Long Wave Flow Interaction with a Single Square Structure on a Sloping Beach

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dc.identifier.uri http://dx.doi.org/10.15488/1581
dc.identifier.uri http://www.repo.uni-hannover.de/handle/123456789/1606
dc.contributor.author Bremm, Gian
dc.contributor.author Goseberg, Nils
dc.contributor.author Schlurmann, Torsten
dc.contributor.author Nistor, Ioan
dc.date.accessioned 2017-05-31T11:16:22Z
dc.date.available 2017-05-31T11:16:22Z
dc.date.issued 2015
dc.identifier.citation Bremm, Gian; Goseberg, Nils; Schlurmann, Torsten; Nistor, Ioan: Long Wave Flow Interaction with a Single Square Structure on a Sloping Beach. In: Journal of Marine Science and Engineering 3 (2015), Nr. 3, S. 821-844. DOI: https://doi.org/10.3390/jmse3030821
dc.description.abstract In the context of dam breaks, tsunami, and flash floods, it is paramount to quantify the time-history of forces by the rapidly transient flow to vertical structures and the characteristics of the induced flow patterns. To resemble on-land tsunami-induced flow, a free-surface-piercing structure is exposed to long leading depression waves in a tsunami flume where long waves run up and down a 1:40 smooth and impermeable sloping beach after its generation by a volume-driven wave maker. The structure and its surrounding were monitored with force transducers, pressure gauges and cameras. Preparatory steady-state experiments were accomplished to determine the drag force coefficient of the square cylinder at various water depths. The flow during wave run-up and draw-down acting on the structure resulted in distinct flow pattern which were characteristic for the type of flow-structure interaction. Besides bow wave propagating upstream, a standing or partially-standing wave was observed in front of the structure together with a wake formation downstream, while a von Kármán vortex street developed during the deceleration phase of the flow motion and during draw-down. Force measurements indicated a sudden increase in the stream-wise total force starting with the arrival of the flow front during initial run-up. Lateral velocities showed significant oscillations in correlation with the von Kármán vortex street development. A comparison of the total measured base force with the analytically-calculated share of the drag force revealed that forces were prevailingly drag-dominated. eng
dc.description.sponsorship EC/FP7/Marie Curie International Outgoing Fellowship
dc.language.iso eng
dc.publisher Basel : MDPI AG
dc.relation.ispartofseries Journal of Marine Science and Engineering 3 (2015), Nr. 3
dc.rights CC BY 4.0 Unported
dc.rights.uri https://creativecommons.org/licenses/by/4.0/
dc.subject drag force eng
dc.subject flow-structure interaction eng
dc.subject inertia force eng
dc.subject tsunami on land flow eng
dc.subject vortex shedding eng
dc.subject.ddc 550 | Geowissenschaften ger
dc.title Long Wave Flow Interaction with a Single Square Structure on a Sloping Beach
dc.type Article
dc.type Text
dc.relation.issn 2077-1312
dc.relation.doi https://doi.org/10.3390/jmse3030821
dc.bibliographicCitation.issue 3
dc.bibliographicCitation.volume 3
dc.bibliographicCitation.firstPage 821
dc.bibliographicCitation.lastPage 844
dc.description.version publishedVersion
tib.accessRights frei zug�nglich


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