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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-10-2663-2010</article-id>
<title-group>
<article-title>Molecular characterization of urban organic aerosol in tropical India: contributions of primary emissions and secondary photooxidation</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Fu</surname>
<given-names>P. Q.</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>Kawamura</surname>
<given-names>K.</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>Pavuluri</surname>
<given-names>C. 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>Swaminathan</surname>
<given-names>T.</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>Chen</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Low Temperature Science, Hokkaido University, Sapporo, 060-0819, Japan</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Chemical Engineering, Indian Institute of Technology Madras, Chennai, 600036, India</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 550002, China</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Graduate School of the Chinese Academy of Sciences, Beijing, 100039, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>19</day>
<month>03</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>6</issue>
<fpage>2663</fpage>
<lpage>2689</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/10/2663/2010/acp-10-2663-2010.html">This article is available from http://www.atmos-chem-phys.net/10/2663/2010/acp-10-2663-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/2663/2010/acp-10-2663-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/2663/2010/acp-10-2663-2010.pdf</self-uri>
<abstract>
<p>Organic molecular composition of PM&lt;sub&gt;10&lt;/sub&gt; samples, collected at Chennai in
tropical India, was studied using capillary gas chromatography/mass
spectrometry. Fourteen organic compound classes were detected in the
aerosols, including aliphatic lipids, sugar compounds, lignin products,
terpenoid biomarkers, sterols, aromatic acids, hydroxy-/polyacids, phthalate
esters, hopanes, Polycyclic Aromatic Hydrocarbons (PAHs), and photooxidation
products from biogenic Volatile Organic Compounds (VOCs). At daytime,
phthalate esters were found to be the most abundant compound class; however,
at nighttime, fatty acids were the dominant one. Di-(2-ethylhexyl)
phthalate, C&lt;sub&gt;16&lt;/sub&gt; fatty acid, and levoglucosan were identified as the most
abundant single compounds. The nighttime maxima of most organics in the
aerosols indicate a land/sea breeze effect in tropical India, although some
other factors such as local emissions and long-range transport may also
influence the composition of organic aerosols. However, biogenic VOC
oxidation products (e.g., 2-methyltetrols, pinic acid, 3-hydroxyglutaric
acid and β-caryophyllinic acid) showed diurnal patterns with daytime
maxima. Interestingly, terephthalic acid was maximized at nighttime, which
is different from those of phthalic and isophthalic acids. A positive
relation was found between 1,3,5-triphenylbenzene (a tracer for plastic
burning) and terephthalic acid, suggesting that the field burning of
municipal solid wastes including plastics is a significant source of
terephthalic acid. Organic compounds were further categorized into several
groups to clarify their sources. Fossil fuel combustion (24–43%) was
recognized as the most significant source for the total identified
compounds, followed by plastic emission (16–33%), secondary oxidation
(8.6–23%), and microbial/marine sources (7.2–17%). In contrast, the
contributions of terrestrial plant waxes (5.9–11%) and biomass burning
(4.2–6.4%) were relatively small. This study demonstrates that, in
addition to fossil fuel combustion and biomass burning, the open-burning of
plastics in urban area also contributes to the organic aerosols in South
Asia.</p>
</abstract>
<counts><page-count count="27"/></counts>
</article-meta>
</front>
<body/>
<back>
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