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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>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-12-6489-2012</article-id>
<title-group>
<article-title>α-pinene photooxidation under controlled chemical conditions – Part 1:  Gas-phase composition in low- and high-NO&lt;sub&gt;x&lt;/sub&gt; environments</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Eddingsaas</surname>
<given-names>N. C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Loza</surname>
<given-names>C. L.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Yee</surname>
<given-names>L. D.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Seinfeld</surname>
<given-names>J. H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wennberg</surname>
<given-names>P. O.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Division of Chemistry and Chemical Engineering, California  Institute of Technology, Pasadena, CA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Division of Engineering  and Applied Science, California Institute of Technology, Pasadena, CA, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Division of Geological and Planetary Sciences, California Institute  of Technology,  Pasadena, CA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>25</day>
<month>07</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>14</issue>
<fpage>6489</fpage>
<lpage>6504</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys.net/12/6489/2012/acp-12-6489-2012.html">This article is available from http://www.atmos-chem-phys.net/12/6489/2012/acp-12-6489-2012.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/12/6489/2012/acp-12-6489-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/12/6489/2012/acp-12-6489-2012.pdf</self-uri>
<abstract>
<p>The OH oxidation of α-pinene under both low- and high-NO&lt;sub&gt;x&lt;/sub&gt;
environments was studied in the Caltech atmospheric chambers. Ozone was kept
low to ensure OH was the oxidant. The initial α-pinene concentration
was 20–50 ppb to ensure that the dominant peroxy radical pathway under
low-NO&lt;sub&gt;x&lt;/sub&gt; conditions is reaction with HO&lt;sub&gt;2&lt;/sub&gt;, produced from reaction
of OH with H&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;2&lt;/sub&gt;, and under high-NO&lt;sub&gt;x&lt;/sub&gt; conditions, reactions
with NO. Here we present the gas-phase results observed. Under low-NO&lt;sub&gt;x&lt;/sub&gt;
conditions the main first generation oxidation products are a number of
α-pinene hydroxy hydroperoxides and pinonaldehyde, accounting for over
40% of the yield. In all, 65–75% of the carbon can be accounted for in
the gas phase; this excludes first-generation products that enter the
particle phase. We suggest that pinonaldehyde forms from RO&lt;sub&gt;2&lt;/sub&gt; + HO&lt;sub&gt;2&lt;/sub&gt;
through an alkoxy radical channel that regenerates OH, a mechanism typically
associated with acyl peroxy radicals, not alkyl peroxy radicals. The OH
oxidation and photolysis of α-pinene hydroxy hydroperoxides leads to
further production of pinonaldehyde, resulting in total pinonaldehyde yield
from low-NO&lt;sub&gt;x&lt;/sub&gt; OH oxidation of ~33%. The low-NO&lt;sub&gt;x&lt;/sub&gt;
OH oxidation of pinonaldehyde produces a number of carboxylic acids and
peroxyacids known to be important secondary organic aerosol components. Under
high-NO&lt;sub&gt;x&lt;/sub&gt; conditions, pinonaldehyde was also found to be the major
first-generation OH oxidation product. The high-NO&lt;sub&gt;x&lt;/sub&gt; OH oxidation
of pinonaldehyde did not produce carboxylic acids and peroxyacids. A number
of organonitrates and peroxyacyl nitrates are observed and identified from
α-pinene and pinonaldehyde.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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