<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<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>6</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acpd-6-11681-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/11681/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/11681/2006/acpd-6-11681-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/11681/2006/acpd-6-11681-2006.pdf</fulltext_pdf>
	<start_page>11681</start_page>
	<end_page>11725</end_page>
	<publication_date>2006-11-21</publication_date>
	<article_title content_type="html">Source apportionment of submicron organic aerosols at an urban site by linear unmixing of aerosol mass spectra</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>V. A. Lanz</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>M. R. Alfarra</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>U. Baltensperger</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>B. Buchmann</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>C. Hueglin</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>A. S. H. Prévôt</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Empa, Swiss Federal Laboratories for Materials Testing and Research, Laboratory for Air Pollution and Environmental Technology, 8600 Duebendorf, Switzerland</affiliation>
		<affiliation numeration="2" content_type="html">PSI, Paul Scherrer Institute, Laboratory for Atmospheric Chemistry, 5232 Villigen PSI, Switzerland</affiliation>
	</affiliations>
	<abstract content_type="html">Submicron ambient aerosol was characterized in summer 2005 at an urban
background site in Zurich, Switzerland, during a three-week measurement
campaign. Highly time-resolved samples of non-refractory aerosol components
were analyzed with an Aerodyne aerosol mass spectrometer (AMS). Positive
matrix factorization (PMF) was used for the first time for AMS data to
identify the main components of the total organic aerosol and their sources.
The PMF retrieved factors were compared to measured reference mass spectra
and were correlated with tracer species of the aerosol and gas phase
measurements from collocated instruments. Six factors were found to explain
virtually all variance in the data and could be assigned either to sources
or to aerosol components such as oxygenated organic aerosol (OOA). Our
analysis suggests that at the measurement site only a small (&amp;lt;10%)
fraction of organic PM&lt;sub&gt;1&lt;/sub&gt; originates from freshly emitted fossil fuel
combustion. Other primary sources identified to be of similar or even higher
importance are charbroiling (10&amp;ndash;15%) and wood burning (~10%),
along with a minor source interpreted to be influenced by food cooking
(6%). The fraction of all identified primary sources is considered as
primary organic aerosol (POA). This interpretation is supported by
calculated ratios of the modelled POA and measured primary pollutants such
as elemental carbon (EC), NO&lt;sub&gt;x&lt;/sub&gt;, and CO, which are in good agreement to
literature values. A high fraction (60&amp;ndash;69%) of the measured organic
aerosol mass is OOA which is interpreted mostly as secondary organic aerosol
(SOA). This oxygenated organic aerosol can be separated into a highly aged
fraction, OOA&amp;nbsp;I, (40&amp;ndash;50%) with low volatility and a mass spectrum similar
to fulvic acid, and a more volatile and probably less processed fraction,
OOA&amp;nbsp;II (on average 20%). This is the first publication of a multiple
component analysis technique to AMS organic spectral data and also the first
report of the OOA&amp;nbsp;II component.</abstract>
	<references>
	</references>
</article>

