Isoprene oxidation produces water-soluble organic gases capable of partitioning to aerosol liquid water. The formation of secondary organic aerosols through such aqueous pathways (aqSOA) can take place either reversibly or irreversibly; however, the split between these fractions in the atmosphere is highly uncertain. The aim of this study was to characterize the reversibility of aqSOA formed from isoprene at a location in the eastern United States under substantial influence from both anthropogenic and biogenic emissions. The reversible and irreversible uptake of water-soluble organic gases to aerosol water was characterized in Baltimore, MD using measurements of particulate water-soluble organic carbon (WSOC<sub>p</sub>) in alternating dry and ambient configurations. WSOC<sub>p</sub> evaporation with drying was observed systematically throughout the late spring and summer, indicating reversible aqSOA formation during these times. We show through time lag analyses that WSOCp concentrations, including the WSOC<sub>p</sub> that evaporates with drying, peak ~&thinsp;6&ndash;11&thinsp;h after isoprene concentrations, with maxima at a time lag of 9&thinsp;h. The absolute reversible aqSOA concentrations, as well as the relative amount of reversible aqSOA, increased with decreasing NO<sub><i>x</i></sub>/isoprene ratios, suggesting that isoprene epoxydiol (IEPOX) or other low-NO<sub><i>x</i></sub> oxidation products were responsible for these effects. The observed relationships with NO<sub><i>x</i></sub> and isoprene suggest that this process occurs widely in the atmosphere, and is likely more important in other locations characterized by higher isoprene and/or lower NO<sub><i>x</i></sub> levels. It is also likely that this phenomenon will increase in importance in the future, given predictions of biogenic and anthropogenic emissions under future regulatory and climate scenarios.
El-Sayed, M. M. H., Ortiz-Montalvo, D. L., & Hennigan, C. J. (2018). The effects of isoprene and NOx on secondary organic aerosols formed through reversible and irreversible uptake to aerosol water. Atmospheric Chemistry and Physics, 18(2), 1171–1184. https://doi.org/10.5194/acp-18-1171-2018