Thermophysical and Electrical Properties of a Natural Zeolite
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F23%3A00373857" target="_blank" >RIV/68407700:21110/23:00373857 - isvavai.cz</a>
Výsledek na webu
<a href="https://doi.org/10.1063/5.0146731" target="_blank" >https://doi.org/10.1063/5.0146731</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1063/5.0146731" target="_blank" >10.1063/5.0146731</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Thermophysical and Electrical Properties of a Natural Zeolite
Popis výsledku v původním jazyce
Thermophysical processes occurring during the firing of zeolite (mined in Nizny Hrabovec, Slovakia) was studied in terms of conventional thermal analyses (differential thermal analysis, thermogravimetry, dilatometry), acoustic emission, scanning electron microscopy, and DC conductivity measurements. The evaporation of the water molecules trapped in the cavities and channels of zeolite led to a continuous gradual decrease in the samples mass up to ~850 °C. Clinoptilolite (the major mineral phase of zeolite) transformed into an amorphous phase above 800 °C. The sintering process started at 900 °C in the presence of liquid phase. DC conductivity revealed that the dominant charge carriers, mostly due to the dehydration of zeolite, are H+ and OH– ions up to the collapse of its structure. At higher temperatures alkali ions Na+, K+, and Ca2+ became the major charge carriers with conduction activation energy of 3.51 eV (from 830 °C to 930 °C). Above 960 °C the appearance of glassy phase supported the DC conductivity carried by the alkali ions and the activation energy reached 1.67 eV.
Název v anglickém jazyce
Thermophysical and Electrical Properties of a Natural Zeolite
Popis výsledku anglicky
Thermophysical processes occurring during the firing of zeolite (mined in Nizny Hrabovec, Slovakia) was studied in terms of conventional thermal analyses (differential thermal analysis, thermogravimetry, dilatometry), acoustic emission, scanning electron microscopy, and DC conductivity measurements. The evaporation of the water molecules trapped in the cavities and channels of zeolite led to a continuous gradual decrease in the samples mass up to ~850 °C. Clinoptilolite (the major mineral phase of zeolite) transformed into an amorphous phase above 800 °C. The sintering process started at 900 °C in the presence of liquid phase. DC conductivity revealed that the dominant charge carriers, mostly due to the dehydration of zeolite, are H+ and OH– ions up to the collapse of its structure. At higher temperatures alkali ions Na+, K+, and Ca2+ became the major charge carriers with conduction activation energy of 3.51 eV (from 830 °C to 930 °C). Above 960 °C the appearance of glassy phase supported the DC conductivity carried by the alkali ions and the activation energy reached 1.67 eV.
Klasifikace
Druh
D - Stať ve sborníku
CEP obor
—
OECD FORD obor
20501 - Materials engineering
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2023
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název statě ve sborníku
Central European Symposium on Thermophysics 2022 (CEST 2022)
ISBN
—
ISSN
1551-7616
e-ISSN
1551-7616
Počet stran výsledku
6
Strana od-do
—
Název nakladatele
AIP Conference Proceedings
Místo vydání
New York
Místo konání akce
Olomouc
Datum konání akce
31. 8. 2022
Typ akce podle státní příslušnosti
WRD - Celosvětová akce
Kód UT WoS článku
—