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ID:33159346
大小:107.00 KB
页数:5页
时间:2019-02-21
《stratification of suspended sediment in open 在开放的悬浮泥沙分层》由会员上传分享,免费在线阅读,更多相关内容在应用文档-天天文库。
1、Rte-bookSuspSedStrat.docSTRATIFICATIONOFSUSPENDEDSEDIMENTINOPENCHANNELFLOWGaryParkerThisdocumentisacompaniontotheExcelworkbookRte-bookSuspSedDensityStrat.xls.DefinitionsConsidersteady,equilibriumopenchannelflowoveranerodiblebedinawidechannelwithupwardnormalprofiles
2、ofstreamwisevelocityandvolumesuspendedsedimentconcentration,wherezdenotesacoordinateupwardnormalfrombed.TheflowhasdepthH,shearvelocityandshearvelocityduetoskinfriction.Thebedhascompositeroughnesskc,wherekcisgivenaswhereUdenotesdepth-averagedflowvelocity.Intheabsenc
3、eofbedformskcbecomesequaltothegrainroughnessks.Intheaboverelations,.Thewaterhasdensityrandkinematicviscosityn.ThesedimentisassumedtobeuniformwithsizeD,densityrsandfallvelocityvs.ThesubmergedspecificgravityofthesedimentisgivenasandtheexplicitparticleReynoldsnumberRe
4、pisgivenaswheregdenotesgravitationalacceleration.ParticlefallvelocityvsisspecifiedbyadimensionlessrelationoftheformwhereandthefunctionalrelationshipitselfisgivenbyDietrich(1982).Basicforms5Rte-bookSuspSedStrat.docTheequationofmomentumconservationfortheflowtakesthef
5、orm(1)wherentdenotesakinematiceddyviscosity.Thecorrespondingformforconservationofsuspendedsedimentis(2)Eddyviscosityntisspecifiedinthefollowingform:(3)wherekdenotestheKarmanconstant,F1andF2arespecifiedfunctions,andRidenotesthegradientRichardsonnumber,givenby(4)Theb
6、ottomboundaryconditionforvelocityisdeterminedbyamatchtotheroughlogarithmiclawatnormalizedreferencebedelevationzr:(5)wherekdenotestheKarmanconstant(0.4).Thebottomboundaryconditionforconcentrationofsuspendedsedimentislikewisegivenintermsofaspecificationofreferencebed
7、concentrationatzr.Intheimplementationoftheworkbookzrissetequalto0.05.DimensionlessformsDefinedimensionlessvelocityandconcentrationasfollows:5Rte-bookSuspSedStrat.docEquations(1),(2),(4)and(5)canthenbereducedto(6)(7)(8)(9)where(10a,b)Inaddition,thenear-bedconditionf
8、ornormalizedconcentrationcbecomes(11)FormsforthefunctionsF1andF2ThestandardformforthefunctionF1istheparabolicone(12)SmithandMcLean(1977)offerthea
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