ClSO and ClSO2 photochemistry: Implications for the Venusian atmosphere.

J Chem Phys

Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, Pennsylvania 19104-6243, USA.

Published: July 2024

AI Article Synopsis

  • - The study used advanced computational methods to explore the electronic structure and properties of ClSOx (x = 1 and 2) isomers, revealing their equilibrium shapes and vibrational frequencies.
  • - It was found that ClSO is unstable under UV light below 280 nm, leading to reactions that produce atomic chlorine and sulfur dioxide (SO2), rather than diatomic ClS.
  • - The research identified a new weakly bound Cl-SO2 isomer and discussed its implications for reactions in Venus's atmosphere, suggesting links to the depletion of water (H2O) and SO2.

Article Abstract

The electronic structure and spectroscopy of ClSOx (x = 1 and 2) isomers were investigated using coupled cluster theory and multireference interaction methods. In this study, the equilibrium geometry and harmonic vibrational frequencies of these isomers in their ground electronic state were shown. Our analysis of the vertical excitation energy and potential energy surface showed the photochemical instability of ClSO for wavelengths below 280 nm. Furthermore, the photodissociation of ClSO was unlikely to cause the formation of diatomic ClS. At the same time, ClSO could form atomic chlorine and SO as a result of photodissociation through the repulsive states. In the case of ClSO2, a novel weakly bound Cl-SO2 isomer was identified, indicating the potential influences on the chlorine and SO2 reactions. The potential energy surface of the most stable ClSO2 isomer also indicated the potential production of SO2 in both its ground and excited states. In addition, the electronic spectrum of ClSO2 was predicted to be broad, with numerous significant peaks in the near-UV‒Vis range. Valuable new insights into the chemical role of chlorine and sulfur in Venus's atmosphere were provided, along with a discussion of a potential mechanism contributing to the H2O and SO2 depletion in Venus's atmosphere.

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http://dx.doi.org/10.1063/5.0218751DOI Listing

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