R. Frost et al., Deintercalation of dimethylsulphoxide intercalated kaolinites - a DTA/TGA and Raman spectroscopic study, THERMOC ACT, 327(1-2), 1999, pp. 155-166
The deintercalation of dimethylsulphoxide intercalated kaolinites was studi
ed using a combination of thermal analysis techniques and Raman spectroscop
y. Thermal analysis shows three endotherms at 77 degrees, 117 degrees and 1
73 degrees C attributed to the loss of water and the loss of DMSO in two st
ages, The use of a thermal stage enabled Raman spectra of the deintercalati
on process to be obtained in situ at elevated temperatures. The Raman spect
ra of the DMSO intercalated kaolinites show two bands at 3620 and 3660 cm(-
1) for the DMSO intercalated low defect kaolinite and 3620 and 3664 cm(-1)
for the high defect intercalated kaolinite. The 3620 cm(-1) band is attribu
ted to the inner hydroxyl of the kaolinite and shows no change upon deinter
calation. The 3660 and 3664 cm(-1) bands are attributed to the inner surfac
e hydroxyls of the kaolinite hydrogen bonded to the DMSO. The intensity of
these bands decreases upon thermal treatment and at the same time, the band
s at 3695 and 3684 cm(-1) increase in intensity. These changes clearly show
s that the 3660 cm(-1) band is attributable to the inner surface hydroxyls
hydrogen bonded to the DMSO. Deintercalation may also be followed by the de
crease in intensity of the CH-stretching bands, The application of the DTA/
TGA patterns to determine the appropriate temperatures for Raman spectrosco
py of the dimethylsulphoxide proved most useful. (C) 1999 Elsevier Science
B.V. All rights reserved.