简介:Accordingtotheclassicalelastictheory,thereisalwaysadiscontinuityofrotationangleontheinterfacebetweendifferentmaterials.Thisillogicresultcanbeovercomebythestraingradientplasticitytheory.Inthelightofthistheory,thereisagroupofboundarylayersolutionsnearthein-terface,whichhavemadeimportantadjustmentoftheclassicalresults.
简介:ThefeedbackstabilizationproblemofanonuniformTimoshenkobeamsystemwithrotorinertiaatthetipofthebeamisstudied.First,asaspecialkindoflinearboundaryforcefeedbackandmomentcontrolisappliedtothebeam'stip,thestrictmathematicaltreatment,asuitablestateHilbertspaceischosen,andthewell-posenessofthecorrespondingclosedloopsystemisprovedbyusingthesemigrouptheoryofboundedlinearoperators.Thentheenergycorrespondingtotheclosedloopsystemisshowntobeexponentiallystable.Finally,inthespecialcaseofuniformbeam,somesufficientandnecessaryconditionsforthecorrespondingclosedloopsystemtobeasymptoticallystablearederived.
简介:Inthisarticle,theauthorsdiscussedtheboundarybehaviorfortheCauchy-typeintegralswithvaluesinaCliffordalgebra,obtainedsomeSochocki–PlemeljformulaeandPrivalov–MuskhelishvilitheoremsfortheCauchy-typeintegraltakenoverasmoothsurfacebyrathersimplemethod.
简介:Inthispaper,thesimultaneouseffectsofboundarylayerandtopographyontheinstabilityofEadywaveareinvestigatedbyusinganewparameterizationoftheverticalvelocityatthetopofPBLandtheinfluencesofthestratificationofthePBL,roughnessandtheslopeofterrainareshown.Furthermore,theeffectsoftheboundarylayerfrictionandtopographyongeneralizedEadywavearealsoinvestigated.
简介:Thetraditionalone-dimensionalultrasonicbeamsteeringhastimedelayandisthusacomplicatedproblem.AnumericalmodelofultrasonicbeamsteeringusingNeumannboundaryconditioninmultiplysicsispresentedinthepresentpaper.Thismodelisbasedonthediscretewavenumbermethodthathasbeenprovedtheoreticallytosatisfythecontinuousconditions.Thepropagatingangleofnovelmodelisafunctionofthedistanceinsteadofthetimedomain.Thepropagatingwavefrontsatdesiredanglesaresimulatedwiththesinglelinesourcesforplanewave.Theresultindicatesthatanybeamanglecanbesteeredbydiscretelineelementsresourceswithoutanytimedelay.
简介:根据一系列重要历史的地图,即,华南海岛,Nansha岛,Zhongsha岛,Xisha岛,Yongxing岛和Shidao岛的地点地图,并且太平天国的岛(在1946由中华民国的内部的部的领土的管理部门转存),并且中华民国的管理区域地图在1948出版了,包围华南海岛的击破的线在华南代表瓷器海边界它是连接与的两个,和延期,中国的陆地边界。在当稳固的线被用来代表陆地boundarya时,击破的线被用来代表水边界的那时间,通用方法在然后国际性地被认出的地图使用了。上述观察在为在华南海区域上的国际海上的定界线是有用的华南海提供瓷器海边界的历史、科学的证据。
简介:Astochasticmodelwasdevelopedtosimulatetheflowinheterogeneousmediasubjecttorandomboundaryconditions.ApproximatepartialdifferentialequationswerederivedbasedontheKarhunen-Loeve(KL)expansionandperturbationexpansion.Theeffectofrandomboundaryconditionsonthetwo-dimensionalflowwasexamined.Itisshownthattheproposedstochasticmodelisefficienttoincludetherandomboundaryconditions.Therandomboundariesleadtotheincreaseofheadvarianceandvelocityvariance.Theinfluenceoftherandomboundaryconditionsonheaduncertaintyisexertedoverthewholesimulatedregion,whiletherandomnessoftheboundaryconditionsleadstotheincreaseofthevelocityvarianceinthevicinityofboundaries.
简介:InthispaperanapproximateequationisderivedtodescribesmoothpartsofthestabilityboundaryforlinearHamiltoniansystems,dependingonarbitrarynumberofparameters.Withthisequation,wecanobtainparameterscorrespondingtothestabilityboundary,aswellastothestabilityandinstabilitydomains,pro-videdthatonepointonthestabilityboundaryisknown.Thendifferentialequationsdescribingtheevolutionofeigenvaluesandeigenvectorsalongacurveonthesta-bilityboundarysurfacearederived.Theseequationsalsoallowustoobtaincurvesbelongingtothestabilityboundary.Applicationstolineargyroscopicsystemsareconsideredandstudiedwithexamples.
