Discrete particle simulations of bubble-to-emulsion phase
mass transfer in single-bubble fluidized beds
Citation for published version (APA):
Tan, L., Roghair, I., & van Sint Annaland, M. (2017). Discrete particle simulations of bubble-to-emulsion phase
mass transfer in single-bubble fluidized beds. Particuology, 33, 80-90.
https://doi.org/10.1016/j.partic.2016.09.008
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10.1016/j.partic.2016.09.008
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ContentslistsavailableatScienceDirect
Particuology
jou rn al h om ep a g e :w w w . e l s e v i e r . c o m / l o c a t e / p a r t i c
Discrete
particle
simulations
of
bubble-to-emulsion
phase
mass
transfer
in
single-bubble
fluidized
beds
Lianghui
Tan,
Ivo
Roghair,
Martin
van
Sint
Annaland
∗ChemicalProcessIntensification,MultiphaseReactorsGroup,DepartmentofChemicalEngineering&Chemistry,EindhovenUniversityofTechnology,P.O. Box513,5600MBEindhoven,TheNetherlands
a
r
t
i
c
l
e
i
n
f
o
Articlehistory: Received4July2016
Receivedinrevisedform22August2016 Accepted8September2016
Availableonline6February2017 Keywords:
Masstransfer Discreteparticlemodel Fluidizedbed Bubble-to-emulsion
a
b
s
t
r
a
c
t
AclassicalEuler–Lagrangianmodelforgas–solidflowswasextendedwithgascomponentmass conser-vationequationsandusedtoobtainfundamentalinsightsintobubble-to-emulsionphasemasstransferin bubblinggas–solidfluidizedbeds.Simulationsofinjectedsinglerisingbubblesunderincipient fluidiza-tionconditionswerecarriedout,usingGeldart-Aand-Bparticles.Phenomenaobservedinthesimulations andthoseofvarioustheoreticalmodelsusedtoderivephenomenologicalmodelswerecomparedto chal-lengetheassumptionsunderlyingthephenomenologicalmodels.Thebubble-to-emulsionphasemass transfercoefficientscalculatedforthesimulationsusingGeldart-Bparticleswereinagoodagreement withpredictionsmadeusingtheDavidsonandHarrison(1963)model.Thebubble-to-emulsionphase masstransfercoefficientsforGeldart-Aparticleswere,however,muchsmallerthanthepredictions obtainedfromtheoreticalmodels(e.g.ChibaandKobayashi(1970)).Thenewlydevelopedmodelallows adetailedanalysisofvarioushydrodynamicaspectsandtheireffectsonthemasstransfercharacteristics inandaroundrisingbubblesinfluidizedbeds.
©2017ChineseSocietyofParticuologyandInstituteofProcessEngineering,ChineseAcademyof Sciences.PublishedbyElsevierB.V.Allrightsreserved.
Introduction
Gas–solid fluidized bed reactors are often used in process
industriesowingtotheirexcellentmixingandheattransfer char-acteristics.Itiswellknownthatbubblesprevailinthesebedsand theirdynamicsareresponsiblefortheagitationofsolidsandthe accompanyingfavorableheatandmasstransfercharacteristicsof fluidizedbeds.Animportantfoundationforarationaldesignof flu-idizedbedreactorsisathoroughunderstandingofthemasstransfer
processes in fluidized beds,specificallythe bubble-to-emulsion
phasemasstransfer.Thisphenomenonoccursviathecombined
effectsofgasdiffusion,coherentgasflowandsolidsmotion car-ryingadsorbedgasatoms (Davidson& Harrison,1963;Kunii&
Levenspiel,1991).
Single-bubblefluidizedbedsandfreelybubblingfluidizedbeds
havebeenusedinpastdecadestostudythebubble-to-emulsion
phase masstransfer, both experimentally and numerically(a.o.
Dang,Kolkman,Gallucci,&vanSintAnnaland,2013;Deshmukh,
vanSintAnnaland,&Kuipers,2007;Hernández-Jiménez,
Gómez-García,Santana,&Acosta-Iborra,2013;Patil,vanSintAnnaland,&
∗ Correspondingauthor.Fax:+31402475833.
E-mailaddress:M.v.SintAnnaland@tue.nl(M.vanSintAnnaland).
Kuipers,2003;Pavlinetal.,2007).Phenomenologicalmodels,used
forthedesign ofindustrial-scalereactors,canonlyprovide reli-ablepredictionswhenaccuratemasstransfercoefficientsareused. Untilnow,mostcorrelationsforthesecoefficientshavebeenbased on(i)analytical considerationsand(ii)experimentsusing
inva-sivemeasurementtechniques.Severalproblemsarisewhenusing
phenomenologicalmodels.First,variousassumptionsaremadeto
reducethemathematicalanalysis,butthescopeoftheirvalidityhas notyetbeenanalyzedindetail.Second,theinvasiveexperimental
techniquesmaydisturbtheflow andare limitedtopoint
mea-surements.Noninvasiveopticaltechniques(e.g.,Dangetal.,2013;
Mülleretal.,2006;Pavlinetal.,2007Roels&Carmeliet,2006)have
beendevelopedinthemeantime,butdetailedunderstandingofthe
underlyingmechanismsremainsoutofreachparticularlyowing
todifficultiesinmeasuringthegasconcentrationintheemulsion phase(Dangetal.,2013).
Numericalsimulations(i.e.,computationalfluiddynamics)can shedmorelightonthedetailedprocessofinterphasemasstransfer.
Patiletal.(2003)andHernández-Jiménezetal.(2013),forinstance,
employedatwo-fluidmodel(TFM,employingtheEuler–Euler
tech-nique)forfluidizedbedscomprisingGeldart-Bparticles.Patiletal.
