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<front>
<journal-meta>
<journal-id journal-id-type="publisher">AMTD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Measurement Techniques Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">AMTD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1867-8610</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/amtd-5-2703-2012</article-id>
<title-group>
<article-title>A disjunct eddy accumulation system for the measurement of BVOC fluxes:  instrument characterizations and field deployment</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Edwards</surname>
<given-names>G. D.</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>Martins</surname>
<given-names>D. K.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Starn</surname>
<given-names>T.</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>Pratt</surname>
<given-names>K.</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>Shepson</surname>
<given-names>P. B.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Chemistry, Eastern Michigan University, Ypsilanti, MI 48197, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Chemistry, Purdue University, West Lafayette, IN 47907, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Chemistry, West Chester University, West Chester, PA 19383, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Purdue Climate Change Research Center, Purdue University, West Lafayette, IN 47907, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>now at: Department of Meteorology, Pennsylvania State University, University Park, PA 16802, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>04</day>
<month>04</month>
<year>2012</year>
</pub-date>
<volume>5</volume>
<issue>2</issue>
<fpage>2703</fpage>
<lpage>2746</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>
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<self-uri xlink:href="http://www.atmos-meas-tech-discuss.net/5/2703/2012/amtd-5-2703-2012.pdf">The full text article is available as a PDF file from http://www.atmos-meas-tech-discuss.net/5/2703/2012/amtd-5-2703-2012.pdf</self-uri>
<abstract>
<p>Biological volatile organic compounds (BVOCs), such as isoprene and monoterpenes, are emitted in large amounts from
      forests. Quantification of the flux of BVOCs is critical in the evaluation of the impact of these compounds on the
      concentrations of atmospheric oxidants and on the production of secondary organic aerosol. A disjunct eddy accumulation (DEA)
      sampler system was constructed for the measurement of speciated BVOC fluxes. Unlike traditional eddy covariance (EC), the
      relatively new technique of disjunct sampling differs by taking short, discrete samples that allows for slower sampling
      frequencies. Disjunct sample airflow is directed into cartridges containing sorbent materials at sampling rates proportional to
      the magnitude of the vertical wind. Compounds accumulated on the cartridges are then quantified by thermal desorption and gas
      chromatography. Herein, we describe our initial tests to evaluate the disjunct sampler including the application of using
      vertical wind measurements to create optimized sampling thresholds. Measurements of BVOC fluxes obtained from DEA during its
      deployment above a mixed hardwood forest at the University of Michigan Biological Station (Pellston, MI) during the 2009
      CABINEX field campaign are reported. Daytime (09:00 a.m. to 05:00 p.m.) isoprene fluxes, when averaged over the footprint of
      the tower were 1.31 mg m&lt;sup&gt;&amp;minus;2&lt;/sup&gt; h&lt;sup&gt;&amp;minus;1&lt;/sup&gt; which is comparable to previous flux measurements at this location. Speciated
      monoterpene fluxes are some of the first to be reported from this site. Daytime averages were
      26.7 &amp;mu;g m&lt;sup&gt;&amp;minus;2&lt;/sup&gt; h&lt;sup&gt;&amp;minus;1&lt;/sup&gt; for &amp;alpha;-pinene and 10.6 &amp;mu;g m&lt;sup&gt;&amp;minus;2&lt;/sup&gt; h&lt;sup&gt;&amp;minus;1&lt;/sup&gt; for &amp;beta;-pinene. These
      measured concentrations and fluxes were compared to the output of an atmospheric chemistry model, and were found to be
      consistent with our knowledge of the variables that control BVOCs fluxes at this site.</p>
</abstract>
<counts><page-count count="44"/></counts>
</article-meta>
</front>
<body/>
<back>
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