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Typ záznamu:
stať ve sborníku (D)
Domácí pracoviště:
Katedra chemie (31500)
Název:
On the Low-Pressure Hysteresis in Gas Sorption Isotherms of Porous Carbons
Citace
Zelenka, T., Zelená, L., Abreu-Jaureguí, C., Silvestre-Albero, J., Zelenková, G. a Slovák, V. On the Low-Pressure Hysteresis in Gas Sorption Isotherms of Porous Carbons.
In:
Porous Materials for Environmental Applications 2024: Porous Materials for Environmental Applications 2024: Book of Abstracts 2024-10-18 Košice.
Košice: Publishing ŠafárikPress, 2024. s. 49-49. ISBN 978-80-574-0351-7.
Podnázev
Rok vydání:
2024
Obor:
Počet stran:
1
Strana od:
49
Strana do:
49
Forma vydání:
Elektronická verze
Kód ISBN:
978-80-574-0351-7
Kód ISSN:
Název sborníku:
Porous Materials for Environmental Applications 2024: Book of Abstracts
Sborník:
Mezinárodní
Název nakladatele:
Publishing ŠafárikPress
Místo vydání:
Košice
Stát vydání:
Sborník vydaný v zahraničí
Název konference:
Porous Materials for Environmental Applications 2024
Místo konání konference:
Košice
Datum zahájení konference:
Typ akce podle státní
příslušnosti účastníků akce:
Evropská akce
Kód UT WoS:
EID:
Klíčová slova anglicky:
porous carbons; hysteresis
Popis v původním jazyce:
This study investigates the origin of low-pressure hysteresis (LPH) in the adsorption and desorption of threedifferent probe molecules: CO2, N2, and Ar, across various adsorption temperatures (from cryogenic to roomtemperature), and within five different carbon materials: synthetic carbons (pristine and one post-syntheticallyoxidized) and natural coal. Significant attention is dedicated to elucidating LPH in oxidized samples outgassed atvarious temperatures (120–350 °C). Experimental results show that insufficient outgassing temperature can leadto unreliable data due to artificial LPH and significantly underestimated textural properties, primarily caused byporosity blockage from substances like moisture. Conversely, in samples where heteroatoms have a stabilizingeffect of texture, such as natural coal, careful consideration of outgassing temperature is crucial due to the risk ofthermal degradation. Other factors contributing to LPH are adsorption temperature, and especially, kineticlimitations at cryogenic temperatures for cellulose-based carbons. Minor factors responsible for LPH are thephysical state of the sample (monolith vs. powder) and the flexibility of the porous system, both studied by CO2sorption.This study constitutes an important piece in the evaluation of LPH, providing practical recommendations andunderlining the importance of experimental design, with implications for further research in this complex field[1].
Popis v anglickém jazyce:
This study investigates the origin of low-pressure hysteresis (LPH) in the adsorption and desorption of threedifferent probe molecules: CO2, N2, and Ar, across various adsorption temperatures (from cryogenic to roomtemperature), and within five different carbon materials: synthetic carbons (pristine and one post-syntheticallyoxidized) and natural coal. Significant attention is dedicated to elucidating LPH in oxidized samples outgassed atvarious temperatures (120–350 °C). Experimental results show that insufficient outgassing temperature can leadto unreliable data due to artificial LPH and significantly underestimated textural properties, primarily caused byporosity blockage from substances like moisture. Conversely, in samples where heteroatoms have a stabilizingeffect of texture, such as natural coal, careful consideration of outgassing temperature is crucial due to the risk ofthermal degradation. Other factors contributing to LPH are adsorption temperature, and especially, kineticlimitations at cryogenic temperatures for cellulose-based carbons. Minor factors responsible for LPH are thephysical state of the sample (monolith vs. powder) and the flexibility of the porous system, both studied by CO2sorption.This study constitutes an important piece in the evaluation of LPH, providing practical recommendations andunderlining the importance of experimental design, with implications for further research in this complex field[1].
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Ohlas
R01:
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