简介:Shearthickeningfluids(STFs)areatypeofnon-Newtonianfluids.Intheequilibriumstate,theSTFsareinliquid-state.However,theybecomesolid-stateunderasuddenstrikeorimpact.Andwhenthestrikeorimpactisremoved,theSTFscanturnbacktotheirequilibriumproperties.Thispaperprovidesadetailedreviewonrelevantliteraturerelatedtotheapplicationswithshearthickeningfluids.Itintroducedthefactorsaffectingshear-thickeningbehaviourincludingvolumefraction,particlesize,particleshape,carrierfluidviscosity,temperatureandsomeotherfactors.
简介:TheIrtyshshearzone(ISZ)ofAltairegionisthelineamentstructureofthecollision-suturetype,wheregranitesofKalbacomplexandgranodioritesofZmeinogorskcomplexareexposedtoregionalgneiss-formationandstress-metamorphicalterations.Thisstudyisbasedondetailedstructuralobservationsatspecialgroundsusingopticalandelectronmicroscopy,andonthebehavioranalysisofisotopicsystemsfromalteredgranitoids.WithintheISZareawehaveestablishedthecontinuousrowsofgranitoidstress-metamorphismfrominitialrecrystallizationofprotolite,itscataclasisandmechanicalflaringuptocompleterecrystallizationwithalterationofmineralcompositionandformationofthestreakycomplexesofgranitetectonitesofblastomyloniteandblastocataclasitetypes.Thedirectedalterationofrockshasseveralimpulseandisexpressedbyachangeinmorphologyofmineralgrainsandtheirrelations,magnificationofdeformationcomponentintherockstructure,andformationofnewmineralphasesonthebasisofinitialoneswithoutsurfacefluidization.Attransformationofisotopicsystemsfromgranitoid,theirfeldspars,biotiteandhornblende,wecanobserve'rejuvenation'oftherocksubstratefrom270-290MaforKalbagranitoidsto220-235Mafortheirtectonites,andforRudnyAltaigranodiorites,theirageschangesfrom285-317Mato232-257Mafortheirtectonites.
简介:Thereisacouplingofthermal,mechanical,chemicalandfluidalprocessesinacontinentalshearzone.BothXincheng-XishuiandHetaishearzonesaretypicalcontinentalcrustshearzonesofgreenschistfaciesenvironment.Therepresentativemylonitezonesoftheshearzonesarestudiedwithwholerockmajorandtraceelementanalyses.Thechemicalcompositionalvariationtendenciesinbothshearzonesareverysimilarandthegain-lossratiosofvariouscomponentsinthemyloniticrocksarereflectedinthemassbalanceequations.Theenrichmentofthoseimmobilehigh-field-strenghelementsisconsideredtoherelatedtothevolumelossofthemyioniticrocksinashearzone.BasedonthevolumelossexpressionCs/Co=1/(1-V),thefractionalvolumelosses(V)are37.5%and36.5%-42.3%respectivelyformylonitesandultramylonitesintheXincheng-Xishuishearzoneand11%and28%respectivelyformylonitesandphyllonitesintheHetaishearzone.ThehighvolumelossandlargeremovalofSiO2from
简介:Thetransitiontoturbulenceinflowswherethelaminarprofileislinearlystablerequiresperturbationsoffiniteamplitude."Optimal"perturbationsaredistinguishedasextremaofcertainfunctionals,anddifferentfunctionalsgivedifferentoptima.Weherediscussthephasespacestructureofa2Dsimplifiedmodelofthetransitiontoturbulenceanddiscussoptimalperturbationswithrespecttothreecriteria:energyoftheinitialcondition,energydissipationoftheinitialcondition,andamplitudeofnoiseinastochastictransition.Wefindthatthestatestriggeringthetransitionaredifferentinthethreecases,butshowthesamescalingwithReynoldsnumber.
简介:ThemeasurementresultsbyLaserDopplerVelocimetry(LDV)arecomparedwiththedirectnumericalsimulationresultbyEggelsetal.^[1]foracylindricalpipeflow.Inthecaseofapipeflow,thebiaserrorformeanvelocityisverysmall,becausethelocalturbulentintensityisverysmallalloverthepipecrosssection.Howeverthedifferenceofthecombinationofu'andv'haveconsiderableeffectsonReynoldsshearstress.Fromourinvestigation,itisfoundthattheselectionofcoincidencetimethatisanecessaryparameterforcombinationofu'andv'ismoreimportantinobtainingtheaccurateReynoldsshearstress.Thesuitablecoincidencetimeisselectedforajetflowandtheeffectivenessofcoincidenttimemethodorequaltimeintervalmethodwithcoincidencedataisshown.
