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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-9-16361-2009</article-id>
<title-group>
<article-title>Characteristics and source apportionment of atmospheric aerosols at the summit of Mount Tai during summertime</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Xu</surname>
<given-names>H.</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>Y.</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>Wen</surname>
<given-names>T.</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>Yang</surname>
<given-names>Y.</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>Zhao</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>LAPC, Institute of Atmospheric Physics, Chinese Academy of Sciences, 100029 Beijing, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Zhejiang Institute of Meteorological Sciences, 310017 Hangzhou, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>31</day>
<month>07</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>4</issue>
<fpage>16361</fpage>
<lpage>16379</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/9/16361/2009/acpd-9-16361-2009.html">This article is available from http://www.atmos-chem-phys-discuss.net/9/16361/2009/acpd-9-16361-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/9/16361/2009/acpd-9-16361-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/9/16361/2009/acpd-9-16361-2009.pdf</self-uri>
<abstract>
<p>To investigate the long-range transport of air pollutants in North China,
aerosol samples were collected at the summit of Mount Tai (Shandong
province) in June of 2006. Water-soluble ion and metal element
concentrations were analyzed using ion chromatography (IC) and inductively
coupled plasma-mass spectrometry (ICP-MS), respectively. Results showed
three different size distributions for the ions and metal elements
characterized, including masses in: (i) the accumulation mode, with a peak
at 0.43 to 1.1 μm (SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2&amp;minus;&lt;/sup&gt;, NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;, K&lt;sup&gt;+&lt;/sup&gt;, Pb, Zn,
Ti); (ii) the coarse particle mode, with a peak at 4.7 to 5.8 μm
(Ca&lt;sup&gt;2+&lt;/sup&gt;, Mg&lt;sup&gt;2+&lt;/sup&gt;, Ca, Mg, Fe, Al, Ba, Mn); and (iii) a bimodal
distribution, with peaks at 0.43 to 0.65 μm and 4.7 to 5.8 μm
(NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt;, Na&lt;sup&gt;+&lt;/sup&gt;, Cl&lt;sup&gt;&amp;minus;&lt;/sup&gt;, Na, Co, Ni, Mo, Cu). When
SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2&amp;minus;&lt;/sup&gt; was in high concentration, the mass median diameter was
between 0.5 μm and 0.8 μm, belonging to the &quot;drop mode&quot;. The
concentrations of SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2&amp;minus;&lt;/sup&gt;, NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt;, NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;, and
K&lt;sup&gt;+&lt;/sup&gt; were quite variable. Interestingly, SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2&amp;minus;&lt;/sup&gt;, NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt;,
and NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; reached their highest concentrations when the humid air
mass was coming from the south. Furthermore, crustal element concentrations
increased when the air mass came from the north and pollution
element concentrations were elevated when the air mass came from the south.</p>
</abstract>
<counts><page-count count="19"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>