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Contraction of the fluvial territory in the Jarama River (Spain)

dc.contributor.authorEnríquez de Salamanca Sánchez-Cámara, Álvaro
dc.date.accessioned2024-07-29T11:13:03Z
dc.date.available2024-07-29T11:13:03Z
dc.date.issued2023
dc.description.abstractRivers are dynamic systems, with mobility due to their changing flows. Variations in flow give rise to floods, forming floodplains, whose human occupation depends on the probability of flooding; the reduction of floods favours human occupation. This study analyses the modification of the fluvial territory of the lower stretch of the Jarama River between 1956 and 2020, through orthophotographic analysis. The regulation of the basin by dams has led to the disappearance of floods, favouring human occupation of the fluvial territory. Concurrently, the length of the river channel has increased by 2.3% due to the excavation of some meanders, favoured by the modification of flows due to the discharge of wastewater treatment plants. As a consequence, the fluvial territory has increased by 0.88 km2 due to erosion, but at the same time has lost 14.36 km2 due to human occupation, with a net loss of 58.3% of the area. Most of the occupied fluvial territory has been used for agriculture, followed by grassland and mining, although much of the grasslands are former mining areas. The current public river domain is very narrow, and is defined as a fixed space, incompatible with fluvial dynamics. Floodplains are a strategic resource, as a defence against floods and to preserve river dynamics, sediment transport and biodiversity. It is necessary to preserve the fluvial territory and expand it by recovering lost land, and to maintain a space of freedom for the river, allowing its natural dynamics.
dc.description.departmentDepto. de Biodiversidad, Ecología y Evolución
dc.description.facultyFac. de Ciencias Biológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.identifier.citationEnríquez-de-Salamanca, Á. (2023) ´ Contraction of the fluvial territory in the Jarama River (Spain). Earth Surface Processes and Landforms, 48(9), 1869–1882
dc.identifier.doi10.1002/esp.5578
dc.identifier.officialurlhttps://doi.org/10.1002/esp.5578
dc.identifier.urihttps://hdl.handle.net/20.500.14352/107176
dc.issue.number9
dc.journal.titleEarth Surface Processes and Landforms
dc.language.isoeng
dc.page.final1882
dc.page.initial1869
dc.publisherWiley
dc.rights.accessRightsrestricted access
dc.subject.cdu551.48
dc.subject.cdu574
dc.subject.keywordFloodplain occupation
dc.subject.keywordFloodplains
dc.subject.keywordLand use change
dc.subject.keywordRiver change
dc.subject.keywordRoom for rivers
dc.subject.ucmEcología (Biología)
dc.subject.ucmHidrología
dc.subject.unesco2506.07 Geomorfología
dc.subject.unesco2508 Hidrología
dc.titleContraction of the fluvial territory in the Jarama River (Spain)
dc.typejournal article
dc.type.hasVersionVoR
dc.volume.number48
dspace.entity.typePublication
relation.isAuthorOfPublication382a0c96-7d8c-4fd3-afc7-78a68f10316f
relation.isAuthorOfPublication.latestForDiscovery382a0c96-7d8c-4fd3-afc7-78a68f10316f

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