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AGU: Journal of Geophysical Research, Atmospheres

 

Keywords

  • atmospheric CO2
  • NDIR
  • isotope effect

Index Terms

  • Atmospheric Composition and Structure: Instruments and techniques
  • Atmospheric Composition and Structure: Troposphere: composition and chemistry
  • Atmospheric Composition and Structure: Geochemical cycles
Abstract
Cited By (2)
 

Abstract

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114, D13302, 12 PP., 2009
doi:10.1029/2009JD011734

Theoretical and experimental evaluation of the isotope effect of NDIR analyzer on atmospheric CO2 measurement

Yasunori Tohjima

Atmospheric Environment Division, National Institute for Environmental Studies, Tsukuba, Japan

Keiichi Katsumata

Scientific Research Division, Global Environmental Forum, Tokyo, Japan

Isamu Morino

Atmospheric Environment Division, National Institute for Environmental Studies, Tsukuba, Japan

Hitoshi Mukai

Atmospheric Environment Division, National Institute for Environmental Studies, Tsukuba, Japan

Toshinobu Machida

Atmospheric Environment Division, National Institute for Environmental Studies, Tsukuba, Japan

Isao Akama

Production Development Section, Japan Fine Products Corp., Kawasaki, Japan

Taketo Amari

Production Development Section, Japan Fine Products Corp., Kawasaki, Japan

Urumu Tsunogai

Earth and Planetary System Science, Faculty of Science, Hokkaido University, Sapporo, Japan

Nondispersive infrared (NDIR) CO2 analyzer could produce erroneous CO2 mole fraction measurements for an air sample when CO2-in-air mixtures having different isotopic compositions than atmospheric CO2 are used as the NDIR calibration gases. This is because (1) an optical band-pass filter equipped in a typical NDIR analyzer to minimize the interference effect from the other infrared-active species is basically designed to transmit only the absorption band of 12C16O2 and (2) absorption bands for the other CO2-related isotopologues, for example, 13C16O2, are shifted to lower wave numbers depending on their isotope effects. To evaluate the effect of the isotopic composition on the NDIR response, we computed the theoretical relative molar response of the instrument to each isotopologue based on the infrared absorptance by the individual isotopologues. We then prepared a gravimetric 13CO2-in-air mixture with CO2 mole fraction of 380 ppm to experimentally determine the optical filter property. The apparent mole fractions of the 13CO2-in-air mixture determined by three NDIR analyzers used in this study were 46, 94, and 27 ppm, indicating that the optical filters in these instruments substantially reduced the response to 13C16O2. Based on these theoretical and experimental analyses, we evaluated the apparent difference in the CO2 mole fraction determined by the three NDIR analyzers from the true value when isotopically lighter CO2-in-air mixtures (δ 13C = −32.4‰ and δ 18O = +11.7‰), as compared to atmospheric CO2 (δ 13C = ∼−8‰ and δ 18O = ∼+40‰), are used as calibration gases. The estimated difference varied with NDIR analyzers, ranging from −0.04 to −0.08 ppm for air samples with 380 ppm CO2.

Received 9 January 2009; accepted 12 May 2009; published 7 July 2009.

Citation: Tohjima, Y., K. Katsumata, I. Morino, H. Mukai, T. Machida, I. Akama, T. Amari, and U. Tsunogai (2009), Theoretical and experimental evaluation of the isotope effect of NDIR analyzer on atmospheric CO2 measurement, J. Geophys. Res., 114, D13302, doi:10.1029/2009JD011734.

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