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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>6</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acpd-6-12389-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/12389/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/12389/2006/acpd-6-12389-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/12389/2006/acpd-6-12389-2006.pdf</fulltext_pdf>
	<start_page>12389</start_page>
	<end_page>12431</end_page>
	<publication_date>2006-12-01</publication_date>
	<article_title content_type="html">Chemical characterization of the inorganic fraction of aerosols and mechanisms of the neutralization of atmospheric acidity in Athens, Greece</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>E. T. Karageorgos</name>
			<email>vkarageo@env.duth.gr</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>S. Rapsomanikis</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>P. Wåhlin</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratory of Atmospheric Pollution and Pollution Control Engineering, Faculty of Engineering, Department of Environmental Engineering, Democritus University of Thrace, P.O. Box 447, 67100 Xanthi, Greece</affiliation>
		<affiliation numeration="2" content_type="html">Department of Atmospheric Environment, NERI, Frederiksborgvej 399, P.O.Box 358, 4000 Roskilde, Denmark</affiliation>
	</affiliations>
	<abstract content_type="html">Mass concentration levels and the inorganic chemical composition of
PM&lt;sub&gt;10&lt;/sub&gt;  (two fractions; PM&lt;sub&gt;10&amp;minus;2.5&lt;/sub&gt; and PM&lt;sub&gt;2.5&lt;/sub&gt;) were determined
during August 2003 and March 2004, in the centre of Athens, Greece. August
2003 monthly mean PM&lt;sub&gt;10&lt;/sub&gt; mass concentration, at 5 m above ground, was 56 &amp;mu;g/m&lt;sup&gt;3&lt;/sup&gt; and the EU imposed daily limit of 50 &amp;mu;g/m&lt;sup&gt;3&lt;/sup&gt; was
exceeded on 16 occasions. The corresponding monthly mean for March 2004 was
92 &amp;mu;g/m&lt;sup&gt;3&lt;/sup&gt; and the aforementioned daily limit was exceeded on 23 occasions. The PM&lt;sub&gt;10&lt;/sub&gt;  (PM&lt;sub&gt;10&amp;minus;2.5&lt;/sub&gt;+PM&lt;sub&gt;2.5&lt;/sub&gt;) mass concentrations at
1.5 m above ground were found to be approximately 20% higher compared to
the respective PM&lt;sub&gt;10&lt;/sub&gt; measured at 5 m. Consequently, for a realistic
estimation of the exposure of citizens to particulate matter, PM&lt;sub&gt;10&lt;/sub&gt;
sampling at a height of 1.5&amp;ndash;3 m above ground, in the &quot;breathing zone&quot; is
necessary. Such data are presented for the first time for the centre of
Athens. In both campaigns, calcium was found to be the predominant component
of the coarse fraction while crust-related aluminosilicates and iron were
found to be the other major components of the same fraction. The above
elements constitute the most important components of the fine fraction,
together with the predominant sulphur. Toxic metals were found to be below
the air quality limits and in lower concentrations compared to older
studies, with the exception of Cu and V for which some increase was
observed. Pb, in particular, appeared mostly in the fine fraction and in
very low concentrations compared to studies dating more than a decade back.
The major ions of the coarse fraction have been found to be Ca&lt;sup&gt;2+&lt;/sup&gt;,
NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt; and Cl&lt;sup&gt;&amp;minus;&lt;/sup&gt;, while SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;&amp;minus;2&lt;/sup&gt;, Ca&lt;sup&gt;2+&lt;/sup&gt; and
NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; were the major ionic components of the fine fraction. The low
molar ratio of NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;/SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;&amp;minus;2&lt;/sup&gt; indicated an ammonium-poor
ambient air, where atmospheric ammonia is not sufficient to neutralize all
acidity and the formation of NH&lt;sub&gt;4&lt;/sub&gt;NO&lt;sub&gt;3&lt;/sub&gt; does not occur to a
significant extend. Calcium predominated the coarse fraction and its good
correlations with NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt; and SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;&amp;minus;2&lt;/sup&gt; indicated its role as
an important neutralizing agent of atmospheric acidity in this particle size
range. In the fine fraction, both Ca&lt;sup&gt;2+&lt;/sup&gt; and NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; participate
in the neutralizing processes with NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; being the major
neutralizing agent of SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;&amp;minus;2&lt;/sup&gt;. Chloride depletion from NaCl or
MgCl&lt;sub&gt;2&lt;/sub&gt; was not found to occur to a significant extend. Total analyzed
inorganic mass (elemental+ionic) was found to be ranging between
approximately 25&amp;ndash;33% of the total coarse particle mass and 35&amp;ndash;42% of
the total fine particle mass.</abstract>
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