Photosensitized Degradation of DMSO Initiated by PAHs at the Air-Water Interface, as an Alternative Source of Organic Sulfur Compounds to the Atmosphere

The photochemical reactions of organic compounds at the water surface lead to the formation of gas-phase molecules that may contribute to new particle formation in the atmosphere. Here, we observe the formation of organic sulfur (OS) compounds that are known secondary organic aerosol (SOA) precursors, upon irradiation of aqueous solutions containing typical polycyclic aromatic hydrocarbons (PAHs) such as pyrene, fluoranthene, and phenanthrene as well as dimethylsulfoxide (DMSO). The reactivity between the excited triplet states of PAHs ((3)PAHs*) and DMSO was determined by transient absorption spectroscopy and a tentative reaction mechanism for DMSO degradation was proposed, supported by theoretical calculations of the reaction Gibbs energies. In all cases, we observe rapid formation of methanesulfonic acid, methanesulfinic acid, methylsulfonylmethane, ethyl methanesulfonate, hydroxymethanesulfonic acid, and 2-hydroxyethanesulfonic acid by use of novel membrane inlet-single photon ionization-time of flight mass spectrometry. These results suggest that ubiquitous PAHs and DMSO at the sea surface may represent an alternative source of OS compounds during daytime, through photochemical processes that should be considered in future models to better represent the SOA formation processes in the atmosphere.

Automated summary

Research has shown that photochemical reactions of organic compounds at the water surface can lead to the formation of organic sulfur (OS) compounds, potentially contributing to new particle formation in the atmosphere. Experiments demonstrated the behavior of typical polycyclic aromatic hydrocarbons (PAHs) and dimethylsulfoxide (DMSO) in aqueous solutions under irradiation, revealing a possible reaction mechanism.