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Thermal Properties of Illite-Zeolite Mixtures up to 1100 °C
Illitic clays are the commonly used material in building ceramics. Zeolites are microporous, hydrated crystalline aluminosilicates, they are widely used due to their structure and absorption properties. In this study, illitic clay (Füzérradvány, Hungary) was mixed with natural zeolite (Nižný Hrabove...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
MDPI
2022
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9099582/ https://www.ncbi.nlm.nih.gov/pubmed/35591365 http://dx.doi.org/10.3390/ma15093029 |
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author | Csáki, Štefan Sunitrová, Ivana Lukáč, František Łagód, Grzegorz Trník, Anton |
author_facet | Csáki, Štefan Sunitrová, Ivana Lukáč, František Łagód, Grzegorz Trník, Anton |
author_sort | Csáki, Štefan |
collection | PubMed |
description | Illitic clays are the commonly used material in building ceramics. Zeolites are microporous, hydrated crystalline aluminosilicates, they are widely used due to their structure and absorption properties. In this study, illitic clay (Füzérradvány, Hungary) was mixed with natural zeolite (Nižný Hrabovec, Slovakia) with up to 50 wt.% of zeolite content. The samples were submitted to thermal analyses, such as differential thermal analysis, differential scanning calorimetry, thermogravimetry, and dilatometry. In addition, the evolution of thermal diffusivity, thermal conductivity, and specific heat capacity in the heating stage of firing were measured and discussed. The amount of the physically bound water in the samples increased along with the amount of zeolite. The temperature of the illite dehydroxylation (peak temperature) was slightly shifted to lower temperatures, from 609 °C to 575 °C (for sample IZ50). On the other hand, the mass loss and the shrinkage of the samples significantly increased with the zeolite content in the samples. Sample IZ50 reached 10.8% shrinkage, while the sample prepared only from the illitic clay contracted by 5.8%. Nevertheless, the temperature of the beginning of the sintering (taken from the dilatometric curves) decreased from 1021 °C (for illitic clay) to 1005 °C (for IZ50). The thermal diffusivity and thermal conductivity values decreased as the amount of zeolite increased in the samples, thus showing promising thermal insulating properties. |
format | Online Article Text |
id | pubmed-9099582 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2022 |
publisher | MDPI |
record_format | MEDLINE/PubMed |
spelling | pubmed-90995822022-05-14 Thermal Properties of Illite-Zeolite Mixtures up to 1100 °C Csáki, Štefan Sunitrová, Ivana Lukáč, František Łagód, Grzegorz Trník, Anton Materials (Basel) Article Illitic clays are the commonly used material in building ceramics. Zeolites are microporous, hydrated crystalline aluminosilicates, they are widely used due to their structure and absorption properties. In this study, illitic clay (Füzérradvány, Hungary) was mixed with natural zeolite (Nižný Hrabovec, Slovakia) with up to 50 wt.% of zeolite content. The samples were submitted to thermal analyses, such as differential thermal analysis, differential scanning calorimetry, thermogravimetry, and dilatometry. In addition, the evolution of thermal diffusivity, thermal conductivity, and specific heat capacity in the heating stage of firing were measured and discussed. The amount of the physically bound water in the samples increased along with the amount of zeolite. The temperature of the illite dehydroxylation (peak temperature) was slightly shifted to lower temperatures, from 609 °C to 575 °C (for sample IZ50). On the other hand, the mass loss and the shrinkage of the samples significantly increased with the zeolite content in the samples. Sample IZ50 reached 10.8% shrinkage, while the sample prepared only from the illitic clay contracted by 5.8%. Nevertheless, the temperature of the beginning of the sintering (taken from the dilatometric curves) decreased from 1021 °C (for illitic clay) to 1005 °C (for IZ50). The thermal diffusivity and thermal conductivity values decreased as the amount of zeolite increased in the samples, thus showing promising thermal insulating properties. MDPI 2022-04-21 /pmc/articles/PMC9099582/ /pubmed/35591365 http://dx.doi.org/10.3390/ma15093029 Text en © 2022 by the authors. https://creativecommons.org/licenses/by/4.0/Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). |
spellingShingle | Article Csáki, Štefan Sunitrová, Ivana Lukáč, František Łagód, Grzegorz Trník, Anton Thermal Properties of Illite-Zeolite Mixtures up to 1100 °C |
title | Thermal Properties of Illite-Zeolite Mixtures up to 1100 °C |
title_full | Thermal Properties of Illite-Zeolite Mixtures up to 1100 °C |
title_fullStr | Thermal Properties of Illite-Zeolite Mixtures up to 1100 °C |
title_full_unstemmed | Thermal Properties of Illite-Zeolite Mixtures up to 1100 °C |
title_short | Thermal Properties of Illite-Zeolite Mixtures up to 1100 °C |
title_sort | thermal properties of illite-zeolite mixtures up to 1100 °c |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9099582/ https://www.ncbi.nlm.nih.gov/pubmed/35591365 http://dx.doi.org/10.3390/ma15093029 |
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