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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>9</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-23955-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/23955/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/23955/2009/acpd-9-23955-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/23955/2009/acpd-9-23955-2009.pdf</fulltext_pdf>
	<start_page>23955</start_page>
	<end_page>23986</end_page>
	<publication_date>2009-11-11</publication_date>
	<article_title content_type="html">Size-resolved aerosol water-soluble ionic compositions in the summer of Beijing: implication of regional secondary formation</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. Guo</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>M. Hu</name>
			<email>minhu@pku.edu.cn</email>
		</author>
		<author numeration="3" affiliations="1">
			<name>Z. B. Wang</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. Slanina</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>Y. L. Zhao</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">State Key Joint Laboratory of Environmental Simulation and Pollution Control, College  of Environmental Sciences and Engineering, Peking University, 100871 Beijing, China</affiliation>
		<affiliation numeration="2" content_type="html">Department of Environmental Science, Policy and Management, University of California, 94720 Berkeley, CA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">To characterize aerosol pollution in Beijing, size-resolved aerosols
      were collected by MOUDIs during CAREBEIJING-2006 field campaign at
      Peking University (urban site) and Yufa (upwind rural site). Fine
      particle concentrations (PM&lt;sub&gt;1.8&lt;/sub&gt; by MOUDI) were
      99.8&amp;plusmn;77.4 &amp;mu;g/m&lt;sup&gt;3&lt;/sup&gt; and 78.2&amp;plusmn;58.4 &amp;mu;g/m&lt;sup&gt;3&lt;/sup&gt;, with PM&lt;sub&gt;1.8&lt;/sub&gt;/PM&lt;sub&gt;10&lt;/sub&gt; ratios of 0.64&amp;plusmn;0.08 and
      0.76&amp;plusmn;0.08 at PKU and Yufa, respectively, and secondary compounds
      accounted for more than 50% in fine particles. PMF model was used
      to resolve the particle modes. Three modes were resolved at Yufa,
      representing condensation, droplet and coarse mode. However, one more
      droplet mode with bigger size was resolved, which was considered
      probably from regional transport. Condensation mode accounted for
      10%–60% of the total mass at both sites, indicating it must be
      taken into account in summer. The formation of sulfate was mainly
      attributed to in-cloud or aerosol droplet process (PKU 80%, Yufa
      70%) and gas condensation process (PKU 14%, Yufa
      22%). According to the thermodynamic instability of
      NH&lt;sub&gt;4&lt;/sub&gt;NO&lt;sub&gt;3&lt;/sub&gt;, size distributions of nitrate were classified as
      three categories by RH. The existence of Ca(NO&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt; in droplet
      mode indicated the reaction of HNO&lt;sub&gt;3&lt;/sub&gt; with crustal particles was
      also important in fine particles. Linear regression gave a rough
      estimation that 69% of the PM&lt;sub&gt;10&lt;/sub&gt; and 87% of the PM&lt;sub&gt;1.8&lt;/sub&gt;
      at PKU were regional contributions. Sulfate, ammonium and oxalate were
      formed regionally, with the regional contributions of 90%, 87%
      and 95% to PM&lt;sub&gt;1.8&lt;/sub&gt;. Nitrate formation was local dominant. In
      summary regional secondary formation led to aerosol pollution in the
      summer of Beijing.</abstract>
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