2018
DOI: 10.1016/j.jclepro.2018.07.171
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Microstructure and engineering properties of Fe2O3(FeO)-Al2O3-SiO2 based geopolymer composites

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Cited by 101 publications
(42 citation statements)
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“…This is due to a typical formation of a new gel phase known as ferrosialate gel as a result of the incorporation of Fe +2 with the activator solution and other ions from the geopolymeric system via a similar chemical process as the Si 4+ , Al 3+, and Ca 2+ . This was stated by Cannio et al (2018) [28] where the ferrosialate has been identified in a geopolymer mix.…”
Section: Compressive Strength Of Fa-based Geopolymer Repair Materialsmentioning
confidence: 61%
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“…This is due to a typical formation of a new gel phase known as ferrosialate gel as a result of the incorporation of Fe +2 with the activator solution and other ions from the geopolymeric system via a similar chemical process as the Si 4+ , Al 3+, and Ca 2+ . This was stated by Cannio et al (2018) [28] where the ferrosialate has been identified in a geopolymer mix.…”
Section: Compressive Strength Of Fa-based Geopolymer Repair Materialsmentioning
confidence: 61%
“…Similarly, Cannio et al (2018) [28] suggested that the formation of fayalite can occur through a chemical reaction of hydrated ferric oxyhydroxide with silica as shown in Equation (3). Figure 9 displays the images of the interfacial transition zone (ITZ) between the FA-based geopolymer paste and OPC substrate as given by the SEM analysis.…”
Section: Phase Analysismentioning
confidence: 97%
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“…Figure 3 depicts the FTIR spectra of sand, binder, and specimens prepared with 20 % and 40 % binder to aggregate ratio. The results show that specimens had little or insigni cant amount of water within the matrix due to lack of H-O-H vibrations around 3600 cm-1 [43]. The absorption bands around 500 cm − 1 usually indicates the bending mode of Si-O-T (T may be Al or Si and in some cases Ca) [44].…”
Section: Ftir Analysis Of Specimens With Different Binder Contentmentioning
confidence: 96%
“…Additionally, the band at 990 cm -1 is most of time assigned symmetrical bending of the Si-O-T bonds [23], and Fe-O-Si when the solid precursor contains a significant amount of Fe 2 O 3 [24,25,26]. On the other hand, the band located at 1649 cm…”
Section: Fig 4 Ir Spectra Of Volcanic Ashmentioning
confidence: 99%