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dc.contributor.authorPuleo, JA
dc.contributor.authorLanckriet, T
dc.contributor.authorConley, Daniel
dc.contributor.authorFoster, D
dc.date.accessioned2016-10-07T16:53:16Z
dc.date.accessioned2017-03-07T19:55:01Z
dc.date.available2016-10-07T16:53:16Z
dc.date.available2017-03-07T19:55:01Z
dc.date.issued2016-07
dc.identifier.issn0378-3839
dc.identifier.issn1872-7379
dc.identifier.otherC
dc.identifier.urihttp://hdl.handle.net/10026.1/8597
dc.descriptionpublisher: Elsevier articletitle: Sediment transport partitioning in the swash zone of a large-scale laboratory beach journaltitle: Coastal Engineering articlelink: http://dx.doi.org/10.1016/j.coastaleng.2015.11.001 content_type: article copyright: © 2015 Elsevier B.V. All rights reserved.
dc.description.abstract

Swash zone sheet flow and suspended sediment transport rates are estimated on a coarse sand beach constructed in a large-scale laboratory wave flume. Three test cases under monochromatic waves with wave heights of 0.74 m and wave periods of 8 and 12.2 s were analyzed. Sediment flux in the sheet flow layer exceeds several hundred kg m− 2 s− 1 during both uprush and backwash. Suspended sediment flux is large during uprush and can exceed 200 kg m− 2 s− 1. Instantaneous sediment flux magnitudes in the sheet layer are nearly always larger than those for suspended sediment flux. However, sediment transport rates, those integrated over depth, indicate that suspended load transport is dominant during uprush for all cases and during the early stages of backwash except in the case for the 12.2 s wave case when the foreshore was steeper. Results could not be obtained for an entire swash event and were particularly truncated during backwash when water depths fell below the elevation of the lowest current meter.

dc.format.extent73-87
dc.languageen
dc.language.isoen
dc.publisherElsevier BV
dc.relation.replaceshttp://hdl.handle.net/10026.1/6284
dc.relation.replaces10026.1/6284
dc.subjectSheet flow
dc.subjectSuspended sediment
dc.subjectSwash zone
dc.subjectSediment flux
dc.subjectVelocity profile
dc.titleSediment transport partitioning in the swash zone of a large-scale laboratory beach
dc.typejournal-article
dc.typeJournal Article
plymouth.author-urlhttps://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000378454800007&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=11bb513d99f797142bcfeffcc58ea008
plymouth.volume113
plymouth.publication-statusPublished
plymouth.journalCoastal Engineering
dc.identifier.doi10.1016/j.coastaleng.2015.11.001
plymouth.organisational-group/Plymouth
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering/School of Biological and Marine Sciences
plymouth.organisational-group/Plymouth/PRIMaRE Publications
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA/UoA07 Earth Systems and Environmental Sciences
plymouth.organisational-group/Plymouth/Research Groups
plymouth.organisational-group/Plymouth/Research Groups/Marine Institute
plymouth.organisational-group/Plymouth/Users by role
plymouth.organisational-group/Plymouth/Users by role/Academics
dcterms.dateAccepted2015-11-02
dc.rights.embargodate2017-07-01
dc.identifier.eissn1872-7379
dc.rights.embargoperiod12 months
rioxxterms.funderEPSRC
rioxxterms.identifier.projectProto-type Experiment of Sediment Transport in Shallow water
rioxxterms.versionofrecord10.1016/j.coastaleng.2015.11.001
rioxxterms.licenseref.urihttp://www.rioxx.net/licenses/under-embargo-all-rights-reserved
rioxxterms.licenseref.startdate2016-07
rioxxterms.typeJournal Article/Review
plymouth.funderProto-type Experiment of Sediment Transport in Shallow water::EPSRC


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