简介:Plantcelllinesdifferredgreatlyintheabilitytowithstandshearstresses.Usingto-baccocellsandlicoricecellsasmodelplantcells,westudiedtheeffectsofshearstressesonthevi-abilityofplantcells.OurexperimentswerecarriedoutonahighshearrateCouetterheometerprovidinghomogeneousandconstantshearstressesoflaminarflow.TheviabilitywasdeterminedbyTTC(2,3,5-Triphenyltetrazoliumchloride).Theresultswereasfollows.(1)Theviability(V)droppedexponentiallywithtime(t),namelyV=Exp(-kt),(k>oisaconstant).Thismeantthetenabilityofstatisticalhomogeneity.(2)Thevalueofkwasafunctionofplantcells’mechanicalpropertiesandtheshearstressactingontheplantcells.Theshearratecorrespondingtok=owasthecriticalshearratethattheplantcellscouldwithstand.Itcanbeeasilydetermindedbyextrapo-lation.For7-day-oldtobaccocells,itwas1090s-1andfor9-day-oldlicoricecells,itwas6566s-1.(3)Theplantcellsuspensionswerepseudoplasticfluidsfittingτ=Kγn.Forthetobaccocellsus-pensiontested,n=O.73,andforthelicoricecellsuspensiontestedn=0.7.Thusthecriticalshearstressforthetobaccocellswas25dynes/cm2andforthelicoricecellsitwas80dynes/cm2.(4)Oneoftheirreasonsforlicoricecellstohavegreatertolerancetoshearstressesthantobacaccocellsmaybethegeometricfeaturesofthecellsandthesizesofthecells.Thelicoricecellswererod-shaped,butthetobaccocellsweresphericalandlargerthanthelicoricecells.
简介:学习shear不稳定性的传统的Kelvin-Helmholtz观点不对与联系的盒子合适砍有大风的线在旋涡表砍。从那以后,shear不稳定性成为旋涡表的theinstability。如果速度被旋涡表导致,不平等(1?Rr+Rid)>0并且U(v,t)>U((t))成为旋涡表不稳定性的标准。这个标准显示那1)环境地的布置制止沿着shear线发展的骚乱。2)在那里多存在在shear的不稳定的过程的鈥攕c淡色啤酒相互作用排队。为不稳定性的必要条件的计算也在这篇论文被介绍。关键词砍线-导致的速度-旋涡表的不稳定性这个工作被工程在严重MesoscaleCovective的动态学习上在资助G1998040907下面并且由关键工程在中国在构词的机制和重要气候和天气灾难的预兆的理论的学习上支持系统在资助No.49735180下面由中国的国家自然科学基金会赞助了。
简介:Experimentalandnumericalstudieshaveshownsimilaritiesbetweenlocalizedturbulenceinchannelandpipeflows.Byscalinganalysisofadisturbed-flowmodel,thispaperproposesalocalReynoldsnumberReMtocharacterizethethresholdoftransitiontriggeredbyfinite-amplitudedisturbances.TheReMrepresentsthemaximumcontributionofthebasicflowtothemomentumratiobetweenthenonlinearconvectionandtheviscousdiffusion.ThelowercriticalReMobservedinexperimentsofplanePoiseuilleflow...
简介:<正>Irtyshshearzoneisastretched,butrelativelynarrownearfaulttectoniczone,whichischaracterizedbythefollowingfeatures:a)generalsturctureanisotropy(310-320o)withpre-dominanceofsymmetricalrelationshipsofplanarandlineartypes;b)predominantdevelop-mentofbendedblastomyolnite,blastocataclasiteandmetamelangefomations;c)regional,butnon-uniformfoliationofricksandgeneralmanifestationofstructuresoftheshearingflow;d)separationofnumerouslensesofmingmatite-likeandpegmatoidformations,smallintrusionsofleucocraticgranites,granite-porphyresandgranite-aplitesanddike-likebodiesofgabbro-dyabaesandultrabasicrlcks,rarely.
简介:Previousconstitutivemodelsofgraniteshearcreephavetwolimitations:(1)althoughmoisturegreatlyaffectsgraniteshearcreepbehavior,currentlytherearenoconstitutivemodelsthatincludethisfactor;(2)therearealsonomodelsthatincludeanaccelerationstage.ThispaperpresentsanimprovedBurgersconstitutivemodelwiththeadditionofadamageparametertocharacterizethemoistureeffectandusesanonlinearrelationequationbetweenstressandstrainforinclusionastheaccelerationstage.Thedamageparameterisdeterminedfromgranitecreepexperimentunderfourdifferentmoisturecontents(0%,0.22%,0.49%,and0.79%).Thenonlinearrelationequationisobtainedbyfittingadatasetofstainversustimeunderfivedifferentloadingstages.Toverifythepresentedmodel,acreepexperimentwasconductedonothergranitesamplesandtheresultsshowthatthemodelagreeswellwiththeexperimentalobservationdata.
简介:THECISKMECHANISMANDTHEINERTIALGRAVITATIONALWAVESINSHEARFLOWWuHong(吴洪);XiaYoulong(夏友龙)andZhengZuguang(郑祖光)(BeijingInstituteofM...
简介:Lyapunov'ssecondmethodwasusedtostudythenonlinearstabilityofparallelshearflowsforstress-freeboundaries.Byintroducinganenergyfunctional,itwasshownthattheplaneCouetteandplanePoiseuilleflowsareconditionallyandasymptoticallystableforallReynoldsnumbers.Inparticular,totwo-dimensionalperturbations,bydefiningnewenergyfunctionalstheunconditionalstabilityofthebasicflowswasproved.