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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-9-5669-2009</article-id>
<title-group>
<article-title>Modeling of secondary organic aerosol yields from laboratory chamber data</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chan</surname>
<given-names>M. N.</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>Chan</surname>
<given-names>A. W. H.</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>Chhabra</surname>
<given-names>P. S.</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>Surratt</surname>
<given-names>J. 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-group><aff id="aff1">
<label>1</label>
<addr-line>Division of Engineering and Applied Science, California Institute of Technology, Pasadena, CA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>10</day>
<month>08</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>15</issue>
<fpage>5669</fpage>
<lpage>5680</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/9/5669/2009/acp-9-5669-2009.html">This article is available from http://www.atmos-chem-phys.net/9/5669/2009/acp-9-5669-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/9/5669/2009/acp-9-5669-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/9/5669/2009/acp-9-5669-2009.pdf</self-uri>
<abstract>
<p>Laboratory chamber data serve as the basis for constraining models of
secondary organic aerosol (SOA) formation. Current models fall into three
categories: empirical two-product (Odum), product-specific, and volatility
basis set. The product-specific and volatility basis set models are applied
here to represent laboratory data on the ozonolysis of α-pinene under
dry, dark, and low-NO&lt;sub&gt;x&lt;/sub&gt; conditions in the presence of ammonium sulfate
seed aerosol. Using five major identified products, the model is fit to the
chamber data. From the optimal fitting, SOA oxygen-to-carbon (O/C) and
hydrogen-to-carbon (H/C) ratios are modeled. The discrepancy between measured
H/C ratios and those based on the oxidation products used in the model
fitting suggests the potential importance of particle-phase reactions. Data
fitting is also carried out using the volatility basis set, wherein oxidation
products are parsed into volatility bins. The product-specific model is most
likely hindered by lack of explicit inclusion of particle-phase accretion
compounds. While prospects for identification of the majority of SOA products
for major volatile organic compounds (VOCs) classes remain promising, for the
near future empirical product or volatility basis set models remain the
approaches of choice.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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</back>
</article>