(2003)foundthattheDavidsonandHarrison(1963)model
pre-dictedthemasstransferforsingleinjectedbubblesreasonablywell, buttheirresultsgaveabubblesizeevolutionandtracergas
con-http://dx.doi.org/10.1016/j.partic.2016.09.008
Nomenclature A Area(m2) c Numberofspecies d Particlediameter(m) Db Bubblediameter(m) D Diffusioncoefficient(m2/s) e Coefficientofrestitution f Volumefraction
Fcontact,a Contactforceofparticlea(N)
g Gravitationalacceleration(m/s2)
I Momentofinertia(kgm2)
k Springstiffness(N/m)
K Masstransfercoefficient(s−1)
ma Particlemass(kg)
M Molarmass(kg/mol)
Np Particlenumber
P Pressure(Pa)
R Gasconstant(J/molK)
Sp Particledragsourceterm(N/m3)
t Time(s)
T Temperature(K)
ug,va Gasandsolidvelocities(m/s)
U Velocity(m/s)
V Volume(m3)
x Molefraction
y Massfraction
Greeksymbols
ˇ Inter-phase momentum exchange coefficient
(kg/m3s)
ε Volumefraction
Dampingcoefficient
Gasphaseshearviscosity(Pas)
f Frictioncoefficient
Density(kg/m3)
Stresstensor(Pa)
Subscripts a,p Particle b Bubble bc Bubble-to-cloud be Bubble-to-emulsion ce Cloud-to-emulsion A,B Gascomponent g Gas i,j Component
mb Minimumbubblingfluidizationcondition
mf Minimumfluidizationcondition
n Normaldirection t Tangentialdirection w Wake inj Injection diff Diffusion Acronyms
CFD Computationalfluiddynamics
DPM Discreteparticlemodel
TFM Two-fluidmodel
centrationthatwereinconsistentwiththeresultsofexperiments conductedbyDangetal.(2013).Hernández-Jiménezetal.(2013), meanwhile,obtainedresultsthatwereingoodagreementwiththe
DavidsonandHarrison(1963)modelforsingle-injectedbubbles
butfoundthatthemasstransfercoefficientsweremorethantwice thosepredictedwhenusingfreelybubblingfluidizedbeds.
Itwillbepossibletoidentifythemostimportantaspectsofthe interphasemasstransferwithmodelsofferinggreaterdetail.While
theTFMmakesvariousassumptions todescribetherheologyof
theemulsion phase,theparticle–particle interactions aretaken intoaccountdeterministicallyinadiscreteparticlemodel(DPM,
employingaEuler–Lagrangetechnique).TheDPMmodelcan
there-foreprovidemoredetailedinsightintotheprevailingphenomena
thantheTFMmodelandallowsthesimulationofsmaller
parti-cles(e.g.,Geldart-Aparticles).Geldart-Aparticlesareoftenusedin industrialfluidizedbeds(typicallyfluidcatalyticcrackingcatalyst) andareofinterestinthedesignofmicrofluidizedbeds(e.g.,Tan,
Roghair,&vanSintAnnaland,2014,2016).
Thepresentworkusesastate-of-the-artDPMmodelextended
withgascomponentconservationequations tocharacterize the
interphasemasstransferprocessesingas–solidfluidizedbeds com-prisingGeldart-BandGeldart-Aparticles.Themodelwillbeused tosimulatesingleinjectedbubblesthatrisethroughanincipiently
fluidizedbed,analogoustotheexperimentscarriedoutbyPatil
etal.(2003)andDangetal.(2013),butwithoutthespecific
lim-itationsinherenttotheirtechniques.Additionally,thetracergas concentrationintheemulsionphaseisnotneglectedbutanalyzed forthecomputationofthemasstransfercoefficient.
Thissectioncontinueswithashortoverviewoftheavailable correlationsforthebubble-to-emulsionphasemasstransfer coeffi-cient,whichwillbeusedinthecomparisonwithsimulationresults.
Inthefollowingthreesections,theDPMmodelisthenoutlined
and a detailed analysisof mass transfer processesin Geldart-B
andsubsequentlyGeldart-Aparticlesisdescribed.Adiscussionand conclusionsarefinallypresented.
Phenomenologicalmodelsforbubble-to-emulsionmasstransfer Severalcorrelationshavebeenreportedintheliteratureforthe predictionofthemasstransfercoefficients.Thederivationofthese correlationsusuallyassumesagascloudbetweenabubbleandthe emulsion(bulk)phase,originallydeemedasathinregion surround-ingthebubblewitharelativelyhighsolidsholdupcomparedwith
thebulkemulsion.Davidsonfirstsuggestedtheexistenceofthe
gascloudingas–solidbubblingfluidizedbeds(Rowe,Partridge,&
Lyall,1964).ThepioneeringmodelofDavidsonandHarrison(1963)
hasbeenwidelyusedinphenomenologicalmodelsforlarge-scale
fluidizedbedreactors.Intheirmodel,thetotalmasstransfer con-sistsofaconvectiveflowfromthebubblestotheemulsionphase anddiffusionfromthebubblestothecloud.KuniiandLevenspiel
(1991)followedtheirapproachandproposedanextension
con-sideringtwoconsecutivetransfersteps,namelythetransferfrom thebubbletothecloudandthatfromthecloudtotheemulsion.
AccordingtothestreamfunctionderivedbyMurray(1965)and
ChibaandKobayashi(1970)assumedthatthegascompositionin
thecloudandbubbleisuniformandthatthemasstransfer limita-tionislargelygovernedbydiffusionthroughthesurfacebetween
thecloudandemulsionphases.Table1summarizestheequations
usedtoestimatethebubble-to-emulsionmasstransfercoefficient
forthemostpopularphenomenologicalmodels,togetherwiththe
mainassumptionsuse
Numericalmethod
Extendeddiscreteparticlemodel
Thesoft-sphereDPMemployedinthisstudyisbasedonthe
pioneeringworkofTsuji,Kawaguchi,andTanaka(1993)andwas
Table1
Phenomenologicalmodelsforthebubble-to-emulsionmasstransfercoefficientKbe.
