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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys.net/inc/acp/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>3</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acp-3-2207-2003</doi>
	<article_url>http://www.atmos-chem-phys.net/3/2207/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/3/2207/2003/acp-3-2207-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/3/2207/2003/acp-3-2207-2003.pdf</fulltext_pdf>
	<start_page>2207</start_page>
	<end_page>2216</end_page>
	<publication_date>2003-12-09</publication_date>
	<article_title content_type="html">Size resolved mass concentration and elemental composition of atmospheric aerosols over the Eastern Mediterranean area</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. Smolík</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>V. Ždímal</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>J. Schwarz</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>M. Lazaridis</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>V. Havárnek</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>K. Eleftheriadis</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>N. Mihalopoulos</name>
		</author>
		<author numeration="8" affiliations="6">
			<name>C. Bryant</name>
		</author>
		<author numeration="9" affiliations="6">
			<name>I. Colbeck</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Chemical Process Fundamentals, ASCR, Prague, Czech Republic</affiliation>
		<affiliation numeration="2" content_type="html">Nuclear Physics Institute AS CR, Prague, Czech Republic</affiliation>
		<affiliation numeration="3" content_type="html">Technical University of Crete, Department of Environmental Engineering, 73100 Chania, Greece</affiliation>
		<affiliation numeration="4" content_type="html">Institute of Nuclear Technology &amp; Radiation Protection, N.C.S.R. Demokritos, 15310 Ag. Paraskevi, Attiki, Greece</affiliation>
		<affiliation numeration="5" content_type="html">Environmental Chemical Processes Lab. (ECPL), Department of Chemistry, University of Crete 71409 Heraklion, Greece</affiliation>
		<affiliation numeration="6" content_type="html">Department of Biological Sciences, University of Essex, UK</affiliation>
	</affiliations>
	<abstract content_type="html">A Berner low pressure impactor was used to collect size-segregated aerosol samples at
      Finokalia, located on the north-eastern coast of Crete, Greece during July 2000 and January 2001.
      Several samples were also collected during the summer campaign aboard the research vessel
      &amp;quot;AEGAIEO&amp;quot; in the Aegean Sea. Gravimetric analysis and inversion techniques yielded daily PM1 and
      PM10 mass concentrations. The samples were also analysed by PIXE giving the elemental size
      distributions of Al, Si, K, Ca, Ti, Mn, Fe, Sr, S, Cl, Ni, V, Cu, Cr, Zn, and Pb. The crustal elements
      and sea-salt had a unimodal supermicron size distribution. Sulphur was found predominantly in
      submicron fractions. K, V, and Ni exhibited a bimodal distribution with a submicron mode produced
      by forest fires and oil combustion. The anthropogenic elements had broad and not well-defined
      distributions. The time series for PM1 and PM10 mass and elemental concentrations showed both
      daily and seasonal variation. Higher mass concentrations were observed during two incursions of
      Saharan dust, whilst higher concentrations of S, Cu, Zn, and Pb were encountered in samples collected
      in air masses arriving from northern Greece or the western coast of Turkey. Elevated concentrations of
      chlorine were found in samples with air masses either originating above the Atlantic Ocean and
      arriving at Finokalia via western Europe or recirculating over the western coast of the Black Sea.</abstract>
	<references>
	</references>
</article>

