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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>5</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-19103-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/19103/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/19103/2009/acpd-9-19103-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/19103/2009/acpd-9-19103-2009.pdf</fulltext_pdf>
	<start_page>19103</start_page>
	<end_page>19157</end_page>
	<publication_date>2009-09-15</publication_date>
	<article_title content_type="html">Contributions from transport, solid fuel burning and cooking to  primary organic aerosols in two UK cities</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. D. Allan</name>
			<email>james.allan@manchester.ac.uk</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>P. I. Williams</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>W. T. Morgan</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>C. L. Martin</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>M. J. Flynn</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>J. Lee</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>E. Nemitz</name>
		</author>
		<author numeration="8" affiliations="4">
			<name>G. J. Phillips</name>
		</author>
		<author numeration="9" affiliations="2">
			<name>M. W. Gallagher</name>
		</author>
		<author numeration="10" affiliations="2">
			<name>H. Coe</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">National Centre for Atmospheric Science, The University of Manchester, Oxford Road, Manchester M13 9PL, UK</affiliation>
		<affiliation numeration="2" content_type="html">School of Earth, Atmospheric and Environmental Sciences, The University of Manchester, Oxford Road, Manchester M13 9PL, UK</affiliation>
		<affiliation numeration="3" content_type="html">National Centre for Atmospheric Science, The University of York, Heslington, York YO10 5DD, UK</affiliation>
		<affiliation numeration="4" content_type="html">Centre for Ecology and Hydrology, Bush Estate, Penicuik, Midlothian EH26 0QB, UK</affiliation>
	</affiliations>
	<abstract content_type="html">Organic matter frequently represents the single largest
      fraction of fine particulates in urban environments and yet
      the exact contributions from different sources and processes
      remain uncertain, owing in part to its substantial chemical
      complexity. Positive Matrix Factorisation (PMF) has recently
      proved to be a powerful tool for the purposes of source
      attribution and profiling when applied to ambient organic
      aerosol data from the Aerodyne Aerosol Mass Spectrometer
      (AMS). Here we present PMF analysis applied to AMS data from
      UK cities for the first time. Three datasets are analysed,
      with the focus on objectivity and consistency. The data were
      collected in London during the Regent&apos;s Park and Tower
      Environmental Experiment (REPARTEE) intensives and
      Manchester. These occurred during the autumn and wintertime,
      such that the primary fraction would be prominent. Ambiguities
      associated with rotationality within sets of potential
      solutions are explored and the most appropriate solution sets
      selected based on comparisons with external data. In addition
      to secondary organic aerosols, three candidate sources of
      primary organic aerosol (POA) were identified according to
      mass spectral and diurnal profiles; traffic emissions, cooking
      and solid fuel burning. Traffic represented, on average, 40% of POA during colder conditions and exhibited
      a hydrocarbon-like mass spectrum similar to those previously
      reported. Cooking aerosols represented 34% of POA and
      through laboratory work, their profile was matched with that
      sampled from the heating of seed oils, rather than
      previously-published spectra derived from charbroiling. This
      suggests that in these locations, oil from frying may have
      contributed more to the particulate than the meat
      itself. Solid fuel aerosols represented 26% of POA during
      cold weather conditions but were not discernable during the
      first REPARTEE experiment, when conditions were warmer than
      the other campaigns. This factor showed features associated
      with biomass burning and occurred mainly at night. Grid-scale
      emission factors of the combustion aerosols suitable for use
      in chemical transport models were derived relative to CO and
      NO&lt;sub&gt;x&lt;/sub&gt;. The traffic aerosols were found to be
      14.4 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; ppm&lt;sup&gt;&amp;minus;1&lt;/sup&gt; relative to CO for
      Manchester and 28 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; ppm&lt;sup&gt;&amp;minus;1&lt;/sup&gt; relative
      to NO&lt;sub&gt;x&lt;/sub&gt; for London. Solid fuel emissions were derived
      as 17.3 &amp;mu;g m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; ppm&lt;sup&gt;&amp;minus;1&lt;/sup&gt; relative to CO for
      Manchester. These correspond to mass emission ratios of 0.012,
      0.021 (as NO) and 0.014 respectively and are of a similar
      order to previously published estimates, derived from other
      regions or using other approaches.</abstract>
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</article>

