds) Progress in Fourier Transform Spectroscopy. Mikrochimica Acta Supplement, vol 14. Springer, Vienna. https://doi.org/10.1007/978-3-7091-6840-0_209
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DOI: https://doi.org/10.1007/978-3-7091-6840-0_209
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