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Chapter4TheRheologyofDispersions
4.1Introduction1.WhatisRheologyRheology(流变学):Thestudyofflowanddeformationofmaterials.Material:
solid,liquid,gas,dispersions,andsoon.Why?(1)Scientifically
Inordertounderstandfullytheflowbehaviorofmaterials,someofthebasicphysicallawsorrulesthatmaterialsfollowwhensubjectedtoexternalforcessothatwecanformulatethetheoriestopredictthedeformationandflowofmatterunderagivencondition.(2)EngineeringMaterialsinacolloidalstatearefrequentlypreferredinindustrialprocessingoperations.Thelargesurfaceareasperunitvolumeofcolloidenhancechemicalreactivity,adsorptivecapacity,heattransferrate,andsoon.(3)TechnicallyColloidsdisplayawiderangeofrheologicalbehavior(elastic(弹性的)
likesolids,viscousbehaviorlikeliquid).Itbecomesimportanttounderstandhowtheinteractionforcesandfluidmechanicsofthedispersionsaffecttheflowbehaviorofdispersions.2.FocusonthischapterObjective(目标,任务):Todiscusstheflowbehavioroffluidsanddispersionsandintroducesomeofthebasicideasandtheoriesthatareessentialforunderstandingthestructureandflowpropertiesofcolloids.Newton’slawofviscosity;TheEinstein’stheoryofviscosityofdispersions;(3)ExaminingsomemajorconditionsunderwhichEinstein’stheorybreakdown;(4)Non-Newtonianbehaviorofdispersions.4.2Newton’slawofviscosityDefinitionofcoefficientofviscosityTheliquidbetweenthetwoplatesflowsasalaminarflow.Newton’slawofviscosity:Theshearstressisproportionaltovelocitygradient,theviscosityη
ofthefluidisthefactorofproportionality。(1)τ
istheshearstress;
Fisaforceparalleltothexdirection;Aisareaoftheplate;
ηistheviscosityofthefluid(mPa.s);
dv/dy
isvelocitygradient;γ
istherateofshear(s-1).Viscosityoffluidisthemeasureoftheforceneededwhilethefluidflows.TheviscosityofNewtonianisafunctionoftemperature.Non-Newtonian:ThefluidsdonotobeytheformpredictedbyEq.1.TheapparentviscosityofNon-Newtonianisafunctionoftemperature,shearrateandtimeofshear.Newtonian:ThefluidsobeytheformpredictedbyEq.1.Basedontheanalysisofthermodynamics(热力学)andfluid-dynamics(流体动力学)viscosityoffluidcanbedefinedas(3)IstherateofenergydissipationperunitvolumeEq.3showsthattherateofenergydissipationisproportionaltothesquareofthevelocitygradient,withtheviscosityofthefluidasthefactorofproportionality.Viscosityoffluidisthemeasureoftheenergydissipationwhilethefluidflows.4.3TheEinstein’stheoryofviscosityofdispersionsTheeffectofparticlesontheviscosityofdispersionsThepresenceofacolloidalsizeparticleintheliquidincreasestheviscositybecauseoftheeffectithasontheflowpattern.Theviscosityisdependontheconcentration,size,shapeoftheparticles.2.Einstein’sequationofviscosityofdispersionsCondition:Rigidsphereandlargeenoughcomparedtothesolventmolecules;Diluteofdispersion(Φ<0.1);Noslippageoftheliquidatthesurfaceofthesphere;Thefluidisalaminarflow.Einstein’sequationofviscosityofdispersions(41)η0theviscosityofthesolvent;Φisthevolumefraction(体积分数)occupiedbythesphere.(42)k1-thecoefficientisameasureofconcentrationeffect.Theresultisindependentofparticlesize.Whenconcentrationofparticleishigh3.Functionalforms(常用名词)1)Relativeviscosity(相对粘度)
ηr
>1η-Theviscosityofdispersion(Solution)η0-Theviscosityofsolvent2)Specificviscosity(增比粘度)
Measuringtheviscosityincreasedbyparticles.c-Concentrationofdispersions(solution)
(kg/dm)Measuringtheviscosityincreasedbytheparticles(solute)ofperunitofconcentration.
