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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EDP Sciences
2021-01-01
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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 |
work_keys_str_mv |
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1721538059007164416 |