Please use this identifier to cite or link to this item: http://repositorio.lnec.pt:8080/jspui/handle/123456789/5868
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dc.contributor.authorPinto, L.pt_BR
dc.contributor.authorFortunato, A. B.pt_BR
dc.contributor.authorFreire, P.pt_BR
dc.date.accessioned2007-07-17T14:23:53Zpt_BR
dc.date.accessioned2010-04-26T07:39:43Zpt_BR
dc.date.accessioned2014-10-20T09:50:11Zpt_BR
dc.date.accessioned2016-04-28T14:12:00Z-
dc.date.available2007-07-17T14:23:53Zpt_BR
dc.date.available2010-04-26T07:39:43Zpt_BR
dc.date.available2014-10-20T09:50:11Zpt_BR
dc.date.available2016-04-28T14:12:00Z-
dc.date.issued2006pt_BR
dc.identifier.urihttps://repositorio.lnec.pt/jspui/handle/123456789/5868-
dc.description.abstractSand transport models are often based on semi-empirical equilibrium transport formulae that relate sediment fluxes to physical properties such as velocity, depth and characteristic sediment grain sizes. In engineering applications, errors in these physical properties affect the accuracy of the sediment fluxes. The present analysis quantifies error propagation from the input physical properties to the sediment fluxes, determines which ones control the final errors, and provides insight into the relative strengths, weaknesses and limitations of four total load formulae (Ackers and White, Engelund and Hansen, van Rijn, and Karim and Kennedy) and one bed load formulation (van Rijn). The various sources of uncertainty are first investigated individually, in order to pinpoint the key physical properties that control the errors. Since the strong non-linearity of most sand transport formulae precludes analytical approaches, a Monte Carlo method is validated and used in the analysis. Results show that the accuracy in total sediment transport evaluations is mainly determined by errors in the current velocity and in the sediment median grain size. For the bed load transport using the van Rijn formula, errors in the current velocity alone control the final accuracy. In a final set of tests, all physical properties are allowed to vary simultaneously in order to analyze the combined effect of errors. The combined effect of errors in all the physical properties is then compared to an estimate of the errors due to the intrinsic limitations of the formulae. Results show that errors in the physical properties can be dominant for typical uncertainties associated with these properties, particularly for small depths. A comparison between the various formulae reveals that the van Rijn formula is more sensitive to basic physical properties. Hence, it should only be used when physical properties are known with precision. Keywords: Sediment transport models; Sensitivity analysis; Uncertainty analysis; Monte Carlo methodpt_BR
dc.description.sponsorship******pt_BR
dc.format.extent73 bytespt_BR
dc.format.extent37 bytespt_BR
dc.format.mimetypetext/plainpt_BR
dc.format.mimetypetext/plainpt_BR
dc.language.isoporpt_BR
dc.publisherContinental Shelf Researchpt_BR
dc.relation.ispartofseries******pt_BR
dc.rightsrestrictedAccesspt_BR
dc.titleSensitivity Analysis of Non-cohesive Sediment Transport Formulaept_BR
dc.typeworkingPaperpt_BR
dc.identifier.localedicao******pt_BR
dc.description.pages1826-1839pt_BR
dc.identifier.seminario******pt_BR
dc.identifier.local******pt_BR
dc.description.volume26/15pt_BR
dc.identifier.proc******pt_BR
dc.description.data******pt_BR
dc.description.price******pt_BR
Appears in Collections:DHA/NEC - Comunicações a congressos e artigos de revista

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