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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<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-12-10125-2012</article-id>
<title-group>
<article-title>Contributions of individual reactive biogenic volatile organic compounds to organic nitrates above a mixed forest</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pratt</surname>
<given-names>K. A.</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>Mielke</surname>
<given-names>L. H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff11">
<sup>11</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="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bryan</surname>
<given-names>A. M.</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>Steiner</surname>
<given-names>A. 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>Ortega</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
<xref ref-type="aff" rid="aff12">
<sup>12</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Daly</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
<xref ref-type="aff" rid="aff13">
<sup>13</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Helmig</surname>
<given-names>D.</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>Vogel</surname>
<given-names>C. S.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Griffith</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Dusanter</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Stevens</surname>
<given-names>P. S.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
<xref ref-type="aff" rid="aff10">
<sup>10</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Alaghmand</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Chemistry, Purdue University, West Lafayette, IN, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, IN, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Purdue Climate Change Research Center, Purdue University, West Lafayette, IN, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Atmospheric, Oceanic and Space Sciences, University of Michigan, Ann Arbor, MI, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO, USA</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>University of Michigan Biological Station, Pellston, MI, USA</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>School of Public and Environmental Affairs, Indiana University, Bloomington, IN, USA</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Université Lille Nord de France, Lille, France</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>École des Mines de Douai, Douai, France</addr-line>
</aff>
<aff id="aff10">
<label>10</label>
<addr-line>Department of Chemistry, Indiana University, Bloomington, IN, USA</addr-line>
</aff>
<aff id="aff11">
<label>11</label>
<addr-line>now at: School of Public and Environmental Affairs, Indiana University, Bloomington, IN, USA</addr-line>
</aff>
<aff id="aff12">
<label>12</label>
<addr-line>now at: Atmospheric Chemistry Division, Earth System Laboratory, National Center for Atmospheric Research,  Boulder, CO, USA</addr-line>
</aff>
<aff id="aff13">
<label>13</label>
<addr-line>now at: Air Pollution Prevention and Control Division, National Risk Management Research Laboratory, US Environmental Protection Agency, Research Triangle Park, NC, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>05</day>
<month>11</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>21</issue>
<fpage>10125</fpage>
<lpage>10143</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-chem-phys.net/12/10125/2012/acp-12-10125-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/12/10125/2012/acp-12-10125-2012.pdf</self-uri>
<abstract>
<p>Biogenic volatile organic compounds (BVOCs) can react in the atmosphere to
form organic nitrates, which serve as NO&lt;sub&gt;x&lt;/sub&gt; (NO + NO&lt;sub&gt;2&lt;/sub&gt;) reservoirs,
impacting ozone and secondary organic aerosol production, the oxidative
capacity of the atmosphere, and nitrogen availability to ecosystems. To
examine the contributions of biogenic emissions and the formation and fate
of organic nitrates in a forest environment, we simulated the oxidation of
57 individual BVOCs emitted from a rural mixed forest in northern Michigan.
Key BVOC-oxidant reactions were identified for future laboratory and field
investigations into reaction rate constants, yields, and speciation of
oxidation products. Of the total simulated organic nitrates, monoterpenes
contributed ~70% in the early morning at ~12 m above the
forest canopy when isoprene emissions were low. In the afternoon, when
vertical mixing and isoprene nitrate production were highest, the simulated
contribution of isoprene-derived organic nitrates was greater than 90% at
all altitudes, with the concentration of secondary isoprene nitrates
increasing with altitude. Notably, reaction of isoprene with NO&lt;sub&gt;3&lt;/sub&gt;
leading to isoprene nitrate formation was found to be significant (~8% 
of primary organic nitrate production) during the daytime, and
monoterpene reactions with NO&lt;sub&gt;3&lt;/sub&gt; were simulated to comprise up 
to ~83% of primary organic nitrate production at night. Lastly, forest
succession, wherein aspen trees are being replaced by pine and maple trees,
was predicted to lead to increased afternoon concentrations of
monoterpene-derived organic nitrates. This further underscores the need to
understand the formation and fate of these species, which have different
chemical pathways and oxidation products compared to isoprene-derived
organic nitrates and can lead to secondary organic aerosol formation.</p>
</abstract>
<counts><page-count count="19"/></counts>
</article-meta>
</front>
<body/>
<back>
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