Reference Equations Dimension Mainassumptions
DavidsonandHarrison(1963) Kbe=
4 Db
0.6D1/2i g Db 1/4 +2Umf 2D (1)masstransferfromthebubbletotheemulsionby moleculardiffusionandabulkflowtoandfromthe bubble;(2)perfectmixinginthebubbleandtheemulsion phase;(3)circularorsphericalbubblewithconstantsize; (4)bubblesinalargevolumebed;(5)diffusionfrom sphericalcapbubblesurfacewithanoseangleof100◦ Kbe=4.5
Umf Db +5.85 D1/2i g1/4 D5/4b 3DKuniiandLevenspiel(1991)
Kbc=4.5
Umf Db +5.85 D1/2i g1/4 D5/4 b3D (1)Davidsonmodelforthebubbleandthegasflowatthe bubble;(2)theemulsionvoidageisobtainedatminimum fluidizingconditions;(3)Higbiepenetrationmodel (Hiegbe,1935)forthecloudtoemulsionmasstransfer coefficient;(4)twoconsecutivesteps:transferfromthe bubbletothecloudandfromthecloudtotheemulsion phase Kce=6.77
DiεmfUb D3 b 1/2 3D Kbe= 1 1 Kbc+ 1 Kce 3DChibaandKobayashi(1970)a Kbe=
4.52 1−fw
D iε2mfUb D3 b 1/22D (1)uniformgascompositioninthecloudandbubble;(2) constantbubblevolumeandbubblerisevelocity;(3) circularorsphericalcapbubbleandcircularorspherical clouds;(4)gasandparticleflowaroundthebubblefollow theanalysisbyMurray(1965);(5)thegasflowinthe emulsionphaseisinplugflow
Kbe= 6.78 1−fw
D iε2mfUb D3 b 1/2 3DaIntheliterature,theChibaandKobayashi(1970)modelisoftencitedwiththeexpressionforthemasstransfercoefficientk
gintermsofthesurfaceareaofthecloud.In
thisstudy,forthesakeofconsistency,wedenotethemasstransfercoefficientKbebasedontheunitarea(twodimensions)orvolume(threedimensions)ofthebubble.
(1996)andYe,VanderHoef,andKuipers(2004).Itisapopular
Euler–Lagrangemodelwithadiscretedescriptionoftheparticulate phaseandacontinuousdescriptionofthegasphase,andithasbeen
widelyusedinhydrodynamicstudiesofgas–solidfluidizedbeds.
Asetofthree-dimensionalvolume-averagedNavier–Stokes
equa-tionsforcompressibleflowaresolvedonthecellsofanEuleriangrid forthegas-phasehydrodynamics,assumingidealgasbehavior.For theparticlephase,Newton’ssecondlawofmotionisappliedtoeach individualparticletotraceitspositionandvelocitywhiletaking intoaccountparticle–particleandparticle-wallcollisions.Because theEuleriangridcellsarelargerthantheparticlediameter,the detailsoftheinteractionsbetweenthegasphaseandparticlesare unresolvedandconstitutivecorrelationsarerequiredtocompute
momentumexchangebetweenthetwophases.
Themainequationsofthemodelusedinthisstudyare summa-rizedinTable2.TheclassicdragforcecorrelationfromErgun(1952)
andWenandYu(1966)isusedforthegas–particleinteraction.The
contactforceresultingfromparticle–particleand/orparticle-wall interactionsiscalculatedusingthelinearspringanddashpotmodel proposedbyCundallandStrack(1979).Theparticlespring
stiff-nessconstantisanimportantinputparameteranditiscommon
practicetouseavaluemuchsmallerthanthetruevaluederived frommaterialproperties,becauseitallowsagreatertimestepto
beusedwithoutnoticeablyaffectingthehydrodynamicsandthus
reducestherequiredcomputationaltime(Tsujietal.,1993).Here,
wechoosevaluessuchthatthemaximumoverlapbetween
inter-actingparticlesandparticle-wallatanytimestepislessthan1% oftheparticlediameter.Foramoredetailedexplanationofthis model,wereferthereadertoourpreviouspapers(Tanetal.,2014, 2016)andreviewsbyDeen,vanSintAnnaland,VanderHoef,and
Kuipers(2007),andZhu,Zhou,Yang,andYu(2008).
The transport of chemical components is described using a
nonstationaryconvection–diffusionequationforcomponenti.For binarygassystemswithcomponentsAandB,Fick’slawcanbeused forthemoleculardiffusionmassfluxji=−DAB
∇
yA,usingyAtodenotethemassfractionofcomponentA,whichisemployedinthe gascomponentconservationequationusedinthisstudy(Table2). ThisnovelaspecthasbeenexplainedindetailbyTanetal.(2016).
TheDPMhasbeenextensivelyusedtoexaminethe
hydrody-namiccharacteristicsofgas–solidfluidizedbedsindetail(e.g.,Li
&Kuipers,2007;Tanetal.,2014;Wang,VanderHoef,&Kuipers,
2010;Xu&Yu,1997;Yeetal.,2004).Theextensionforthe
com-ponent conservation calculation has been carefully verified by
carryingoutsimulationsforsimplifiedsystemsandcomparingthe resultswiththeoreticalsolutions,aspresentedbyTanetal.(2016). Simulationconfiguration
Bubble-to-emulsionphasemasstransferisinvestigatedby sim-ulatingsingle-bubbleinjectionsofCO2 tracergasintoafluidized
Table2
Maingoverningequationsofthesoft-sphereDPMextendedwithgascomponent conservationequations.
