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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>8</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-14643-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/14643/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/14643/2008/acpd-8-14643-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/14643/2008/acpd-8-14643-2008.pdf</fulltext_pdf>
	<start_page>14643</start_page>
	<end_page>14716</end_page>
	<publication_date>2008-07-31</publication_date>
	<article_title content_type="html">Isoprene photooxidation mechanism: resonance channels and implications for the production of nitrates and acids</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">Division 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
resonance 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 cis branch dominates the chemistry of the isoprene
resonance channel with less than 5% of the carbon following the trans branch. We find that the
yield of isoprene nitrates is approximately 11%. The oxidation of these nitrates releases
nearly 50% of the NO&lt;sub&gt;x&lt;/sub&gt;. Methacrolein nitrates (15% yield) and methylvinylketone nitrates
(10% yield) are also observed. Propanone nitrate is produced with a yield of 1% and
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 inclusion in global
chemical transport models.</abstract>
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</article>

