4.8 Article

Nonequilibrium Behavior in Isoprene Secondary Organic Aerosol

期刊

ENVIRONMENTAL SCIENCE & TECHNOLOGY
卷 57, 期 38, 页码 14182-14193

出版社

AMER CHEMICAL SOC
DOI: 10.1021/acs.est.3c03532

关键词

isoprene; secondary organicaerosol (SOA); equilibrium partitioning; diffusion limitations

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Recent studies have shown that the assumptions of instantaneous gas-particle equilibrium partitioning cannot accurately predict the formation of secondary organic aerosols (SOA), even at high humidity. This study investigates the minimum aging time scale required to observe nonequilibrium partitioning between the gas and aerosol phase. The results suggest that the equilibrium partitioning assumption breaks down after as short as 20 minutes of aging for isoprene SOA, even in the dark. Modeling and mass spectrometric analysis support the existence of a semisolid phase state and the observed nonequilibrium partitioning behavior.
Recent studies have shown that instantaneous gas-particle equilibrium partitioning assumptions fail to predict SOA formation, even at high relative humidity (similar to 85%), and photochemical aging seems to be one driving factor. In this study, we probe the minimum aging time scale required to observe nonequilibrium partitioning of semivolatile organic compounds (SVOCs) between the gas and aerosol phase at similar to 50% RH. Seed isoprene SOA is generated by photo-oxidation in the presence of effloresced ammonium sulfate seeds at <1 ppbv NOx, aged photochemically or in the dark for 0.3-6 h, and subsequently exposed to fresh isoprene SVOCs. Our results show that the equilibrium partitioning assumption is accurate for fresh isoprene SOA but breaks down after isoprene SOA has been aged for as short as 20 min even in the dark. Modeling results show that a semisolid SOA phase state is necessary to reproduce the observed particle size distribution evolution. The observed nonequilibrium partitioning behavior and inferred semisolid phase state are corroborated by offline mass spectrometric analysis on the bulk aerosol particles showing the formation of organosulfates and oligomers. The unexpected short time scale for the phase transition within isoprene SOA has important implications for the growth of atmospheric ultrafine particles to climate-relevant sizes.

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