A GC-IRMS method for measuring sulfur isotope ratios of carbonyl sulfide from small air samples

Sophie L Baartman; Maarten C Krol; Thomas Röckmann; Shohei Hattori; Kazuki Kamezaki; Naohiro Yoshida; Maria Elena Popa

doi:10.12688/openreseurope.13875.2

A GC-IRMS method for measuring sulfur isotope ratios of carbonyl sulfide from small air samples

Open Res Eur. 2022 Mar 8:1:105. doi: 10.12688/openreseurope.13875.2. eCollection 2021.

Authors

Sophie L Baartman¹, Maarten C Krol^{1

2}, Thomas Röckmann¹, Shohei Hattori^{3

4}, Kazuki Kamezaki^{5

6}, Naohiro Yoshida^{5

7

8}, Maria Elena Popa¹

Affiliations

¹ Institute for Marine and Atmospheric research Utrecht (IMAU), Utrecht University, Utrecht, 3584 CS, The Netherlands.
² Meteorology and Air Quality, Wageningen University & Research Center, Wageningen, 6708 PB, The Netherlands.
³ Department of Chemical Science and Engineering, School of Materials and Chemical Technology, Tokyo Institute of Technology, Yokohama, 226-8502, Japan.
⁴ International Center for Isotope Effects Research (ICIER), Nanjing University, Nanjing, 210023, China.
⁵ Department of Material and Life Sciences, Faculty of Science & Technology, Sophia University, Tokyo, 102-8554, Japan.
⁶ Environmental Management Research Institute, National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba, 305-8569, Japan.
⁷ Earth-Life Science Institute, Tokyo Institute of Technology, Tokyo, 152-8550, Japan.
⁸ National Institute of Information and Communications Technology, Tokyo, 184-8795, Japan.

Abstract

A new system was developed for measuring sulfur isotopes δ ³³S and δ ³⁴S from atmospheric carbonyl sulfide (COS) on small air samples of several liters, using pre-concentration and gas chromatography - isotope ratio mass spectrometry (GC-IRMS). Measurements of COS isotopes provide a tool for quantifying the COS budget, which will help towards better understanding climate feedback mechanisms. For a 4 liter sample at ambient COS mixing ratio, ~500 parts per trillion (ppt), we obtain a reproducibility error of 2.1 ‰ for δ ³³S and 0.4 ‰ for δ ³⁴S. After applying corrections, the uncertainty for an individual ambient air sample measurement is 2.5 ‰ for δ ³³S and 0.9 ‰ for δ ³⁴S. The ability to measure small samples allows application to a global-scale sampling program with limited logistical effort. To illustrate the application of this newly developed system, we present a timeseries of ambient air measurements, during the fall and winter of 2020 and 2021 in Utrecht, the Netherlands. The observed background values were δ ³³S = 1.0 ± 3.4 ‰ and δ ³⁴S = 15.5 ± 0.8 ‰ (VCDT). The maximum observed COS mixing ratios was only 620 ppt. This, in combination with the relatively high δ ³⁴S suggests that the Netherlands receives little COS-containing anthropogenic emissions. We observed a change in COS mixing ratio and δ ³⁴S with different air mass origin, as modelled with HYSPLIT backward trajectory analyses. An increase of 40 ppt in mean COS mixing ratio was observed between fall and winter, which is consistent with the expected seasonal cycle in the Netherlands. Additionally, we present the results of samples from a highway tunnel to characterize vehicle COS emissions and isotopic composition. The vehicle emissions were small, with COS/CO ₂ being 0.4 ppt/ppm; the isotopic signatures are depleted relatively to background atmospheric COS.

Keywords: atmosphere; biosphere; carbonyl sulfide; mass spectrometry; sulfur isotope.

Grants and funding

This project has received funding from the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation program under grant agreement No 742798 (COS-OCS; to M. C. Krol) and by Japan Society for the Promotion of Science KAKENHI Grants 20J01445 (K.K.), JP17H06105 (N.Y. and S.H.), and JP20H01975 (S.H.) under the Ministry of Education, Culture, Sports, Science and Technology, Japan.