<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!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>7</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/hess-7-33-2003</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/7/33/2003/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/7/33/2003/hess-7-33-2003.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/7/33/2003/hess-7-33-2003.pdf</fulltext_pdf>
	<start_page>33</start_page>
	<end_page>42</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Characterising and modelling groundwater discharge in anagricultural wetland on the French Atlantic coast</article_title>
	<authors>
		<author numeration="1" affiliations="1,3">
			<name>Ph. Weng</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>F. Giraud</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>P. Fleury</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>C. Chevallier</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Bureau de Recherches Géologiques et Minières, Service EAU/RMD, 1039 rue de Pinville, 34000 Montpellier, France</affiliation>
		<affiliation numeration="2" content_type="html">INRA-SAD, 545, rue Bois Maché,17450 Saint-Laurent-de-la-Prée, France</affiliation>
		<affiliation numeration="3" content_type="html">E-mail for corresponding author: p.weng@brgm.fr</affiliation>
	</affiliations>
	<abstract content_type="html">Interaction between a wetland and its surrounding aquifer was studied in 
        the Rochefort agricultural marsh (150 km&lt;sup&gt;2&lt;/sup&gt;). Groundwater discharge in the marsh 
        was measured with a network of nested piezometers. Hydrological modelling of the wetland 
        showed that a water volume of 770,000 m&lt;sup&gt;3&lt;/sup&gt; yr&lt;sup&gt;–1&lt;/sup&gt; is discharging into 
        the marsh, but that this water flux essentially takes place along the lateral borders of 
        the wetland. However, this natural discharge volume represents only 20% of the artificial 
        freshwater injected each year into the wetland to maintain the water level close to the 
        soil surface. Understanding and quantifying the groundwater component in wetland hydrology 
        is crucial for wetland management and conservation.&lt;/b&gt;&lt;/p&gt;

&lt;p style=&quot;line-height: 20px;&quot;&gt;&lt;b&gt;Keywords: &lt;/b&gt;wetland, hydrology, groundwater, modelling, marsh</abstract>
	<references>
	</references>
</article>

