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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>7</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acpd-7-10589-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/10589/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/10589/2007/acpd-7-10589-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/10589/2007/acpd-7-10589-2007.pdf</fulltext_pdf>
	<start_page>10589</start_page>
	<end_page>10629</end_page>
	<publication_date>2007-07-23</publication_date>
	<article_title content_type="html">PM speciation and sources in Mexico during the MILAGRO-2006 Campaign</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>X. Querol</name>
			<email>xavier.querol@ija.csic.es</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. Pey</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. C. Minguillón</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>N. Pérez</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>A. Alastuey</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>M. Viana</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>T. Moreno</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>R. M. Bernabé</name>
		</author>
		<author numeration="9" affiliations="2">
			<name>S. Blanco</name>
		</author>
		<author numeration="10" affiliations="2">
			<name>B. Cárdenas</name>
		</author>
		<author numeration="11" affiliations="3">
			<name>E. Vega</name>
		</author>
		<author numeration="12" affiliations="3">
			<name>G. Sosa</name>
		</author>
		<author numeration="13" affiliations="3">
			<name>S. Escalona</name>
		</author>
		<author numeration="14" affiliations="3">
			<name>H. Ruiz</name>
		</author>
		<author numeration="15" affiliations="4">
			<name>B. Artíñano</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Instituto de Ciencias de la Tierra &quot;Jaume Almera&quot;, CSIC. C/ Lluís Solé i Sabarís s/n, 08028 Barcelona, Spain</affiliation>
		<affiliation numeration="2" content_type="html">Centro Nacional de Investigación y Capacitación Ambiental, CENICA. Periférico 5000, Col. Insurgentes Cuicuilco, C.P. 04530, Delegación Coyoacán, México D.F., Mexico</affiliation>
		<affiliation numeration="3" content_type="html">Instituto Mexicano del Petróleo, Eje Central Lázaro Cárdenas 152, Col. San Bartolo Atepehuacan. Delegación Gustavo A. Madero. 07730, México, D.F, Mexico</affiliation>
		<affiliation numeration="4" content_type="html">CIEMAT, Avda. Complutense 22,  28040 Madrid, Spain</affiliation>
	</affiliations>
	<abstract content_type="html">Levels of PM&lt;sub&gt;10&lt;/sub&gt;, PM&lt;sub&gt;2.5&lt;/sub&gt; and PM&lt;sub&gt;1&lt;/sub&gt; and chemical speciation of
PM&lt;sub&gt;10&lt;/sub&gt; and PM&lt;sub&gt;2.5&lt;/sub&gt; were measured during the MILAGRO campaign (1
to 31 March 2006, but extended in some cases until 6 April) at
four urban, one suburban, two rural, two rural background sites with
different degree of industrial influence in the Mexico City Metropolitan
Area (MCMA) and adjacent regions. PM&lt;sub&gt;10&lt;/sub&gt; and PM&lt;sub&gt;2.5&lt;/sub&gt; daily levels
varied between 50&amp;ndash;56 &amp;mu;g/m³ and 24&amp;ndash;46 &amp;mu;g/m³ at the urban
sites, 22&amp;ndash;35 &amp;mu;g/m³ and 13&amp;ndash;25 &amp;mu;g/m³ at the rural sites,
and 75 &amp;mu;g/m³ and 31 $\mu $g/m³ at the industrial hotspot,
respectively; lower than those recorded at some Asian mega-cities and
similar to those recorded at other South American cities. At the urban
sites, hourly PM&lt;sub&gt;2.5&lt;/sub&gt; and PM&lt;sub&gt;1&lt;/sub&gt; concentrations showed a marked impact
of road traffic emissions (at rush hours), with levels of coarse PM
remaining elevated during daytime. At the suburban and rural sites,
different PM daily patterns were registered according to the influence of
the pollution plume from MCMA and also on local soil resuspension.
&lt;br&gt;&lt;br&gt;
The speciation studies showed that mineral matter accounted for 25&amp;ndash;27%
of bulk PM&lt;sub&gt;10&lt;/sub&gt; at the urban sites and a higher proportion (up to 43%)
at the suburban and rural sites. This pattern is repeated in PM&lt;sub&gt;2.5&lt;/sub&gt;,
with 15% at urban and 28% at suburban and rural sites. Carbonaceous
compounds accounted for a similar proportion at the urban sites (24&amp;ndash;32%
in PM&lt;sub&gt;10&lt;/sub&gt;, and up to 37% in PM&lt;sub&gt;2.5&lt;/sub&gt;), markedly reduced at the
suburban and rural sites (17% in PM&lt;sub&gt;10&lt;/sub&gt;, and 23&amp;ndash;38% in PM&lt;sub&gt;2.5&lt;/sub&gt;).
The secondary inorganic aerosols accounted for 10&amp;ndash;20% of bulk PM&lt;sub&gt;10&lt;/sub&gt;
at urban, suburban, rural and industrial sites, with a higher proportion
(40%) at the industrial background site. A relatively high proportion of
nitrate in rural sites was present in the coarse fraction.
&lt;br&gt;&lt;br&gt;
Typically anthropogenic elements (As, Cr, Zn, Cu, Pb, Sn, Sb, Ba, among
others) showed considerably high levels at the urban sites; however levels
of particulate Hg and crustal trace elements (Rb, Ti, La, Sc, Ga) were
generally higher at the suburban site.
&lt;br&gt;&lt;br&gt;
Principal component analysis identified three common factors: crustal,
regional background and road traffic. Moreover, some specific factors were
obtained for each site.</abstract>
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