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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-11-7301-2011</article-id>
<title-group>
<article-title>Secondary organic aerosol formation from the photooxidation of isoprene, 1,3-butadiene, and 2,3-dimethyl-1,3-butadiene under high NO&lt;sub&gt;x&lt;/sub&gt; conditions</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sato</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Nakao</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Clark</surname>
<given-names>C. H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Qi</surname>
<given-names>L.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cocker III</surname>
<given-names>D. R.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Bourns College of Engineering – Center for Environmental Research &amp; Technology, University of California, Riverside, 1084 Columbia Ave., Riverside, CA 92507, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Asian Environment Research Group, National Institute for Environmental Studies, 16-2 Onogawa, Tsukuba, Ibaraki, 305-8506, Japan</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Chemical and Environmental Engineering, University of California, Riverside, CA 92521, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>now at: Center for Regional Environmental Research, National Institute for Environmental Studies, 16-2 Onogawa, Tsukuba, Ibaraki, 305-8506, Japan</addr-line>
</aff>
<pub-date pub-type="epub">
<day>25</day>
<month>07</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>14</issue>
<fpage>7301</fpage>
<lpage>7317</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2011 K. Sato et al.</copyright-statement>
<copyright-year>2011</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/articles/11/7301/2011/acp-11-7301-2011.html">This article is available from https://acp.copernicus.org/articles/11/7301/2011/acp-11-7301-2011.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/11/7301/2011/acp-11-7301-2011.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/11/7301/2011/acp-11-7301-2011.pdf</self-uri>
<abstract>
<p>Secondary organic aerosol (SOA) formation from atmospheric oxidation of
isoprene has been the subject of multiple studies in recent years; however,
reactions of other conjugated dienes emitted from anthropogenic sources
remain poorly understood. SOA formation from the photooxidation of isoprene,
isoprene-1-&lt;sup&gt;13&lt;/sup&gt;C, 1,3-butadiene, and 2,3-dimethyl-1,3-butadiene is
investigated for high NO&lt;sub&gt;x&lt;/sub&gt; conditions. The SOA yield measured in the
1,3-butadiene/NO&lt;sub&gt;x&lt;/sub&gt;/H&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;2&lt;/sub&gt; irradiation system (0.089–0.178) was
close to or slightly higher than that measured with isoprene under similar
NO&lt;sub&gt;x&lt;/sub&gt; conditions (0.077–0.103), suggesting that the photooxidation of
1,3-butadiene is a possible source of SOA in urban air. In contrast, a very
small amount of SOA particles was produced in experiments with
2,3-dimethyl-1,3-butadiene. Off-line liquid chromatography – mass
spectrometry analysis revealed that the signals of oligoesters comprise a
major fraction (0.10–0.33) of the signals of the SOA products observed from
all dienes investigated. The oligoesters originate from the unsaturated
aldehyde gas phase diene reaction products; namely, semi-volatile compounds produced
by the oxidation of the unsaturated aldehyde undergo particle-phase
oligoester formation. Oligoesters produced by the dehydration reaction
between nitrooxypolyol and 2-methylglyceric acid monomer or its oligomer
were also characterized in these experiments with isoprene as the starting
diene. These oligomers are possible sources of the 2-methyltetrols found in
ambient aerosol samples collected under high NO&lt;sub&gt;x&lt;/sub&gt; conditions.
Furthermore, in low-temperature experiments also conducted in this study,
the SOA yield measured with isoprene at 278 K was 2–3 times as high as that
measured at 300 K under similar concentration conditions. Although
oligomerization plays an important role in SOA formation from isoprene
photooxidation, the observed temperature dependence of SOA yield is largely
explained by gas/particle partitioning of semi-volatile compounds.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
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