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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-9-5087-2009</article-id>
<title-group>
<article-title>Observational study of aerosol hygroscopic growth factors over rural area near Beijing mega-city</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pan</surname>
<given-names>X. L.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</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>Yan</surname>
<given-names>P.</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>Tang</surname>
<given-names>J.</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>Ma</surname>
<given-names>J. 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>Wang</surname>
<given-names>Z. F.</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>Gbaguidi</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Chinese Academy of Meteorological Science, China Meteorological Administration, Beijing, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Nansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Graduate University of Chinese Academy of Sciences, Beijing, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>25</day>
<month>02</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>1</issue>
<fpage>5087</fpage>
<lpage>5118</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/9/5087/2009/acpd-9-5087-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/9/5087/2009/acpd-9-5087-2009.pdf</self-uri>
<abstract>
<p>We investigated aerosol hygroscopic growth property and its influence on
scattering coefficient using M9003 nephelometers in coupling with a relative
humidity controlled inlet system at a rural site near Beijing mega-city
(Jingjintang) from 24th April to15th May 2006. Inlet relative humidity was
controlled in an increasing range of 40%–90% while the aerosol
hygroscopic growth factor, &lt;i&gt;f&lt;/i&gt;(RH=80%), varied in a range of 1.07–2.35
during the measurement. Estimated periodic mean values of aerosol
hygroscopic growth factors are 1.27–1.34, 1.17–1.23, 1.55–1.59 and 2.33–2.48
for clean, dust, urban pollution and mixed pollution periods respectively.
An examination of chemical composition of daily filter samples highlighted
that aerosol hygroscopicity was generally enhanced with the increasing ratio
of ammonium sulfate (AS) to organic matter (OMC). Furthermore, strong
hygroscopic organic aerosols were observed on 11th (&lt;i&gt;f&lt;/i&gt;(RH=80%)=2.23) and
15th (&lt;i&gt;f&lt;/i&gt;(RH=80%)=2.21) of May with organic carbon proportions of
PM&lt;sub&gt;2.1&lt;/sub&gt; reaching 42.3% and 43.0% respectively. Back-trajectory
analysis indicated that solar radiation and vertical convective movement
along the air mass pathway might strongly influence the hygroscopic
properties of organic matter.</p>
</abstract>
<counts><page-count count="32"/></counts>
</article-meta>
</front>
<body/>
<back>
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