2015
DOI: 10.1016/j.ceramint.2015.06.073
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A comparative study of two methods to produce geopolymer composites from volcanic scoria and the role of structural water contained in the volcanic scoria on its reactivity

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Cited by 61 publications
(15 citation statements)
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References 21 publications
(33 reference statements)
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“…3(a)] and corresponding to the out-of-plane bending vibrations of the CO 3 2À group can be related to the reaction between excess of NaOH and atmospheric CO 2 . A similar reaction was observed by Tchakoute et al 32 during geopolymer synthesis from alkali fusion of VA. For alkaliactivated oyster shell-VA, this band (864 cm À1 ) might be due to the carbonation of free sodium ion and the presence of remaining oyster shell that has not reacted. This is supported by the presence of a band at 714 cm À1 [ Fig.…”
Section: ) Characterization Techniquessupporting
confidence: 81%
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“…3(a)] and corresponding to the out-of-plane bending vibrations of the CO 3 2À group can be related to the reaction between excess of NaOH and atmospheric CO 2 . A similar reaction was observed by Tchakoute et al 32 during geopolymer synthesis from alkali fusion of VA. For alkaliactivated oyster shell-VA, this band (864 cm À1 ) might be due to the carbonation of free sodium ion and the presence of remaining oyster shell that has not reacted. This is supported by the presence of a band at 714 cm À1 [ Fig.…”
Section: ) Characterization Techniquessupporting
confidence: 81%
“…The bands observed at 1625–1644 and 3350–3480 cm −1 are characteristic of bending and stretching vibrations, respectively, of O–H bond of water molecules contained in alkali‐activated VA. The bands at 650–666 cm −1 and 750 cm −1 are attributed to the Si–O–Al IV stretching of tetrahedral network from aluminosilicate gel . The main difference on these figures are the bands at 714, 864, and 1400–1494 cm −1 corresponding to the presence of carbonate ions (CO 3 2− ).…”
Section: Resultsmentioning
confidence: 96%
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“…Both spectra exhibited the bond characteristic of the asymmetric stretching vibrations of Si-O-T (T = Si or Al) with peaks at around 1030 and 1161 cm −1 for VA and MSWI-FA, respectively [26,27]. The peaks center at 579 (VA) and 675 cm −1 (MSWI-FA) and correspond to Si-O bending vibration of quartz [28] and the peak at 472 cm −1 for VA represents the vibration of Si-O-Fe bond [29]. The characteristic bonds of silanol group and water molecules are situated at 3421 and 1643 cm −1 for VA and at 3436 cm −1 and 1621 cm −1 for MSWI-FA, respectively.…”
Section: Methodsmentioning
confidence: 99%
“…Many previous works have reported the formation of geopolymer materials from calcined clays [9] [10], granulated blast furnace slag and fly ash as industrial by-products or wastes [11] [12], volcanic ashes [13] [14] [15], ground perlite [16], ground aplite rock [17], granite waste [18], Taftan and esite and Shahindej [19], alkali-feldspars [20] [21], a pumice-type natural pozzolan [22], basaltic ash [23].…”
Section: Introductionmentioning
confidence: 99%