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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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-13-3419-2013</article-id>
<title-group>
<article-title>Investigation of the connections between atmospheric new particle formation and organics at an urban site of Beijing</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wang</surname>
<given-names>Z. B.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hu</surname>
<given-names>M.</given-names>
<ext-link>https://orcid.org/0000-0003-4816-9123</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wu</surname>
<given-names>Z. J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Yue</surname>
<given-names>D. 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>Zheng</surname>
<given-names>J.</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>Zhang</surname>
<given-names>R. Y.</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>Pei</surname>
<given-names>X. 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>Paasonen</surname>
<given-names>P.</given-names>
<ext-link>https://orcid.org/0000-0002-4625-9590</ext-link>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Dal Maso</surname>
<given-names>M.</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>Boy</surname>
<given-names>M.</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>Wiedensohler</surname>
<given-names>A.</given-names>
<ext-link>https://orcid.org/0000-0001-8298-491X</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Leibniz Institute for Tropospheric Research, Permoserstr. 15, 04318 Leipzig, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Atmospheric Science, Texas A&amp;M University, College Station, Texas 77843, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Physics, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>International Institute for Applied Systems Analysis, Schlossplatz 1, 2361 Laxenburg, Austria</addr-line>
</aff>
<pub-date pub-type="epub">
<day>06</day>
<month>02</month>
<year>2013</year>
</pub-date>
<volume>13</volume>
<issue>2</issue>
<fpage>3419</fpage>
<lpage>3450</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 Z. B. Wang et al.</copyright-statement>
<copyright-year>2013</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/preprints/13/3419/2013/acpd-13-3419-2013.html">This article is available from https://acp.copernicus.org/preprints/13/3419/2013/acpd-13-3419-2013.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/preprints/13/3419/2013/acpd-13-3419-2013.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/preprints/13/3419/2013/acpd-13-3419-2013.pdf</self-uri>
<abstract>
<p>The role of low-volatility organic vapors in atmospheric new particle formation
      has been studied based on a data set of 17 nucleation      events observed during the CAREBeijing 2008 campaign. The particle
      formation rates show good correlations with sulfuric acid and organic
      vapors implying that both play an important role in the atmospheric new particle formation. High correlation coefficients are observed in all
      investigated nucleation mechanisms. The best fit (&lt;i&gt;R&lt;/i&gt; = 0.73,
      slope = 1.1) between the observed and modelled particle formation
      rates is achieved with the homogenous nucleation theory of sulfuric
      acid (both homomolecularly and hetermolecularly) with separate
      coefficients in
      &lt;i&gt;J=K&lt;/i&gt;&lt;sub&gt;SA1&lt;/sub&gt;[H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;]&lt;sup&gt;2&lt;/sup&gt;+&lt;i&gt;K&lt;/i&gt;&lt;sub&gt;SA2&lt;/sub&gt;[H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt;][Org]. The
      contributions of the sulfuric acid and the organics involving terms
      have been 43% and 57%, respectively. In addition, the higher particle
      formation rates are observed on polluted nucleation days, indicating the organic vapors should be involved in  the new particle formation process
in the polluted urban environment of Beijing with high background
      aerosol loading.</p>
</abstract>
<counts><page-count count="32"/></counts>
</article-meta>
</front>
<body/>
<back>
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