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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-12-11415-2012</article-id>
<title-group>
<article-title>Particle hygroscopicity during atmospheric new particle formation events: implications for the chemical species contributing to particle growth</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wu</surname>
<given-names>Z.</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>Birmili</surname>
<given-names>W.</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>Poulain</surname>
<given-names>L.</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>Merkel</surname>
<given-names>M.</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>Fahlbusch</surname>
<given-names>B.</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>van Pinxteren</surname>
<given-names>D.</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>Herrmann</surname>
<given-names>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>Wiedensohler</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Leibniz Institute for Tropospheric Research, Permoserstraße 15, 04318 Leipzig, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>03</day>
<month>05</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>5</issue>
<fpage>11415</fpage>
<lpage>11443</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-discuss.net/12/11415/2012/acpd-12-11415-2012.html">This article is available from http://www.atmos-chem-phys-discuss.net/12/11415/2012/acpd-12-11415-2012.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/12/11415/2012/acpd-12-11415-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/12/11415/2012/acpd-12-11415-2012.pdf</self-uri>
<abstract>
<p>This study examines the hygroscopicity of newly formed particles (smaller than 50 nm in particle mobility diameter)
      during two atmospheric new particle formation events with and without clear growth process at mid-level mountain range in
      Central Germany based on HCCT field campaign. Particle hygroscopicity measurements show that the particle soluble fractions at
      the end of event for two events are, respectively 60% (45 nm particles for the event with clear growth) and 20%
      (30 nm particles for the event without clear growth), stressing that non-soluble organic compounds may play a key role
      in particle growth during new particle formation event. Such significant difference in particle hygroscopicity also suggests
      that the chemical species responsible for nucleation particle growth are considerably different between the two selected NPF
      events. During both events, the hygroscopicity of newly formed particles decreased with particle growth, indicating that more
      less-hygroscopic compounds contribute to the subsequent condensation in contrast to the earlier stage. Sulfuric acid was
      considered to be responsible of the NPF event and represent the highly hygroscopic compounds. However, calculation demonstrated
      that sulfuric acid condensation failed to fully explain the observed soluble fraction in the nucleation mode
      particles. Therefore, we hypothesize that some water-soluble matters may explain the missing soluble fraction.</p>
</abstract>
<counts><page-count count="29"/></counts>
</article-meta>
</front>
<body/>
<back>
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