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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-6-787-2006</article-id>
<title-group>
<article-title>Cluster activation theory as an explanation of the linear dependence between formation rate of 3nm particles and sulphuric acid concentration</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kulmala</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>Lehtinen</surname>
<given-names>K. E. J.</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>Laaksonen</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>University of Helsinki, Department of Physical Sciences, P.O. Box 64, FIN-00014 Helsinki, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Finnish Meteorological Institute and University of Kuopio, Department of Applied Physics, P.O.Box 1627, FIN-70211 Kuopio, Finland</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>University of Kuopio, Department of Applied Physics, P.O.Box 1627, FIN-70211 Kuopio, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>10</day>
<month>03</month>
<year>2006</year>
</pub-date>
<volume>6</volume>
<issue>3</issue>
<fpage>787</fpage>
<lpage>793</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/6/787/2006/acp-6-787-2006.html">This article is available from http://www.atmos-chem-phys.net/6/787/2006/acp-6-787-2006.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/6/787/2006/acp-6-787-2006.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/6/787/2006/acp-6-787-2006.pdf</self-uri>
<abstract>
<p>According to atmospheric observations new particle formation seems to be a
function of sulphuric acid concentration to the power from one to two. The
nucleation theorem then predicts that the critical cluster contains one to
two sulphuric acid molecules. However, existing nucleation theories predicts
that the power is more (or equal) than 2. Here we present an activation
theory, which can explain the observed slope. In cluster activation the
clusters containing one sulphuric acid molecule will activate for further
growth due to heterogeneous nucleation, heterogeneous chemical reactions
including polymerization or activation of soluble clusters. In the
activation process organic vapours are typically needed as condensing
agents.</p>
</abstract>
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</article-meta>
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