Gasphasecontinuityequation: ∂(εgg)
∂t + (∇·εggug)=0 Gasphasemomentumequation:
∂(εggug)
∂t +∇· (εggugug)=−εg∇Pg−Sp−∇·(εgg)+εggg Gasphaseequationofstate:
g=MRTgPgwithMg=
yi Mi −1 Gasphasestresstensor:g=g
∇ug+∇uTg −g−23g (∇·ug) I Gas–solidmomentumexchangerate:ˇ=
⎧
⎨
⎩
3 4CD gεg(1−εg)ug−va dp ε−2.65g εg≥0.8 150(1−εg) 2 g εgd2p +1.75g(1−εg)ug−va dp εg<0.8 TheporosityinDPMsimulation:εg,cell=1−Vcell1
∀a∈cell fa cellV a pEquationsofmotionforeveryparticle: madvdta =mad
2ra
dt2 =−Va∇Pg+Vεapˇ(ug−va)+mag+Fcontact,a Iadwdta=Ta
Gascomponentconservationequations: ∂
∂t(εggyi)+∇· (εggyiug)=∇· (εggDi∇yi) Closureequationforcomponenti=0:y0=1−
c
i=1 yi
Viscosityofagasmixture:g=
i xii jxiij ij=1+ij 1/2Mj Mi 1/42 81+Mi Mj 1/2
Fig.1. Snapshotsofthetracergasconcentrationinthecentralsliceofthefluidizedbedatdifferentmomentsintimefromthebeginningoftheinjection(fromt=0to 0.16swithstepsof0.02s),wherethebubbleisdepictedwithdifferentthresholdvaluesoftheporosity(0.7−0.85)(bedwidth=6×10−2m,dp=400–600m,Uinj=6m/s, tinj=0.075s).
bedmaintainedatminimumfluidization(forbedsusingGeldart-B particles)orminimumbubblingconditions(forbedsusing Geldart-Aparticles).N2isusedasthebackgroundfluidizationgas.Afteran
initial1sofincipientfluidization,thebubbleisinjectedby set-tingthecentralcellsatthebottomboundary(i.e.,thenozzle)to theinflowofCO2 usingaprescribedinjectionvelocity.Thecells
areswitchedbacktoN2attheincipientfluidizationvelocityafter
theinjectionis finished.Theinjectiontime required for gener-atingspecificbubblesizesisdeterminedinseparatesimulations beforehand.
Aconstantmolecular(binary)diffusioncoefficientofCO2inN2
isusedtodescribethetracergasdiffusivity.ForGeldart-Aparticle simulations,thediffusioncoefficientofCO2isalsoincreasedbya
factorof3toinvestigatetheeffectofgasdiffusivity.Thenozzlefor gasinjectionisatthecenterofthebottomplate.
ThesimulationsusingGeldart-Bparticlesaresetupaccording totheconditionsofexperimentsconductedbyDangetal.(2013). Thebedwidthtakesvaluesof4cm(matchingthebedwidthinthe experiments),5and6cm.Similartothecaseintheexperiments, Geldart-Bparticleshaveadensityof2525kg/m3andaverage
Fig.2.Snapshotsofthestreamlinesthroughthebubbleinthecentralsliceofafluidizedbedfrom0.06to0.12safterthetracergasisinjected(bedwidth=6×10−2m,
dp=400–600m,Uinj=6m/s, tinj=0.075s).
with=5.0×10−5m).Theminimumfluidizationvelocityofthese
particlesis determined bysimulations using thepressure drop
methodas0.22m/s(0.206m/s inthereferencedpaper).No-slip
boundaryconditionsareappliedtothesidewallsofthebedinthese simulations.
The Geldart-A particles employed in the present study are
monodispersedparticleswithadiameterof100manddensity
of1500kg/m3.VanderWaalsforcesareneglectedinthisstudy.
Heretheminimumbubblingfluidizationvelocity(9.0×10−3m/s), determinedinsimulationsaccordingtothestandarddeviationof thepressuredropoverthebed,isusedasthebackground fluidiza-tionvelocity.Becausemanyparticlesareusedtoallowthebubble
somerisingtime,pseudo-two-dimensional(2D)fluidizedbedsare
simulatedtoreducethecomputationalcost.Thebeddepthisonly 6timestheparticlediameterandafree-slipboundaryconditionis thusappliedtothefrontandbackwalls.
Forallsimulations,thepressureatthetopoutletisspecifiedas theatmosphericpressure(101,325Pa).Particlesareinitiallyplaced regularlylayerbylayeratthebottomofthebedwithsmall ran-domfluctuating translationalandrotational velocitiestoensure thatthesystemisinanasymmetricfluidizedstatefromthestart, andthesystemisleftatminimumfluidizationconditionsfor1s.
Table3summarizesthemainparametersusedinthesimulations.
TheparametersintheDPMmodelforGeldart-Bparticles,suchas therestitutionandfrictioncoefficients,werefirsttestedwith sim-ulationsettingsclosesttotheexperimentalsettingsusedbyDang
etal.(2013).Goodagreementwasfoundwithregardtothemass
transferphenomena(seethesnapshotsshowninFig.1),andthe bubblesizeasafunctionoftimecompareswellwiththeresultsof theexperiments.Notethatdespitethegreatsimilarity,the simula-tionscannotbeusedforanexactone-to-onecomparisonwiththe experiments.Theanalysisandresultingmasstransfercoefficient aresensitivetothegasinjectionandbubbleformationtime,and
Dangetal.(2013)usedahighinjectionvelocityandstoppedthe
injectionbeforethebubbleformationwascomplete.Additionally, theiranalysisforthebubble-to-emulsionmasstransfercoefficients
startedbeforethebubblehadcompletelyformedanddetached.
Theseaspectscanbecontrolledmuchmoreaccuratelyinthe sim-ulationsandhencedifferfromthoseintheexperiments.
Calculationofthemasstransfercoefficient
ThemasstransfercoefficientKbecanbecalculatedfroman
inte-gralmassbalanceofthetracergasinthebubble(definedasan
enclosedregionwithporosityexceedingapredefinedthreshold): d
CCO2,bVb dt =−Kbe CCO2,b−CCO2,e Vb. (1)ToanalyticallysolveEq.(1),theaverageconcentrationofthe tracergas(inthiscaseCO2)intheemulsionphaseisassumed
neg-ligible(andthus settozero). Wekeep thebubblevolume(and
thusdiameter)constantbyintegratingoverashorttimeduring
whichthebubblediameterisrelativelyconstant.Weusethe time-averageddiameterforfurtheranalysis.AspresentedbyDangetal.
