Moroccan clays for potential use as aluminosilicate precursors for geopolymer synthesis

Three Moroccan clays, denoted A1, A3 and A5, were sampled from the Fez region with the aim of potential use as aluminosilicate precursors for geopolymer synthesis. Each clay was subjected to calcination at 700 °C and analyzed using DTA/TG, grain size distribution measurements, XRD, and FTIR spectros...

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Main Authors: El Khomsi Anass, Ghaezouni Ameni, Idrissi kandri Noureddine, Zerouale Abdelaziz, Rossignol Sylvie
Format: Article
Language:English
Published: EDP Sciences 2021-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/16/e3sconf_joe2021_03001.pdf
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spelling doaj-ea5e24b0d30b4e23b77bf9104c4362e12021-04-06T13:46:57ZengEDP SciencesE3S Web of Conferences2267-12422021-01-012400300110.1051/e3sconf/202124003001e3sconf_joe2021_03001Moroccan clays for potential use as aluminosilicate precursors for geopolymer synthesisEl Khomsi AnassGhaezouni Ameni0Idrissi kandri Noureddine1Zerouale Abdelaziz2Rossignol Sylvie3IRCER, Ecole Nationale Supérieure de Céramique IndustrielleLaboratoire Signaux Systèmes & Composants, Faculté des Sciences et TechniquesLaboratoire Signaux Systèmes & Composants, Faculté des Sciences et TechniquesIRCER, Ecole Nationale Supérieure de Céramique IndustrielleThree Moroccan clays, denoted A1, A3 and A5, were sampled from the Fez region with the aim of potential use as aluminosilicate precursors for geopolymer synthesis. Each clay was subjected to calcination at 700 °C and analyzed using DTA/TG, grain size distribution measurements, XRD, and FTIR spectroscopy before and after heat treatment. The results showed that the three clays contain kaolinite in different proportions in addition to some associated minerals, such as quartz, hematite, calcite and dolomite. Heat treatment successfully activated the clay by the amorphization of kaolinite, which is essential for geopolymerization. Some other changes were observed in the associated minerals, especially carbonates, which partially or totally decomposed depending on the clay, while other minerals remained intact. The SBET and NBO values are in accordance with the degree of polymerization, and the obtention of consolidated materials is possible by alkali activation of the calcined clays.https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/16/e3sconf_joe2021_03001.pdf
collection DOAJ
language English
format Article
sources DOAJ
author El Khomsi Anass
Ghaezouni Ameni
Idrissi kandri Noureddine
Zerouale Abdelaziz
Rossignol Sylvie
spellingShingle El Khomsi Anass
Ghaezouni Ameni
Idrissi kandri Noureddine
Zerouale Abdelaziz
Rossignol Sylvie
Moroccan clays for potential use as aluminosilicate precursors for geopolymer synthesis
E3S Web of Conferences
author_facet El Khomsi Anass
Ghaezouni Ameni
Idrissi kandri Noureddine
Zerouale Abdelaziz
Rossignol Sylvie
author_sort El Khomsi Anass
title Moroccan clays for potential use as aluminosilicate precursors for geopolymer synthesis
title_short Moroccan clays for potential use as aluminosilicate precursors for geopolymer synthesis
title_full Moroccan clays for potential use as aluminosilicate precursors for geopolymer synthesis
title_fullStr Moroccan clays for potential use as aluminosilicate precursors for geopolymer synthesis
title_full_unstemmed Moroccan clays for potential use as aluminosilicate precursors for geopolymer synthesis
title_sort moroccan clays for potential use as aluminosilicate precursors for geopolymer synthesis
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2021-01-01
description Three Moroccan clays, denoted A1, A3 and A5, were sampled from the Fez region with the aim of potential use as aluminosilicate precursors for geopolymer synthesis. Each clay was subjected to calcination at 700 °C and analyzed using DTA/TG, grain size distribution measurements, XRD, and FTIR spectroscopy before and after heat treatment. The results showed that the three clays contain kaolinite in different proportions in addition to some associated minerals, such as quartz, hematite, calcite and dolomite. Heat treatment successfully activated the clay by the amorphization of kaolinite, which is essential for geopolymerization. Some other changes were observed in the associated minerals, especially carbonates, which partially or totally decomposed depending on the clay, while other minerals remained intact. The SBET and NBO values are in accordance with the degree of polymerization, and the obtention of consolidated materials is possible by alkali activation of the calcined clays.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/16/e3sconf_joe2021_03001.pdf
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