(代表单位浓度的质点(溶质)对粘度的贡献。)3)Reducedviscosity(比浓粘度)(ηred)
Measuringtheviscosityincreasedbyonlyoneparticle(solutemolecule).
代表单个质点(溶质分子)对粘度的贡献。
4)Intrinsicviscosity(特性粘度)4.Deviations(偏差)
fromtheEiensteinmodel(1)Effectofhighvolumefractions(48)TheviscositycanbecalculatedwithEq.48.(2)EffectsofsolvationandshapesThevolumeofthesolvatedParticleisincreased.Vsol=V2+V1,bVsol-volumeofsolvatedparticleV2-volumeofunsolvatedparticleV1,b-volumeofboundsolventV
Φ(53)m1,b-Themassofboundsolventm2-ThemassofparticleForellipsoids(椭球体)Iftheparticlesaretoolarge,theywilladoptapreferredorientation(定向)intheflowingliquid.IftheyaresmallenoughtobesweptthroughallorientationsbyBrownianmotion,thentheywillincreaseviscositymorethanasphericalparticleofthesamemass.(3)Electroviscous
(电粘性)EffectParticleionsElectricaldoublelayer(双电层)“size”oftheparticleincreased;Theionsdragtheparticlegoback;
Interparticleinteraction4.4Non-NewtonianbehaviorReasonsforNon-NewtonianbehaviorInterparticlehydrodynamicinteraction;Colloidalforces
Electrostaticeffect(静电效应)Polymerlayeradsorbedontheparticles.1.TypesofNon-Newtonianfluids(1)Time-independentfluidA.Binghamplastics(Bingham塑性体)τ-τy=ηplD(τ>τy)(1)
τy-yieldvalue(stress)(屈服值)
ηpl-plasticviscosity(塑性粘度)
D(dv/dy)-rateofshear(剪切速率)Characteristics:a.Thematerialsrequireaminimumamountofstressbeforedeformation;b.Whenτ>τy,fluidstarttoflow;c.ThefluidlikeaNewtonianwhileflows;ηpl=f(T)B.
Pseudoplastic(shear-thinning)fluid(假塑性流体)τ=KDn
(0<n<1)(2)
K-Viscouscoefficient(稠度系数),
K↑→ViscosityD-Rateofshear
,
n-powerfactor(流变指数)
Thedifferencebetweennand1,TheNon-Newtonianbehavior.Characteristics:
Themicrostructureofdispersedphaseisinthestateofanetworkinthreedimensions.apparentviscosity(表观粘度):D,ηa
ηa=f(T,D)C.
Dilatant(shearthickening)fluid(胀流体)τ=KDn
(n>1)(3)
D,ηa
ηa=f(T,D)Characteristics:Thedispersedphaseisparticles.Wetbeachsand.A.
Thixotropicfluid(触变性流体)
whenTandDarefixed,t↑→ηa↓,
ηa=f(T,D,t)
t-timeofshear(2)Time-dependentfluidCharacteristics:Themicrstructureofthefluidprogressivelybreakdownandtheapparentviscositydecreases.Drillingmud,paint.Athixotropic
hysteresisloop(触变滞后环)canbeobtainedbymeasuringthenon-equilibriumshearstressastheshearrateisfirstincreasedandthendecreasedinastandardway.thixotropic
hysteresis
loopofathixotropicfluid.
B.
Rheopecticfluid(反触变性流体)
whenTandDarefixed,t↑→ηa↑ηa=f(T,D,t)Characteristics:Theappliedshearpromotegradualformationoflocalstructureandtheapparentviscosityincreases.Theseparatedparticlesshallbecomeaggregateornetworkundershearing.Suchas
slurry
(水泥砂浆).Rheopectic
hysteresisloop
ofarheopecticfluid.
Asphalteneparticlesat
interphasebetweenoilandwater.C.
Rheapexy(震粘性流体)
Characteristics:Apparentviscosityisincreasedunderlowshearrate,butasshearrateincreasedtheviscositydecreasedagain.Apparentviscositycanberecoveredasoriginalvalueaftershearisstoppedforawhile.
suchasslurryofstarch(淀粉浆糊)D.Visco-elasticfluids(粘弹性流体)Visco-elasticmaterialsdisplay
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