简介:Glowdischargeisintroducedasanartificialdisturbancetoinvestigatetheevolutionoffirst-andsecond-modeinstabilitiesinahypersonicflatplateboundarylayer.ExperimentsareconductedinaMach6.5quietwindtunnelusingRayleighscatteringvisualizationandparticleimagevelocimetry(PIV).Detailedanalysisoftheexperimentalobservationsisprovided.Itisfoundthattheartificiallyintroduced17kHzdisturbance,whichbelongstothefirst-modefrequencyband,caneffectivelyenhancefirst-modewaves.Moreover,itcanenhancesecond-modewavesevenmoreintensely.Possiblemechanismstoexplainthisphenomenonarediscussed.
简介:Thispaperdescribesthenumericalsimulationofunsteadyflowsduetoincomingwakesand/orvaryingbackpressure,Thesolutionmethodisbasedupontheone-stepfinite-volumeTVDLax-Wendroffscheme.Dualtime-stepapproachandmultigridalgorithmareadoptedtoimprovethecomputationalefficiencyofthebaselinescheme.NumericalresultsforthetransonicunsteadyflowinachannelbumpandtheunsteadyflowinaflatplatecascadeandtheVKIcascadearepresented.
简介:Theglidingbehaviorofedgedislocationnearagrainboundary(GB)incopperunderpureshearstressesissimulatedbyusingmoleculardynamics(MD)method.Many-bodypotentialincorporatingtheembeddedatommethod(EAM)isused.ThecriticalshearstressesforasingledisocationtopassacrossGBsurfaceareobtainedatvaluesofσ_c=23MPa~68MPaand137MPa~274MPafor∑=165smallangletiltGBat300Kand20K,respectively.Thefirstresultagreeswiththeexper-imentalyieldstressσ_y(=42MPa)quitewell.ItsuggeststhattheremightbeoneofthereasonsofinitialplasticyieldingcausedbysingledislocationglidingacrossGB.Inaddition,theremightbepossibilitytoobtainyieldstrengthfrommicroscopicanal-ysis.Moreover,theexperimentalvalueofσ_yatlowtemperatureisgenerallyhigherthanthatatroomtemperature.So,theseresultsareinconformityqualitativelywithexperimentalfact.Ontheotherhand,the∑=25GBistoostronganobstacletothedislocation.Inthiscase,adislocationisabletopassacrossGBunderrelativelylowstressonlywhenitisdrivenbyotherdislocations.Thisistakentomeanthatdislocationpile-upmustbebuiltupinfrontofthiskindofGB,ifthisGBmaytakeeffectontheprocessofplasticdeformation.
简介:SequenceboundaryisstudiedindetailinreferencetothePermianGuadalupianLopingianboundary,basedonhighresolutioncorrelationofconodootzones.Aconceptualsynchronousstratigraphicboundary,correspondingtotheageofthesequenceboundarydatedintheconformableportionofthesequenceboundary,isdefinedasthesequencechronostratigraphicboundary(SCB).Thesequenceboundaryisprovedtobedualinnatureinregardstothesynchronyanddiachroneityofstratigraphicboundaries.Themeritsofthesequenceboundaryinstratigraphicsubdivision,correlationandclassificationareelucidatedincomparisonwiththelithostratigraphicboundary,thebiostratigraphicboundaryandthetraditionalapproachoftheglobalstratotypesectionandpoint(GSSP).ByintegratingthevirtuesofthesequenceboundaryandtheGSSP,itisproposedthattheGSSPshouldbeestablishedintheconformableportionoftherelatedsequenceboundary.Theboundaryestablishedinlightofthisapproachisdefinedas
简介:Thispapergivesanintroductionintothedissipationintegralmethod.Thegeneralintegralequationsforthethree-dimensionalcasearederved.Itisfoundthatforapracticalcalculationalgorithmtheintegralmonentumequationandtheintegralenergyequationaremsotuseful.UsingTwodifferentsetsofmeanvelocityprofilesthehyperbolicalcharacterofadissipationintegralmethodisshown.Testcasesfortwo-andthree-dimensionalboundarylayersareanalysedanddiscussed.Thepaperconcludeswithadiscussionoftheadvantagesandlimitsofdissipationintegralmethods.