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Previous laboratory studies have suggested that sulfate radical addition to olefinic biogenic volatile organic compounds (BVOCs) is a potential formation mechanism for some organosulfates detected in ambient secondary organic aerosol (SOA). However, these studies propose conflicting reaction products, possibly because laboratory dissolved oxygen levels did not accurately reflect atmospheric conditions.
Download Hi-Res ImageDownload to MS-PowerPointCite This:Environ. Sci. Technol. Lett. 2020, XXXX, XXX Alix E. Rodowa Emerson Christie Emerson Christie Department of Environmental and Molecular Toxicology, Oregon State University, Corvallis, Oregon 97331, United States Jane Sedlak Jane Sedlak Department of Physics, University of Notre Dame, Notre Dame, Indiana 46556, United States Graham F.
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