Photochemistry of tropospheric CS2, a new chemical pathway
- 1Sophia University, Faculty of Science and Technology, Tokyo, Japan (liyuanzhe@eagle.sophia.ac.jp)
- 2Sophia University, Faculty of Science and Technology, Tokyo, Japan (kamezaki-k@sophia.ac.jp)
- 3Sophia University, Faculty of Science and Technology, Tokyo, Japan (sebastian.d@sophia.ac.jp)
Photochemistry of tropospheric CS2, a new chemical pathway
Yuanzhe Li1, Kazuki Kamezaki1 and Sebastian Danielache1
1 Faculty of Science and Technology, Sophia University
Abstract
Carbon disulfide (CS2) is an atmospheric trace gas and is mainly produced by anthropogenic emissions. Its oxidation end-products in the atmosphere are carbonyl sulfide (OCS) and sulfur dioxide (SO2). Therefore, CS2 indirectly contributes to the production of sulfate aerosol, which influences atmospheric radiative properties and stratospheric ozone depletion.
Current understanding suggests that the main sink of CS2 is the reaction with the OH radical which shares of 75-88% CS2 global removal (Khan et al., 2017). This reaction pathway generates an adduct SCSOH, followed by oxidation with O2 to form OCS and SO2. UV induced processes are usually considered irrelevant in the troposphere. Tropospheric CS2 photo-oxidation mechanism was first suggested by Wine et al. (1981). The CS2 UV-absorption spectrum has a strong absorption band (280-360 nm), which generates a photo-excited (CS2(3A2) often presented as CS2* state) fragment, which gets further oxidized by O2 to produce OCS and SO2. The solar flux spectrum in the troposphere satisfies conditions for a CS2 photo-excitation, enabling a potential CS2 photo-oxidation pathway in the troposphere.
In this study, CS2 photochemistry is revised and studied by a 1-D atmospheric model (PATMO) capable of handling photochemistry with a high-resolution spectrum. Simulated main reduced sulfur species (CS2, OCS and SO2) reproduce field measurements. Under strong light conditions, the CS2 photo-excitation reaction is followed by two CS2* excited state quenching reactions. The reaction rate r for the net CS2 photo-induced oxidation and CS2 + OH reactions at 1 km are 71 and 26 molecule cm-3 s-1 respectively. These results indicate that, under favorable light conditions photochemistry is a relevant tropospheric sink of CS2.
References
Khan, A., Razis, B., Gillespie, S., Percival, C., Shallcross, D., Global analysis of carbon disulfide (CS2) using the 3-D chemistry transport model STOCHEM, Aims Environ. Sci. 2017, 4, 484–501.
Wine, P. H., Chameides, W. L., Ravishankara, A. R., Potential role of CS2 photooxidation in tropospheric sulfur chemistry, Geophys. Res. Lett. 1981, 8, 543-546.
How to cite: Li, Y., Kamezaki, K., and Danielache, S.: Photochemistry of tropospheric CS2, a new chemical pathway, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-4062, https://doi.org/10.5194/egusphere-egu21-4062, 2021.