摘要
Theinteractionbetweenthewaveandfluidmudlayerplaysanimportantroleinthedevelopmentofsiltcoast.Sedimentisessentiallytransportedintheformofrheologicalflowofmudlayerunderthewaveaction,andontheotherhand,thefluidmudlayerdampsthewaveconsiderably.Thispaperstudiesthelawsofwaveenergydissipationandmudbeddeformation,andthemovementofmudlayerthroughlaboratoryexperiments.Theresultsshowthatthewaveenergydissipationfollowsanexponentiallawalongthepropagationdistance.Thebulkdensityofthemudlayeraffectstherateofthewaveenergydissipationgreatly.Thewavedampingcoefficient(Ki)isafuctionofthemuddensityaffectedgreatlybytherelativewaveheight(H/h).Analysisalsoindicatesthatthemuddensityaffecttherateofmudtransportandthemovingvelocity(Vmax)ofthesurfacemudisinverselyproportionaltothemuddensity.Boththerelativewaveheight(H/h)andwave-dampingcoefficient(Ki)areproportionaltotheVmax.Analysisalsoshowsthatthemudtransportrate(Tr)isproportionaltothewavedampingrate(1-H0/H15),therelativewaveheight(H/h),andinverselyproportionaltothevolumeconcentration(Cv)anddimensionlesscoefficientofH/gT2.
出版日期
2001年02月12日（中国期刊网平台首次上网日期，不代表论文的发表时间）
