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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-10-4953-2010</article-id>
<title-group>
<article-title>The roles of sulfuric acid in new particle formation and growth in the mega-city of Beijing</article-title>
</title-group>
<contrib-group><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>Hu</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>Zhang</surname>
<given-names>R. Y.</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>Wang</surname>
<given-names>Z. 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>Zheng</surname>
<given-names>J.</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>Wu</surname>
<given-names>Z. J.</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>Wiedensohler</surname>
<given-names>A.</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>He</surname>
<given-names>L. 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>Huang</surname>
<given-names>X. F.</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>Zhu</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</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>Department of Atmospheric Science, Texas A&amp;M University, College Station, Texas 77843, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Leibniz Institute for Tropospheric Research, Permoserstrasse 15, Leipzig 04318, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Key Laboratory for Urban Habitat Environmental Science and Technology, Shenzhen Graduate School of Peking University, Shenzhen 518055, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>28</day>
<month>05</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>10</issue>
<fpage>4953</fpage>
<lpage>4960</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/10/4953/2010/acp-10-4953-2010.html">This article is available from http://www.atmos-chem-phys.net/10/4953/2010/acp-10-4953-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/4953/2010/acp-10-4953-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/4953/2010/acp-10-4953-2010.pdf</self-uri>
<abstract>
<p>Simultaneous measurements of gaseous sulfuric acid and particle number size
distributions were performed to investigate aerosol nucleation and growth
during CAREBeijing-2008. The analysis of the measured aerosols and sulfuric
acid with an aerosol dynamic model shows the dominant role of sulfuric acid
in new particle formation (NPF) process but also in the subsequent growth in
Beijing. Based on the data of twelve NPF events, the average formation rates
(2–13 cm&lt;sup&gt;−3&lt;/sup&gt; s&lt;sup&gt;−1&lt;/sup&gt;) show a linear correlation with the sulfuric acid
concentrations (&lt;i&gt;R&lt;/i&gt;&lt;sup&gt;2&lt;/sup&gt;=0.85). Coagulation seems to play a significant role
in reducing the number concentration of nucleation mode particles with the
ratio of the coagulation loss to formation rate being 0.41&amp;plusmn;0.16. The
apparent growth rates vary from 3 to 11 nm h&lt;sup&gt;−1&lt;/sup&gt;. Condensation of
sulfuric acid and its subsequent neutralization by ammonia and coagulation
contribute to the apparent particle growth on average 45&amp;plusmn;18% and
34&amp;plusmn;17%, respectively. The 30% higher concentration of sulfate
than organic compounds in particles during the seven sulfur-rich NPF events
but 20% lower concentration of sulfate during the five sulfur-poor type
suggest that organic compounds are an important contributor to the growth of
the freshly nucleated particles, especially during the sulfur-poor cases.</p>
</abstract>
<counts><page-count count="8"/></counts>
</article-meta>
</front>
<body/>
<back>
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