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The effect of synthesis temperature on the FT-Raman and FT-IR spectra of saponites
Saponites hydrothermally synthesised between 125°C and 280°C were studied by Fourier transform (FT)-Raman and FT-infrared (IR) spectroscopy and compared to natural saponite. FT-IR spectra with increasing synthesis temperature showed saponite crystallisation and disappearance of amorphous material. T...
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Published in: | Vibrational spectroscopy 2000-04, Vol.23 (1), p.119-127 |
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Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Saponites hydrothermally synthesised between 125°C and 280°C were studied by Fourier transform (FT)-Raman and FT-infrared (IR) spectroscopy and compared to natural saponite. FT-IR spectra with increasing synthesis temperature showed saponite crystallisation and disappearance of amorphous material. The 457 cm
−1 gel band developed at higher temperatures in two components at 447 cm
−1 and 465 cm
−1 ascribed to e
1
2 of SiO
2 and AlOH translation modes of saponite. Above 150°C, minor octahedral sheet vibrations appeared at ±530 cm
−1 (MgOH perpendicular mode) followed by a band around 750 cm
−1 (AlOH deformation mode) above 200°C. At this temperature, two bands due to the a
1
2 SiO
2 and apical AlO bond of AlO
4 in the tetrahedral sheet became visible at 691 and 837 cm
−1, respectively. The strongest SiO
2 band showed a continuous shift from 1043 to 1013 cm
−1 with increasing synthesis temperature. Two overlapping bands around 660 and 690 cm
−1 appeared almost simultaneously before the wide amorphous material band around 1240 cm
−1 had disappeared, indicating that in the saponite structure, the octahedral and tetrahedral layers form almost simultaneously. Sharpening of other bands associated with various SiO modes was not observed up to 200°C. The FT-Raman spectra only revealed the formation of internal tetrahedral vibrational modes. Upon increasing temperature, the first band observed was at 683 cm
−1 at 150°C followed by the 360 cm
−1 band at 175°C. Around 240–280°C, two bands around 430–465 cm
−1 were observed. The increase in intensity of these bands with temperature confirmed the concept that the silica in the gel rapidly changes its configuration. |
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ISSN: | 0924-2031 1873-3697 |
DOI: | 10.1016/S0924-2031(00)00056-4 |