2015
DOI: 10.1016/j.jascer.2014.12.003
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Effect of the rate of calcination of kaolin on the properties of metakaolin-based geopolymers

Abstract: Please cite this article in press as: B.B. Diffo Kenne, et al., Effect of the rate of calcination of kaolin on the properties of metakaolin-based geopolymers, J. Asian Ceram. Soc. (2014), http://dx. a b s t r a c tKaolin samples of the same mass were treated at 700 • C for the same duration of 30 min by varying the rate of calcination (1, 2.5, 5, 10, 15 and 20 • C/min) in order to obtain metakaolins which were used to produce geopolymers. Depending on the nature of each type of material, kaolin, metakaolins an… Show more

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Cited by 129 publications
(42 citation statements)
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“…An increase in intensity of stretching and bending vibrations of CKT assigned to O H at 3452 and 1622 cm −1 , respectively, was observed in the spectrum of G MK 0 and can be explained by increase of the nonbridging oxygens (Si O − Na + , Al O − Na + ) resulted from reaction of aluminosilicates with alkali [40]. The main band between 800 and 1250 cm −1 is attributed to the asymmetric and symmetrical stretching vibration [10] of the Si O T group (T: tetrahedral Si Or Al) in the geopolymer gel [43]. The band around 1650 cm −1 corresponds to the vibration of the H OH group.…”
Section: Ftir Characterizationmentioning
confidence: 99%
See 1 more Smart Citation
“…An increase in intensity of stretching and bending vibrations of CKT assigned to O H at 3452 and 1622 cm −1 , respectively, was observed in the spectrum of G MK 0 and can be explained by increase of the nonbridging oxygens (Si O − Na + , Al O − Na + ) resulted from reaction of aluminosilicates with alkali [40]. The main band between 800 and 1250 cm −1 is attributed to the asymmetric and symmetrical stretching vibration [10] of the Si O T group (T: tetrahedral Si Or Al) in the geopolymer gel [43]. The band around 1650 cm −1 corresponds to the vibration of the H OH group.…”
Section: Ftir Characterizationmentioning
confidence: 99%
“…The band around 1650 cm −1 corresponds to the vibration of the H OH group. The band between 2700 and 3750 cm −1 also corresponds to Si OH, Al OH [40] and the vibration of the OH group present in the water molecule [10]. Bands between 750 and 550 cm −1 correspond to unreacted metakaolin molecules.…”
Section: Ftir Characterizationmentioning
confidence: 99%
“…During the calcination of kaolin, kaolinite transforms into amorphous metakaolinite 23 . In the diffraction patterns of both sample series (A and B), no signifi cant refl ections originating from kaolinite phase were observed (Fig.…”
Section: Xrd Studiesmentioning
confidence: 99%
“…Geopolymer source materials commonly researched on are calcined clay or metakaolin, blast furnace slag, fly-ash and rice husk ash. Metakaolin, calcined form of kaolin clay is a consistent material used in geopolymer research [6][7][8][9][10][11].…”
Section: Introductionmentioning
confidence: 99%