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dc.contributor.advisorMoe, Geir
dc.contributor.advisorAlf, Tørum
dc.contributor.authorMoshagen, Hermann
dc.date.accessioned2019-10-15T12:36:55Z
dc.date.available2019-10-15T12:36:55Z
dc.date.issued1984
dc.identifier.issn0809-103X
dc.identifier.urihttp://hdl.handle.net/11250/2622275
dc.description.abstractThe problem of sand wave generation in free surface flow has been presented and its engineering and scientific significance has been pointed out. A survey of the existing literature on the subject has been performed. The survey concludes with a need for improved understanding of the responsible instability mechanism. An in detail study of depth effects on Helmholtz instability, particularly in layers, leads to a generalised version the classical Kelvinthin fluid of the K-H stability model, which in turn is applied to a free surface flow with bed shear. This model is discussed theoretically and physically. As part of this some qualitative experiments are presented and commented on with a view to the theoretical model. The study shows that the actual K-H model contains several of the basic features of sand wave generation.nb_NO
dc.language.isoengnb_NO
dc.publisherNTHnb_NO
dc.relation.ispartofseriesDoktor ingeniøravhandling;Thesis no. P-1-84
dc.subjectsand waves, sediment flow, channel flow, instability, kelvin-helmholtznb_NO
dc.titleSand waves in free surface flow : a study with emphasis on hydrodynamic aspectsnb_NO
dc.typeDoctoral thesisnb_NO
dc.subject.nsiVDP::Technology: 500::Marine technology: 580nb_NO
dc.description.localcodeNTH Thesis - Division of Port and Ocean Engineering, 1984nb_NO


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