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Automated Cold Volume Calibration of Temperature Variation in Cryogenic Hydrogen Isotope Sorption Isothermopen access

Authors
Park, JaewooOh, Hyunchul
Issue Date
May-2019
Publisher
MATERIALS RESEARCH SOC KOREA
Keywords
calibration method; cryogenic measurements; cold volume and temperature calibrations; accuracy; adsorption isotherm
Citation
KOREAN JOURNAL OF MATERIALS RESEARCH, v.29, no.5, pp 336 - 341
Pages
6
Indexed
SCOPUS
ESCI
KCI
Journal Title
KOREAN JOURNAL OF MATERIALS RESEARCH
Volume
29
Number
5
Start Page
336
End Page
341
URI
https://scholarworks.gnu.ac.kr/handle/sw.gnu/72967
DOI
10.3740/MRSK.2019.29.5.336
ISSN
1225-0562
2287-7258
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. N-2 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.
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