(2013),forapseudo-2Dbedhavingasinglebubblewithaninitial
averagedtracergasconcentrationofCCO2,b(0),andassuminga neg-ligibleconcentrationintheemulsionphase(CCO2,e=0),integration yields CCO2,b(t) CCO2,b(0)
D b(t) Db(0) 2 =exp (−Kbet) , (2)whereDb(0) istheinitialbubblediameterandDb(t) isthebubble
diameterattimet.Byplottingln
CCO2,b(t) D2
b(t) /CCO2,b(0) D
2 b(0)
asafunctionoftime,themasstransfercoefficientKbecanbe
cal-culatedfromtheslopeofthelinearcorrelationaccordingtoEq.
Table3
SummaryofthemainsimulationparametersintheDPM.
Geldart-Btype Geldart-Atype
Particlediameter,dp(m) 400–600 100
Particlenumber,Np 72500 279000
Particledensity,g(kg/m3) 2525 1500
Normalrestitutioncoefficients,en 0.97 0.95
Tangentialrestitutioncoefficients,et 0.33 0.95
Frictioncoefficient(particle–particle/wall),f 0.1 0.3
Normalspringstiffness,kn(N/m) 3500 28
Tangentialspringstiffness,kt(N/m) 1000 8
CFDtimestep,t(s) 1.0×10−5 1.0×10−5
Particledynamicstimestep,tp(s) 1.0×10−6 1.0×10−6
Domainheight(m) 1.5×10−1 3.6×10−2
Domainwidth(m) 4.0,5.0,6.0×10−2 2.32/3.0×10−2
Domaindepth(m) 5.0×10−3 6.0×10−4
Numberofgridcells 150×40/50/60×5 90×58/75×2
DiffusivityofCO2,Ddiff(m2/s) 1.65×10−5 1.65/4.95×10−5
Injectionvelocity,Uinj(m/s) 5.0,6.0 0.1,0.2
Injectiontime, tinj(s) 0.07,0.075 0.035,0.036
Nozzlearea(mm2) 20(4×5gridcells) 0.96(4×2gridcells)
Minimumfluidizationvelocity,Umf(m/s) 0.22 5.9×10−3
Bubblingfluidizationvelocity,Umb(m/s) – 9.0×10−3
FluidizedbedscomprisingGeldart-Bparticles Characteristicsofbubble-to-emulsionphasemasstransfer
Thetracergasconcentrationinthecentralsliceofthefluidized bedis shown inFig. 1for thesimulation usinga bed widthof 6×10−2mandaninjectionvelocityof6m/s.Whiletheactualvalue issomewhatarbitrary,aporosityof0.85isusedtodefinethebubble contour.Inthefigure,arangeofporositycontoursforthebubble
isprovidedtoshowthepronouncedphenomenonofparticle
rain-ingthatleadstobubblecollapse.Thebubbleshapeandbubblesize continuetochangeovertimeasfoundbyPatiletal.(2003)and
Dangetal.(2013).Thesameholdsforthetracergasconcentration
insidethebubble.
ThreestagescanbediscernedfromthesnapshotsinFig.1.First, itisnotedthatthebubblestartstoformshortlyaftertheinjection andthetracergasappearsatthenozzleevenbeforethebubbleis distinguishable.Thegasflowtrajectories,showninFig.2,indicate thatboththeCO2tracergas(viathemiddle)andtheN2background
fluidizationgas(viathebubblesides)contributetotheformationof thebubble,whiletheCO2tracergasimmediatelyflowsthroughthe
topofthebubbleintotheemulsionphase.Afterthebubbleforms, thesecondstagestarts,whereN2backgroundfluidizationgasflows
intothebubblealsoviathebottomandreplacestheCO2that
con-tinuestoleavethebubblethroughitsroof.Themasstransferisthus stronglydominatedbyconvectioninthiscaseofGeldart-B parti-cles,asreportedbyDangetal.(2013).AsmallpartoftheCO2that
leavestheemulsionphaseisrecycledthroughtheleftandright vortices,backintothebubble(seeFig.2).Duringthelaststage,the lasttracesofCO2 thataretrappedinthevorticescanonlyleave
throughdiffusion,which isaslowprocesssuchthatthebubble
concentrationremainsfairlyconstantwhilethebubblecollapses, asalsoshownbytheexperimentalresultsofDangetal.(2013).
Fig.3(a)shows theaverageCO2 concentrationinthebubble
andemulsionphases,wherethethreestagesdescribedabovecan
againbedistinguished.Theemulsionphaseconcentrationis non-zeroandattimesevenlargerthanthebubbleconcentration,but
becausethe majority of CO2 is founddownstream of the
bub-ble(andisincapableofre-enteringthebubble),theassumption ofanegligibleemulsionphaseCO2concentrationtodescribethe
bubble-to-emulsionphase masstransferseemsjustified.Fig.3b
showstheequivalentbubblediameterDb=
4Ab/andreveals
thatthebubblestartstocollapseshortlyafteraninitialgrowth,
whichisconsistentwithexperimentalresultsobtainedbyDang
Fig.3. (a)AverageCO2concentrationintheemulsionphaseandinthebubblewith
itsspatialstandarddeviation(shadedbar)asafunctionoftime;(b)equivalent bub-blediameterasafunctionoftimeaftertheinjectionstarts(bedwidth=6×10−2m,
dp=400–600m,Uinj=6m/s, tinj=0.075s).
et al. (2013). However, Patil et al. (2003) failed to predict the
decreasingbubblesizeatthelater stagein 2DTFMsimulations
andpresentedaslowincreaseintheequivalentbubblediameter, explainingthediscrepancydescribedabove.
