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Thermal Properties of Illite-Zeolite Mixtures up to 1100 degrees C

  1. 1.
    0558615 - ÚFP 2023 RIV CH eng J - Článek v odborném periodiku
    Csáki, Š. - Sunitrova, I. - Lukáč, František - Lagod, G. - Trník, A.
    Thermal Properties of Illite-Zeolite Mixtures up to 1100 degrees C.
    Materials. Roč. 15, č. 9 (2022), č. článku 3029. E-ISSN 1996-1944
    Institucionální podpora: RVO:61389021
    Klíčová slova: natural zeolite * structural-characterization * clinoptilolite * diffraction * dehydration * orientation * performance * ceramics * clays * illitic clay * zeolite * clinoptilolite * thermal expansion * thermal diffusivity * thermal conductivity * specific heat capacity
    Obor OECD: Materials engineering
    Impakt faktor: 3.4, rok: 2022
    Způsob publikování: Open access
    https://www.mdpi.com/1996-1944/15/9/3029

    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 (Fuzerradvany, Hungary) was mixed with natural zeolite (NiznATIN SMALL LETTER Y WITH ACUTE 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 degrees C to 575 degrees 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 degrees C (for illitic clay) to 1005 degrees 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.
    Trvalý link: http://hdl.handle.net/11104/0332250

     
     
Počet záznamů: 1  

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