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오현철

Oh, Hyunchul
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Automated Cold Volume Calibration of Temperature Variation in Cryogenic Hydrogen Isotope Sorption Isotherm

Alternative Title
극저온(20K) 수소동위원소 흡착 등온선의 온도 변화에 대한 자동 저온 부피 교정
Author(s)
Park, JawooOh, Hyunchul
Issued Date
2019-05
DOI
10.3740/mrsk.2019.29.5.336
URI
https://scholarworks.unist.ac.kr/handle/201301/57807
Fulltext
http://journal.mrs-k.or.kr/journal/article.php?code=66833
Citation
Korean Journal of Materials Research, v.29, no.5, pp.336 - 341
Abstract
The gas adsorption isotherm requires accurate measurement for the analysis of porous materials and is used as an index of surface area, pore distribution, and adsorption amount of gas. Basically, adsorption isotherms of porous materials are measured conventionally at 77K and 87K using liquid nitrogen and liquid argon. The cold volume calibration in this conventional method is done simply by splitting a sample cell into two zones (cold and warm volumes) by controlling the level sensor in a Dewar filled with liquid nitrogen or argon. As a result, BET measurement for textural properties is mainly limited to liquefied gases (i.e. N2 or Ar) at atmospheric pressure. In order to independently investigate other gases (e.g. hydrogen isotopes) at cryogenic temperature, a novel temperature control system in the sample cell is required, and consequently cold volume calibration at various temperatures becomes more important. In this study, a cryocooler system is installed in a commercially available BET device to control the sample cell temperature, and the automated cold volume calibration method of temperature variation is introduced. This developed calibration method presents a reliable and reproducible method of cryogenic measurement for hydrogen isotope separation in porous materials, and also provides large flexibility for evaluating various other gases at various temperature. © Materials Research Society of Korea.
Publisher
The Materials Research Society of Korea
ISSN
1225-0562
Keyword (Author)
AccuracyAdsorption isothermCalibration methodCold volume and temperature calibrationsCryogenic measurements

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