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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-6-2465-2006</article-id>
<title-group>
<article-title>Cloud Condensation Nuclei properties of model and atmospheric HULIS</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Dinar</surname>
<given-names>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>Taraniuk</surname>
<given-names>I.</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>Graber</surname>
<given-names>E. 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>Katsman</surname>
<given-names>S.</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>Moise</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>Anttila</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mentel</surname>
<given-names>T. F.</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>Rudich</surname>
<given-names>Y.</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 Environmental Sciences, Weizmann Institute of Science, Rehovot 76100, Israel</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute of Soil, Water and Environmental Sciences, The Volcani Center, A.R.O., Bet Dagan 50250, Israel</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institute for Tropospheric Chemistry, Research Center Jülich, Jülich Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>current address: Research and Development, Finnish Meteorological Institute, 00101 Helsinki, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>29</day>
<month>06</month>
<year>2006</year>
</pub-date>
<volume>6</volume>
<issue>9</issue>
<fpage>2465</fpage>
<lpage>2482</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/6/2465/2006/acp-6-2465-2006.html">This article is available from http://www.atmos-chem-phys.net/6/2465/2006/acp-6-2465-2006.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/6/2465/2006/acp-6-2465-2006.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/6/2465/2006/acp-6-2465-2006.pdf</self-uri>
<abstract>
<p>Humic like substances (HULIS) have been identified as a major fraction of
the organic component of atmospheric aerosols. These large multifunctional
compounds of both primary and secondary sources are surface active and water
soluble. Hence, it is expected that they could affect activation of organic
aerosols into cloud droplets. We have compared the activation of aerosols
containing atmospheric HULIS extracted from fresh, aged and pollution
particles to activation of size fractionated fulvic acid from an aquatic
source (Suwannee River Fulvic Acid), and correlated it to the estimated
molecular weight and measured surface tension. A correlation was found
between CCN-activation diameter of SRFA fractions and number average
molecular weight of the fraction. The lower molecular weight fractions
activated at lower critical diameters, which is explained by the greater
number of solute species in the droplet with decreasing molecular weight.
The three aerosol-extracted HULIS samples activated at lower diameters than
any of the size-fractionated or bulk SRFA. The Köhler model was found to
account for activation diameters, provided that accurate physico-chemical
parameters are known.</p>
</abstract>
<counts><page-count count="18"/></counts>
</article-meta>
</front>
<body/>
<back>
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