EGU2020-18624
https://doi.org/10.5194/egusphere-egu2020-18624
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

N2O isotope research: development of reference materials and metrological characterization of OIRS analyzers within the SIRS project

Joachim Mohn1, Joanna Rupacher1, Heiko Moossen2, Sakae Toyoda3, Christina Biasi4, Jan Kaiser5, Stephen Harris6, Jesper Liisberg7, Benjamin Wolf8, Longlong Xia8, Matti Barthel9, Longfei Yu1, Kristýna Kantnerová1, Jing Wei1, Ruth Pearce10, Eric Mussell Webber10, Bryce Kelly6, Thomas Blunier7, Naohiro Yoshida3,11, Paul Brewer10, and the Additional co-authors*
Joachim Mohn et al.
  • 1Empa, Air Pollution & Environmental Technology, Dübendorf, Switzerland (joachim.mohn@empa.ch)
  • 2Max-Planck-Institute for Biogeochemistry (MPI-BGC), Stable Isotope Laboratory (BGC-IsoLab), Jena, Germany
  • 3Tokyo Institute of Technology, Department of Chemical Science and Engineering, Yokohama, Japan
  • 4University of Eastern Finland, Biogeochemistry Research Group, Kuopio, Finland
  • 5University of East Anglia (UEA), Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, Norwich, UK
  • 6UNSW Sydney, School of Biological, Earth and Environmental Sciences, Sydney, Australia
  • 7University of Copenhagen, Centre for Ice and Climate, Niels Bohr Institute, Copenhagen, Denmark
  • 8Karlsruhe Institute of Technology, IMK-IFU, Garmisch-Partenkirchen, Germany
  • 9ETH Zürich, Department of Environmental Systems Science, Zürich, Switzerland
  • 10National Physical Laboratory, Gas and Particle Metrology, Teddington, UK
  • 11Tokyo Institute of Technology, Earth-Life Science Institute, Tokyo, Japan
  • *A full list of authors appears at the end of the abstract

Measurements of the four most abundant stable isotopocules of N2O (14N14N16O, 15N14N16O, 14N15N16O, and 14N14N18O) can provide a valuable constraint on source attribution of atmospheric N2O. N2O isotopocules at natural abundance levels can be analyzed by isotope-ratio mass-spectrometry (IRMS) [1] and more recently optical isotope ratio spectroscopy (OIRS) [2]. OIRS instruments can analyze the N2O isotopic composition in gaseous mixtures in a continuous-flow mode, providing real-time data with minimal or no sample pretreatment, which is highly attractive to better resolve the temporal complexity of N2O production and consumption processes. Most importantly, OIRS laser spectroscopy is selective for position-specific 15N substitution due to the existence of characteristic rotational-vibrational spectra.

By allowing both in-situ application and measurements in high temporal resolution, laser spectroscopy has established a new quality of data for research on N2O in particular and N cycling in general. However, applications remain challenging and are still scarce as a metrological characterization of OIRS analyzers, reporting factors limiting their performance is still missing. In addition, only since recently two pure N2O isotopocule reference materials have been made available through the United States Geological Survey (USGS), which however, only offer a small range of δ15N and δ18O values (< 1 ‰) and are therefore not suited for a two-point calibration approach [3].

This presentation will highlight the recent progress achieved within the framework of the EMPIR project “Metrology for Stable Isotope Reference Standards (SIRS)”, namely:

  • (1) The development of pure and diluted N2O reference materials (RMs), covering the range of isotope values required by the scientific community. These gaseous standards are available as pure N2O or N2O diluted in whole air. N2O RMs were analyzed by an international group of laboratories for δ15N, δ18O (MPI-BGC, Tokyo Institute of Technology, UEA), δ15Nα, δ15Nß (Empa, Tokyo Institute of Technology) and δ17O (UEA) traceable to the existing isotope ratio scales.
  • (2) The metrological characterization of the three most common commercial N2O isotope OIRS analyzers (with/without precon QCLAS, OA-ICOS and CRDS) for gas matrix effects, spectral interferences of enhanced trace gas concentrations (CO2, CH4, CO, H2O), short-term and long-term repeatability, drift and dependence of isotope deltas on N2O concentrations [4].

In summary, the authors suggest to include appropriate RMs following the identical treatment (IT) principle during every OIRS measurement to retrieve compatible and accurate results. Remaining differences between sample and reference gas composition have to be corrected, by applying analyzer-specific correction algorithms.

 

[1] Toyoda, S. and N. Yoshida (1999). "Determination of nitrogen isotopomers of nitrous oxide on a modified isotope ratio mass spectrometer." Anal. Chem. 71(20): 4711-4718.

[2] Brewer, P. J. et al. (2019). "Advances in reference materials and measurement techniques for greenhouse gas atmospheric observations." Metrologia 56(3).

[3] Ostrom, N. E. et al. (2018). "Preliminary assessment of stable nitrogen and oxygen isotopic composition of USGS51 and USGS52 nitrous oxide reference gases and perspectives on calibration needs." Rapid Commun. Mass Spectrom. 32(15): 1207-1214.

[4] Harris, S. J., J. Liisberg et al. (2019). "N2O isotopocule measurements using laser spectroscopy: analyzer characterization and intercomparison." Atmos. Meas. Tech. Discuss. (in review).

 

Additional co-authors:

Kerstin Zeyer, Empa, Laboratory for Air Pollution/Environmental Technology, Dübendorf, Switzerland; Aimee Hillier, National Physical Laboratory, Gas and Particle Metrology, Teddington, UK

How to cite: Mohn, J., Rupacher, J., Moossen, H., Toyoda, S., Biasi, C., Kaiser, J., Harris, S., Liisberg, J., Wolf, B., Xia, L., Barthel, M., Yu, L., Kantnerová, K., Wei, J., Pearce, R., Webber, E. M., Kelly, B., Blunier, T., Yoshida, N., and Brewer, P. and the Additional co-authors: N2O isotope research: development of reference materials and metrological characterization of OIRS analyzers within the SIRS project, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18624, https://doi.org/10.5194/egusphere-egu2020-18624, 2020

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