2021
DOI: 10.1016/j.jnoncrysol.2021.120777
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Investigation of Phosphate based geopolymers formation mechanism

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Cited by 47 publications
(14 citation statements)
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“…A new peak formed at the chemical shift between 0 and −20 ppm, which is the characteristic peak of phosphate-based geopolymer, corresponding to Al VI in Al(OP) 6−x (SiO) x [ 33 ]. According to previous studies, this deconvolution reveals the presence of two resonances [ 34 ]. The resonance located at −12 ppm is attributed to Al VI in condensed aluminosilicate networks and the other one located at −18 ppm is assigned to Al VI in polymerized phosphate aluminum networks.…”
Section: Resultsmentioning
confidence: 82%
“…A new peak formed at the chemical shift between 0 and −20 ppm, which is the characteristic peak of phosphate-based geopolymer, corresponding to Al VI in Al(OP) 6−x (SiO) x [ 33 ]. According to previous studies, this deconvolution reveals the presence of two resonances [ 34 ]. The resonance located at −12 ppm is attributed to Al VI in condensed aluminosilicate networks and the other one located at −18 ppm is assigned to Al VI in polymerized phosphate aluminum networks.…”
Section: Resultsmentioning
confidence: 82%
“…We notice the disappearance of phases like kaolinite, illite, montmorillonite and the appearance of others like anorthite and mullite as a consequence of a series of physic‐chemical transformations occurred 40,41 . The densification of mixtures proceeded through a viscous sintering (by melt flow) due to the apparition of amorphous phase, which is clearly shown by a diffuse reflection on diffractogram shapes (broad hump between 18 and 40°) 42,43 . From the identification of XRD patterns, we notice the apparition of anorthite in all mixture except sample number 3 and 3* composed by 100% kaolin.…”
Section: Resultsmentioning
confidence: 87%
“…40,41 The densification of mixtures proceeded through a viscous sintering (by melt flow) due to the apparition of amorphous phase, which is clearly shown by a diffuse reflection on diffractogram shapes (broad hump between 18 and 40 • ). 42,43 From the identification of XRD patterns, we notice the apparition of anorthite in all mixture except sample number 3 and 3* composed by 100% kaolin. Mullite phase appears in all mixtures containing kaolin (K).…”
Section: Mineralogical Analysis By X-ray Diffractionmentioning
confidence: 88%
“…In the published literature, we have noticed that some scholars have used room temperature in their studies [ 29 , 48 ], while most others have used elevated temperature curing. The main heating range is between 40 °C and 90 °C, such as 40 °C [ 23 ], 60 °C [ 17 , 19 , 41 , 49 , 50 ], 80 °C [ 51 , 52 , 53 ], and 90 °C [ 54 ]. There is no obvious promoting effect when the heating temperature is too low, and if the heating temperature is too high, it may lead to the cracking of the geopolymer structure or transformation into other types of materials, such as zeolite [ 1 , 55 ].…”
Section: The Preparation Process Of Asp Geopolymersmentioning
confidence: 99%
“…At present, with regard to research on the reaction mechanism of ASP geopolymers, scholars have generally divided the geopolymerization process of ASP geopolymers into three or even four steps with depolymerization (the dealumination process) and condensation as the core [ 20 , 25 , 49 ]. The mainstream geopolymerization schematic diagram is shown in Figure 5 , and the mainstream geopolymerization process is as follows: The first is the dealumination process of the aluminosilicate precursor.…”
Section: The Preparation Process Of Asp Geopolymersmentioning
confidence: 99%