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dc.contributor.authorPLUS Martinen_GB
dc.contributor.authorLA JEUNESSE Isabelleen_GB
dc.contributor.authorBOURAOUI FAYCALen_GB
dc.contributor.authorZALDIVAR COMENGES JOSE'en_GB
dc.contributor.authorCHAPELLE Annieen_GB
dc.contributor.authorLAZURE Pascalen_GB
dc.date.accessioned2010-02-25T14:36:06Z-
dc.date.available2006-03-17en_GB
dc.date.available2010-02-25T14:36:06Z-
dc.date.issued2006en_GB
dc.date.submitted2006-01-19en_GB
dc.identifier.citationECOLOGICAL MODELLING vol. 193 p. 69-89en_GB
dc.identifier.urihttp://publications.jrc.ec.europa.eu/repository/handle/JRC32205-
dc.description.abstractThe Soil and Water Assessment Tool (SWAT model, 2001 Version) has been applied to the Thau lagoon catchment area in order to simulate water discharges and nutrient inputs into the lagoon over a 10 years period (1989–1999), and to provide routing inflows to a previously developed lagoon ecosystem model. The watershed model has been calibrated and validated using measured data available for the two main rivers. The results indicate that the mean annual nitrogen inputs into the Thau lagoon is 117±57 tons y−1, with the two main rivers, contributing for 80% of total annual nitrogen export. The variations of outputs to the lagoon are nonetheless important from 1 year to another. Due to the local agricultural practices and a reduced in-stream natural depuration, point sources seem to be the main factor affecting the fresh water quality. The coupling with the lagoon model allowed to estimate the impact of those terrestrial inputs on the lagoon nitrogen cycling and primary productivity. Influence of river discharges makes itself felt essentially near the river outlets. The northern bordure of the lagoon is then characterised by highly variable dissolved inorganic nitrogen concentrations, especially during flood events, while more stable and lower concentrations were simulated in the southern part of the lagoon. Simulated chlorophyll a ranged 1–15 microg l−1, with maximums in March. Mean annual phytoplankton production was 364±142 gCm−2. The simulations showed that maximum annual productions are due to macrophytes (up to 1300 gCm−2 y−1), but at the whole lagoon scale, annual phytoplankton production resulted greater. From our results it also appeared that the greatest part of primary producers nitrogen requirements is satisfied by nutrient regeneration within the lagoon.en_GB
dc.description.sponsorshipJRC.H.5-Rural, water and ecosystem resourcesen_GB
dc.format.mediumPrinteden_GB
dc.languageENGen_GB
dc.publisherELSEVIERen_GB
dc.relation.ispartofseriesJRC32205en_GB
dc.titleModelling Water Discharges and Nutrient Inputs into a Mediterranean Lagoon. Impact on the Primary Productionen_GB
dc.typeArticles in periodicals and booksen_GB
JRC Directorate:Sustainable Resources

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