The effects of isoprene and NO<sub><i>x</i></sub> on secondary organic aerosols formed through reversible and irreversible uptake to aerosol water

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 atmospher...

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Main Authors: M. M. H. El-Sayed, D. L. Ortiz-Montalvo, C. J. Hennigan
Format: Article
Language:English
Published: Copernicus Publications 2018-01-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/18/1171/2018/acp-18-1171-2018.pdf
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spelling doaj-897a1d5ba8c84f03b438c1b4368e2da02020-11-25T00:18:59ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242018-01-01181171118410.5194/acp-18-1171-2018The effects of isoprene and NO<sub><i>x</i></sub> on secondary organic aerosols formed through reversible and irreversible uptake to aerosol waterM. M. H. El-Sayed0D. L. Ortiz-Montalvo1C. J. Hennigan2Department of Chemical, Biochemical and Environmental Engineering, University of Maryland, Baltimore County, Baltimore, MD, USANational Institute of Standards and Technology (NIST), Gaithersburg, MD, USADepartment of Chemical, Biochemical and Environmental Engineering, University of Maryland, Baltimore County, Baltimore, MD, USAIsoprene 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, Maryland, USA, 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 WSOC<sub>p</sub> concentrations, including the WSOC<sub>p</sub> that evaporates with drying, peak 6 to 11 h after isoprene concentrations, with maxima at a time lag of 9 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 may be 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. This work underscores the importance of accounting for both reversible and irreversible uptake of isoprene oxidation products to aqueous particles.https://www.atmos-chem-phys.net/18/1171/2018/acp-18-1171-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. M. H. El-Sayed
D. L. Ortiz-Montalvo
C. J. Hennigan
spellingShingle M. M. H. El-Sayed
D. L. Ortiz-Montalvo
C. J. Hennigan
The effects of isoprene and NO<sub><i>x</i></sub> on secondary organic aerosols formed through reversible and irreversible uptake to aerosol water
Atmospheric Chemistry and Physics
author_facet M. M. H. El-Sayed
D. L. Ortiz-Montalvo
C. J. Hennigan
author_sort M. M. H. El-Sayed
title The effects of isoprene and NO<sub><i>x</i></sub> on secondary organic aerosols formed through reversible and irreversible uptake to aerosol water
title_short The effects of isoprene and NO<sub><i>x</i></sub> on secondary organic aerosols formed through reversible and irreversible uptake to aerosol water
title_full The effects of isoprene and NO<sub><i>x</i></sub> on secondary organic aerosols formed through reversible and irreversible uptake to aerosol water
title_fullStr The effects of isoprene and NO<sub><i>x</i></sub> on secondary organic aerosols formed through reversible and irreversible uptake to aerosol water
title_full_unstemmed The effects of isoprene and NO<sub><i>x</i></sub> on secondary organic aerosols formed through reversible and irreversible uptake to aerosol water
title_sort effects of isoprene and no<sub><i>x</i></sub> on secondary organic aerosols formed through reversible and irreversible uptake to aerosol water
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2018-01-01
description 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, Maryland, USA, 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 WSOC<sub>p</sub> concentrations, including the WSOC<sub>p</sub> that evaporates with drying, peak 6 to 11 h after isoprene concentrations, with maxima at a time lag of 9 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 may be 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. This work underscores the importance of accounting for both reversible and irreversible uptake of isoprene oxidation products to aqueous particles.
url https://www.atmos-chem-phys.net/18/1171/2018/acp-18-1171-2018.pdf
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