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Volume 6, issue 9 | Copyright

Special issue: Carbon dioxide, other greenhouse gases, and related measurement...

Atmos. Meas. Tech., 6, 2293-2299, 2013
https://doi.org/10.5194/amt-6-2293-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 05 Sep 2013

Research article | 05 Sep 2013

High-precision analysis of SF6 at ambient level

J. S. Lim1, D. M. Moon1, J. S. Kim1, W.-T. Yun2, and J. Lee1 J. S. Lim et al.
  • 1Korea Research Institute of Standards and Science (KRISS), Division of Metrology for Quality Life, P.O. Box 102, Yuseong, Daejeon, South Korea
  • 2Climate Policy Division, Climate Science Bureau, Korea Meteorological Administration, 61 16-gil, Yeouidaebang-ro, Dongjak-gu, Seoul 156-720, South Korea

Abstract. This work reports on the development of a technique for the precise analysis of ambient SF6. This technique, which involves a gas chromatograph/electron capture detector (GC-ECD) coupled with an Activated Alumina-F1 (AA-F1) column, performed well in the measurements, particularly in terms of accuracy, which complies with the World Meteorological Organization (WMO)-recommended compatibility of 0.02 ppt. Compared to the Porapak Q technique, we observed a sharper peak shape for the SF6 stream, which substantiates the improvement in the analytical precision. The traceability to the WMO scale was tested by calibrating the GC-ECD/AA-F1 analyser using five SF6 standards provided by the WMO/Global Atmosphere Watch (GAW) Central Calibration Laboratory (CCL) for SF6 (NOAA, United States of America). After calibration by various methods, the GC-ECD/AA-F1 accurately estimated the mole fraction of SF6 in the working standard prepared by the World Calibration Centre for SF6 operated by the Korea Meteorological Administration (KMA)/Korea Research Institute of Standards and Science (KRISS). Among the calibration methods, the two-point calibration method emerged to be the most economical procedure in terms of the data quality and measurement time. It was found that the KRISS scale of SF6/N2 was biased by 0.13 ppt when compared to the WMO scale of SF6/air; this bias is probably due to a different matrix.

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