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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>3</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-3773-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/3773/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/3773/2005/acpd-5-3773-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/3773/2005/acpd-5-3773-2005.pdf</fulltext_pdf>
	<start_page>3773</start_page>
	<end_page>3809</end_page>
	<publication_date>2005-06-08</publication_date>
	<article_title content_type="html">Size distribution of EC and OC in the aerosol of Alpine valleys during summer and winter</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J.-L. Jaffrezo</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>G. Aymoz</name>
		</author>
		<author numeration="3" affiliations="1,2">
			<name>J. Cozic</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratoire de Glaciologie et G&amp;eacute;ophysique de l’Environnement (LGGE), 54 rue Moli&amp;egrave;re, 38402 Saint Martin d’H&amp;egrave;res Cedex, France</affiliation>
		<affiliation numeration="2" content_type="html">*now at: Laboratory for Atmospheric Chemistry, Paul Scherrer Institute, CH-5232 Villigen, PSI, Switzerland</affiliation>
	</affiliations>
	<abstract content_type="html">Collections of samples were conducted for the determination of the size
distributions of EC and OC during the intensive sampling campaigns of the
POVA program, in two Alpine valleys of the French Alps, in summer and in
winter. The comparison of concentrations obtained for samples collected in
parallel with impactor- and filter-based methods indicates that the
correction of pyrolysis seems to work for the impactor samples despite non
even deposits. The size distributions of the concentrations of EC and OC
present large evolutions between winter and summer, and between a suburban
and a rural site. In winter, an overwhelming proportion of the mass fraction
of both species is found in the droplet and accumulation modes, often (but
not always) in association with sulfate and other chemical species resulting
from secondary formation processes. Some indications of gas/particles
exchanges can be found for the other parts of the size spectrum (the Aitken
and super micron modes) in the case of the rural site. In summer, the
changes are more drastic with, according to the case, a dominant droplet or
accumulation mode. Particularly at the rural site, the large extent of
processing of the aerosol due to gas/particles exchanges is evident for
the Aitken and super micron modes, with increasing of the OC mass fractions
in these size ranges. All of these observations give indications on the
degree of internal vs. external mixing of the species investigated in the
different modes.</abstract>
	<references>
	</references>
</article>

