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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-6-1733-2006</article-id>
<title-group>
<article-title>Sources and transformations of particle-bound polycyclic aromatic hydrocarbons in Mexico City</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Marr</surname>
<given-names>L. C.</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>Dzepina</surname>
<given-names>K.</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>Jimenez</surname>
<given-names>J. L.</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>Reisen</surname>
<given-names>F.</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>Bethel</surname>
<given-names>H. L.</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>Arey</surname>
<given-names>J.</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>Gaffney</surname>
<given-names>J. S.</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>Marley</surname>
<given-names>N. A.</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>Molina</surname>
<given-names>L. 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>Molina</surname>
<given-names>M. J.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Dept. of Civil and Environmental Engineering, Virginia Polytechnic Inst. and State Univ., Blacksburg, Virginia, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Dept. of Earth, Atmospheric, and Planetary Sciences, Massachusetts Inst. of Technology, Cambridge, Massachusetts, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Dept. of Chemistry and Biochemistry, and Cooperative Inst. for Research in Environmental Sciences (CIRES), Univ. of Colorado, Boulder, Colorado, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Air Pollution Research Center and Department of Environmental Sciences, Univ. of California, Riverside, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Argonne National Laboratory, Illinois, USA</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>now at: Dept. of Chemistry and Biochemistry, Univ. of California, San Diego, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>23</day>
<month>05</month>
<year>2006</year>
</pub-date>
<volume>6</volume>
<issue>6</issue>
<fpage>1733</fpage>
<lpage>1745</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/6/1733/2006/acp-6-1733-2006.html">This article is available from http://www.atmos-chem-phys.net/6/1733/2006/acp-6-1733-2006.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/6/1733/2006/acp-6-1733-2006.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/6/1733/2006/acp-6-1733-2006.pdf</self-uri>
<abstract>
<p>Understanding sources, concentrations, and transformations of polycyclic
aromatic hydrocarbons (PAHs) in the atmosphere is important because of their
potent mutagenicity and carcinogenicity. The measurement of particle-bound
PAHs by three different methods during the Mexico City Metropolitan Area
field campaign in April 2003 presents a unique opportunity for
characterization of these compounds and intercomparison of the methods. The three
methods are (1) collection and analysis of bulk samples for time-integrated
gas- and particle-phase speciation by gas chromatography/mass spectrometry;
(2) aerosol photoionization for fast detection of PAHs on particles&apos;
surfaces; and (3) aerosol mass spectrometry for fast analysis of size and
chemical composition. This research represents the first time aerosol mass
spectrometry has been used to measure ambient PAH concentrations and the
first time that fast, real-time methods have been used to quantify PAHs
alongside traditional filter-based measurements in an extended field
campaign. Speciated PAH measurements suggest that motor vehicles and garbage
and wood burning are important sources in Mexico City. The diurnal
concentration patterns captured by aerosol photoionization and aerosol mass
spectrometry are generally consistent. Ambient concentrations of particle-phase PAHs
typically peak at ~110 ng m&lt;sup&gt;-3&lt;/sup&gt; during the morning rush hour and rapidly
decay due to changes in source activity patterns and dilution as the boundary
layer rises, although surface-bound PAH concentrations decay faster. The
more rapid decrease in surface versus bulk PAH concentrations during the
late morning suggests that freshly emitted combustion-related particles are
quickly coated by secondary aerosol material in Mexico City&apos;s atmosphere and
may also be transformed by heterogeneous reactions.</p>
</abstract>
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