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dc.contributor.authorChavarrías Borrás, Víctor
dc.contributor.authorBlom, Astrid
dc.contributor.authorOrrú, Clara
dc.contributor.authorMartín Vide, Juan Pedro
dc.contributor.authorViparelli, Enrica
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament d'Enginyeria Civil i Ambiental
dc.date.accessioned2018-06-19T07:48:29Z
dc.date.available2018-06-19T07:48:29Z
dc.date.issued2018-05
dc.identifier.citationChavarrías, V., Blom, Astrid, Orrú, C., Martín-Vide, J.P., Viparelli, E. A sand-gravel Gilbert delta subject to base level change. "Journal of Geophysical Research: Earth Surface", Maig 2018, vol. 123, núm. 5, p. 1160-1179.
dc.identifier.issn2169-9011
dc.identifier.otherhttps://repository.tudelft.nl/islandora/object/uuid%3Ae0188634-8b62-4439-8fd2-e5b1a1ce3447
dc.identifier.urihttp://hdl.handle.net/2117/118164
dc.description.abstractLaboratory experiments were conducted on a sand-gravel Gilbert delta to gain insight on its dynamics under varying base level. Base level rise results in intensified aggradation over the topset, as well as a decrease in topset slope and topset surface coarsening, the signals of which migrate in an upstream direction. Preferential deposition of coarse sediment in the topset results in a finer load at the topset-foreset break, which creates a fine signature in the foreset deposit. Base level fall has the opposite effects. Entrainment of the topset mobile armor causes a coarsening of the load at the topset-foreset break and so a coarse signature in the foreset deposit. The entrainment of the topset substrate and fine top part of the foreset may follow, which causes a fining of the load and a fine signature in the foreset deposit. The fact that the upstream sediment supply requires a certain slope and bed surface texture to be transported downstream under quasi-equilibrium conditions counteracts the effects of base level change. This information travels in the downstream direction. In nature base level change is likely so slow that the upstream sediment load maintains the topset slope and bed surface texture and so keeps the topset in a quasi-equilibrium state. Base level change is therefore not expected to leave a clear signal in a mixed-sediment Gilbert delta other than a change in elevation of the topset-foreset interface.
dc.format.extent20 p.
dc.language.isoeng
dc.publisherAmerican Geophysical Union (AGU)
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Spain
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subjectÀrees temàtiques de la UPC::Enginyeria civil::Enginyeria hidràulica, marítima i sanitària::Ports i costes
dc.subjectÀrees temàtiques de la UPC::Enginyeria civil::Geologia::Hidrologia
dc.subject.lcshSediments (Geology)
dc.subject.lcshDeltas
dc.subject.otherGilbert delta mixed-sediment morphodynamics image analysis size stratification
dc.titleA sand-gravel Gilbert delta subject to base level change
dc.typeArticle
dc.subject.lemacDeltes
dc.subject.lemacSediments (Geologia)
dc.identifier.doi10.1029/2017JF004428
dc.description.peerreviewedPeer Reviewed
dc.relation.publisherversionhttps://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2017JF004428
dc.rights.accessOpen Access
drac.iddocument23182395
dc.description.versionPostprint (published version)
upcommons.citation.authorChavarrías, V., Blom, Astrid, Orrú, C., Martín-Vide, J.P., Viparelli, E.
upcommons.citation.publishedtrue
upcommons.citation.publicationNameJournal of Geophysical Research: Earth Surface
upcommons.citation.volume123
upcommons.citation.number5
upcommons.citation.startingPage1160
upcommons.citation.endingPage1179


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