ht materials-phase change
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AShortCoursebyRezaToossi,Ph.D.,P.E.CaliforniaStateUniversity, LongBeach
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PhaseChangeMaterials Applications
Properties
Modeling
MeltingandSolidification
Evaporation
AerosolJetImpingement
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Abhat,A.,Lowtemperaturelatentheatthermalenergystorage:heatenergystoragematerials,SolarEnergy,30(1983)313332.
Exothermic(warmingprocesses) Melting
Point(oC)LatentHeat
Density(kg/m3)
on ensat on Steamradiators
Freezing Orangegrowerssprayorangeswithicedwater
Deposition Snowydaysarewarmerthancleardaysinthe
winter
Endothermic(coolingprocesses) Evaporation/Boiling
Steel 1400 247 7800
Copper 1086 206 8900
Ice 0 335 917
SodiumSulfate
32 252 1495
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weat
Alcoholiscool
Melting Meltingiceindrinks
Sublimation Coolingwithdryice
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SolidLi uid Temperaturecontrol
Ablation
Coating
LiquidVapor vaporat vecoo ng
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EnergyStorageinBuildings
Passiveheatingandcooling
ThermoelectricRefrigeration
Transportoftemperaturesensitivematerials ThermalControl
IndustrialForming(casting,laserdrilling)
FoodandPharmaceuticalProcessing
TelecomShelters
Humancomfortfootwearandclothes
ermosan coo ers
ElectricalGeneration Cogeneration
ThermoelectricPowerGeneration
SecurityofEnergySupply Flowthroughheatexchangers
MicroencapsulatedPCMs
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Thermod namicCriteria
Ameltingpointatthedesiredoperatingtemperature
Ahighlatentheatoffusionperunitmass
Ahighdensity
Ahighspecificheat
Congruentmelting
Smalldensitydifferencesbetweenphases
Littlesupercoolingduringfreezing
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ChemicalCriteria Chemicalstability
Noncorrosive,nonflammable,nontoxic Others Longshelflife
A licabilit
Reliability Commercialavailability
Lowcost
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Withoutenca sulation containersha eandmaterial)
Encapsulation Buildingmaterials(PCM5080%,unsaturatedpolyester
matrix4510%,andwater510%)
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Availabilit ofsmallnumberofmaterialsinthetemperaturerangeofinterest
UsefullifeMaintenanceStability
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OrganicCompounds Paraffins
FattyAcids
SaltBasedCompounds SaltHydrates
Eutectics Others Iceandwater
Zeolite
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Advantages Awiderangeofmeltingpoints
Nontoxic,noncorrosive
Chemicallystable
Compatiblewithmostbuildingmaterials
Highlatentheatperunitmass
Meltingcongruity
Negligiblesupercooling
Areavailableforwiderangeoftemperatures
Expensive
Lowdensity
Lowthermalconductivity(comparedtoinorganiccompounds)
Largecoefficientofthermalexpansion
Flammable
Donothaveawelldefinedmeltingtemperatures.
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Advanta es Lowercost
Highlatentheatperunitmassandvolume
Highthermalconductivity
Widerangeofmeltingpoints(7117oC)
Disadvantages Highrateofwaterloss
Corrosive
Phaseseparation
SubstantialSubcooling
Phasesegregation(lackofthermalstability)
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Coolin 1 oC)TemperdiurnalswingsHeatpumpsSolarhotwaterheatingsystemsAbsorptionairconditioner
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Roof
Wall
Window
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Velraj,R.,andPasupathy,A.,PHASECHANGEMATERIALBASEDTHERMALSTORAGEFORENERGYCONSERVATIONINBUILDINGARCHITECTUREInstituteforEnergyStudies,CEG,AnnaUniversity,Chennai 600025.INDIA.
Basedon m2 ofsolarcollectorarea
TES Systems Cost($) Volume(m3)
Water 54 0.72
Rock 217@$8/ton 2.46
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Glaubers Salt 146 0.18
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ConventionalCD(readonly)CDR(recordable)CDRW(readandwrite)
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Sodiumacetate trih drate) Tsl =54
oC
hsl =1.86x105 J/kg
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MeltingofSolids
Boiling FilmBoiling
PoolBoiling
Condensation FilmCondensation
DropwiseCondensation
eroso e pray Nucleation
Impingement
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Oneregion
Multipleregion
Tworegion
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ContactMelting(meltingofasolidunderitsownweight)
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Solid Scaleanalysis
Liquid
B.C
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Governing Equations (Neumannproblem):
BoundaryConditions
Solution:
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Analytical 1Dandsome2Dconductioncontrolled
Strong(Classical)numericalsolution Velocityu andpressurep satisfyNavierStokesequationspointwisein
spacetime.
Weak(FixedGrid)solution EnthalpyMethod(Shamsunder andSparrow,1975)
e qu va en ea apac y e o onac na e a .,1973 TheTemperatureTransformingModel(CaoandFaghri,1990)
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TwoRegionMeltingofaSlab Assumedensitiesoftheli uidandsolid hasearee ual.
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1. ChoosetandxtomeetNeumannsstabilitycriterion
2. Determinetheinitialenthalpyateverynodehjo (j=1)
3. Calculatetheenthalpyafterthefirsttimestepatnodes(j=2,...,N 1)byusingequation(1).
4. Determinethetemperatureafterthefirsttimestepatnode(j=1,...,N)byusingequations(2)and(3).
5. Findacontrolvolumeinwhichtheenthalpyfallsbetween0andhsl ,anddeterminethelocationofthesolidliquidinterfacebyusingequation(4).
