2017
DOI: 10.1016/j.ceramint.2016.11.070
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Structural study of geopolymers obtained from alkali-activated natural pozzolan feldspars

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Cited by 46 publications
(11 citation statements)
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“…The band located at ~429 cm −1 is due to deformation of O–Si–O bond. K–O stretching is observed at around ~467 cm −1 , which is also coupled with Si–O–Si bending vibration . Saikia et al., also, declare that Fe bearing bonds such as Fe–O are located approximately at around ~532 cm −1 .…”
Section: Resultsmentioning
confidence: 94%
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“…The band located at ~429 cm −1 is due to deformation of O–Si–O bond. K–O stretching is observed at around ~467 cm −1 , which is also coupled with Si–O–Si bending vibration . Saikia et al., also, declare that Fe bearing bonds such as Fe–O are located approximately at around ~532 cm −1 .…”
Section: Resultsmentioning
confidence: 94%
“…Absorption at ~776 cm −1 is correlated with Si–O–Si stretching vibration of quartz . Absorptions located in the range of 1000‐1150 cm −1 are ascribed to Si–O stretching vibrations and the maximum absorption, which is seen at around ~1036 cm −1 is due to the stretching vibration of Si–O bonds . At FTIR spectra of minerals, O–H bonds usually fall in the range of 1600‐3700 cm −1 .…”
Section: Resultsmentioning
confidence: 98%
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“…The changes that have been characterized correspond to the second and third stages of the geopolymerization process [15]. Geopolimerization mechanism involves dissolving and hydrolysing aluminum and silicon in alkaline solution, transport and orientation of dissolved species accompanied by polycondensation and the creation of three-dimensional aluminosilicate networks [16].The changes in XRDP and FTIR spectrum indicate that there are fine changes of the aluminosilicates structure as the geopolymer synthesis progresses.…”
Section: Resultsmentioning
confidence: 99%
“…Besides metakaolin and fly ash, other types of precursors that have low amounts of calcium have reaction mechanisms typical of geopolymers. For example, other types of burnt clay can be cited as illite-smectites [43] or feldspars [44], [45]. There are also other precursors such as volcanic ash, natural pozzolans, and metallurgical slags with low amounts of calcium [46]- [49].…”
Section: Main Low-calcium Precursorsmentioning
confidence: 99%