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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-7-2765-2007</article-id>
<title-group>
<article-title>Estimating the NH&lt;sub&gt;3&lt;/sub&gt;:H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; ratio of nucleating clusters in atmospheric conditions using quantum chemical methods</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kurtén</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>Torpo</surname>
<given-names>L.</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>Sundberg</surname>
<given-names>M. R.</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>Kerminen</surname>
<given-names>V.-M.</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>Vehkamäki</surname>
<given-names>H.</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>Kulmala</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Division of Atmospheric Sciences, Department of Physical Sciences, P.O. Box 64, FI-00014 University of Helsinki, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Laboratory of Inorganic Chemistry, Department of Chemistry, P.O. Box 55, FI-00014 University of Helsinki, Finland</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Finnish Meteorological Institute, Air Quality Research, Sahaajankatu 20 E, FI-00880 Helsinki, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>25</day>
<month>05</month>
<year>2007</year>
</pub-date>
<volume>7</volume>
<issue>10</issue>
<fpage>2765</fpage>
<lpage>2773</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/7/2765/2007/acp-7-2765-2007.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/7/2765/2007/acp-7-2765-2007.pdf</self-uri>
<abstract>
<p>We study the ammonia addition reactions of H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;&amp;middot;NH&lt;sub&gt;3&lt;/sub&gt;
molecular clusters containing up to four ammonia and two sulfuric acid
molecules using the ab initio method RI-MP2 (Resolution of Identity 2nd order
Møller-Plesset perturbation theory). Together with results from previous
studies, we use the computed values to estimate an upper limit for the
ammonia content of small atmospheric clusters, without having to explicitly
include water molecules in the quantum chemical simulations. Our results
indicate that the NH&lt;sub&gt;3&lt;/sub&gt;:H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; mole ratio of small molecular
clusters in typical atmospheric conditions is probably around 1:2. High
ammonia concentrations or low temperatures may lead to the formation of
ammonium bisulfate (1:1) clusters, but our results rule out the formation of
ammonium sulfate clusters (2:1) anywhere in the atmosphere. A sensitivity
analysis indicates that the qualitative conclusions of this study are not
affected even by relatively large errors in the calculation of electronic
energies or vibrational frequencies.</p>
</abstract>
<counts><page-count count="9"/></counts>
</article-meta>
</front>
<body/>
<back>
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