Molecular composition and volatility of multi-generation products formed from isoprene oxidation by nitrate radical
<p>Isoprene oxidation by nitrate radical (NO<span class="inline-formula"><sub>3</sub></span>) is a potentially important source of secondary organic aerosol (SOA). It is suggested that the second or later-generation products are the more substantial contributo...
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2021-07-01
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Series: | Atmospheric Chemistry and Physics |
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record_format |
Article |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
R. Wu R. Wu L. Vereecken E. Tsiligiannis S. Kang S. R. Albrecht S. R. Albrecht L. Hantschke D. Zhao A. Novelli H. Fuchs R. Tillmann T. Hohaus P. T. M. Carlsson J. Shenolikar F. Bernard J. N. Crowley J. L. Fry B. Brownwood J. A. Thornton S. S. Brown S. S. Brown A. Kiendler-Scharr A. Wahner M. Hallquist T. F. Mentel |
spellingShingle |
R. Wu R. Wu L. Vereecken E. Tsiligiannis S. Kang S. R. Albrecht S. R. Albrecht L. Hantschke D. Zhao A. Novelli H. Fuchs R. Tillmann T. Hohaus P. T. M. Carlsson J. Shenolikar F. Bernard J. N. Crowley J. L. Fry B. Brownwood J. A. Thornton S. S. Brown S. S. Brown A. Kiendler-Scharr A. Wahner M. Hallquist T. F. Mentel Molecular composition and volatility of multi-generation products formed from isoprene oxidation by nitrate radical Atmospheric Chemistry and Physics |
author_facet |
R. Wu R. Wu L. Vereecken E. Tsiligiannis S. Kang S. R. Albrecht S. R. Albrecht L. Hantschke D. Zhao A. Novelli H. Fuchs R. Tillmann T. Hohaus P. T. M. Carlsson J. Shenolikar F. Bernard J. N. Crowley J. L. Fry B. Brownwood J. A. Thornton S. S. Brown S. S. Brown A. Kiendler-Scharr A. Wahner M. Hallquist T. F. Mentel |
author_sort |
R. Wu |
title |
Molecular composition and volatility of multi-generation products formed from isoprene oxidation by nitrate radical |
title_short |
Molecular composition and volatility of multi-generation products formed from isoprene oxidation by nitrate radical |
title_full |
Molecular composition and volatility of multi-generation products formed from isoprene oxidation by nitrate radical |
title_fullStr |
Molecular composition and volatility of multi-generation products formed from isoprene oxidation by nitrate radical |
title_full_unstemmed |
Molecular composition and volatility of multi-generation products formed from isoprene oxidation by nitrate radical |
title_sort |
molecular composition and volatility of multi-generation products formed from isoprene oxidation by nitrate radical |
publisher |
Copernicus Publications |
series |
Atmospheric Chemistry and Physics |
issn |
1680-7316 1680-7324 |
publishDate |
2021-07-01 |
description |
<p>Isoprene oxidation by nitrate radical (NO<span class="inline-formula"><sub>3</sub></span>) is a potentially important
source of secondary organic aerosol (SOA). It is suggested that the second
or later-generation products are the more substantial contributors to SOA.
