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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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-14-6677-2014</article-id>
<title-group>
<article-title>The impact of monoaromatic hydrocarbons on OH reactivity in the coastal UK boundary layer and free troposphere</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lidster</surname>
<given-names>R. T.</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>Hamilton</surname>
<given-names>J. F.</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>Lee</surname>
<given-names>J. D.</given-names>
<ext-link>https://orcid.org/0000-0001-5397-2872</ext-link>
</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>Lewis</surname>
<given-names>A. 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>Hopkins</surname>
<given-names>J. R.</given-names>
<ext-link>https://orcid.org/0000-0002-0447-2633</ext-link>
</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>Punjabi</surname>
<given-names>S.</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>Rickard</surname>
<given-names>A. 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 contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Young</surname>
<given-names>J. C.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>The Department of Chemistry, The University of York, Heslington, UK</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>National Centre for Atmospheric Science, University of York, Heslington, York, UK</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>School of Chemistry, University of Leeds, Leeds, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>02</day>
<month>07</month>
<year>2014</year>
</pub-date>
<volume>14</volume>
<issue>13</issue>
<fpage>6677</fpage>
<lpage>6693</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2014 R. T. Lidster et al.</copyright-statement>
<copyright-year>2014</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/articles/14/6677/2014/acp-14-6677-2014.html">This article is available from https://acp.copernicus.org/articles/14/6677/2014/acp-14-6677-2014.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/14/6677/2014/acp-14-6677-2014.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/14/6677/2014/acp-14-6677-2014.pdf</self-uri>
<abstract>
<p>Reaction with the hydroxyl radical (OH) is the dominant removal mechanism for
virtually all volatile organic compounds (VOCs) in the atmosphere; however,
it can be difficult to reconcile measured OH reactivity with known sinks.
Unresolved higher molecular weight VOCs contribute to OH sinks, of which
monoaromatics are potentially an important sub-class. A method based on
comprehensive two-dimensional gas chromatography coupled to time-of-flight
mass spectrometry (GC × GC-TOFMS) has been developed that extends
the degree with which larger VOCs can be individually speciated from whole
air samples (WAS). The technique showed excellent sensitivity, resolution and
good agreement with an established gas chromatography–flame 
ionisation (GC-FID) method, for compounds amenable to
analysis on both instruments. Measurements have been made of VOCs within the
UK east coast marine boundary layer and free troposphere, using samples
collected from five aircraft flights in winter 2011. Ten monoaromatic
compounds with an array of different alkyl ring substituents have been
quantified, in addition to the simple aromatics, benzene, toluene, ethyl
benzene and Σ&lt;i&gt;m&lt;/i&gt;- and &lt;i&gt;p&lt;/i&gt;-xylene. These additional
compounds were then included in constrained box model simulations of
atmospheric chemistry occurring at two UK rural and suburban field sites in
order to assess the potential impact of these larger monoaromatics species on
OH reactivity; they have been calculated to contribute an additional 2–6%
to the overall modelled OH loss rate, providing a maximum additional OH sink
of ~0.9 s&lt;sup&gt;−1&lt;/sup&gt;.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
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