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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-11-4505-2011</article-id>
<title-group>
<article-title>Detailed heterogeneous oxidation of soot surfaces in a particle-resolved aerosol model</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kaiser</surname>
<given-names>J. C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Riemer</surname>
<given-names>N.</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>Knopf</surname>
<given-names>D. A.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Physics and Astronomy, Stony Brook University, Stony Brook, NY, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Atmospheric Sciences, University of Illinois at Urbana-Champaign, Urbana, IL, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institute for Terrestrial and Planetary Atmospheres, School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, NY, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>currently at: Department of Physics and Astronomy, Universität Würzburg, Würzburg, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>12</day>
<month>05</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>9</issue>
<fpage>4505</fpage>
<lpage>4520</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/11/4505/2011/acp-11-4505-2011.html">This article is available from http://www.atmos-chem-phys.net/11/4505/2011/acp-11-4505-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/4505/2011/acp-11-4505-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/4505/2011/acp-11-4505-2011.pdf</self-uri>
<abstract>
<p>Using the particle-resolved aerosol model PartMC-MOSAIC, we simulate the
heterogeneous oxidation of a monolayer of polycyclic aromatic
hydrocarbons (PAHs) on soot particles in an urban atmosphere. We
focus on the interaction of the major atmospheric oxidants (O&lt;sub&gt;3&lt;/sub&gt;,
NO&lt;sub&gt;2&lt;/sub&gt;, OH, and NO&lt;sub&gt;3&lt;/sub&gt;) with PAHs and include competitive
co-adsorption of water vapour for a range of atmospheric conditions. For
the first time detailed heterogeneous chemistry based on the
Pöschl-Rudich-Ammann (PRA) framework is modelled on soot particles
with a realistic size distribution and a continuous range of chemical
ages. We find PAHs half-lives, &amp;tau;&lt;sub&gt;1/2&lt;/sub&gt;, on the order of seconds
during the night, when the PAHs are rapidly oxidised by the
gas-surface reaction with NO&lt;sub&gt;3&lt;/sub&gt;. During the day, &amp;tau;&lt;sub&gt;1/2&lt;/sub&gt; is
on the order of minutes and determined mostly by the surface layer
reaction of PAHs with adsorbed O&lt;sub&gt;3&lt;/sub&gt;. Such short half-lives of
surface-bound PAHs may lead to efficient conversion of hydrophobic
soot into more hygroscopic particles, thus increasing the particles&apos;
aerosol-cloud interaction potential. Despite its high reactivity OH
appears to have a negligible effect on PAH degradation which can be
explained by its very low concentration in the atmosphere. An increase
of relative humidity (RH) from 30 % to 80 % increases
PAH half-lives by up to 50 % for daytime degradation and
by up to 100 % or more for nighttime degradation. Uptake
coefficients, averaged over the particle population, are found to be
relatively constant over time for O&lt;sub&gt;3&lt;/sub&gt; (&amp;sim;2 &amp;times; 10&lt;sup&gt;&amp;minus;7&lt;/sup&gt; to
&amp;sim;2 &amp;times; 10&lt;sup&gt;&amp;minus;6&lt;/sup&gt;) and NO&lt;sub&gt;2&lt;/sub&gt; (&amp;sim;5 &amp;times; 10&lt;sup&gt;&amp;minus;6&lt;/sup&gt; to
&amp;sim;10&lt;sup&gt;&amp;minus;5&lt;/sup&gt;) at the different levels of NO&lt;sub&gt;x&lt;/sub&gt; emissions and RH
considered in this study. In contrast, those for OH and NO&lt;sub&gt;3&lt;/sub&gt;
depend strongly on the surface concentration of PAHs. We do not
find a significant influence of heterogeneous reactions on soot
particles on the gas phase composition. The derived half-lives of surface-bound PAHs and the time and particle population averaged
uptake coefficients for O&lt;sub&gt;3&lt;/sub&gt; and NO&lt;sub&gt;2&lt;/sub&gt; presented in this paper can be used as parameterisations for the
treatment of heterogeneous chemistry in large-scale atmospheric chemistry models.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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