Fig.4.Linearcorrelationsofthebubble-to-emulsionmasstransfercoefficientsfordifferentcasesusingparticlesof400–600mindiameter:(a)bedwidth=5×10−2m,
Uinj=5m/s, tinj=0.07sandDb=0.0231m;(b)bedwidth=6×10−2m,Uinj=6m/s, tinj=0.075sandDb=0.0277m.
Fig.5.SnapshotsoftherisingbubbleinGeldart-Aparticlebedsatdifferenttimesteps.Atthetop,theCO2concentrationinthecentralsliceisshown.Thebubbleisplotted
byvaryingthethresholdvalueofporosityfrom0.8to0.85.Atthebottom,thestreamlinesoftherelativegasphaseinthebubbleandtheemulsionphasesareshown.From topandbottom:thestreamlinesinthelefthalfofthebubblearecoloredusingtherelativegasvelocityinthezdirectionwhilethoseintherighthalfofthebubblearecolored withtheCO2concentration.(Bedwidth=2.32×10−2m,dp=100m,Uinj=0.1m/s,Ddiff=1.65×10−5m2/s, tinj=0.035s).
Table4
Comparisonofthesimulatedbubble-to-emulsionmasstransfercoefficientswithpredictionsmadeusingtheDavidsonandHarrison(1963)model,includingtheindividual contributionsofdiffusion-andconvection-basedmasstransfers.
Cases Averagedbubblediameter(m) MasstransfercoefficientKbe(s−1)
DavidsonandHarrisonmodel(1963) Thisstudy Difference
Bedwidth=5cm,Uinj=5m/s 0.0231 27.08(Conv24.90+Diff2.18) 28.89 6.69%
Fig.6. (a)Equivalentbubblediameterasafunctionoftimeafterthestartofinjection withthetracergaseshavingdiffusivitiesdifferingbyafactorof3and(b)theaverage CO2concentrationinthebubblesanditsspatialstandarddeviation(shadedbar)as
afunctionoftime,insingle-bubblefluidizedbedscomprisingGeldart-Aparticles (dp=100m,p=1500kg/m3,Ddiff=1.65×10−5m2/s, tinj=0.035and0.036s).
Coefficientofbubble-to-emulsionphasemasstransfer
Theprevioussectionhasjustifiedtheassumptionofa
negli-gibleemulsionCO2concentration,Eq.(2)canthusbeemployed
tocalculateKbe.Toexcludewalleffectsasmuchaspossible,the
evolutionofthegasstreamlinesisstudiedtofindthetimethat
elapsesbeforewalleffectsbecomedominant.Subsequently,Kbe
isobtainedfromthelinearizedEq.(2),usingtwodifferentbubble sizes(Fig.4).Table4presentsthecomparisonofKbebetweenthe
simulationsandpredictionsmadewiththeDavidsonandHarrison
(1963)model.
In Table4, thedifferences between thevalues calculated in
thesimulationsandthepredictionsmadewiththeDavidsonand
Harrison(1963)modelarelessthan10%,showinggoodagreement.
TheshorttimeusedtocalculateKbeallowstherelevant
assump-tions,suchasaconstantbubblediameter,aconstantmasstransfer coefficientandzerotracergasintheemulsionphase,tobemade.
Table4alsoshowsthattheconvectivecontributionisindeed
dom-Fig.7. AverageCO2concentrationinthebubbleandemulsionphasesfor
single-bubblefluidizedbedscomprisingGeldart-Aparticlesandthetracergaseswith diffusivitiesdifferingbyafactorof3(dp=100m,p=1500kg/m3,Uinj=0.1m/s,
tinj=0.035s).
inantandthatalargervalueofKbeisobtainedforasmallerbubble,
whichisconsistentwiththeresultspresentedaboveandwiththe resultsofpreviousstudies(Patiletal.,2003;Dangetal.,2013).
FluidizedbedscomprisingGeldart-Aparticles
TheDPMtechniqueisalsosuitedtosimulatingGeldart-A parti-cles,whichareusedinmanyindustrialfluidizationprocesses.This sectionusesparticleswithadiameterof100mandadensityof 1500kg/m3.Singlebubbleinjections,similartothoseinthe
pre-viouscases,areperformedusingaporosityof0.85todefinethe bubblecontour.Thebubblesrisesteadilythroughthebeduntilthey breakupatthebedsurface.
Characteristicsofbubble-to-emulsionphasemasstransfer
Fig.5showstheconcentrationfieldandgasphasestreamlines forasimulationusinganinjectionvelocityof0.1m/s.TheCO2
con-centrationinthemiddleofthebubbleisrelativelyhigh.TheCO2
transferredtotheemulsionphaseisfoundmainlyalongthepath behindthebubble.Thisconcentrationprofileissimilartothe pro-fileofgasbubblesrisinginaliquid(e.g.,Stöhr,Schanze,&Khalili, 2009)withtherebeingatailbehindthebubble.
Thesnapshotsindicateamasstransferprocessdifferentfrom
that whenusing Geldart-B particles.Thegas phase streamlines
recirculateinsidethebubbleandintheimmediatesurroundings
ofthebubble(i.e.,thecloud),keepingthetracergaslocaltothe bubble.Additionally,thereisnosignofbubblecollapseinthe snap-shots.ThesecharacteristicsarehighlightedinFig.6,showingthat thebubbleevencontinuestogrowwhilerisingthroughthebed.A simulationwith3timesthetracerdiffusivitybutotherwise iden-ticalsettingsshowsthatthediffusivityofthegashasanegligible effectonthebubblesize.TheaverageCO2concentrationinthe
bub-blecontinuestodecreasewithtimewhileitremainsmoreorless uniformlydistributed.Moreover,asshowninFig.7,overtime,the
averageCO2 concentrationintheemulsionphaseismuchlower
thantheaverageCO2 concentrationinthebubble,andthemass
transferrateincreaseswithincreaseddiffusivity.
