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Atmospheric Measurement Techniques An interactive open-access journal of the European Geosciences Union
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Discussion papers
https://doi.org/10.5194/amtd-6-7633-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/amtd-6-7633-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Submitted as: research article 22 Aug 2013

Submitted as: research article | 22 Aug 2013

Review status
This discussion paper is a preprint. It has been under review for the journal Atmospheric Measurement Techniques (AMT). The revised manuscript was not accepted.

Flask sample measurements for CO2, CH4 and CO using cavity ring-down spectrometry

J.-L. Wang1, G. Jacobson2, C. W. Rella2, C.-Y. Chang3, I. Liu4, W.-T. Liu1, C. Chew3, C.-F. Ou-Yang1,5, W.-C. Liao1, and C.-C. Chang3 J.-L. Wang et al.
  • 1Department of Chemistry, National Central University, 320 Chungli, Taiwan
  • 2Picarro, Inc., Santa Clara, CA, USA
  • 3Research Center for Environmental Changes, Academia Sinica, 11529 Taipei, Taiwan
  • 4Jusun Inc., 231 New Taipei City, Taiwan
  • 5Department of Atmospheric Sciences, National Central University, 320 Chungli, Taiwan

Abstract. In recent years, cavity ring-down spectrometry (CRDS) has been demonstrated to be a highly sensitive, stable and fast analytical technique for real-time in situ measurements of greenhouse gases. In this study, we propose the technique (which we call flask-CRDS) of analyzing whole air flask samples for CO2, CH4 and CO using a custom gas manifold designed to connect to a CRDS analyzer. Extremely stable measurements of these gases can be achieved over a large pressure range in the flask, from 175 to 760 Torr. The wide pressure range is conducive to flask sample measurement in three ways: (1) flask samples can be collected in low-pressure environments (e.g. high-altitude locations); (2) flask samples can be first analyzed for other trace gases with the remaining low-pressure sample for CRDS analysis of CO2, CH4 and CO; and (3) flask samples can be archived and re-analyzed for validation. The repeatability of this method (1σ of 0.07 ppm for CO2, 0.4 ppb for CH4, and 0.5 ppb for CO) was assessed by analyzing five canisters filled with the same air sample to a pressure of 200 Torr. An inter-comparison of the flask-CRDS data with in-situ CRDS measurements at a high-altitude mountain baseline station revealed excellent agreement, with differences of 0.10 ± 0.09 ppm (1σ) for CO2 and 0.9 ± 1.0 ppb for CH4. This study demonstrated that the flask-CRDS method was not only simple to build and operate but could also perform highly accurate and precise measurements of atmospheric CO2, CH4 and CO in flask samples.

J.-L. Wang et al.
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J.-L. Wang et al.
J.-L. Wang et al.
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