2022
DOI: 10.1016/j.clay.2022.106410
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Alkali-activated geopolymerization of a low illitic raw clay and waste brick mixture. An alternative to traditional ceramics

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Cited by 26 publications
(28 citation statements)
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“…The distinctive bands at 424/427 and 530/538 cm −1 (CGW/GW) again present the part of the footprint of feldspars [40,42]. Nonetheless, the second band at 530/538 cm −1 may also correspond to trace amounts of hematite [31]. Besides, in the sample GW, the band is detected at 590 cm −1 , showing O-Si(Al)-O bending vibrations in feldspars.…”
Section: Characterization Of Initial Materialsmentioning
confidence: 81%
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“…The distinctive bands at 424/427 and 530/538 cm −1 (CGW/GW) again present the part of the footprint of feldspars [40,42]. Nonetheless, the second band at 530/538 cm −1 may also correspond to trace amounts of hematite [31]. Besides, in the sample GW, the band is detected at 590 cm −1 , showing O-Si(Al)-O bending vibrations in feldspars.…”
Section: Characterization Of Initial Materialsmentioning
confidence: 81%
“…Additionally, the mild and wide band at 1630 cm −1 indicates the bending vibration of the physically adsorbed water molecules to illite-mica. A weak band of illite-mica was observed at around 848 cm −1 [31]. All the previously mentioned peaks are missing in the GW samples.…”
Section: Characterization Of Initial Materialsmentioning
confidence: 88%
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