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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>5</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-4143-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/4143/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/4143/2005/acpd-5-4143-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/4143/2005/acpd-5-4143-2005.pdf</fulltext_pdf>
	<start_page>4143</start_page>
	<end_page>4182</end_page>
	<publication_date>2005-06-28</publication_date>
	<article_title content_type="html">Characterization of ambient aerosols in Mexico City during the MCMA-2003 campaign with Aerosol Mass Spectrometry – Part I: quantification, shape-related collection efficiency, and comparison with collocated instruments</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>D. Salcedo</name>
		</author>
		<author numeration="2" affiliations="2,3">
			<name>K. Dzepina</name>
		</author>
		<author numeration="3" affiliations="4">
			<name>T. B. Onasch</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>M. R. Canagaratna</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>Q. Zhang</name>
		</author>
		<author numeration="6" affiliations="2,3">
			<name>A.. R. Huffman</name>
		</author>
		<author numeration="7" affiliations="2,5">
			<name>P. F. DeCarlo</name>
		</author>
		<author numeration="8" affiliations="4">
			<name>J. T. Jayne</name>
		</author>
		<author numeration="9" affiliations="4,10">
			<name>P. Mortimer</name>
		</author>
		<author numeration="10" affiliations="4">
			<name>D. R. Worsnop</name>
		</author>
		<author numeration="11" affiliations="4">
			<name>C. E. Kolb</name>
		</author>
		<author numeration="12" affiliations="6">
			<name>K. S. Johnson</name>
		</author>
		<author numeration="13" affiliations="6,11">
			<name>B. Zuberi</name>
		</author>
		<author numeration="14" affiliations="6,12">
			<name>L. C. Marr</name>
		</author>
		<author numeration="15" affiliations="6">
			<name>L. T. Molina</name>
		</author>
		<author numeration="16" affiliations="6">
			<name>M. J. Molina</name>
		</author>
		<author numeration="17" affiliations="7">
			<name>R. M. Bernabé</name>
		</author>
		<author numeration="18" affiliations="7">
			<name>B. Cardenas</name>
		</author>
		<author numeration="19" affiliations="7">
			<name>C. Márquez</name>
		</author>
		<author numeration="20" affiliations="8">
			<name>J. S. Gaffney</name>
		</author>
		<author numeration="21" affiliations="8">
			<name>N. A. Marley</name>
		</author>
		<author numeration="22" affiliations="9">
			<name>A. Laskin</name>
		</author>
		<author numeration="23" affiliations="9">
			<name>V. Shutthanandan</name>
		</author>
		<author numeration="24" affiliations="2,3">
			<name>J. L. Jimenez</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Centro de Investigaciones Qu&amp;#237;micas, Universidad Aut&amp;#243;noma del Estado de Morelos, Cuernavaca, Morelos, Mexico</affiliation>
		<affiliation numeration="2" content_type="html">Cooperative Institute for Research in the Environmental Sciences (CIRES), University of Colorado at Boulder, Boulder, CO, USA</affiliation>
		<affiliation numeration="3" content_type="html">Department of Chemistry and Biochemistry, University of Colorado at Boulder, Boulder, CO, USA</affiliation>
		<affiliation numeration="4" content_type="html">Center for Aerosol and Cloud Chemistry, Aerodyne Research Inc., Billerica, MA, USA</affiliation>
		<affiliation numeration="5" content_type="html">Program in Atmospheric and Oceanic Sciences, University of Colorado at Boulder, Boulder, CO, USA</affiliation>
		<affiliation numeration="6" content_type="html">Department of Earth, Atmospheric and Planetary Sciences and Department of Chemistry, Massachusetts Institute of Technology, Cambridge, MA, USA</affiliation>
		<affiliation numeration="7" content_type="html">Centro Nacional de Investigaci&amp;#243;n Capacitaci&amp;#243;n Ambiental, Instituto Nacional de Ecolog&amp;#237;a, México D.F., Mexico</affiliation>
		<affiliation numeration="8" content_type="html">Argonne National Laboratory, Argonne, IL, USA</affiliation>
		<affiliation numeration="9" content_type="html">William R. Wiley Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, WA, USA</affiliation>
		<affiliation numeration="10" content_type="html">now at: John Hopkins University, Baltimore, MD, USA</affiliation>
		<affiliation numeration="11" content_type="html">now at: GEO2 Technologies, Woburn, MA, USA</affiliation>
		<affiliation numeration="12" content_type="html">now at: Department of Civil and Environmental Engineering, Virginia Polytechnic Institute and State University, Blacksburg, VA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">An Aerodyne Aerosol Mass Spectrometer (AMS) was deployed at the CENICA
Supersite, while another was deployed in the Aerodyne Mobile Laboratory
(AML) during the Mexico City Metropolitan Area field study (MCMA-2003) from
31 March&amp;ndash;4 May 2003 to investigate particle concentrations, sources, and
processes. This is the first of a series of papers reporting the AMS results
from this campaign. The AMS provides real time information on mass
concentration and composition of the non-refractory species in particulate
matter less than 1 &amp;micro;m (NR-PM&lt;sub&gt;1&lt;/sub&gt;) with high time and
size-resolution. For the first time, we report field results from a beam
width probe, which was used to study the shape and mixing state of the
particles and to quantify potential losses of irregular particles due to
beam broadening inside the AMS. Data from this probe show that no
significant amount of irregular particles was lost due to excessive beam
broadening. A comparison of the CENICA and AML AMSs measurements is
presented, being the first published intercomparison between two quadrupole
AMSs. The speciation, and mass concentrations reported by the two AMSs
compared relatively well. The differences found are likely due to the
different inlets used in both instruments. In order to account for the
refractory material in the aerosol, we also present measurements of Black
Carbon (BC) using an aethalometer and an estimate of the aerosol soil
component obtained from Proton-Induced X-ray Emission Spectrometry (PIXE)
analysis of impactor substrates. Comparisons of AMS + BC + soil mass
concentration with other collocated particle instruments (a LASAIR Optical
Particle Counter, a Tapered Element Oscillating Microbalance (TEOM) and a
DustTrak Aerosol Monitor) are also presented. The comparisons show that the
AMS + BC + soil mass concentration during MCMA-2003 is a good approximation
to the total PM&lt;sub&gt;2.5&lt;/sub&gt; mass concentration.</abstract>
	<references>
	</references>
</article>

