2016
DOI: 10.1016/j.fuel.2016.07.116
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A comparative study on fly ash, geopolymer and faujasite block for Pb removal from aqueous solution

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Cited by 165 publications
(79 citation statements)
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“…For the CGCS, the typical band near 1616 and 3444 cm −1 is assigned to the vibration of the hydroxyl groups of absorbed water [28]. In the spectrum of the SiO 2 /Al 2 O 3 molar ratios of 5.20 and 3.40, the bands around 1644 and 3448 cm −1 are caused by the solid phase hydrate in the hydroxyl group or the zeolite channel [22,29]. In the raw material CGCS and NaP zeolite, the bands around 1040 and 994 cm −1 are different.…”
Section: Sem Results Analysismentioning
confidence: 99%
See 1 more Smart Citation
“…For the CGCS, the typical band near 1616 and 3444 cm −1 is assigned to the vibration of the hydroxyl groups of absorbed water [28]. In the spectrum of the SiO 2 /Al 2 O 3 molar ratios of 5.20 and 3.40, the bands around 1644 and 3448 cm −1 are caused by the solid phase hydrate in the hydroxyl group or the zeolite channel [22,29]. In the raw material CGCS and NaP zeolite, the bands around 1040 and 994 cm −1 are different.…”
Section: Sem Results Analysismentioning
confidence: 99%
“…The silicon-aluminum ratio leads to the continuous generation of crystal nuclei in the gel layer, and a complex and ordered grid-like channel structure appears, which is conducive to the diffusion of the molecules in the inner layer and accelerates the silicate condensation and crystallization. With the extension of time, crystal particles such as Na + accumulated on the surface of CGCS finally formed a stable NaP zeolite structure [22,23].…”
Section: Influence Of Crystallization Timementioning
confidence: 99%
“…In raw fly ash, the broad peak at 3412 cm -1 and 1622 cm -1 were ascribed to the stretching and deformation vibrations of OH and H-O-H groups from the water molecules. While for Gr3, the broad bands are strong and these bands belong to the weakly bound water molecules which were adsorbed on the surface or trapped in the large cavities between the rings of geopolymer [2,19]. In the raw fly ash the strong peak at 1383 cm -1 was due to CO deformation vibration, and for Gr3 the weak peak at 1425 cm -1 was attributed to CO bending vibration.…”
Section: Characterizationmentioning
confidence: 97%
“…The negative value of DG 0 conrms the spontaneous nature of the process. 46,52,53 However, the positive value of DG 0 implies that the adsorption process is not spontaneous, thus requiring the mechanical agitation. 54…”
Section: Thermodynamic Analysismentioning
confidence: 99%