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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-5-3187-2005</article-id>
<title-group>
<article-title>On the effects of organic matter and sulphur-containing compounds on the CCN activation of combustion particles</article-title>
</title-group>
<contrib-group><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="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gysel</surname>
<given-names>M.</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>Vancassel</surname>
<given-names>X.</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>Hitzenberger</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Puxbaum</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Vrochticky</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Weingartner</surname>
<given-names>E.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Baltensperger</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</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="aff7">
<sup>7</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institut für Physik der Atmosphäre, DLR Oberpfaffenhofen, 82 234 Wessling, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>School of Earth, Atmospheric and Environmental Sciences, University of Manchester, P.O. Box 88, Manchester M60 1QD, UK</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Atmospheric, Oceanic and Planetary Physics, University of Oxford, Clarendon Laboratory, Parks Road, Oxford OX1 3PU, UK</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Institute for Experimental Physics, University of Vienna, Boltzmanngasse 5, 1090 Vienna, Austria</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Institute for Chemical Technologies and Analytics, Vienna University of Technology, Getreidemarkt 9/164UPA, 1060 Vienna, Austria</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Laboratory of Atmospheric Chemistry, Paul Scherrer Institute (PSI), 5232 Villigen, Switzerland</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Université Louis Pasteur, 28, rue Goethe, 67 000 Strasbourg, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>01</day>
<month>12</month>
<year>2005</year>
</pub-date>
<volume>5</volume>
<issue>12</issue>
<fpage>3187</fpage>
<lpage>3203</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/5/3187/2005/acp-5-3187-2005.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/5/3187/2005/acp-5-3187-2005.pdf</self-uri>
<abstract>
<p>The European PartEmis project (Measurement and prediction of
emissions of aerosols and gaseous precursors from gas turbine engines) was focussed on the characterisation and
quantification of exhaust emissions from a gas turbine engine. The
combustion aerosol characterisation included on-line measurements of mass
and number concentration, size distribution, mixing state, thermal stability
of internally mixed particles, hygroscopicity, cloud condensation nuclei
(CCN) activation potential, and off-line analysis of chemical composition.
Based on this extensive data set, the role of sulphuric acid coating and of
the organic fraction of the combustion particles for the CCN activation was
investigated. Modelling of CCN activation was conducted using microphysical
and chemical properties obtained from the measurements as input data.
Coating the combustion particles with water-soluble sulphuric acid,
increases the potential CCN activation, or lowers the activation diameter,
respectively. The adaptation of a K&amp;#246;hler model to the experimental data
yielded coatings from 0.1 to 3 vol-% of water-soluble matter, which
corresponds to an increase in the fraction of CCN-activated combustion
particles from &amp;#x2264;10&lt;sup&gt;&amp;minus;4&lt;/sup&gt; to &amp;#x224C;10&lt;sup&gt;&amp;minus;2&lt;/sup&gt; at a water vapour
saturation ratio S&lt;sub&gt;w&lt;/sub&gt;=1.006. Additional particle coating by coagulation
of combustion particles and aqueous sulphuric acid particles formed by
nucleation further reduces the CCN activation diameter. In contrast,
particles containing a large fraction of non-volatile organic compounds grow
significantly less at high relative humidity than particles with a lower
content of non-volatile OC. The resulting reduction in the potential CCN
activation with an increasing fraction of non-volatile OC becomes visible as
a trend in the experimental data. While a coating of water-soluble sulphuric
acid increases the potential CCN activation, or lowers the activation
diameter, respectively, the non-volatile organic compounds, mainly found at
lower combustion temperatures, can partially compensate this sulphuric
acid-related enhancement of CCN activation of carbonaceous combustion
aerosol particles.</p>
</abstract>
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