2007
DOI: 10.1016/j.ecoleng.2006.09.003
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The restoration of El Partido stream watershed (Doñana Natural Park)

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Cited by 22 publications
(27 citation statements)
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“…During that flooding cycle the northwestern area of the marsh showed a relevant increase in hydroperiod values, as revealed by the anomaly image. The accretion of a large depositional delta with sandy sediments from El Partido tributary stream [72] has dammed the surface inflow waters and re-drawn the original water course, bringing more water to areas that previously did not receive so much (label 4 in Figure 7b). The flooding of artificial ponds in the Caracoles restored area [69] is also evident (label 5 in Figure 7b).…”
Section: Hydroperiod Historical Trend and Anomaliesmentioning
confidence: 99%
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“…During that flooding cycle the northwestern area of the marsh showed a relevant increase in hydroperiod values, as revealed by the anomaly image. The accretion of a large depositional delta with sandy sediments from El Partido tributary stream [72] has dammed the surface inflow waters and re-drawn the original water course, bringing more water to areas that previously did not receive so much (label 4 in Figure 7b). The flooding of artificial ponds in the Caracoles restored area [69] is also evident (label 5 in Figure 7b).…”
Section: Hydroperiod Historical Trend and Anomaliesmentioning
confidence: 99%
“…The Doñana marshes are a vast seasonal freshwater wetland of international importance, considered as Western Europe's largest sanctuary for migratory birds. In 1969 they were declared a national park, then a Biosphere Reserve in 1980, an Important Wetland Site under the Ramsar Convention in 1982, and a Natural World Heritage Site in 1984 [1]. Doñana is also recognized as a Long-Term Socio-Ecological Research (LTSER) platform integrated in the LTER-Europe network [37] by applying harmonized protocols for long-term socio-ecological research.…”
Section: Study Areamentioning
confidence: 99%
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“…3): i) a silty-clay floodplain (about 23,000 ha) with a seasonally flooded marshland mainly fed by rainfall and the overflow of streams and rivers; ii) an area of sand dunes fixed by the vegetation; and iii) an active sand dune system with several dune fronts (up to 32 m high, 15 km long and 3 km wide) running parallel to the coast line in a South-West/North-East direction (García-Novo and Marín, 2006). The ecotone or border between the two main units (marshland and sand dunes) also forms a distinct landscape of seasonal wet meadows (Fig.…”
Section: The Doñana Wetlandsmentioning
confidence: 99%