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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>9</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acp-9-1479-2009</doi>
	<article_url>http://www.atmos-chem-phys.net/9/1479/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/9/1479/2009/acp-9-1479-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/9/1479/2009/acp-9-1479-2009.pdf</fulltext_pdf>
	<start_page>1479</start_page>
	<end_page>1501</end_page>
	<publication_date>2009-02-23</publication_date>
	<article_title content_type="html">Isoprene photooxidation: new insights into the production of acids and organic nitrates</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>F. Paulot</name>
			<email>paulot@caltech.edu</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>J. D. Crounse</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>H. G. Kjaergaard</name>
		</author>
		<author numeration="4" affiliations="2,4">
			<name>J. H. Kroll</name>
		</author>
		<author numeration="5" affiliations="1,2">
			<name>J. H. Seinfeld</name>
		</author>
		<author numeration="6" affiliations="1,5">
			<name>P. O. Wennberg</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Environmental Science and Engineering, California Institute of Technology, Pasadena, CA, USA</affiliation>
		<affiliation numeration="2" content_type="html">Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA</affiliation>
		<affiliation numeration="3" content_type="html">Department of Chemistry, University of Otago, Dunedin, New Zealand</affiliation>
		<affiliation numeration="4" content_type="html">Center for Aerosol and Cloud Chemistry, Aerodyne Inc., Billerica, MA, USA</affiliation>
		<affiliation numeration="5" content_type="html">Division of Geophysical and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">We describe a nearly explicit chemical mechanism for isoprene photooxidation
guided by chamber studies that include time-resolved observation of an
extensive suite of volatile compounds. We provide new constraints on the
chemistry of the poorly-understood isoprene δ-hydroxy channels, which
account for more than one third of the total isoprene carbon flux and a
larger fraction of the nitrate yields. We show that the &lt;i&gt;cis&lt;/i&gt; branch
dominates the chemistry of the δ-hydroxy channel with less than 5% of
the carbon following the &lt;i&gt;trans&lt;/i&gt; branch. The modelled yield of
isoprene nitrates is 12&amp;plusmn3% with a large difference between the
δ and β branches. The oxidation of these nitrates releases about
50% of the NO&lt;sub&gt;x&lt;/sub&gt;. Methacrolein nitrates (modelled yield
&lt;u&gt;~&lt;/u&gt;15&amp;plusmn;3% from methacrolein) and methylvinylketone nitrates
(modelled yield &lt;u&gt;~&lt;/u&gt;11&amp;plusmn;3% yield from methylvinylketone) are also
observed. Propanone nitrate, produced with a yield of 1% from isoprene,
appears to be the longest-lived nitrate formed in the total oxidation of
isoprene. We find a large molar yield of formic acid and suggest a novel
mechanism leading to its formation from the organic nitrates. Finally, the
most important features of this mechanism are summarized in a condensed
scheme appropriate for use in global chemical transport models.</abstract>
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</article>

