2020
DOI: 10.1016/j.clay.2019.105375
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Geopolymerization of halloysite via alkali-activation: Dependence of microstructures on precalcination

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Cited by 92 publications
(37 citation statements)
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“…3-6 have a structure characteristic of the geopolymers after the curing process (min. 28 days) [26][27][28]. In Fig.…”
Section: Resultsmentioning
confidence: 92%
See 1 more Smart Citation
“…3-6 have a structure characteristic of the geopolymers after the curing process (min. 28 days) [26][27][28]. In Fig.…”
Section: Resultsmentioning
confidence: 92%
“…8. The charts are typical for geopolymers [27][28][29] The main element is silica due to the composition of raw materials -sand and fly ash. EDS analysis also shows a high content of oxygen, which is composed of oxides of various elements.…”
Section: Resultsmentioning
confidence: 99%
“…Kaze et al [24] showed that calcined halloysite at 600 °C is suitable for geopolymers with good mechanical properties and long-term durability. Zhang et al [25] in their investigation claimed that 700 °C appeared as optimal calcination temperature of halloysite-clay that insured high strength. Recently, Tchakounté et al [26] produced geopolymer binder from calcined halloysite and kaolinite clays at 700 °C, consolidated with sodium alkaline solution.…”
Section: Introductionmentioning
confidence: 99%
“…A broad band at range of 900-1,000 cm −1 (986 cm −1 ) was attributed to the Si-O-Si stretching vibration mode 53 . Besides, due to the formation of geopolymer structure, the Si-O-Si stretching vibration mode has shifted to the lower wavenumbers 53 . A broad band Fig.…”
Section: Resultsmentioning
confidence: 99%
“…According to this spectrum, the band amplification and high transmittance percentage of OH groups have been increased; also, an observed strong absorbance band around 1,430 cm −1 51 , 52 was confirmed the existence of C–O–C asymmetric vibration mode of CO 3 2– ion which has been determined in all spectra of geopolymer samples. A broad band at range of 900–1,000 cm −1 (986 cm −1 ) was attributed to the Si–O–Si stretching vibration mode 53 . Besides, due to the formation of geopolymer structure, the Si–O–Si stretching vibration mode has shifted to the lower wavenumbers 53 .…”
Section: Resultsmentioning
confidence: 99%