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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>5</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-4335-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/4335/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/4335/2005/acpd-5-4335-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/4335/2005/acpd-5-4335-2005.pdf</fulltext_pdf>
	<start_page>4335</start_page>
	<end_page>4371</end_page>
	<publication_date>2005-07-04</publication_date>
	<article_title content_type="html">A TGA/FT-IR study for OC and EC quantification applied to carbonaceous aerosol collected in Milan (Italy)</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. Fermo</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. Piazzalunga</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>R. Vecchi</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>G. Valli</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>M. Ceriani</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Dipartimento di Chimica Inorganica, Metallorganica e Analitica, University of Milan, Via Venezian 21, 20133 Milan, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Istituto di Fisica Generale Applicata, University of Milan, via Celoria 16, 20133 Milan, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">Carbon analysis consists in the evaluation of the carbonaceous content of
the aerosol (TC) but, more importantly, of its distribution between
the two components EC (Elemental Carbon) and OC (Organic Carbon) that are
characterized by different physical-chemical properties. In spite of the
numerous studies focused on this topic, nowadays, a universal methodology
for the determination of the two components EC and OC is not available. In
fact OC and EC (also known as black carbon or soot) are operationally
defined by the method of analysis and, as a consequence, different methods
can produce different results.

&lt;br&gt;&lt;br&gt;
In this paper we present results on the application of TGA/FT-IR
(Thermogravimetric Analysis/Fourier Transformed Infrared Spectroscopy) to
the characterization of carbonaceous aerosols. The analytical methodology
was applied to PM10 four-hour time resolution samples collected in Milan
urban area. The method is a two-steps thermal one and bases itself on the
different thermal behaviour of OC and EC. It has been set up analyzing
suitable standards containing both organic and elemental carbon. Carbon
quantification is achieved by on-line, continuous monitoring of CO&lt;sub&gt;2&lt;/sub&gt; infrared absorption at 2361 cm&lt;sup&gt;&amp;minus;1&lt;/sup&gt;. A good separation between OC and EC
on particulate matter samples has been obtained. Ranges and average values
were respectively 12&amp;ndash;70 &amp;micro;g/m&lt;sup&gt;3&lt;/sup&gt; and 20 &amp;micro;g/m&lt;sup&gt;3&lt;/sup&gt; for OC and
0.2&amp;ndash;6 &amp;micro;g/m&lt;sup&gt;3&lt;/sup&gt; and 2 &amp;micro;g/m&lt;sup&gt;3&lt;/sup&gt; for EC. On average OC
and EC made up respectively 29.3 (&amp;plusmn;12.8) % and 2.5 (&amp;plusmn;1.8)
% of PM10 fraction. The method reliability has been verified by
comparison with TOT (Thermal Optical Transmission) technique. OC and EC
values determined for ambient samples of PM10 were also correlated with
meteorological parameters as well as with Radon concentrations.</abstract>
	<references>
	</references>
</article>

