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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-10-11401-2010</article-id>
<title-group>
<article-title>Composition of semi-volatile organic compounds in the urban atmosphere of Singapore: influence of biomass burning</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>He</surname>
<given-names>J.</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>Zielinska</surname>
<given-names>B.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Balasubramanian</surname>
<given-names>R.</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-group><aff id="aff1">
<label>1</label>
<addr-line>Singapore – Delft Water Alliance, Block E1, #08-25, 1 Engineering Drive 2, National University of Singapore,  Singapore 117576, Singapore</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Division of Environmental Science and Engineering, Block EA, #03-12, 9 Engineering Drive 1, National University of Singapore, Singapore 117576, Singapore</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Division of Atmospheric Sciences, Desert Research Institute, 2215 Raggio Parkway Reno, NV 89512-1095, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>01</day>
<month>12</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>23</issue>
<fpage>11401</fpage>
<lpage>11413</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/10/11401/2010/acp-10-11401-2010.html">This article is available from http://www.atmos-chem-phys.net/10/11401/2010/acp-10-11401-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/11401/2010/acp-10-11401-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/11401/2010/acp-10-11401-2010.pdf</self-uri>
<abstract>
<p>An intensive field study was conducted in the urban atmosphere of Singapore
to investigate the composition of organic compounds in both gaseous and
particulate phases during the period of August to early November 2006. 17
atmospheric samples were collected. These samples were subjected to
accelerated solvent extraction with a mixture of dichloromethane and acetone
and separated into functional group fractions for analyses by GC/MS. Over
180 organic compounds belonging to three major fractions (n-alkanes,
polycyclic aromatic hydrocarbons – PAHs, and polar organic compounds – POCs)
were identified and quantified. The characteristics and abundance of the
n-alkanes, PAHs, mono and dicarboxylic acids, methoxylated phenols and other
POCs were determined. The composition of these organic compounds fluctuated
temporally with most of them being relatively higher in October than those
in other months of the sampling period. 3-D backward air mass trajectory
analyses together with the carbon preference index (CPI), molecular
diagnostic ratios and molecular markers were used to investigate the origin
of organic species measured in this study. Based on these diagnostic tools,
the increased abundance of atmospheric organic species during October could
be attributed to the occurrence of regional smoke haze episodes due to
biomass burning in Indonesia. Among the POCs investigated, phthalic acid and
cis-pinonic acid were abundant during October 2006. These two acids showed
strong linear relationships with maximum daily ozone concentrations
throughout the entire sampling period. This correlation with ozone suggested
that the secondary aerosol constituents such as phthalic and cis-pinonic
acids were probably formed through O&lt;sub&gt;3&lt;/sub&gt;-induced photochemical
transformation.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
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