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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-9-1431-2009</doi>
	<article_url>http://www.atmos-chem-phys.net/9/1431/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/9/1431/2009/acp-9-1431-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/9/1431/2009/acp-9-1431-2009.pdf</fulltext_pdf>
	<start_page>1431</start_page>
	<end_page>1449</end_page>
	<publication_date>2009-02-23</publication_date>
	<article_title content_type="html">Organic nitrate and secondary organic aerosol yield from NO&lt;sub&gt;3&lt;/sub&gt; oxidation of β-pinene evaluated using a gas-phase kinetics/aerosol partitioning model</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. L. Fry</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. Kiendler-Scharr</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>A. W. Rollins</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>P. J. Wooldridge</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>S. S. Brown</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>H. Fuchs</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>W. Dubé</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>A. Mensah</name>
		</author>
		<author numeration="9" affiliations="2">
			<name>M. dal Maso</name>
		</author>
		<author numeration="10" affiliations="2">
			<name>R. Tillmann</name>
		</author>
		<author numeration="11" affiliations="2">
			<name>H.-P. Dorn</name>
		</author>
		<author numeration="12" affiliations="2">
			<name>T. Brauers</name>
		</author>
		<author numeration="13" affiliations="1">
			<name>R. C. Cohen</name>
			<email>rccohen@berkeley.edu</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Chemistry, University of California, Berkeley, CA, USA</affiliation>
		<affiliation numeration="2" content_type="html">ICG-2: Troposphäre, Forschungszentrum Jülich, 52425 Jülich, Germany</affiliation>
		<affiliation numeration="3" content_type="html">Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The yields of organic nitrates and of secondary organic aerosol (SOA)
particle formation were measured for the reaction NO&lt;sub&gt;3&lt;/sub&gt;+β-pinene under
dry and humid conditions in the atmosphere simulation chamber SAPHIR at
Research Center Jülich. These experiments were conducted at low
concentrations of NO&lt;sub&gt;3&lt;/sub&gt; (NO&lt;sub&gt;3&lt;/sub&gt;+N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;&lt;10 ppb) and
β-pinene (peak~15 ppb), with no seed aerosol. SOA formation was
observed to be prompt and substantial (~50% mass yield under both
dry conditions and at 60% RH), and highly correlated with organic nitrate
formation. The observed gas/aerosol partitioning of organic nitrates can be
simulated using an absorptive partitioning model to derive an estimated
vapor pressure of the condensing nitrate species of &lt;i&gt;p&lt;/i&gt;&lt;sub&gt;vap&lt;/sub&gt;~5&amp;times;10&lt;sup&gt;&amp;minus;6&lt;/sup&gt; Torr
(6.67&amp;times;10&lt;sup&gt;&amp;minus;4&lt;/sup&gt; Pa), which constrains
speculation about the oxidation mechanism and chemical identity of the
organic nitrate. Once formed the SOA in this system continues to evolve,
resulting in measurable aerosol volume decrease with time. The observations
of high aerosol yield from NO&lt;sub&gt;x&lt;/sub&gt;-dependent oxidation of monoterpenes
provide an example of a significant &lt;i&gt;anthropogenic&lt;/i&gt; source of SOA from &lt;i&gt;biogenic&lt;/i&gt; hydrocarbon
precursors. Estimates of the NO&lt;sub&gt;3&lt;/sub&gt;+β-pinene SOA source strength for
California and the globe indicate that NO&lt;sub&gt;3&lt;/sub&gt; reactions with monoterpenes
are likely an important source (0.5–8% of the global total) of organic
aerosol on regional and global scales.</abstract>
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</article>

