2016
DOI: 10.1016/j.jallcom.2016.07.297
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Intrinsic parameters involved in the synthesis of metakaolin based geopolymer: Microstructure analysis

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Cited by 16 publications
(6 citation statements)
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“…Fluorite (CaF 2 , PDS-00-035-0846) was used as an internal standard. The crystal structure information of the refined phases O-H stretching and bending modes of absorbed molecular water in the metakaolin structure 11,13,15 . The band in the wavenumber range 3500-3300 cm -1 is weaker for MK2 than that for MK1 and the signals located in the range 3700-3600 cm -1 are almost imperceptible, which confirms the lower kaolinite content of MK2 when compared to that of MK1 15 .…”
Section: Materials and Characterizationmentioning
confidence: 99%
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“…Fluorite (CaF 2 , PDS-00-035-0846) was used as an internal standard. The crystal structure information of the refined phases O-H stretching and bending modes of absorbed molecular water in the metakaolin structure 11,13,15 . The band in the wavenumber range 3500-3300 cm -1 is weaker for MK2 than that for MK1 and the signals located in the range 3700-3600 cm -1 are almost imperceptible, which confirms the lower kaolinite content of MK2 when compared to that of MK1 15 .…”
Section: Materials and Characterizationmentioning
confidence: 99%
“…As well as in the metakaolins analyses, this peak at 3434 cm -1 for G1 was more intense than for G2 due to the higher amount of kaolinite found by the Rietveld refinement in G1. Figure 6 presents other characteristic bands of geopolymers, described as follows: below 700 cm -1 , related to the asymmetric vibration of the Si-O-(Si, Al) bonds, around 1000 cm -1 , related to Si-O-Si bonds and around 1600 cm -1 , attributed to stretching vibrations (H-O) of absorbed or structural water molecules present in the geopolymer porosity [11][12][13] .…”
Section: Ftir Analysismentioning
confidence: 99%
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“…In this environment, a three-dimensional network structure of geopolymers is formed due to the rapid dissolution and reunion reaction of silica-aluminum active substances. The geopolymer structure mainly contains three different sialate units [4], namely, poly sialate (-Si-O-Al-), poly sialate-siloxo (-Si-O-Al-O-Si-), and polysialate-disiloxo (-Si-O-Al-O-Si-O-Si-), shown in Figure 1. The properties of the final products are highly dependent on the cross-linking degree of the different silico-aluminate polymeric chains [5].…”
Section: Introductionmentioning
confidence: 99%
“…It should be noted that not only fly ash but also other aluminosilicate materials [11,12,14,17,24], such as different types of slags [25,26] or metakaolin [26][27][28][29][30], can be applied as starting materials for geopolymers. However, fly ashes from different sources [26,31,32], mixtures made of different fly ashes [33] or compositions of fly ash and other materials [34] still arouse interest.…”
Section: Introductionmentioning
confidence: 99%