Thebubblesaresurroundedbycloudsaccordingtothecriteria foracloudedbubblepresentedbyDavidsonandHarrison(1963).
Fig.5showsthatthegasflowingoutofthebubbleviaitsroofflows
downwardsalongthebubbleedgeandcirculatesbackthroughthe
cloudintothebubble.Themaindifferencesbetweenthecalculated
Fig.8.(a)GasandparticleflowpatternsnearabubblebasedonexperimentsandMurray’stheory(Roweetal.,1964)( 2.5).(ReprintedfromRoweetal.(1964)with permissionfromElsevier.)(b)ThesymbolizedmodelusedbyChibaandKobayashi(1970)(ReprintedfromChibaandKobayashi(1970)withpermissionfromElsevier).
cloudedbubbleinDavidsonandHarrison(1963)arethebubble
shapeandthegasflowprofilesinthewakeofthebubble.Thebubble isassumedtobeideallysphericalandnowakeisdefinedintheory whereastheoppositeisseeninsimulations.
Coefficientofbubble-to-emulsionphasemasstransfer
ThestreamlinesshowninFig.5aresimilartopredictionsbased
onthetheoryofMurray(1965)andusedbyChibaandKobayashi
(1970)toprovidea correlationforthemasstransfercoefficient
(Fig.8).
Eq.(1)isusedtocalculateKbe,basedontheaverageCO2
con-centrationthroughouttheemulsionphase,asafunctionoftime.
Fig.9showsthatwhilethebubblerises,Kbedecreaseswithtimeas
aresultofbubblegrowth(Fig.6(a)).Togetherwiththeaveraged
bubblediameter,thetime-averaged Kbe is presentedin Table5
(inthe“bulkemulsion”column)andcomparedwithpredictions
madeusingclassicphenomenologicalmodels:D&H(Davidson&
Harrison,1963),K&L(Kunii&Levenspiel,1991),andC&K(Chiba&
Kobayashi,1970).ThelargedifferencesinthepredictionsofKbeare
relatedtothedifferencesintheunderlyingassumptions.Notethat thebubblerisingvelocityUbcalculatedfromsimulationresultshas
beenusedinthecomputationofKbewiththesephenomenological
models.
Despitethesimilaritybetweenthegasstreamlines(Fig.5)and thetheoryofMurray(1965)(Fig.8)usedintheChibaandKobayashi
(1970)model,theC&K modeldoesnot givethebestprediction
ofKbe for thesesimulations.Thisis mostprobablybecausethe
phenomenaobservedinthesimulationsarenotconsistentwith
theassumptionsfortheprocessusedinthederivationoftheC&K model,suchasaconstantbubblevolume(andhencecloudvolume) andthesphericalshapeandsizeofthecloud.
TheeffectofbubblediameterontheaverageKbe isanalyzed
first.Thechangeintheamountoftracergasinthebubbleconsists oftwoparts:acontributionduetothechangeinbubblesizeanda contributionduetothechangeinCO2concentrationinthebubble.
Fig.9.Bubble-to-emulsionphasemasstransfercoefficientasafunctionoftime cal-culatedfromthesimulationsofasingleinjectedbubbleinafluidizedbedcomprising Geldart-Aparticles(dp=100m,p=1500kg/m3,Uinj=0.1and0.2m/s, tinj=0.035
and0.036s,Ddiff=1.65×10−5m2/s).
Theanalysisisthuscarriedoutforthesetwotermsseparately.It turnsoutthatthefirsttermcontributesover60%ofthetotalchange intheamountofCO2inthebubble.
Eq.(1)computesthetotalmasstransferbasedonthemass trans-fercoefficientandthedrivingforce,definedastheconcentration differencebetweenthebubbleandtheemulsionphaseintherestof thebed.AsshowninFig.5,however,amoreaccuratedrivingforce
canbetheconcentrationdifferencebetweenthebubbleandthe
emulsionphasearoundthebubble(orthecloud).Here,the emul-sionaroundthebubblewithaCO2concentrationhigherthan62.5%
and73%(correspondingtodifferentcloudsizes)oftheaverageCO2
Table5
ComparisonofmasstransfercoefficientsKbecomputedfromthesimulationresultsandfromphenomenologicalmodels.
Uinj(m/s) Db(m) Kbe(s−1)(predictions) Kbe(s−1)(simulations)
D&H K&L C&K Bulkemulsion 62.5%Cb 73%Cb Diffusioncoefficient=1.65×10−5 0.1 0.003 27.37 11.85 16.93 2.07 10.61 15.36 0.2 0.004 18.64 7.74 10.61 1.63 9.30 13.55 Diffusioncoefficient=4.95×10−5 0.1 0.003 42.34 19.12 28.11 4.33 20.48 29.16 0.2 0.004 28.98 12.66 17.88 3.47 14.42 19.60
concentrationhasbeenusedtocalculateKbe.Thisgivesan
emul-sionphaseconcentrationthatismuchmorelocalthantheaverage overtheentirebed.InTable5,thevaluesofKbeincolumnslabelled
62.5%Cband73%CbcomputedusingtheCO2concentrationinthe
surroundingsofthebubbleforthedrivingforceareinmuchbetter
agreementwiththepredictionsmadeusingthemodelsofKunii
andLevenspiel(1991)andChibaandKobayashi(1970).
