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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-10-29051-2010</article-id>
<title-group>
<article-title>Atmospheric homogeneous nucleation of H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; and H&lt;sub&gt;2&lt;/sub&gt;O</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Benson</surname>
<given-names>D. R.</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>Erupe</surname>
<given-names>M. E.</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>Yu</surname>
<given-names>J. 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>Markovich</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>Lee</surname>
<given-names>S.-H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Kent State University, Department of Chemistry, Kent, Ohio 44240, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>25</day>
<month>11</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>11</issue>
<fpage>29051</fpage>
<lpage>29073</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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<abstract>
<p>We report laboratory observations of H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; and H&lt;sub&gt;2&lt;/sub&gt;O
homogeneous nucleation made under atmospherically relevant conditions
([H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;] of 10&lt;sup&gt;6&lt;/sup&gt; â€“ 10&lt;sup&gt;7&lt;/sup&gt; cm&lt;sup&gt;âˆ’3&lt;/sup&gt; and 287 K). Our
observations show that nucleation takes place at [H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;] of
10&lt;sup&gt;6&lt;/sup&gt; â€“ 10&lt;sup&gt;7&lt;/sup&gt; cm&lt;sup&gt;âˆ’3&lt;/sup&gt;, as observed in the atmosphere. The slope of
nucleation rate (&lt;i&gt;J&lt;/i&gt;) vs. [H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;] ranges between 4â€“6, consistent
with thermodynamic predictions of neutral H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; clusters, but is
higher than those observed in the atmosphere. These results indicate that
ternary aerosol precursors are needed to reduce the slope to 1â€“2 in the
atmosphere. This study also discusses the effects of experimental parameters
on laboratory observation results, in order to properly interpret the
experimental data.</p>
</abstract>
<counts><page-count count="23"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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