6. Solvethephasechangeproblematthenexttimestepwiththesameprocedure.
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Unconditionallystablebutismorecomplexecause woun nownvar a esen a pyan
temperatureareinvolved.[SeeAlexiades, A.,andSolomon,A.D.,1993,MathematicalModelingofMeltingandFreezingProcesses,Hemisphere,Washington,DC.]
Transformtheenergyequationintoanonlinearequationwithasinglevariableh.[SeeCao,Y.,andFaghri ,A.,1989,"ANumericalAnalysisofStefanProblemofGeneralizedMultiDimensionalPhaseChangeStructuresUsingtheEnthalpyTransformingModel,"InternationalJournalofHeatandMassTransfer,Vol .32,pp.12891298.]
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3DConductioncontrolledmelting/solidification
Heatcapacityduringthephasechangeisinfinite. AssumeCp andkchangelinearlyfromliquidtosolid
Advantage:Simplicity Disadvantage:
Unstableifrightchoicesforx,t,andTarenotmade.
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Combinationofthetwomethods[Cao,Y.,andFaghri ,A.,1990a,"ANumericalAnalysisofPhaseChangeProblemincludingNaturalConvection,"ASMEJournalofHeatTransfer,Vol .112,pp.812815.]
UsefinitevolumeapproachbyPatankar tosolvethediffusionequation.
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Assumptions EnthalpyMethodapproachisconsidered
Newtonianincompressiblefluidwithconstantproperties,exceptthedensitythatisevaluatedslinearfunctionoftemperature(Bousinessqapproximation)
Effectiveconductivityinthemushyzone
Isotropic
Heattransferbyconduction,convectionand
43CARLOS HERNNSALINASLIRA1,SOLIDIFICATIONINSQUARESECTION,Theoria,Vol.10:4756,2001.
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EulerianAveraging Avera edovers ace time orbothwithinthedomainofinte ration
Basedontimespacedescriptionofphysicalphenomena
Consistentwiththec.v.analysisusedtodevelopgoverningequations.
Euleriantimeaveraging
Eulerianvolumeaveraging
Phaseaverages: Intrinsicphaseaverage
Extrinsicphaseaverage
agrang an verag ng Followaparticleandaverageitspropertiesduringtheflight
MolecularStatisticalAveraging Boltzmannstatisticaldistributionratherthanindividualparticleisthe
independentvariable.
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Governing Equations:
Jany,P.,andBejan,1988,"ScalingTheoryofMeltingwithNaturalConvectioninanEnclosure,"InternationalJournalofHeatandMassTransfer,Vol.31,pp.12211235.
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Nucleation Homogeneous
Heterogeneous Filmwise
Dropwise
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Liquidandgasproperties , lg
Surfacetensionattheinterface,Phasedensitydifference,(l g)SurfaceroughnessandorientationContactangle,
c
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InspiredbyNamibdesertbeetleMimicswingwithamicroscopic
patternofwaterattractingandwaterrepellingareas
Alsoseenonlotusleaves
ApplicationsincludeSelfdecontaminatin surfaces
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AntifoggingsurfacesMicrofluidicchips
HarvestingdewsasdrinkablewaterPocketsizedchemicaltestingdevices
video.mpg
RubnerandCohen,NanoLetters6(6),12131217(2006)
Nanostructuredfilmmadeofalternatinglayersofpositivelyandnegativelychargedpolymersandsilicananoparticles
Dualqualitymaterialcanbepatternedtorepelwaterin
someareas sp er ca droplets)andattractitinothers(flattenedones).
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Thet eofboilin de endson PoolBoiling(waterinapanontopofastove)
Subcooled(local)Tliq
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Effectofsubstrate(Layeredstructureofanelectricheater)
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enhancedwallfunction Macroscale(jetflow) Microscale(dropletdynamics)
Impactofsingledroplet
Impactofmultipledroplets
Garbero,etal.,Gas/surfaceheattransferinspraydepositionprocesses,Intl.J.HeatandFluidFlow,Vol.27,Issue1,Feb2006,pp.105122
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Singleroundjet:
Multiplejets:
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SingleDroplet WeD
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B Correlationnumber D jet/nozzlediameter d dropletdiameter K dropletsplashing criterion n numberofdroplets numberfluxofdroplets Nu Nusseltnumber,hD/k Nu0 Nusseltnumberinabsence
o part c es massloading surfacetension
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ComparisonwithparallelflowExample:SubstratecoolingofaplasticsheetL=20cm,Ts =95
OC,Tf,=20OC,
Uf,=5m/sforparallelflow;=25m/sinnozzleFluid:water
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Beforeimpact
AfterimpactDropletdeformation(spreading)duringimpact
(dp = 200m,Up = 10 m/s).
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Contoursoftotalsurfaceheatflux(seenfrombelow)
Velocityvectorsduringtheimpactofthreedroplets:threedroplet
Garbero,Vanni,andFritscling,Gas/surfaceheattransferinspraydepositionprocesses,IntlJ.HeatandFluidFlow,Vol.27,Issue1.Feb2006,pp.105122. 78
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Bai and Gosman (1995): Drop collision model, , , ,
inducedbreakup,Randombreakup,Splash) Wang and Watkins (1990)
We80
Park,K.,andWatkins,A.P.,Comparisonofwallsprayimpactionmodelswithexperimentaldataondropvelocitiesandsizes, Int.J.HeatandFluidFlow,Vol.17,No.4,August1996.
Where,
Cwb =1/3
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Rebound, Rebound with breakup, Break-up, and Splash(Park and Watkins, 1996)
Spreading velocity
Film thickness
SplashingCriteria(Bussmann,2000)K
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For additional questions, Pleaseemail [email protected].
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Embedding
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