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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>7</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acpd-7-2133-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/2133/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/2133/2007/acpd-7-2133-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/2133/2007/acpd-7-2133-2007.pdf</fulltext_pdf>
	<start_page>2133</start_page>
	<end_page>2168</end_page>
	<publication_date>2007-02-14</publication_date>
	<article_title content_type="html">Size-segregated fluxes of mineral dust from a desert area of northern China by eddy covariance</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. Fratini</name>
			<email>gfratini@unitus.it</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>P. Ciccioli</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>A. Febo</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>A. Forgione</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>R. Valentini</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Forest Sciences and Resources (DiSAFRi), Università della Tuscia, 01100, Viterbo, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Istituto di Metodologie Chimiche, Area della Ricerca del C.N.R. di Roma, 00016, Monterotondo Scalo, Italy</affiliation>
		<affiliation numeration="3" content_type="html">Istituto di Inquinamento Atmosferico, Area della Ricerca del C.N.R. di Roma, 00016, Monterotondo Scalo, Italy</affiliation>
		<affiliation numeration="4" content_type="html">FAI Instruments s.r.l., Rome, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">Mineral dust emission accounts for a substantial portion of particles
present in the troposphere. It is emitted most from desert areas, mainly
through intense storm episodes. The aim of this work was to quantify
size-segregated fluxes of mineral dust particles emitted during storm events
occurring in desert areas of northern China (Alashan desert, Inner
Mongolia), known to act as one of the strongest sources of mineral dust
particles in the Asian continent. Long-range transport of mineral dust
emitted in this area is responsible for the high particle concentrations
reached in densely populated areas, including the city of Beijing. Based on
a theoretical analysis, an eddy covariance system was built to get
size-segregated fluxes of mineral dust particles with optical diameters
ranging between 0.26 and 7.00 &amp;mu;m. The system was optimised to measure
fluxes under intense storm event conditions. It was tested in two sites
located in the Chinese portion of the Gobi desert. During the field
campaign, an intense storm event was recorded in one of them. Data obtained
during this event indicate that particle number fluxes were dominated by the
finer fraction, whereas in terms of volume, coarser particle accounted for
the largest portion. It was found that during the storm event, ratios of
size-segregated particle volume fluxes remained substantially constant and a
simple parameterization of particle emission from total volume fluxes was
possible. A strong correlation was also found between particle volume fluxes
and the friction velocity. This relationship is extremely useful to
investigate mechanisms of particle formation by wind erosion.</abstract>
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</article>