Discussionandconclusions
Discussion
Thesimulationsnapshotsandanalysisshowthatthemass trans-ferprocessisgreatlyaffectedbythegasflowpatternatandaround thebubble.AslearnedfromDavidsonandHarrison(1963),thegas flowpatternatthebubbleisdeterminedbytheratioofthebubble risingvelocitytotheinterstitialgasvelocity(Ub/u0).Forslowly
ris-ingbubbles(Ub/u0<1)insingle-bubblefluidizedbedscomprising
Geldart-Bparticles,themasstransferisdeterminedbythe
convec-tiveflowsfromtheemulsiontothebubbleandfromthebubble
backtotheemulsion.Thesimulationsinthepresentworkshow
thatthetracergasinthebubbletransfersintotheemulsionphase firstbythe(convective)depletionofthecenterofthebubbleand thenbydiffusionviathevorticesattheleftandrightsidesofthe
bubblebeforethebubblecollapses.Theemulsionphase
concen-trationcanbeassumedtobezerobecausetheinjectedtracergas escapesthroughthebubble.Animportantissueremains,however, intermsofhowtheupstreamconcentrationprofilecanbe incorpo-ratedinthecorrelations,especiallyiftheprofileisnotuniform.Any tracergasthatexistsupstream(i.e.,belowthebubble)willlikely traveltowardsthebubble,enterviathebottomandleavethrough theroof.Thisaspectofmasstransferisnotcapturedinexisting correlationsbutiscrucialforfreelybubblingfluidizedbeds.
Forquickly risingbubbles(Ub/u0∼5)influidized beds
com-prisingGeldart-Aparticles,thephenomenaobservedinthemass
transferprocessaredifferentfromthoseintheGeldart-Bparticle
simulations.Noobviousvolumetricflowratebetweenthebubble
andtheemulsionbulkisobserved,andratherastronggas circu-lationinthebubbleandthelocalemulsionphase (i.e.,cloud)is distinguished.Someofthetracergasisleftbehindviathewakeat thebottomofthebubble,butalsoalargepartofthetracergasis trappedinthebubbleandisreleasedonlywhenthebubblebreaks upatthebedsurface.Themasstransfercoefficientscomputedwith thetheoreticalmodelsdonotagreewiththoseobtainedfromthe simulations,unlessalocalemulsionphaseconcentrationistaken intoaccount.Whilethelocalemulsionphaseisclearlythemost
influentialzoneandusingalocalemulsionphaseconcentration
canbejustified,itisimportanttoacknowledgethatthetheoretical modelsaretypicallyusedforfreelybubblingfluidizedbeds. Bub-blebreakupandcoalescencecangreatlyincreasethemasstransfer
betweenthebubbleandemulsionphases.Thismaygiveagood
additionalexplanationonwhyvaluesofKbecalculatedfromthe simulationresultsaremuchlowerthananyofthepredictionsmade usingthephenomenologicalmodelsderivedforfreelybubbling
flu-idizedbeds.Thescopeofthisstudy,however,remainsassingle risingbubbles.
Theusedcorrelations incorporatethediffusioncoefficientby includingD0.5
i inthediffusiveterms.Increasingthediffusion
coef-ficientbyafactor3wouldthereforegiveapredictionofanincrease inthemasstransfercoefficientbyafactorof30.5=1.73;however,
thesimulationstypicallyyieldamasstransfercoefficientthatis largerbyafactorof2,showingthattheeffectofthediffusiveflux ismoreimportantthananticipatedbythecorrelations.
Conclusions
ADPMextendedwithgascomponentconservationequations
wasusedtoinvestigatethebubble-to-emulsionphasemass
trans-ferby carrying out simulationsonsingle-bubble fluidized beds
comprisingGeldart-Aand-Bparticles.Newinsightsonthespatial distributionandtemporalevolutionofthetracergasconcentration
inthebubbleandemulsionweredeveloped.Detailedinformation
onchangesinthebubblesize,tracergasconcentrationandgasflow
atthebubblewereusedtoaccuratelyanalyzethemasstransfer
characteristicsandtocalculatethemasstransfercoefficient.
This work challenged the validity of the assumptions used
inpopularphenomenologicalmodelsforthebubble-to-emulsion
masstransfer coefficient.For single-bubblefluidized beds
com-prising Geldart-B particles,the bubble-to-emulsion phase mass
transfer process is dominated byconvective gasflow from the
emulsionphasetothebubblephaseandthenbacktothe
emul-sionphase.Nouniformgasconcentrationinthebubbleorconstant bubblesizeandshapecanbeassumedforthesecases.
TheDavidsonandHarrison(1963)modelassumesaconstant
volumetricflow-rateintothebubblefromtheemulsionbulkand
out of the bubble into the emulsion bulk. Because convective
transferis dominant(byfar)for Geldart-Bparticles,this model reasonablypredictsmasstransfercoefficientsfortheseparticles, providedthataconstantbubblesizeandzerotracergas
concentra-tionintheemulsionphasecanbeassumed.Thefirstassumption
isassuredbytakingashorttimeinterval(whichkeepsthesize relativelyconstant),andtheconcentrationintheemulsionphase
canbeassumedtobezerobecausethetracergasconcentration
profileextendsonlydownstreamofthebubble.Infreelybubbling fluidizedbeds,however,concentrationprofilesmayexistupstream ofabubbleandshouldbetakenintoaccount.
Thebubblescannotbeassumedtobeconstantinsizeorhavea circular(orspherical)shapeinthecaseofGeldart-Aparticles,and itwasshownthatthebubble-to-emulsionmasstransfercoefficient
changesovertime.Thesefindingsconfirmandextendthefindings
ofpreviousexperimentalandnumericalstudies.Notalltracergasis ultimatelyexchangedwiththeemulsioninsidethebeds,withsome beingreleasedatthebedsurfacewhenthebubblesbreakup.Hence, aproperdefinitionofthecloudaroundthebubbleandtheuseof theaveragetracergasconcentrationinthecloudarenecessaryto calculatethemasstransfercoefficient.Inthiscase,theKuniiand
Levenspiel(1991)andChibaandKobayashi(1970)modelsgivethe
hasadistinctiveeffectonthebubble-to-emulsionmasstransferin thebeds,whichisunderestimatedbythemodels.
Acknowledgment
ThisprojectisfinanciallysupportedbytheNetherlands
Orga-nizationforScientificResearch(NWO)underSTWVIDIGrantNo.
10244.
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