Articles | Volume 18, issue 16
https://doi.org/10.5194/acp-18-12433-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-18-12433-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Constraining nucleation, condensation, and chemistry in oxidation flow reactors using size-distribution measurements and aerosol microphysical modeling
Anna L. Hodshire
CORRESPONDING AUTHOR
Department of Atmospheric Science, Colorado State University, Fort
Collins, CO 80523, USA
Brett B. Palm
Dept. of Chemistry and Cooperative Institute for Research in
Environmental Sciences (CIRES), University of Colorado, Boulder, CO 80309,
USA
now at: Department of Atmospheric Sciences, University of Washington,
Seattle, WA 98195, USA
M. Lizabeth Alexander
Environmental and Molecular Sciences Laboratory, Pacific Northwest
National Laboratory, Richland, WA 99352, USA
Qijing Bian
Department of Atmospheric Science, Colorado State University, Fort
Collins, CO 80523, USA
Pedro Campuzano-Jost
Dept. of Chemistry and Cooperative Institute for Research in
Environmental Sciences (CIRES), University of Colorado, Boulder, CO 80309,
USA
Eben S. Cross
Department of Civil and Environmental Engineering, Massachusetts
Institute of Technology, Cambridge, MA 02139, USA
now at: Center for Aerosol and Cloud Chemistry, Aerodyne Research,
Inc., Billerica, MA 01821, USA
Douglas A. Day
Dept. of Chemistry and Cooperative Institute for Research in
Environmental Sciences (CIRES), University of Colorado, Boulder, CO 80309,
USA
Suzane S. de Sá
School of Engineering and Applied Sciences, Harvard University,
Cambridge, MA 02138, USA
Alex B. Guenther
Department of Earth System Science, University of California, Irvine,
Irvine, CA 92697, USA
Division of Atmospheric Sciences & Global Change, Pacific Northwest
National Laboratory, Richland, WA 99352, USA
Armin Hansel
Institute of Ion and Applied Physics, University of Innsbruck,
Innsbruck, 6020, Austria
James F. Hunter
Department of Civil and Environmental Engineering, Massachusetts
Institute of Technology, Cambridge, MA 02139, USA
Werner Jud
Institute of Ion and Applied Physics, University of Innsbruck,
Innsbruck, 6020, Austria
now at: Institute of Biochemical Plant Pathology, Research Unit
Environmental Simulation, Helmholtz Zentrum München, Munich, 85764,
Germany
Thomas Karl
Institute for Atmospheric and Cryospheric Sciences, University of
Innsbruck, Innsbruck, 6020, Austria
Saewung Kim
Department of Earth System Science, University of California, Irvine,
Irvine, CA 92697, USA
Jesse H. Kroll
Environmental and Molecular Sciences Laboratory, Pacific Northwest
National Laboratory, Richland, WA 99352, USA
Department of Chemical Engineering, Massachusetts Institute of
Technology, Cambridge, MA 02139, USA
Jeong-Hoo Park
National Center for Atmospheric Research, Boulder, CO 80305, USA
now at: Climate and Air Quality Research Department, National Institute
of Environmental Research (NIER), Incheon, 22689, Republic of Korea
Dept. of Chemistry and Cooperative Institute for Research in
Environmental Sciences (CIRES), University of Colorado, Boulder, CO 80309,
USA
Roger Seco
Department of Earth System Science, University of California, Irvine,
Irvine, CA 92697, USA
James N. Smith
Department of Chemistry, University of California, Irvine, CA
92697, USA
Jose L. Jimenez
Dept. of Chemistry and Cooperative Institute for Research in
Environmental Sciences (CIRES), University of Colorado, Boulder, CO 80309,
USA
Jeffrey R. Pierce
Department of Atmospheric Science, Colorado State University, Fort
Collins, CO 80523, USA
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Latest update: 25 Nov 2025
Short summary
We investigate the nucleation and growth processes that shape the aerosol size distribution inside oxidation flow reactors (OFRs) that sampled ambient air from Colorado and the Amazon rainforest. Results indicate that organics are important for both nucleation and growth, vapor uptake was limited to accumulation-mode particles, fragmentation reactions were important to limit particle growth at higher OH exposures, and an H2SO4-organics nucleation mechanism captured new particle formation well.
We investigate the nucleation and growth processes that shape the aerosol size distribution...
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