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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-11-893-2011</article-id>
<title-group>
<article-title>Modeling secondary organic aerosol formation from isoprene oxidation under dry and humid conditions</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Couvidat</surname>
<given-names>F.</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>Seigneur</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>CEREA, Joint Laboratory Ècole des Ponts ParisTech/EDF R&amp;D, Université Paris-Est, 77455 Marne la Vallée, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>31</day>
<month>01</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>2</issue>
<fpage>893</fpage>
<lpage>909</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/11/893/2011/acp-11-893-2011.html">This article is available from http://www.atmos-chem-phys.net/11/893/2011/acp-11-893-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/893/2011/acp-11-893-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/893/2011/acp-11-893-2011.pdf</self-uri>
<abstract>
<p>A new model for the formation of secondary organic aerosol (SOA)
 from isoprene was developed. This model uses surrogate molecular
  species (hydroxy-hydroperoxides, tetrols, methylglyceric acid,
  organic nitrates) to represent SOA formation. The development
  of this model used available experimental data on yields and
  molecular composition of SOA from isoprene and methacrolein
   oxidation. This model reproduces the amount of particles measured
   in smog chambers under both low-NO&lt;sub&gt;x&lt;/sub&gt; and high-NO&lt;sub&gt;x&lt;/sub&gt;
   conditions. Under low-NO&lt;sub&gt;x&lt;/sub&gt; conditions, the model reproduces the
   transitional formation of hydroxy-hydroperoxides particles, which are photolyzed
   and lead to SOA mass decrease after reaching a maximum. Under high-NO&lt;sub&gt;x&lt;/sub&gt;
   conditions, particles are assumed to be formed mostly from the photo-oxidation of a
    PAN-type molecule derived from methacrolein (MPAN). This model successfully reproduces
     the complex NO&lt;sub&gt;x&lt;/sub&gt;-dependence of isoprene oxidation and suggests a possible
      yield increase under some high-NO&lt;sub&gt;x&lt;/sub&gt; conditions. Experimental data correspond
      to dry conditions (RH &lt; 10%). However, particles formed from
      isoprene are expected to be highly hydrophilic, and isoprene
      oxidation products would likely partition between an aqueous
      phase and the gas phase at high humidity in the atmosphere.
      The model was extended to take into account the hydrophilic
      properties of SOA, which are relevant under atmospheric conditions,
      and investigate the effect of particulate liquid water on SOA
       formation. An important increase in SOA mass was estimated
       for humid conditions due to the hydrophilic properties.
        Experiments under high relative humidity conditions should
         be conducted to confirm the results of this study, which
         have implications for SOA modeling.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
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