2011
DOI: 10.1127/0935-1221/2010/0022-2070
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Silicate-, aluminosilicate and calciumsilicate gels for building materials: chemical and mechanical properties during ageing

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Cited by 38 publications
(23 citation statements)
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“…The red circles mark the main amorphous signature of MK, that is also present in GP, and implied that a significant amount of unreacted MK remains. The presence of unreacted MK is no disadvantage, but rather protects the long polysiloxo chains during aging, an important property for a long-standing mechanical strength (Rüscher et al 2011). The additional broad contribution in the GP centered around 28 • (2) is clearly related to the geopolymer framework.…”
Section: Mineralogical Characterizationmentioning
confidence: 99%
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“…The red circles mark the main amorphous signature of MK, that is also present in GP, and implied that a significant amount of unreacted MK remains. The presence of unreacted MK is no disadvantage, but rather protects the long polysiloxo chains during aging, an important property for a long-standing mechanical strength (Rüscher et al 2011). The additional broad contribution in the GP centered around 28 • (2) is clearly related to the geopolymer framework.…”
Section: Mineralogical Characterizationmentioning
confidence: 99%
“…The lowest absorption band at 1620 cm −1 is attributed to the O H bending vibrations of water molecule bonds. The peak at 1076 cm −1 was assigned to a density of states peak maximum (DOSPM) of asymmetric stretching vibrations of SiO4-units of various connections (Si-O-Al and Si-O-Si) (Rüscher et al, 2011), including quartz. The peaks observed at 800, 685, 546 and 466 cm −1 are attributed to the presence of quartz along with the characteristic peaks of dehydrated kaolinite, too.…”
Section: Characterization Of Raw Materials and Sodium Waterglass Frommentioning
confidence: 99%
“…[12,20,21]. The peak at 1076 cm −1 is assigned to the asymmetric stretching vibration modes of Si-O-Al and Si-O-Si [22,23]. The absorption band at 817 cm −1 is attributed to the bending vibration modes of Si-O-Si.…”
Section: Methods Of Characterizations Of the Starting Materials And Mmentioning
confidence: 99%
“…Alkali activation results in a new peak at 1004 cm −1 arising both from the geopolymeric structure with Si-O-Al bond (23) as well as influence of Ca ions on the Si-O vibration mode in the geopolymer structure (26). The raw pond ash contains 5.5 wt.% CaO and can be suggested that bound mostly to glass phase.…”
Section: Characterization Of the Geopolymer Pastesmentioning
confidence: 99%