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Unsteady Boussinesq-type flow equations for gradually-eroded beds: application to dike breaches
Dike breach due to overtopping involves unsteady flow over a curved bed continuously deforming in time due to erosion. The curvatures and slopes on the water surface and the bed profiles indicate that the shallow-water-equations may be inappropriate for modelling purposes. The next degree of mathema...
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Published in: | Journal of hydraulic research 2013-04, Vol.51 (2), p.203-208 |
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description | Dike breach due to overtopping involves unsteady flow over a curved bed continuously deforming in time due to erosion. The curvatures and slopes on the water surface and the bed profiles indicate that the shallow-water-equations may be inappropriate for modelling purposes. The next degree of mathematical approximation is given by the Boussinesq equations accounting for vertical inertia effects. Herein novel unsteady flow equations for a curved erodible bed are developed. Using a Boussinesq-type closure, expressions for the vertical velocity, the pressure distribution and the momentum function are presented. These depend on two parameters relating to the temporal and spatial derivatives of the flow depth, namely bottom elevation and average flow velocity. The model equations are compared with previous unsteady Boussinesq-type models, indicating that the novel formulation is a generalization for erodible beds. The Boussinesq coefficients are further investigated using selected experiments conducted at VAW, ETH. |
doi_str_mv | 10.1080/00221686.2012.739579 |
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The curvatures and slopes on the water surface and the bed profiles indicate that the shallow-water-equations may be inappropriate for modelling purposes. The next degree of mathematical approximation is given by the Boussinesq equations accounting for vertical inertia effects. Herein novel unsteady flow equations for a curved erodible bed are developed. Using a Boussinesq-type closure, expressions for the vertical velocity, the pressure distribution and the momentum function are presented. These depend on two parameters relating to the temporal and spatial derivatives of the flow depth, namely bottom elevation and average flow velocity. The model equations are compared with previous unsteady Boussinesq-type models, indicating that the novel formulation is a generalization for erodible beds. 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Hydrogeology ; Marine and continental quaternary ; Mathematical analysis ; Mathematical models ; open channel flow ; Studies ; Surficial geology ; Unsteady ; Unsteady flow</subject><ispartof>Journal of hydraulic research, 2013-04, Vol.51 (2), p.203-208</ispartof><rights>Copyright International Association for Hydro-Environment Engineering and Research 2013</rights><rights>2014 INIST-CNRS</rights><rights>Copyright International Association for Hydro-Environment Engineering and Research</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c497t-48777225a30dbd89c2cc0c65caeead9bc7e3e2a3294295efa7953832b08a37843</citedby><cites>FETCH-LOGICAL-c497t-48777225a30dbd89c2cc0c65caeead9bc7e3e2a3294295efa7953832b08a37843</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27903,27904</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=27406726$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Castro-Orgaz, Oscar</creatorcontrib><creatorcontrib>Hager, Willi H.</creatorcontrib><title>Unsteady Boussinesq-type flow equations for gradually-eroded beds: application to dike breaches</title><title>Journal of hydraulic research</title><description>Dike breach due to overtopping involves unsteady flow over a curved bed continuously deforming in time due to erosion. 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Hydrogeology</topic><topic>Marine and continental quaternary</topic><topic>Mathematical analysis</topic><topic>Mathematical models</topic><topic>open channel flow</topic><topic>Studies</topic><topic>Surficial geology</topic><topic>Unsteady</topic><topic>Unsteady flow</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Castro-Orgaz, Oscar</creatorcontrib><creatorcontrib>Hager, Willi H.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of hydraulic research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Castro-Orgaz, Oscar</au><au>Hager, Willi H.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Unsteady Boussinesq-type flow equations for gradually-eroded beds: application to dike breaches</atitle><jtitle>Journal of hydraulic research</jtitle><date>2013-04-01</date><risdate>2013</risdate><volume>51</volume><issue>2</issue><spage>203</spage><epage>208</epage><pages>203-208</pages><issn>0022-1686</issn><eissn>1814-2079</eissn><coden>JHYRAF</coden><abstract>Dike breach due to overtopping involves unsteady flow over a curved bed continuously deforming in time due to erosion. The curvatures and slopes on the water surface and the bed profiles indicate that the shallow-water-equations may be inappropriate for modelling purposes. The next degree of mathematical approximation is given by the Boussinesq equations accounting for vertical inertia effects. Herein novel unsteady flow equations for a curved erodible bed are developed. Using a Boussinesq-type closure, expressions for the vertical velocity, the pressure distribution and the momentum function are presented. These depend on two parameters relating to the temporal and spatial derivatives of the flow depth, namely bottom elevation and average flow velocity. The model equations are compared with previous unsteady Boussinesq-type models, indicating that the novel formulation is a generalization for erodible beds. 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subjects | Boussinesq equation Boussinesq equations Curvature Curved curved bed dike Dikes Earth sciences Earth, ocean, space erodible bed Exact sciences and technology Flow control Flow velocity hydraulics Hydrology Hydrology. Hydrogeology Marine and continental quaternary Mathematical analysis Mathematical models open channel flow Studies Surficial geology Unsteady Unsteady flow |
title | Unsteady Boussinesq-type flow equations for gradually-eroded beds: application to dike breaches |
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