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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-4-439-2004</article-id>
<title-group>
<article-title>Volatile particles formation during PartEmis: a modelling study</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Vancassel</surname>
<given-names>X.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sorokin</surname>
<given-names>A.</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>Mirabel</surname>
<given-names>P.</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>Petzold</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wilson</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Centre de Géochimie de la Surface, Université Louis Pasteur, Strasbourg, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Central Institute for Aviation Motors, Moskow, Russia</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Deutsches Zentrum für Luft- und Raumfahrt, Oberpfaffenhofen, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>QinetiQ, Farnborough, UK</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>now at: Atmospheric, Oceanic and Planetary Physics, University of Oxford, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>03</month>
<year>2004</year>
</pub-date>
<volume>4</volume>
<issue>2</issue>
<fpage>439</fpage>
<lpage>447</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/4/439/2004/acp-4-439-2004.html">This article is available from http://www.atmos-chem-phys.net/4/439/2004/acp-4-439-2004.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/4/439/2004/acp-4-439-2004.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/4/439/2004/acp-4-439-2004.pdf</self-uri>
<abstract>
<p>A modelling study of the formation of volatile particles in a combustor exhaust has been
carried out in the frame of the PartEmis European project. A kinetic model has been used in
order to investigate nucleation efficiency of the H&lt;sub&gt;2&lt;/sub&gt;O-H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; binary mixture in the sampling
system. A value for the fraction &lt;IMG WIDTH=&quot;10&quot; HEIGHT=&quot;13&quot; ALIGN=&quot;BOTTOM&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-439-img1.gif&quot;  
 ALT=&quot;$varepsilon$&quot;&gt; of the fuel sulphur S(IV) converted into S(VI) has been
indirectly deduced from comparisons between model results and measurements. In the present
study, &lt;IMG WIDTH=&quot;10&quot; HEIGHT=&quot;13&quot; ALIGN=&quot;BOTTOM&quot; BORDER=&quot;0&quot;
   src=&quot;acp-4-439-img1.gif&quot;  
 ALT=&quot;$varepsilon$&quot;&gt; ranges between roughly 2.5% and 6%, depending on the combustor settings and on
the value assumed for the parameter describing sulphuric acid wall losses. Soot particles hygroscopicity has also been investigated as
their activation is a key parameter for contrail formation. Growth factors of monodisperse
particles exposed to high relative humidity (95%) have been calculated and compared with
experimental results. The modelling study confirms that the growth factor increases as the
soot particle size decreases.</p>
</abstract>
<counts><page-count count="9"/></counts>
</article-meta>
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