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<!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>3</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acpd-6-3997-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/3997/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/3997/2006/acpd-6-3997-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/3997/2006/acpd-6-3997-2006.pdf</fulltext_pdf>
	<start_page>3997</start_page>
	<end_page>4022</end_page>
	<publication_date>2006-05-19</publication_date>
	<article_title content_type="html">Aerosol composition and source apportionment in the Mexico City Metropolitan Area with PIXE/PESA/STIM and multivariate analysis</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>K. S. Johnson</name>
		</author>
		<author numeration="2" affiliations="1,4">
			<name>B. de Foy</name>
		</author>
		<author numeration="3" affiliations="1,5">
			<name>B. Zuberi</name>
		</author>
		<author numeration="4" affiliations="1,4">
			<name>L. T. Molina</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>M. J. Molina</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>Y. Xie</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>A. Laskin</name>
		</author>
		<author numeration="8" affiliations="3">
			<name>V. Shutthanandan</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Chemistry and of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA</affiliation>
		<affiliation numeration="2" content_type="html">Applied Geology and Geochemistry Technical Group, Pacific Northwest National Laboratory, Richland, WA, USA</affiliation>
		<affiliation numeration="3" content_type="html">William R. Wiley Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, WA, USA</affiliation>
		<affiliation numeration="4" content_type="html">now at: Molina Center for Energy and the Environment, La Jolla, CA, USA</affiliation>
		<affiliation numeration="5" content_type="html">now at: GEO2 Technologies, Inc., Woburn, MA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Aerosols play an important role in the atmosphere but are poorly
characterized, particularly in urban areas like the Mexico City Metropolitan
Area (MCMA). The chemical composition of urban particles must be known to
assess their effects on the environment, and specific particulate emissions
sources should be identified to establish effective pollution control
standards. For these reasons, samples of particulate matter &amp;#x2264;2.5 &amp;mu;m (PM&lt;sub&gt;2.5&lt;/sub&gt;) were collected during the MCMA-2003 Field Campaign for
elemental and multivariate analyses. Proton-Induced X-ray Emission (PIXE),
Proton-Elastic Scattering Analysis (PESA) and Scanning Transmission Ion
Microscopy (STIM) techniques were done to determine concentrations of 19
elements from Na to Pb, hydrogen, and total mass, respectively. The most
abundant elements from PIXE analysis were S, Si, K, Fe, Ca, and Al, while
the major emissions sources associated with these elements were industry,
wind-blown soil, and biomass burning. Wind trajectories suggest that metals
associated with industrial emissions came from northern areas of the city
whereas soil aerosols came from the southwest and increased in concentration
during dry conditions. Elemental markers for fuel oil combustion V and Ni
correlated with a large SO&lt;sub&gt;2&lt;/sub&gt; plume to suggest an anthropogenic, rather
than volcanic, emissions source. By subtracting major components of soil and
sulfate determined by PIXE analysis from STIM total mass measurements, we
estimate that approximately 50% of non-volatile PM&lt;sub&gt;2.5&lt;/sub&gt; consisted of carbonaceous
material.</abstract>
	<references>
	</references>
</article>

