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简介：Theresultsofmathematicalmodellingofunsteadyflowconditionscoupledwithspecificsedimenttransportrelationsarepresentedhere.SimultaneoussolutionsofthedeSaintVenantequationswiththreedifferenttransportrelations,namelytheEngelund-Hansenequation,Grafequation,andanempiricalequationarepresented.TheresultsobtainedwerecomparedwiththosefromtheFluvial-12programunderthesameinputconditionsandreasonablecorrelationwasobserved.Theadvantagesofthecoupledmethodforsimultaneoussolutionoftheequationscompriseahigherdegreeofaccuracy,thepossibilityofintroductionofanydesiredtransportequationintothemodelandthepossibilityofintroducinganyboundaryconditionsintothemodelalongsideacompleteunsteadyflowmodelling.

简介：Researchonin-channelsandminingisimperativeasitmayhaveasignificantimpactonchannelmorphology.Followingthisquesttoquantitativelycomprehendthephenomenon,experimentalstudiesweredonetoinvestigatethedynamiccharacteristicsofthemigrationofaminingpit.Theevaluationofthemigrationrateofaminingpitinaphysicalscalemodelhasfoundariseinthemigrationrateofthepit'supstreamedgewithincreasingdischarge.Awaveletanalysisappliedforanalyzingscale-dependentmigrationofthebedprofileofaminingpitalsorevealedsimilarfindings.Additionally,thewaveletanalysisexaminedthelength-scaledependentmigrationofaminingpitandadecreaseinthemigrationratehasbeenobservedwithanincreaseinthelengthscale.Theplanformofapit(length-to-widthratio)governstheerosionanddepositionprocessesaroundthepit.Bothphysicalandstatisticalapproachesshowanincreaseinthemigrationratewithanincreaseinthelength-to-widthratioofthepit.Anempiricalformulationhasbeendevelopedforcalculatingthemigrationrateoftheupstreamedgeofaminingpitbasedonpitgeometry(length-to-widthratio),averageflowvelocity,andcriticalshearstressofthebedmaterial.Theresultsalsoshowahigherbedloadtransportrateinthechannelsubjectedtominingascomparedtoaplainbedchannel.

简介：RillerosionisadominantprocessofmorphologicalevolutionoftheLoessPlateauinChina,anddeliveriesmuchloesssedimenttorivers.Datafromtwoflumeexperimentsconductedonthebareandglass-coveredbedsindicatedthatthefillflowdevelopsintoaseriesofrollingwaves.Theshearstressontherillbeddistributesunevenlybothspatiallyandtemporally.Anewmethodbasedontheenergyconservationlawisproposedinthisstudy.Thustherelationshipbetweentherunoffenergyconsumptionfromtheinteractionofwaterflowandslopebedandsoildetachmentisformulated.Theresultsshowedthatthedataforthesoildetachmentrateonslope(Dr)andtheenergyconsumptionofrunoff(E1)fittedwellwithnewly-developedfunction.Therillerosionoccurswhentherunoffenergyconsumptionexceedsacriticalvalue.

简介：在沉积运输的调查，区分休息(AoR)的角度的各种各样的定义是必要的在文学可得到。静态的AoR，斜坡的上面、更低的角度镇静，就在斜坡不稳定性前后的形式，当当沉积谷物连续地是动人的时，动态AoR能被观察时，击倒一个斜面。在现在的学习，一系列实验室实验被进行与0.28-4.38的中部的直径为一致自然沉积测量休息的静态、动态的角度?公里。结果证明不同斜坡角度有不同特征。上面、动态的AoR稍微与增加谷物直径增加，当更低的AoR不对在沉积的变化敏感时，缩放并且可以假定经常的价值。上面、更低的AoR的一般水准等价于动态AoR，并且他们之间的差别与增加谷物直径增加。当在运输，沙丘移植和本地人搜索的水流带来的碎石的调查使用开发时，现在的学习建议休息的不同角度应该小心地被对待。