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dc.contributor.authorHassan, Marwan A.
dc.contributor.authorChartrand, Shawn M.
dc.contributor.authorRadic, Valentina
dc.contributor.authorFerrer Boix, Carles
dc.contributor.authorBuckrell, Emma
dc.contributor.authorMcDowell, Conor
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament d’Enginyeria Gràfica i de Disseny
dc.date.accessioned2022-09-13T13:34:01Z
dc.date.available2023-08-31T00:30:03Z
dc.date.issued2022-09
dc.identifier.citationHassan, M.A. [et al.]. Experiments on the sediment transport along pool-riffle unit. "Water resources research", Setembre 2022, vol. 58, núm. 9, p. e2022WR032796:1-e2022WR032796:76.
dc.identifier.issn0043-1397
dc.identifier.urihttp://hdl.handle.net/2117/372711
dc.descriptionThis is the peer reviewed version of the following article: [Hassan, M. A., Chartrand, S. M., Radić, V., Ferrer-Boix, C., Buckrell, E., & McDowell, C. (2022). Experiments on the sediment transport along pool-riffle unit. Water Resources Research, 58, e2022WR032796. https://doi.org/10.1029/2022WR032796], which has been published in final form at https://doi.org/10.1029/2022WR032796. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Self-Archiving.
dc.description.abstractThis study examines channel dynamics and mixed-load bed load transport through a riffle and pool sequence forced by downstream channel width variations within an experimental flume. The experiment consisted of four runs across which we compare and contrast local and spatially-averaged bed surface texture and topography, sediment transport rates and sediment mobility at five locations across a pool-riffle pair. Sediment transport was measured using mini Helley-Smith (HS) samplers and particle tracers seeded in the monitored riffle and pool. In this study, “local” sediment transport rates were highly variable across the five monitoring locations. The lowest sediment transport rate was recorded at the riffle tail whereas the highest rates were measured at the riffle head and the pool centre. The texture of the bed surface and transported load do not explain measured bedload transport trends and depending on how the measurements are aggregated differing interpretations are supported. In general, the bed texture in the pool was finer than the texture in the riffle, however specific grain-size percentile classes derived from pooled population analysis suggests little to no difference between pool and riffle texture. The combined results highlight the importance of acknowledging and applying analysis techniques to better understand the inherent variability of bedload transport within channel reaches where morphology differs, such as pools and riffles.
dc.language.isoeng
dc.subjectÀrees temàtiques de la UPC::Enginyeria civil::Geologia::Hidrologia
dc.subject.lcshSediment transport
dc.subject.otherGravel-bed streams
dc.subject.otherPool-riffle
dc.subject.otherBed adjustment
dc.subject.otherSediment transport rate
dc.subject.otherParticle mobility
dc.subject.otherPrincipal component analysis
dc.subject.otherSelf-organizing maps (SOM)
dc.titleExperiments on the sediment transport along pool-riffle unit
dc.typeArticle
dc.subject.lemacSediments (Geologia) -- Transport
dc.identifier.doi10.1029/2022WR032796
dc.description.peerreviewedPeer Reviewed
dc.relation.publisherversionhttps://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2022WR032796
dc.rights.accessOpen Access
local.identifier.drac34223732
dc.description.versionPostprint (author's final draft)
local.citation.authorHassan, M. A.; Chartrand, S. M.; Radic, V.; Ferrer-Boix, C.; Buckrell, E.; McDowell, C.
local.citation.publicationNameWater resources research
local.citation.volume58
local.citation.number9
local.citation.startingPagee2022WR032796:1
local.citation.endingPagee2022WR032796:76


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