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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-10-7643-2010</article-id>
<title-group>
<article-title>Structure-activity relationships to estimate the effective Henry&apos;s law constants of organics of atmospheric interest</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Raventos-Duran</surname>
<given-names>T.</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>Camredon</surname>
<given-names>M.</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>Valorso</surname>
<given-names>R.</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>Mouchel-Vallon</surname>
<given-names>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>Aumont</surname>
<given-names>B.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>LISA, UMR CNRS/INSU 7583, Université Paris Est Créteil et  Université Paris Diderot, Institut Pierre Simon Laplace,  94010 Créteil Cedex, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>08</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>16</issue>
<fpage>7643</fpage>
<lpage>7654</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>
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<self-uri xlink:href="http://www.atmos-chem-phys.net/10/7643/2010/acp-10-7643-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/7643/2010/acp-10-7643-2010.pdf</self-uri>
<abstract>
<p>The Henry&apos;s law constant is a key property needed to address the multiphase
behaviour of organics in the atmosphere. Methods that can reliably predict
the values for the vast number of organic compounds of atmospheric interest
are therefore required. The effective Henry&apos;s law constant &lt;i&gt;H&lt;/i&gt;&lt;sup&gt;*&lt;/sup&gt; in air-water
systems at 298 K was compiled from literature for 488 organic compounds bearing
functional groups of atmospheric relevance. This data set was used to assess the
 reliability of the HENRYWIN bond contribution method and the SPARC approach for
  the determination of &lt;i&gt;H&lt;/i&gt;&lt;sup&gt;*&lt;/sup&gt;. Moreover, this data set was used to develop GROMHE,
   a new Structure Activity Relationship (SAR) based on a group contribution
    approach. These methods estimate log&lt;i&gt;H&lt;/i&gt;&lt;sup&gt;*&lt;/sup&gt; with a Root Mean Square Error
    (RMSE) of 0.38, 0.61, and 0.73 log units for GROMHE, SPARC and HENRYWIN
    respectively. The results show that for all these methods the reliability
    of the estimates decreases with increasing solubility. The main differences
    among these methods lie in &lt;i&gt;H&lt;/i&gt;&lt;sup&gt;*&lt;/sup&gt; prediction for compounds with &lt;i&gt;H&lt;/i&gt;&lt;sup&gt;*&lt;/sup&gt; greater
     than 10&lt;sup&gt;3&lt;/sup&gt; M atm&lt;sup&gt;&amp;minus;1&lt;/sup&gt;. For these compounds, the predicted values
      of log&lt;i&gt;H&lt;/i&gt;&lt;sup&gt;*&lt;/sup&gt; using GROMHE are more accurate (RMSE = 0.53) than the estimates from SPARC or HENRYWIN.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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