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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-12-2809-2012</article-id>
<title-group>
<article-title>Reactions of H&lt;sup&gt;+&lt;/sup&gt;(pyridine)&lt;sub&gt;&lt;i&gt;m&lt;/i&gt;&lt;/sub&gt;(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;&lt;i&gt;n&lt;/i&gt;&lt;/sub&gt; and H&lt;sup&gt;+&lt;/sup&gt;(NH&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;1&lt;/sub&gt;(pyridine)&lt;sub&gt;&lt;i&gt;m&lt;/i&gt;&lt;/sub&gt;(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;&lt;i&gt;n&lt;/i&gt;&lt;/sub&gt; with NH&lt;sub&gt;3&lt;/sub&gt;: experiments and kinetic modelling</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ryding</surname>
<given-names>M. J.</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>Å. M. Jonsson</surname>
<given-names></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>Zatula</surname>
<given-names>A. S.</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>Andersson</surname>
<given-names>P. U.</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>Uggerud</surname>
<given-names>E.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Chemistry, Atmospheric Science, University of Gothenburg, 412 96 Göteborg, Sweden</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>IVL Swedish Environmental Research Institute Ltd., P.O. Box 5302, 400 14 Göteborg, Sweden</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Mass Spectrometry Laboratory and Centre for Theoretical and Computational Chemistry, Department of Chemistry, University of Oslo, P.O. Box 1033 Blindern, 0315 Oslo, Norway</addr-line>
</aff>
<pub-date pub-type="epub">
<day>16</day>
<month>03</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>6</issue>
<fpage>2809</fpage>
<lpage>2822</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/12/2809/2012/acp-12-2809-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/12/2809/2012/acp-12-2809-2012.pdf</self-uri>
<abstract>
<p>Reactions between pyridine containing water cluster ions,
H&lt;sup&gt;+&lt;/sup&gt;(pyridine)&lt;sub&gt;1&lt;/sub&gt;(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;&lt;i&gt;n&lt;/i&gt;&lt;/sub&gt;,
H&lt;sup&gt;+&lt;/sup&gt;(pyridine)&lt;sub&gt;2&lt;/sub&gt;(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;&lt;i&gt;n&lt;/i&gt;&lt;/sub&gt; and
H&lt;sup&gt;+&lt;/sup&gt;(NH&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;1&lt;/sub&gt;(pyridine)&lt;sub&gt;1&lt;/sub&gt;(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;&lt;i&gt;n&lt;/i&gt;&lt;/sub&gt; (&lt;i&gt;n&lt;/i&gt; up to 15) with
NH&lt;sub&gt;3&lt;/sub&gt; have been studied experimentally using a quadrupole time-of-flight
mass spectrometer. The product ions in the reaction between
H&lt;sup&gt;+&lt;/sup&gt;(pyridine)&lt;sub&gt;&lt;i&gt;m&lt;/i&gt;&lt;/sub&gt;(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;&lt;i&gt;n&lt;/i&gt;&lt;/sub&gt; (&lt;i&gt;m&lt;/i&gt; = 1 to 2) and NH&lt;sub&gt;3&lt;/sub&gt; have
been determined for the first time. It is found that the reaction mainly
leads to cluster ions of the form
H&lt;sup&gt;+&lt;/sup&gt;(NH&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;1&lt;/sub&gt;(pyridine)&lt;sub&gt;&lt;i&gt;m&lt;/i&gt;&lt;/sub&gt;(H&lt;sub&gt;2&lt;/sub&gt;O)&lt;sub&gt;&lt;i&gt;n-x&lt;/i&gt;&lt;/sub&gt;, with &lt;i&gt;x&lt;/i&gt; = 1 or 2
depending on the initial size of the reacting cluster ion. For a given number
of water molecules (from 5 to 15) in the cluster ion, rate coefficients are
found to be slightly lower than those for protonated pure water clusters
reacting with ammonia. The rate coefficients obtained from this study are
used in a kinetic cluster ion model under tropospheric conditions. The
disagreement between ambient ground level measurements and previous models
are discussed in relation to the results from our model and future
experimental directions are suggested.</p>
</abstract>
<counts><page-count count="14"/></counts>
</article-meta>
</front>
<body/>
<back>
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