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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-2-183-2002</article-id>
<title-group>
<article-title>New particle formation during &lt;font face=&quot;Symbol&quot;    &gt;a&lt;/font&gt;- and &lt;font face=&quot;Symbol&quot;    &gt;b&lt;/font&gt;-pinene oxidation by O&lt;sub&gt;3&lt;/sub&gt;, OH and NO&lt;sub&gt;3&lt;/sub&gt;, and the influence of water vapour: particle size distribution studies</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bonn</surname>
<given-names>B.</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>Moorgat</surname>
<given-names>G. K.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Max-Planck-Institute für Chemie, Atmospheric Chemistry Division, Mainz, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>31</day>
<month>07</month>
<year>2002</year>
</pub-date>
<volume>2</volume>
<issue>3</issue>
<fpage>183</fpage>
<lpage>196</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/2/183/2002/acp-2-183-2002.html">This article is available from http://www.atmos-chem-phys.net/2/183/2002/acp-2-183-2002.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/2/183/2002/acp-2-183-2002.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/2/183/2002/acp-2-183-2002.pdf</self-uri>
<abstract>
<p>New particle formation during the oxidation of

      

      &lt;font face=&quot;Symbol&quot;    &gt;a&lt;/font&gt;- and

      

      &lt;font face=&quot;Symbol&quot;    &gt;b&lt;/font&gt;-pinene
      (C&lt;sub&gt;10&lt;/sub&gt;H&lt;sub&gt;16&lt;/sub&gt;) by ozone, OH and NO&lt;sub&gt;3&lt;/sub&gt; was studied by measuring the particle size
      distributions with a scanning mobility particle sizer (TSI 3936). The results indicate a drastically higher nucleation potential of
      the ozonolysis than in the reaction with either OH or NO&lt;sub&gt;3&lt;/sub&gt;. On the contrary, the contribution of the individual
      oxidation reactions to form new aerosol volume was found to depend on the location of the carbon double bond to be oxidised: for the
      &lt;i&gt;endocyclic&lt;/i&gt; &lt;font face=&quot;Symbol&quot;    &gt;a&lt;/font&gt;-pinene reactions the ozonolysis
      contributed mostly to the aerosol volume yield, whereas for the &lt;i&gt;exocyclic&lt;/i&gt;&amp;nbsp;
      &lt;font face=&quot;Symbol&quot;    &gt;b&lt;/font&gt;-pinene reactions the oxidation
      by O&lt;sub&gt;3&lt;/sub&gt;, OH and NO&lt;sub&gt;3&lt;/sub&gt; yielded a similar aerosol volume.&lt;br&gt;
      &lt;br&gt;
      In a second part of this study the influence of water vapour on the nucleation in all three possible oxidation routes was
      examined. The observations revealed only an effect of water vapour during the ozonolysis reactions.</p>
</abstract>
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