1989
DOI: 10.1016/0040-6031(89)87244-2
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Comparison of attapulgites from different sources using TG/DTG and FTIR

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Cited by 39 publications
(15 citation statements)
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“…The peak at 1662 cm −1 was associated with the hydroxyl deformation mode of zeolitic water, and the peak at 982 cm −1 was the bending vibration of SiOSi group. The peaks agreed well with the values reported by Xu et al and Khorami and Lemieux .…”
Section: Resultssupporting
confidence: 91%
“…The peak at 1662 cm −1 was associated with the hydroxyl deformation mode of zeolitic water, and the peak at 982 cm −1 was the bending vibration of SiOSi group. The peaks agreed well with the values reported by Xu et al and Khorami and Lemieux .…”
Section: Resultssupporting
confidence: 91%
“…4, the weight loss around 100°C is very obvious, which is due to the release of physically adsorbed water [26]. In the temperature range of 100-280°C, the weight loss is mainly attributed to the removal of the superficially adsorbed water, less severely bonded zeolitic H 2 O and a little part of the first coordinated water [27]. In the temperature range of 280-590°C, the residual first coordinated water and all the second coordinated water should be released from the crystal framework [28].…”
Section: Tg Analysismentioning
confidence: 99%
“…At the edges exposed OH groups are neutralized by protons forming more resistant H 2 O molecules coordinated to the octahedral elements. The discernment of IR absorption bands due to these different kinds of water molecules and to the presence of OH groups coordinated to the metallic cations have been reported [1][2][3][4][5][6][7]. Frost et al [6] carried out this investigation not only in the mid-infrared region but also in the near-infrared region.…”
Section: Modification Of Palygorskite By Hcl and Organic Compoundsmentioning
confidence: 99%