However, there are few studies investigating the multi-generation chemistry
of isoprene-NO<span class="inline-formula"><sub>3</sub></span> reaction, and information about the volatility of
different isoprene nitrates, which is essential to evaluate their potential
to form SOA and determine their atmospheric fate, is rare. In this work, we
studied the reaction between isoprene and NO<span class="inline-formula"><sub>3</sub></span> in the SAPHIR chamber
(Jülich) under near-atmospheric conditions. Various oxidation products
were measured by a high-resolution time-of-flight chemical ionization mass
spectrometer using Br<span class="inline-formula"><sup>−</sup></span> as the reagent ion. Most of the products
detected are organic nitrates, and they are grouped into monomers (C<span class="inline-formula"><sub>4</sub></span>
and C<span class="inline-formula"><sub>5</sub></span> products) and dimers (C<span class="inline-formula"><sub>10</sub></span> products) with 1–3 nitrate
groups according to their chemical composition. Most of the observed
products match expected termination products observed in previous studies,
but some compounds such as monomers and dimers with three nitrogen atoms
were rarely reported in the literature as gas-phase products from isoprene
oxidation by NO<span class="inline-formula"><sub>3</sub></span>. Possible formation mechanisms for these compounds are
proposed. The multi-generation chemistry of isoprene and NO<span class="inline-formula"><sub>3</sub></span> is
characterized by taking advantage of the time behavior of different
products. In addition, the vapor pressures of diverse isoprene nitrates are
calculated by different parametrization methods. An estimation of the vapor
pressure is also derived from their condensation behavior. According to our
results, isoprene monomers belong to intermediate-volatility or
semi-volatile organic compounds and thus have little effect on SOA
formation. In contrast, the dimers are expected to have low or extremely low
volatility, indicating that they are potentially substantial contributors to
SOA. However, the monomers constitute 80 % of the total<span id="page10800"/> explained signals
on average, while the dimers contribute less than 2 %, suggesting that the
contribution of isoprene NO<span class="inline-formula"><sub>3</sub></span> oxidation to SOA by condensation should be
low under atmospheric conditions. We expect a SOA mass yield of about 5 %
from the wall-loss- and dilution-corrected mass concentrations, assuming that
all of the isoprene dimers in the low- or extremely low-volatility organic
compound (LVOC or ELVOC) range will condense completely.</p> |
url |
https://acp.copernicus.org/articles/21/10799/2021/acp-21-10799-2021.pdf |
work_keys_str_mv |
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spelling |
doaj-a29616dd68cb43059fa1c97b0671fb952021-07-16T11:41:05ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242021-07-0121107991082410.5194/acp-21-10799-2021Molecular composition and volatility of multi-generation products formed from isoprene oxidation by nitrate radicalR. Wu0R. Wu1L. Vereecken2E. Tsiligiannis3S. Kang4S. R. Albrecht5S. R. Albrecht6L. Hantschke7D. Zhao8A. Novelli9H. Fuchs10R. Tillmann11T. Hohaus12P. T. M. Carlsson13J. Shenolikar14F. Bernard15J. N. Crowley16J. L. Fry17B. Brownwood18J. A. Thornton19S. S. Brown20S. S. Brown21A. Kiendler-Scharr22A. Wahner23M. Hallquist24T. F. Mentel25Institute of Energy and Climate Research, Troposphere (IEK-8), Forschungszentrum Jülich GmbH, 52428 Jülich, GermanyCollege of Environmental Sciences and Engineering, State Key Joint Laboratory of Environmental Simulation and Pollution Control, Peking University, 100871, Beijing, ChinaInstitute of Energy and Climate Research, Troposphere (IEK-8), Forschungszentrum Jülich GmbH, 52428 Jülich, GermanyDepartment of Chemistry and Molecular Biology, University of Gothenburg, 41296, Gothenburg, SwedenInstitute of Energy and Climate Research, Troposphere (IEK-8), Forschungszentrum Jülich GmbH, 52428 Jülich, GermanyInstitute of Energy and Climate Research, Troposphere (IEK-8), Forschungszentrum Jülich GmbH, 52428 Jülich, Germanypresent address: SOLIDpower GmbH, 52525 Heinsberg, GermanyInstitute of Energy and Climate Research, Troposphere (IEK-8), Forschungszentrum Jülich GmbH, 52428 Jülich, GermanyDepartment of Atmospheric and Oceanic Sciences & Institute of Atmospheric Sciences, Fudan University, 200438, Shanghai, ChinaInstitute of Energy and Climate Research, Troposphere (IEK-8), Forschungszentrum Jülich