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Carbonyl sulfide (COS) and carbon disulfide (CS) are volatile sulfur compounds that are critical precursors to sulfate aerosols, which enable climate cooling. COS and CS stem from the indirect photolysis of organic sulfur precursors in natural waters, but currently the chemistry behind how this occurs remains unclear. This study evaluated how different organic sulfur precursors, water quality constituents, which can form important reactive intermediates (RIs), and temperature affected COS and CS formation. Nine natural waters ranging in salinity were spiked with cysteine, cystine, dimethylsulfide (DMS), or methionine and exposed to simulated sunlight over varying times and water quality conditions. Results indicated that COS and CS formation increased up to 11× and 4×, respectively, after 12 h of sunlight, while diurnal cycling exhibited varied effects. COS and CS formation was also strongly affected by the DOC concentration, organic sulfur precursor type, O concentration, and temperature, while salinity differences and CO addition did not play a significant role. Overall, important factors in forming COS and CS were identified, which may ultimately impact their atmospheric concentrations.

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Sunlight photolysis of cysteine and dissolved organic matter (DOM) from freshwater to open ocean water sources generates carbonyl sulfide (COS) but not carbon disulfide (CS2).