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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>9</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-14315-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/14315/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/14315/2009/acpd-9-14315-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/14315/2009/acpd-9-14315-2009.pdf</fulltext_pdf>
	<start_page>14315</start_page>
	<end_page>14359</end_page>
	<publication_date>2009-07-01</publication_date>
	<article_title content_type="html">Determination of OM/OC ratios and specific attenuation coefficients (SAC) in ambient fine PM at a rural site in southern Ontario: implications for emission sources, particle aging, and radiative forcing</article_title>
	<authors>
		<author numeration="1" affiliations="1,4">
			<name>T. W. Chan</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>L. Huang</name>
			<email>lin.huang@ec.gc.ca</email>
		</author>
		<author numeration="3" affiliations="1">
			<name>W. R. Leaitch</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>S. Sharma</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>J. R. Brook</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>J. G. Slowik</name>
		</author>
		<author numeration="7" affiliations="2">
			<name>J. P. D. Abbatt</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>P. C. Brickell</name>
		</author>
		<author numeration="9" affiliations="1">
			<name>J. Liggio</name>
		</author>
		<author numeration="10" affiliations="1">
			<name>S.-M. Li</name>
		</author>
		<author numeration="11" affiliations="3">
			<name>H. Moosmüller</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">ATSD/STB, Environment Canada, 4905 Dufferin Street, Toronto, Ontario, M3H 5T4, Canada</affiliation>
		<affiliation numeration="2" content_type="html">Department of Chemistry, University of Toronto, Lash Miller Chemical Laboratories, 80 St. George Street, Toronto, Ontario, M5S 3H6, Canada</affiliation>
		<affiliation numeration="3" content_type="html">Division of Atmospheric Sciences, Desert Research Institute, 2215 Raggio Parkway, Reno, Nevada, 89512-1095, USA</affiliation>
		<affiliation numeration="4" content_type="html">now at: ASTD/STB, Environment Canada, 335 River Road, Ottawa, Ontario, K1A 0H3, Canada</affiliation>
	</affiliations>
	<abstract content_type="html">Ambient particulate matter (PM) samples were collected on quartz filters at
a rural site in southern Ontario during intensive studies in 2005 and 2007.
The concentrations of organic carbon (OC), pyrolysis organic carbon (POC),
and elemental carbon (EC) were determined by thermal analysis. These results
were compared to the organic aerosol mass concentration (OM) measured by an
Aerodyne Aerosol Mass Spectrometer (AMS) and to the particle absorption
coefficient (&lt;i&gt;b&lt;/i&gt;_asp) obtained from a Radiance Research Particle Soot
Absorption Photometer (PSAP). The total organic mass to organic carbon
ratios (OM/OC) and specific attenuation coefficients (SAC) were also
derived. According to the results, the POC mass is proportional to the
approximated oxygen mass in the aerosols and OM/OC ratios can be estimated
directly from thermal measurements. The study also suggests that the air
masses from the south, with relatively low OC/EC ratios, high EC, sulphate
contents and OM/OC ratios, were originated from urban and industrial
emissions and subsequently experienced photo-oxidations in the atmosphere,
implying that the oxygenated organics could come from both primary and
secondary sources. Whereas the air masses from the north, with relatively
high OC/EC ratios, low EC, sulphate contents and OM/OC ratios, were dominant
by the background clean air with relatively larger contributions from
biogenic emissions.
&lt;br&gt;&lt;br&gt;

The mean SAC derived from the 2005 and 2007 studies are 4.9 m&lt;sup&gt;2&lt;/sup&gt; g&lt;sup&gt;&amp;minus;1&lt;/sup&gt;
and 3.8 m&lt;sup&gt;2&lt;/sup&gt; g&lt;sup&gt;&amp;minus;1&lt;/sup&gt;, respectively. When POC mass approaching zero
(i.e. the impact of atmospheric aging is minimized), the SAC for primary
emitted soot is estimated to be 5.8 m&lt;sup&gt;2&lt;/sup&gt; g&lt;sup&gt;&amp;minus;1&lt;/sup&gt; and
6.3 m&lt;sup&gt;2&lt;/sup&gt; g&lt;sup&gt;&amp;minus;1&lt;/sup&gt; for the northern and southern air masses, respectively,
supported by the corresponding values when particulate sulphate
concentration approaches zero. A decreasing trend in the SAC value with
atmospheric aging of the aerosol was observed at the site, suggesting that
during the study, the light absorption enhancement due to the presence of
coating on particles was likely to be offset by the decrease in light
absorption caused by increasing soot particle diameter and collapsing of
soot particle structure. This result may imply that model simulations of
atmospheric warming by BC could be 50% too high.</abstract>
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</article>

