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<article language="en">
	<journal>
		<journal_title>Atmospheric Measurement Techniques Discussions</journal_title>
		<journal_url>www.atmos-meas-tech-discuss.net</journal_url>
		<eissn>1867-8610</eissn>
		<volume_number>1</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/amtd-1-401-2008</doi>
	<article_url>http://www.atmos-meas-tech-discuss.net/1/401/2008/</article_url>
	<abstract_html>http://www.atmos-meas-tech-discuss.net/1/401/2008/amtd-1-401-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech-discuss.net/1/401/2008/amtd-1-401-2008.pdf</fulltext_pdf>
	<start_page>401</start_page>
	<end_page>433</end_page>
	<publication_date>2008-12-04</publication_date>
	<article_title content_type="html">Measurement of atmospheric sesquiterpenes by proton transfer reaction-mass spectrometry (PTR-MS)</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>S. Kim</name>
			<email>saewung@ucar.edu</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>T. Karl</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>D. Helmig</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>R. Daly</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>R. Rasmussen</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>A. Guenther</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Advanced Study Program, National Center for Atmospheric Research, Boulder, CO, USA</affiliation>
		<affiliation numeration="2" content_type="html">Atmospheric Chemistry Division, National Center for Atmospheric Res., Boulder, CO, USA</affiliation>
		<affiliation numeration="3" content_type="html">Institute of Arctic and Alpine Research, University of Colorado, Boulder CO, USA</affiliation>
		<affiliation numeration="4" content_type="html">Oregon Graduate Institute, Beaverton, OR, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The ability to measure sesquiterpenes (SQT; C&lt;sub&gt;15&lt;/sub&gt;H&lt;sub&gt;24&lt;/sub&gt;) by a
Proton-Transfer-Reaction Mass Spectrometer (PTR-MS) was investigated with SQT
standards, prepared by a capillary diffusion method, and the estimated
mixing ratios, derived from the counts of product ions and proton transfer
reaction constants were intercompared with measured mixing ratios, measured
by a complementary Gas Chromatograph (GC) coupled to a Flame Ionization
Detector (GC-FID). Product ion distributions due to soft-ionization
occurring in a selected ion drift tube via proton transfer were measured as
a function of collision energies. Results after the consideration of the
mass discrimination of the PTR-MS system suggest that quantitative SQT
measurements within 20% accuracy can be achieved with PTR-MS if two
major product ions (&lt;i&gt;m/z&lt;/i&gt; 149&lt;sup&gt;+&lt;/sup&gt; and 205&lt;sup&gt;+&lt;/sup&gt;) out of seven major product
ions (&lt;i&gt;m/z&lt;/i&gt; 81&lt;sup&gt;+&lt;/sup&gt;, 95&lt;sup&gt;+&lt;/sup&gt;, 109&lt;sup&gt;+&lt;/sup&gt;, 123&lt;sup&gt;+&lt;/sup&gt;, 135&lt;sup&gt;+&lt;/sup&gt;, 149&lt;sup&gt;+&lt;/sup&gt; and
205&lt;sup&gt;+&lt;/sup&gt;) are accounted for. Bicyclic sesquiterpenes, i.e. β-caryophyllene and α-humulene, showed considerable fragmentation
causing the accuracy of their analysis to be reduced to 50% if only the
parent ion (&lt;i&gt;m/z&lt;/i&gt; 205) is considered. These findings were applied to a field
dataset collected above a deciduous forest at the PROPHET (Program for
Research on Oxidants: Photochemistry, Emissions, and Transport) research
station in 2005. Inferred Average daytime ecosystem scale mixing ratios
(fluxes) of isoprene, sum of monoterpenes (MT), and sum of SQT exhibited
values of 15 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; (4.5 mg m&lt;sup&gt;&amp;minus;2&lt;/sup&gt; h&lt;sup&gt;&amp;minus;1&lt;/sup&gt;), 1.2 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;
(0.21 mg m&lt;sup&gt;&amp;minus;2&lt;/sup&gt; h&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) and 0.0016 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; (0.10 mgm&lt;sup&gt;&amp;minus;2&lt;/sup&gt; h&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) respectively. A range of MT and SQT reactivities with
respect to the OH radical was calculated and compared to an earlier study
inferring significantly underestimated OH reactivities due to unknown
terpenes above this deciduous forest. The results indicate that MT and SQT
can resolve ~30% of missing OH reactivity, reported from this site.</abstract>
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</article>

