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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-11-2197-2011</article-id>
<title-group>
<article-title>Summer and winter variations of dicarboxylic acids, fatty acids and benzoic acid in PM&lt;sub&gt;2.5&lt;/sub&gt;  in Pearl Delta River Region, China</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ho</surname>
<given-names>K. F.</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>Ho</surname>
<given-names>S. S. H.</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>Lee</surname>
<given-names>S. C.</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>Kawamura</surname>
<given-names>K.</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>Zou</surname>
<given-names>S. C.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cao</surname>
<given-names>J. 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>Xu</surname>
<given-names>H. M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi&apos;an, 710075, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Research Center of Urban Environmental Technology and Management, Department of Civil and Structural Engineering, The Hong Kong Polytechnic University, Hung Hom, Kowloon, Hong Kong, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Division of Atmospheric Sciences, Desert Research Institute, Reno, NV 89512, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Institute of Low Temperature Science, Hokkaido University, Sapporo, Japan</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>School of Marine Sciences, Institute of Marine Science and Technology, Sun Yat-Sen University, Guangzhou, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>11</day>
<month>03</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>5</issue>
<fpage>2197</fpage>
<lpage>2208</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.net/11/2197/2011/acp-11-2197-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/2197/2011/acp-11-2197-2011.pdf</self-uri>
<abstract>
<p>Ground-based PM&lt;sub&gt;2.5&lt;/sub&gt; samples collected at four different sites in Pearl
River Delta region (PRD) during winter and summer (from 14 December 2006 to
28 January 2007 in winter and from 4 July to 9 August 2007 in summer)
were analyzed for 30 water-soluble organic species, including dicarboxylic
acids, ketocarboxylic acids and dicarbonyls, nine fatty acids, and benzoic
acid. Molecular distributions of dicarboxylic acids demonstrated that oxalic
acid (C&lt;sub&gt;2&lt;/sub&gt;) was the most abundant species followed by phthalic acid (Ph)
in PRD region. The concentrations of total dicarboxylic acids ranged from 99
to 1340 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, with an average of 438 ± 267 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; in PRD.
The concentrations of total ketocarboxylic acids ranged from 0.6 to 207 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; (43 ± 48 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; on average) while the concentrations of total &lt;i&gt;α&lt;/i&gt;-dicarbonyls, including glyoxal and methylglyoxal, ranged
from 0.2 to 89 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, with an average of 11 ± 18 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; in
PRD. The total quantified water-soluble compounds (TQWOC) (organic carbon)
accounted for 3.4 ± 2.2% of OC and 14.3 ± 10.3% of water-soluble
OC (WSOC). Hexadecanoic acid (C&lt;sub&gt;16:0&lt;/sub&gt;), octadecanoic acid (C&lt;sub&gt;18:0&lt;/sub&gt;)
and oleic acid (C&lt;sub&gt;18:1&lt;/sub&gt;) were the three most abundant fatty acids in PRD.
The distributions of fatty acids were characterized by a strong even carbon
number predominance with a maximum (C&lt;sub&gt;max&lt;/sub&gt;) at hexadecanoic acid
(C&lt;sub&gt;16:0&lt;/sub&gt;). Ratio of C&lt;sub&gt;18:1&lt;/sub&gt; to C&lt;sub&gt;18:0&lt;/sub&gt; acts as an indicator for
aerosol aging. In PRD, an average of C&lt;sub&gt;18:1&lt;/sub&gt;/C&lt;sub&gt;18:0&lt;/sub&gt; ratio was
0.53 ± 0.39, suggesting an enhanced photochemical degradation of
unsaturated fatty acid. Moreover, the concentrations of benzoic acid ranged
from 84 to 306 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, (165 ± 48 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; on average), which can
be emitted as primary pollutant from motor vehicles exhaust, or formed from
photochemical degradation of aromatic hydrocarbons. Seasonal variations of
the organic specie concentrations were found in the four sampling cities.
Higher concentrations of TQWOC were observed in winter (598 ± 321 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;) 
than in summer (372 ± 215 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;). However, the abundances
of TQWOC in OC mass were higher in summer (0.9–12.4%, 4.5 ± 2.7%
on average) than in winter (1.1–5.7, 2.5 ± 1.2% on average), being
consistent with enhanced secondary production of dicarboxylic acids in
warmer weather. Spatial variations of water-soluble dicarboxylic acids were
characterized by higher concentrations in Hong Kong and lower concentrations
in Guangzhou (GZ)/Zhaoqing (ZQ) during winter whereas the highest
concentrations were observed in GZ/ZQ during summer. These spatial and
seasonal distributions are consistent with photochemical production and the
subsequent accumulation under different meteorological conditions.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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