Heat Chap14134.docx

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Heat Chap14134.docx

HeatChap14134

14-134Acircularpanfilledwithwateriscoolednaturally.Therateofevaporationofwater,therateofheattransferbynaturalconvection,andtherateofheatsupplytothewaterneededtomaintainitstemperatureconstantaretobedetermined.

Assumptions1Thelowmassfluxmodelandthustheanalogybetweenheatandmasstransferisapplicablesincethemassfractionofvaporintheairislow(about2percentforsaturatedairat25C).2ThecriticalReynoldsnumberforflowoveraflatplateis500,000.3Radiationheattransferisnegligible.4Bothairandwatervaporareidealgases.

PropertiesTheair-watervapormixtureisassumedtobedilute,andthuswecanusedryairpropertiesforthemixtureattheaveragetemperatureof

=(15+20)/2=17.5C=290.5K.Thepropertiesofdryairat290.5Kand1atmare,fromTableA-15,

Themassdiffusivityofwatervaporinairattheaveragetemperatureof290.5Kis,fromEq.14-15,

Thesaturationpressureofwaterat20Cis

Propertiesofwaterat15Care

(TableA-9).Thespecificheatofwaterattheaveragetemperatureof(15+20)/2=17.5CisCp=4.184kJ/kg.C.ThegasconstantsofdryairandwaterareRair=0.287kPa.m3/kg.KandRwater=0.4615kPa.m3/kg.K(TableA-1).

Analysis(a)Theairatthewatersurfaceissaturated,andthusthevaporpressureatthesurfaceissimplythesaturationpressureofwateratthesurfacetemperature(1.7051kPaat15C).Thevaporpressureofairfarfromthewatersurfaceisdeterminedfrom

Treatingthewatervaporandtheairasidealgasesandnotingthatthetotalatmosphericpressureisthesumofthevaporanddryairpressures,thedensitiesofthewatervapor,dryair,andtheirmixtureatthewater-airinterfaceandfarfromthesurfacearedeterminedtobe

 

Atthesurface:

and

 

Awayfromthesurface:

Notethat

andthusthiscorrespondstohotsurfacefacingdown.Theareaofthetopsurfaceofthewater

anditsperimeteris

.Therefore,thecharacteristiclengthis

Thenusingdensities(insteadoftemperatures)sincethemixtureisnothomogeneous,theGrashoffnumberisdeterminedtobe

Recognizingthatthisisanaturalconvectionproblemwithcoldhorizontalsurfacefacingup,theNusseltnumberandtheconvectionheattransfercoefficientsaredeterminedtobe(Eq.14-13)

and

Thentherateofheattransferfromtheairtothewaterbyforcedconvectionbecomes

(towater)

(b)Utilizingtheanalogybetweenheatandmassconvection,themasstransfercoefficientisdeterminedthesamewaybyreplacingPrbySc.TheSchmidtnumberisdeterminedfromitsdefinitiontobe

Therefore,theSherwoodnumberinthiscaseisdeterminedfromTable14-13tobe

UsingthedefinitionofSherwoodnumber,themasstransfercoefficientisdeterminedtobe

Thentheevaporationrateandtherateofheattransferbyevaporationbecome

and

(c)Thenetrateofheattransfertothewaterneededtomaintainitstemperatureconstantat15Cis

DiscussionNotethatifnoheatissuppliedtothewater(byaresistanceheater,forexample),thetemperatureofthewaterinthepanwoulddropuntiltheheatgainbyconvectionequalstheheatlossbyevaporation.

14-135Airisblownoveracircularpanfilledwithwater.Therateofevaporationofwater,therateofheattransferbyconvection,andtherateofenergysupplytothewatertomaintainitstemperatureconstantaretobedetermined.

Assumptions1Thelowmassfluxmodelandthustheanalogybetweenheatandmasstransferisapplicablesincethemassfractionofvaporintheairislow(about2percentforsaturatedairat25C).2ThecriticalReynoldsnumberforflowoveraflatplateis500,000.3Radiationheattransferisnegligible.4Bothairandwatervaporareidealgases.

PropertiesTheair-watervapormixtureisassumedtobedilute,andthuswecanusedryairpropertiesforthemixtureattheaveragetemperatureof

=(15+20)/2=17.5C=290.5K.Thepropertiesofdryairat290.5Kand1atmare,fromTableA-15,

Themassdiffusivityofwatervaporinairattheaveragetemperatureof290.5Kis,fromEq.14-15,

Thesaturationpressureofwaterat20Cis

Propertiesofwaterat15Care

(TableA-9).Also,thegasconstantsofwaterisRwater=0.4615kPa.m3/kg.K(TableA-1).

