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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>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-10-23169-2010</article-id>
<title-group>
<article-title>Glycine in aerosol water droplets: a critical assessment of Köhler  theory by predicting surface tension from molecular dynamics simulations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Li</surname>
<given-names>X.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hede</surname>
<given-names>T.</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>Tu</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Leck</surname>
<given-names>C.</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>Ågren</surname>
<given-names>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>Department of Theoretical Chemistry, School of Biotechnology, Royal  Institute of Technology, 10691 Stockholm, Sweden</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Meteorology, Stockholm University, 10691 Stockholm, Sweden</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Laboratory for Advanced Materials and Institute of Fine Chemicals, East China  University of Science and Technology, Shanghai 200237, China</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>School of Science and Technology, Örebro University, 70182 Örebro,  Sweden</addr-line>
</aff>
<pub-date pub-type="epub">
<day>07</day>
<month>10</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>10</issue>
<fpage>23169</fpage>
<lpage>23196</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-discuss.net/10/23169/2010/acpd-10-23169-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/10/23169/2010/acpd-10-23169-2010.pdf</self-uri>
<abstract>
<p>Aerosol particles in the atmosphere are important participants in the
      formation of cloud droplets and have significant impact on cloud
      albedo and global climate. According to the Köhler theory which
      describes the nucleation and the equilibrium growth of cloud droplets,
      the surface tension of an aerosol droplet is one of the most important
      factors that determine the critical supersaturation of droplet
      activation. In this paper, with specific interest to remote marine
      aerosol, we predict the surface tension of aerosol droplets by
      performing molecular dynamics simulations on two model systems; the
      pure water droplets and glycine in water droplets. The curvature
      dependence of the surface tension is interpolated by a quadratic
      polynomial over the nano-sized droplets and the limiting case of
      a planar interface, so that the so-called Aitken mode particles which
      are critical for droplet formation could be covered and the Köhler
      equation could be improved by incorporating surface tension
      corrections.</p>
</abstract>
<counts><page-count count="28"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>