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dc.contributor.authorWang, Jingbo
dc.contributor.authorFaltinsen, Odd Magnus
dc.contributor.authorLugni, Claudio
dc.date.accessioned2019-12-19T08:13:53Z
dc.date.available2019-12-19T08:13:53Z
dc.date.created2019-08-28T09:39:24Z
dc.date.issued2019
dc.identifier.citationPhysics of Fluids. 2019, 31 (2), .nb_NO
dc.identifier.issn1070-6631
dc.identifier.urihttp://hdl.handle.net/11250/2634070
dc.description.abstractWe investigate the unsteady hydrodynamic force of solid objects vertically entering water with an air cavity behind the falling body. Physical models are proposed to represent the force components corresponding to the body acceleration, the gravity, and the velocity of the body and the fluid particles. The theoretical or numerical solutions of the physical models are presented to understand the evolution of the force components. The body-acceleration force component is expressed as the high-frequency added mass times the body acceleration. Near the undisturbed free surface, the added mass grows strongly with increasing the submerged depth. It tends to be steady after the submerged depth is greater than a few characteristic lengths. The gravity force component consists of an upward hydrostatic term and a downward dynamic term. Generally, the hydrostatic term, which is obtained by integrating the gravity term in Bernoulli’s equation over the wetted body surface, is much larger than the gravity force component. For the three-dimensional bodies, the gravity force component is found to vary as a power of the submerged depth, where the exponent is about 0.83. The velocity force component is represented as the drag coefficient defined by the V-squared law, which is characterized by the body geometry. The drag coefficient may experience three successive stages with increasing the submerged depth.nb_NO
dc.language.isoengnb_NO
dc.publisherAIP Publishing, American Institute of Physicsnb_NO
dc.titleUnsteady hydrodynamic forces of solid objects vertically entering the water surfacenb_NO
dc.typeJournal articlenb_NO
dc.typePeer reviewednb_NO
dc.description.versionacceptedVersionnb_NO
dc.source.pagenumber18nb_NO
dc.source.volume31nb_NO
dc.source.journalPhysics of Fluidsnb_NO
dc.source.issue2nb_NO
dc.identifier.doi10.1063/1.5057744
dc.identifier.cristin1719373
dc.description.localcodeThis is the authors’ accepted and refereed manuscript to the article. This article may be downloaded for personal use only. Any other use requires prior permission of the author and AIP Publishing. The following article appeared in Physics of Fluids 31, 027101 (2019) and may be found at https://doi.org/10.1063/1.5057744nb_NO
cristin.unitcode194,64,20,0
cristin.unitnameInstitutt for marin teknikk
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.qualitycode2


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