Analysis(a)Takingtheradiusofthepanr0=0.15mtobethecharacteristiclength,theReynoldsnumberforflowoverthepanis

whichislessthan500,000,andthustheflowislaminarovertheentiresurface.TheNusseltnumberandtheheattransfercoefficientare

Thentherateofheattransferfromtheairtothewaterbyforcedconvectionbecomes

(towater)

(b)Utilizingtheanalogybetweenheatandmassconvection,themasstransfercoefficientisdeterminedthesamewaybyreplacingPrbySc.TheSchmidtnumberisdeterminedfromitsdefinitiontobe

Therefore,theSherwoodnumberinthiscaseisdeterminedfromTable14-13tobe

UsingthedefinitionofSherwoodnumber,themasstransfercoefficientisdeterminedtobe

Theairatthewatersurfaceissaturated,andthusthevaporpressureatthesurfaceissimplythesaturationpressureofwateratthesurfacetemperature(1.7051kPaat15C).Thevaporpressureofairfarfromthewatersurfaceisdeterminedfrom

Treatingthewatervaporandtheairasidealgases,thevapordensitiesatthewater-airinterfaceandfarfromthesurfacearedeterminedtobe

Atthesurface:

Awayfromthesurface:

Thentheevaporationrateandtherateofheattransferbyevaporationbecome

and

(c)Thenetrateofheattransfertothewaterneededtomaintainitstemperatureconstantat15Cis

DiscussionNotethatifnoheatissuppliedtothewater(byaresistanceheater,forexample),thetemperatureofthewaterinthepanwoulddropuntiltheheatgainbyconvectionequalstheheatlossbyevaporation.

Also,therateofevaporationcouldbedeterminedalmostasaccuratelyusingmassfractionsofvaporinsteadofvaporfractionsandtheaverageairdensityfromtherelation

.

14-136Asphericalnaphthaleneballishangedinacloset.Thetimeittakesforthenaphthalenetosublimatecompletelyistobedetermined.

Assumptions1Theconcentrationofnaphthaleneintheairisverysmall,andthelowmassfluxconditionsexistsothattheChilton-Colburnanalogybetweenheatandmasstransferisapplicable(willbeverified).2Bothairandnaphthalenevaporareidealgases.3Thenaphthaleneandthesurroundingairareatthesametemperature.4Theradiationeffectsarenegligible.

PropertiesThemolarmassofnaphthaleneis128.2kg/kmol.Becauseoflowmassfluxconditions,wecanusedryairpropertiesforthemixtureatthespecifiedtemperatureof298Kand1atm,atwhich

and

(TableA-15).

AnalysisTheincomingairisfreeofnaphthalene,andthusthemassfractionofnaphthaleneatfreestreamconditionsiszero,wA,=0.Notingthatthevaporpressureofnaphthaleneatthesurfaceis11Pa,themassfractionofnaphthaleneontheairsideofthesurfaceis

Normallywewouldexpectnaturalconvectioncurrentstodeveloparoundthenaphthaleneballbecausetheamountofnaphthalenenearthesurfaceismuchlarger,anddeterminetheNusseltnumber(anditscounterpartinmasstransfer,theSherwoodnumber)fromEq.14-16,

Butthemassfractionvaluedeterminedaboveindicatesthattheamountofnaphthaleneintheairissolowthatitwillnotcauseanysignificantdifferenceinthedensityofair.Withnodensitygradient,therewillbenonaturalconvectionandthustheRayleighnumbercanbetakentobezero.ThentheNusseltnumberrelationabovewillreducetoNu=2oritsequivalentSh=2.ThenusingthedefinitionofSherwoodnumber,themasstransfercoefficientcanbeexpressedas

Themassofnaphthaleneballcanbeexpressedas

.Therateofchangeofthemassofnaphthaleneisequaltotherateofmasstransferfromnaphthalenetotheair,andisexpressedas

Simplifyingandrearranging,

Integratingfrom

attimet=0toD=0(completesublimation)attimet=tgives

Substituting,thetimeittakesforthenaphthalenetosublimatecompletelyisdeterminedtobe

14-137EAswimmerextendshiswetarmsintothewindyairoutside.Therateatwhichwaterevaporatesfrombotharmsandthecorrespondingrateofheattransferbyevaporationaretobedetermined.

Assumptions1Thelowmassfluxmodelandthustheanalogybetweenheatandmasstransferisapplicablesincethemassfractionofvaporintheairislow(about2percentforsaturatedairat60F).2Thearmcanbemodeledasalongcylinder.

PropertiesBecauseoflowmassfluxconditions,wecanusedryairpropertiesforthemixtureattheaveragetemperatureof(40+80)/2=60Fand1atm,forwhich=0.159×10-3ft2/s,and=0.077lbm/ft3(TableA-15E).Thesaturationpressureofwaterat40ºFis0.1217psia.Also,at80ºF,thesaturationpressureis0.5073psiaandtheheatofvaporizationis1048Btu/lbm(TableA-9E).ThemolarmassofwaterisR=0.5956psia.ft3/lbm.R(TableA-1E).Themassdiffusivityofwatervaporinairat60ºF=520R=288.9KisdeterminedfromEq.14-15tobe

AnalysisTheReynoldsnumberforflowoveracylinderis

TheSchmidtnumberinthiscaseis

Thenutilizingtheanalogybetweenheatandmassconvection,theSherwoodnumberisdeterminedfromEq.10-32byreplacingPrnumberbytheSchmidtnumbertobe

UsingthedefinitionofSherwoodnumber,themasstransfercoefficientisdeterminedtobe

Theairatthewatersurfaceissaturated,andthusthevaporpressureatthesurfaceissimplythesaturationpressureofwateratthesurfacetemperature(0.5073p

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