Vortex tubes in the wave bottom boundary layer

M. Henriquez, A.J.H.M. Reniers, B. Gerben Ruessink, M.J.F. Stive

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Abstract

The cause of sediment suspension events during flow reversal under waves in the nearshore is not well understood. Vortex tubes and horizontal pressure gradients have been suggested to be the cause of the suspension events. A medium sized wave flume experiment has been conducted to give insight in the hydrodynamics of the wave bottom boundary layer over a fixed single-barred profile. Flow measurements were made with PIV and the swirling strength of the velocity fields were analyzed. Around flow reversal vortex tubes were identified. The vortex tubes had similar size and swirling strength as vortices generated by vortex shedding over a rippled bed. Therefore, vortex tubes under waves in the nearshore could explain the sediment suspension events around flow reversal.
Original languageEnglish
Title of host publicationJubilee Conference Proceedings NCK-days 2012
Subtitle of host publicationCrossing borders in coastal research
EditorsW.M. Kranenburg, E.M. Horstman, K.M. Wijnberg
PublisherUniversity of Twente
Number of pages4
ISBN (Print)978-90-365-3342-3
DOIs
Publication statusPublished - 2012
Externally publishedYes
EventNCK-Days 2012: Crossing borders in coastal research - Enschede, Netherlands
Duration: 13 Mar 201216 Mar 2012

Conference

ConferenceNCK-Days 2012
Country/TerritoryNetherlands
CityEnschede
Period13/03/1216/03/12

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