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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-12-1189-2012</article-id>
<title-group>
<article-title>Deposition nucleation on mineral dust particles: a  case against classical nucleation theory with the assumption of a single contact angle</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wheeler</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>Bertram</surname>
<given-names>A. K.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Chemistry, University of British Columbia, Vancouver,  BC V6T 1Z1, Canada</addr-line>
</aff>
<pub-date pub-type="epub">
<day>30</day>
<month>01</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>2</issue>
<fpage>1189</fpage>
<lpage>1201</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>Deposition nucleation on two mineral species, kaolinite and illite, was
studied using a flow cell coupled to an optical microscope. The results show
that the &lt;i&gt;S&lt;/i&gt;&lt;sub&gt;ice&lt;/sub&gt; conditions when ice first nucleated, defined as the
onset &lt;i&gt;S&lt;/i&gt;&lt;sub&gt;ice&lt;/sub&gt; (&lt;i&gt;S&lt;/i&gt;&lt;sub&gt;ice,onset&lt;/sub&gt;), is a strong function
of the surface area available for nucleation, varying from 100% to 125%
at temperatures between 242 and 239 K. The surface area dependent data could
not be described accurately using classical nucleation theory and the
assumption of a single contact angle (defined here as the single-α
model). These results suggest that caution should be applied when using
contact angles determined from &lt;i&gt;S&lt;/i&gt;&lt;sub&gt;ice,onset&lt;/sub&gt; data and the
single-α model. In contrast to the single-α model, the active
site model, the deterministic model, and a model with a distribution of
contact angles fit the data within experimental uncertainties. Parameters
from the fits to the data are presented.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
<back>
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