Articles | Volume 17, issue 8
https://doi.org/10.5194/acp-17-5331-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-5331-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Secondary organic aerosol formation from in situ OH, O3, and NO3 oxidation of ambient forest air in an oxidation flow reactor
Brett B. Palm
Cooperative Institute for Research in Environmental Sciences,
University of Colorado, Boulder, CO, USA
Department of Chemistry and Biochemistry, University of Colorado, Boulder, CO, USA
Pedro Campuzano-Jost
Cooperative Institute for Research in Environmental Sciences,
University of Colorado, Boulder, CO, USA
Department of Chemistry and Biochemistry, University of Colorado, Boulder, CO, USA
Douglas A. Day
Cooperative Institute for Research in Environmental Sciences,
University of Colorado, Boulder, CO, USA
Department of Chemistry and Biochemistry, University of Colorado, Boulder, CO, USA
Amber M. Ortega
Cooperative Institute for Research in Environmental Sciences,
University of Colorado, Boulder, CO, USA
Department of Atmospheric and Oceanic Science, University of Colorado,
Boulder, CO, USA
now at: Air Pollution Control Division, Colorado Department of Public
Health and Environment, Denver, CO, USA
Juliane L. Fry
Department of Chemistry, Reed College, Portland, OR, USA
Steven S. Brown
Department of Chemistry and Biochemistry, University of Colorado, Boulder, CO, USA
NOAA Earth System Research Laboratory, Chemical Sciences Division,
Boulder, CO, USA
Kyle J. Zarzana
Cooperative Institute for Research in Environmental Sciences,
University of Colorado, Boulder, CO, USA
Department of Chemistry and Biochemistry, University of Colorado, Boulder, CO, USA
now at: NOAA Earth System Research Laboratory, Chemical Sciences Division,
Boulder, CO, USA
William Dube
Cooperative Institute for Research in Environmental Sciences,
University of Colorado, Boulder, CO, USA
NOAA Earth System Research Laboratory, Chemical Sciences Division,
Boulder, CO, USA
Nicholas L. Wagner
Cooperative Institute for Research in Environmental Sciences,
University of Colorado, Boulder, CO, USA
NOAA Earth System Research Laboratory, Chemical Sciences Division,
Boulder, CO, USA
Danielle C. Draper
Department of Chemistry, Reed College, Portland, OR, USA
now at: Department of Chemistry, University of California, Irvine,
USA
Lisa Kaser
Atmospheric Chemistry Observations & Modeling Laboratory, National
Center for Atmospheric Research, Boulder, CO, USA
Werner Jud
Institute of Ion Physics and Applied Physics, University of Innsbruck,
Austria
now at: Research Unit Environmental Simulation (EUS),
Institute of Biochemical Plant Pathology (BIOP), Helmholtz Zentrum
München GmbH, Oberschleißheim, Germany
Thomas Karl
Institute of Atmospheric and Cryospheric Sciences, University of
Innsbruck, Austria
Armin Hansel
Institute of Ion Physics and Applied Physics, University of Innsbruck,
Austria
Cándido Gutiérrez-Montes
Departamento de Ingeniería, Mecánica y Minera, Universidad de
Jaen, Jaen, Spain
Jose L. Jimenez
CORRESPONDING AUTHOR
Cooperative Institute for Research in Environmental Sciences,
University of Colorado, Boulder, CO, USA
Department of Chemistry and Biochemistry, University of Colorado, Boulder, CO, USA
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Latest update: 08 Oct 2024
Short summary
Ambient forest air was oxidized by OH, O3, or NO3 inside an oxidation flow reactor, leading to formation of particulate matter from any gaseous precursors found in the air. Closure was achieved between the amount of particulate mass formed from O3 and NO3 oxidation and the amount predicted from speciated gaseous precursors, which was in contrast to previous results for OH oxidation (Palm et al., 2016). Elemental analysis of the particulate mass formed in the reactor is presented.
Ambient forest air was oxidized by OH, O3, or NO3 inside an oxidation flow reactor, leading to...
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