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Dryad

Photosensitized reactions of sulfate ions alter aerosol chemistry and climate effects

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Sep 18, 2026 version files 3.37 MB

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Abstract

Sulfate aerosols are ubiquitious in Earth’s atmosphere, driving air quality and climate impacts. The liquid water of sulfate aerosols can reach high ionic strength with low hydration. This special environment was recently shown to promote unexpected photochemical reactivity of the sulfate ions (HSO4–, SO42–) under tropospheric radiation, potentially through the formation of sulfur-centered free radicals. Yet, knowledge of the SO42– photochemistry is still insufficiently constrained, which hinders fundamental understanding and incorporation into computational models. This work provides direct spectroscopic evidence that sulfate solutions absorb surface-level sunlight and eject electrons, forming reactive sulfate radicals (SO4•–) in a concentration-dependent manner on a transient (< microsecond) timescale. Quantification of radical production rates at long timescales (hours) was performed via radical trapping coupled with liquid chromatography high-resolution mass spectrometry analyses. Once formed, SO4•– accelerate the oxidative processing of organic aerosol constituents, reshaping aerosol composition, size, and properties. We show that compounds emitted from biomass fires photosensitize the SO4•– production from sulfate up to a factor of 5, with rates comparable to hydroxyl radical production. This photosensitized chemistry alters the aerosol direct and indirect climate effects through formation of light-absorbing brown carbon (BrC) and cloud-activating organosulfates, respectively. In particular, the formation of secondary BrC transforms the negative radiative forcing of sulfate aerosols to positive.  These findings have important implications for aerosol oxidant budgets, sulfur cycle reactions, and model representations of aerosol-chemistry-climate interactions.