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<!DOCTYPE article SYSTEM "http://www.hydrol-earth-syst-sci.net/inc/hess/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Hydrology and Earth System Sciences</journal_title>
		<journal_url>www.hydrol-earth-syst-sci.net</journal_url>
		<issn>1027-5606</issn>
		<eissn>1607-7938</eissn>
		<volume_number>10</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/hess-10-31-2006</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/10/31/2006/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/10/31/2006/hess-10-31-2006.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/10/31/2006/hess-10-31-2006.pdf</fulltext_pdf>
	<start_page>31</start_page>
	<end_page>48</end_page>
	<publication_date>2006-02-08</publication_date>
	<article_title content_type="html">Transport at basin scales: 2. Applications</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Rinaldo</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>G. Botter</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>E. Bertuzzo</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>A. Uccelli</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>T. Settin</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>M. Marani</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">International Centre for Hydrology “Dino Tonini&quot; and Dipartimento IMAGE, Università di Padova, via Loredan 20, 35 131 Padova, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">In this paper, the second of a series, we apply the
models discussed in Part&amp;nbsp;1 to a significant case study. The nature
of the catchment under study, the transport phenomena investigated
(i.e. nitrates moving as solutes within runoff waters) and the
scales involved in space and time, provide an elaborate test for
theory and applications. Comparison of modeling predictions with
field data (i.e. fluxes of carrier flow and solute nitrates)
suggests that the framework proposed for geomorphic transport
models is capable to describe well large-scale transport phenomena
driven and/or controlled by spatially distributed hydrologic
fields (e.g. rainfall patterns in space and time, drainage
pathways, soil coverage and type, matter stored in immobile
phases). A sample MonteCarlo mode of application of the model is
also discussed where hydrologic forcings and external nitrate
applications (through fertilization) are treated as random
processes.</abstract>
	<references>
	</references>
</article>

