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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-7-3909-2007</article-id>
<title-group>
<article-title>Secondary organic aerosol formation from &lt;i&gt;m&lt;/i&gt;-xylene, toluene, and benzene</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ng</surname>
<given-names>N. 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>Kroll</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>Chan</surname>
<given-names>A. W. H.</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>Chhabra</surname>
<given-names>P. S.</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>Flagan</surname>
<given-names>R. 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>Seinfeld</surname>
<given-names>J. H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Departments of Chemical Engineering and Environmental Science and Engineering, California Institute of Technology, Pasadena, CA 91125, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>now at: Aerodyne Research, Inc. 45 Manning Road, Billerica, MA 01821, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>24</day>
<month>07</month>
<year>2007</year>
</pub-date>
<volume>7</volume>
<issue>14</issue>
<fpage>3909</fpage>
<lpage>3922</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/7/3909/2007/acp-7-3909-2007.html">This article is available from http://www.atmos-chem-phys.net/7/3909/2007/acp-7-3909-2007.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/7/3909/2007/acp-7-3909-2007.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/7/3909/2007/acp-7-3909-2007.pdf</self-uri>
<abstract>
<p>Secondary organic aerosol (SOA) formation from the photooxidation of
&lt;i&gt;m&lt;/i&gt;-xylene, toluene, and benzene is investigated in the Caltech environmental
chambers. Experiments are performed under two limiting NO&lt;sub&gt;x&lt;/sub&gt; conditions;
under high-NO&lt;sub&gt;x&lt;/sub&gt; conditions the peroxy radicals (RO&lt;sub&gt;2&lt;/sub&gt;) react only
with NO, while under low-NO&lt;sub&gt;x&lt;/sub&gt; conditions they react only with HO&lt;sub&gt;2&lt;/sub&gt;.
For all three aromatics studied (&lt;i&gt;m&lt;/i&gt;-xylene, toluene, and benzene), the SOA
yields (defined as the ratio of the mass of organic aerosol formed to the
mass of parent hydrocarbon reacted) under low-NO&lt;sub&gt;x&lt;/sub&gt; conditions
substantially exceed those under high-NO&lt;sub&gt;x&lt;/sub&gt; conditions, suggesting the
importance of peroxy radical chemistry in SOA formation. Under low-NO&lt;sub&gt;x&lt;/sub&gt;
conditions, the SOA yields for &lt;i&gt;m&lt;/i&gt;-xylene, toluene, and benzene are constant
(36%, 30%, and 37%, respectively), indicating that the SOA formed
is effectively nonvolatile under the range of &lt;i&gt;M&lt;sub&gt;o&lt;/sub&gt;&lt;/i&gt;(&gt;10 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;) studied. Under high-NO&lt;sub&gt;x&lt;/sub&gt; conditions, aerosol growth
occurs essentially immediately, even when NO concentration is high. The SOA
yield curves exhibit behavior similar to that observed by Odum et al.  (1996,
1997a, b), although the values are somewhat higher than in the earlier study.
The yields measured under high-NO&lt;sub&gt;x&lt;/sub&gt; conditions are higher than previous
measurements, suggesting a &quot;rate effect&quot; in SOA formation, in which SOA
yields are higher when the oxidation rate is faster. Experiments carried out
in the presence of acidic seed aerosol reveal no change of SOA yields from
the aromatics as compared with those using neutral seed aerosol.</p>
</abstract>
<counts><page-count count="14"/></counts>
</article-meta>
</front>
<body/>
<back>
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