dc.creatorFranklin, ED
dc.date2013
dc.date36951
dc.date2014-07-30T14:06:33Z
dc.date2015-11-26T16:23:07Z
dc.date2014-07-30T14:06:33Z
dc.date2015-11-26T16:23:07Z
dc.date.accessioned2018-03-28T23:04:27Z
dc.date.available2018-03-28T23:04:27Z
dc.identifierApplied Mathematical Modelling. Elsevier Science Inc, v. 37, n. 5, n. 3193, n. 3199, 2013.
dc.identifier0307-904X
dc.identifierWOS:000316768900046
dc.identifier10.1016/j.apm.2012.07.027
dc.identifierhttp://www.repositorio.unicamp.br/jspui/handle/REPOSIP/58232
dc.identifierhttp://repositorio.unicamp.br/jspui/handle/REPOSIP/58232
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1268207
dc.descriptionThree-dimensional sand ripples can be observed under steady liquid flows in both nature and industry. Some examples are the ripples observed on the bed of rivers and in petroleum pipelines conveying sand. Although of importance, the formation of these patterns is not completely understood. There are theoretical and experimental evidence that aquatic ripples grow from two-dimensional bed instabilities, so that a straight vortex is formed just downstream of their crests. The proposition of Raudkivi (2006) [18], that three-dimensionality has its origin in a vortex instability, is employed here. This paper presents a linear stability analysis of the downstream vortex in order to obtain the transverse scales of three-dimensional ripples. The obtained wavelength is compared with experimentally observed ripples. (C) 2012 Elsevier Inc. All rights reserved.
dc.description37
dc.description5
dc.description3193
dc.description3199
dc.descriptionPetrobras S.A. [0050.0045763.08.4]
dc.descriptionPetrobras S.A. [0050.0045763.08.4]
dc.languageen
dc.publisherElsevier Science Inc
dc.publisherNew York
dc.publisherEUA
dc.relationApplied Mathematical Modelling
dc.relationAppl. Math. Model.
dc.rightsfechado
dc.rightshttp://www.elsevier.com/about/open-access/open-access-policies/article-posting-policy
dc.sourceWeb of Science
dc.subjectLiquid flow
dc.subjectSediment transport
dc.subjectBed-load
dc.subjectSand ripples
dc.subjectVortex instability
dc.subjectTurbulent Liquid Flow
dc.subjectErodible-bed
dc.subjectNonlinear Instabilities
dc.subjectDune Shapes
dc.subjectVelocities
dc.subjectSelection
dc.subjectChannels
dc.titleThree-dimensional sand ripples as the product of vortex instability
dc.typeArtículos de revistas


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