GmbH, 52428 Jülich, GermanyInstitute of Energy and Climate Research, Troposphere (IEK-8), Forschungszentrum Jülich GmbH, 52428 Jülich, GermanyInstitute of Energy and Climate Research, Troposphere (IEK-8), Forschungszentrum Jülich GmbH, 52428 Jülich, GermanyInstitute of Energy and Climate Research, Troposphere (IEK-8), Forschungszentrum Jülich GmbH, 52428 Jülich, GermanyInstitute of Energy and Climate Research, Troposphere (IEK-8), Forschungszentrum Jülich GmbH, 52428 Jülich, GermanyAtmospheric Chemistry Department, Max Planck Institut für Chemie, 55128 Mainz, GermanyInstitut de Combustion, Aérothermique, Réactivité et Environnement (ICARE), UPR CNRS, 45071 Orléans, FranceAtmospheric Chemistry Department, Max Planck Institut für Chemie, 55128 Mainz, GermanyDepartment of Chemistry, Reed College, Portland, OR 97202, USADepartment of Chemistry, Reed College, Portland, OR 97202, USADepartment of Atmospheric Sciences, University of Washington, Seattle, WA 98195, USANOAA Chemical Sciences Laboratory, Boulder, CO 80305, USADepartment of Chemistry, University of Colorado, Boulder, CO 80309, USAInstitute of Energy and Climate Research, Troposphere (IEK-8), Forschungszentrum Jülich GmbH, 52428 Jülich, GermanyInstitute of Energy and Climate Research, Troposphere (IEK-8), Forschungszentrum Jülich GmbH, 52428 Jülich, GermanyDepartment of Chemistry and Molecular Biology, University of Gothenburg, 41296, Gothenburg, SwedenInstitute of Energy and Climate Research, Troposphere (IEK-8), Forschungszentrum Jülich GmbH, 52428 Jülich, Germany<p>Isoprene oxidation by nitrate radical (NO<span class="inline-formula"><sub>3</sub></span>) is a potentially important source of secondary organic aerosol (SOA). It is suggested that the second or later-generation products are the more substantial contributors to SOA. However, there are few studies investigating the multi-generation chemistry of isoprene-NO<span class="inline-formula"><sub>3</sub></span> reaction, and information about the volatility of different isoprene nitrates, which is essential to evaluate their potential to form SOA and determine their atmospheric fate, is rare. In this work, we studied the reaction between isoprene and NO<span class="inline-formula"><sub>3</sub></span> in the SAPHIR chamber (Jülich) under near-atmospheric conditions. Various oxidation products were measured by a high-resolution time-of-flight chemical ionization mass spectrometer using Br<span class="inline-formula"><sup>−</sup></span> as the reagent ion. Most of the products detected are organic nitrates, and they are grouped into monomers (C<span class="inline-formula"><sub>4</sub></span> and C<span class="inline-formula"><sub>5</sub></span> products) and dimers (C<span class="inline-formula"><sub>10</sub></span> products) with 1–3 nitrate groups according to their chemical composition. Most of the observed products match expected termination products observed in previous studies, but some compounds such as monomers and dimers with three nitrogen atoms were rarely reported in the literature as gas-phase products from isoprene oxidation by NO<span class="inline-formula"><sub>3</sub></span>. Possible formation mechanisms for these compounds are proposed. The multi-generation chemistry of isoprene and NO<span class="inline-formula"><sub>3</sub></span> is characterized by taking advantage of the time behavior of different products. In addition, the vapor pressures of diverse isoprene nitrates are calculated by different parametrization methods. An estimation of the vapor pressure is also derived from their condensation behavior. According to our results, isoprene monomers belong to intermediate-volatility or semi-volatile organic compounds and thus have little effect on SOA formation. In contrast, the dimers are expected to have low or extremely low volatility, indicating that they are potentially substantial contributors to SOA. However, the monomers constitute 80 % of the total<span id="page10800"/> explained signals on average, while the dimers contribute less than 2 %, suggesting that the contribution of isoprene NO<span class="inline-formula"><sub>3</sub></span> oxidation to SOA by condensation should be low under atmospheric conditions. We expect a SOA mass yield of about 5 % from the wall-loss- and dilution-corrected mass concentrations, assuming that all of the isoprene dimers in the low- or extremely low-volatility organic compound (LVOC or ELVOC) range will condense completely.</p>https://acp.copernicus.org/articles/21/10799/2021/acp-21-10799-2021.pdf |