003
0038-08-092X/0192X/01 /$ /$ - see - see frofront nt matmatterter www.elsevier.com/locate/solener
www.elsevier.com/locate/solener
AN ANALYSIS OF ISOTHERMAL PHASE CHANGE OF PHASE CHANGE
AN ANALYSIS OF ISOTHERMAL PHASE CHANGE OF PHASE CHANGE
MATERIAL WITHIN RECTANGULAR AND CYLINDRICAL CONTAINERS
MATERIAL WITHIN RECTANGULAR AND CYLINDRICAL CONTAINERS
†, †, 11
B. ZIVKOVIC and I. FUJII B. ZIVKOVIC and I. FUJII
Meiji University, Department of Mechanical Engineering, 1-1-1 Higashi-Mita, Tama-ku, 214-8571 Meiji University, Department of Mechanical Engineering, 1-1-1 Higashi-Mita, Tama-ku, 214-8571
Kawasaki, Japan Kawasaki, Japan
Received 10 January 2000; revised version accepted 7 June 2000 Received 10 January 2000; revised version accepted 7 June 2000
Communicated by ERICH HAHNE Communicated by ERICH HAHNE
Abstract
Abstract—In this paper, a simple computational model for isothermal phase change of phase change material—In this paper, a simple computational model for isothermal phase change of phase change material (PCM) encapsulated in a single container is presented. The mathematical model was based on an enthalpy (PCM) encapsulated in a single container is presented. The mathematical model was based on an enthalpy formulation with equations cast in such a form that the only unknown variable is the PCM’s temperature. The formulation with equations cast in such a form that the only unknown variable is the PCM’s temperature. The theoretical model was verified with a test problem and an experiment performed in order to assess the validity theoretical model was verified with a test problem and an experiment performed in order to assess the validity of
of the the assassumpumptitions ons of of the the mamathethematmaticaical l modmodel. Witel. With h ververy y googood d agragreemeement ent betbetweeween n expexperierimenmental tal andand computational data, it can be concluded that conduction within the PCM in the direction of heat transfer fluid computational data, it can be concluded that conduction within the PCM in the direction of heat transfer fluid flow, thermal resistance of the container’s wall, and the effects of natural convection within the melt can be flow, thermal resistance of the container’s wall, and the effects of natural convection within the melt can be ignored for the conditions investigated in this study. The numerical analysis of the melting time for rectangular ignored for the conditions investigated in this study. The numerical analysis of the melting time for rectangular and cylindrical containers was then performed using the computational model presented in this paper. Results and cylindrical containers was then performed using the computational model presented in this paper. Results show that
show that the rectangthe rectangular containular container requires nearly half er requires nearly half of of the melting time as the melting time as for the for the cylicylindricndrical containeal container r of of the same volume and heat transfer area.
the same volume and heat transfer area. ©© 2001 Published by Elsevier Science Ltd.2001 Published by Elsevier Science Ltd.
1.
1. INTROINTRODUCTIDUCTIONON Ghoneim, 1989). Using the shell-and-tube modelGhoneim, 1989). Using the shell-and-tube model for
for the the LHELHES S uniunit, t, MorMorrisrison on and and AbdAbdel-el-KhaKhalik lik Effective and economic thermal energy storage of
Effective and economic thermal energy storage of
(197
(1978) 8) perperforformed med a a lonlong-tg-term erm ananalyalysis sis of of air air--a
a daidaily ly sursurpluplus s of of irrirradadiatiated ed solsolar ar eneenergy is rgy is anan
bas
based ed ((air air as as HTF) HTF) and and liqliquiduid-b-baseased d ((watwater er asas unavoidable necessity for the efficient use of solar
unavoidable necessity for the efficient use of solar
HTF)
HTF) solsolar ar heaheatinting g syssystemtems, s, assassumiuming ng thathat t thethe ene
energy rgy for for heaheatinting g pupurporposes ses (Duf(Duffie fie anand d BeBeck-
ck-thermal conductivity of the PCM in the direction thermal conductivity of the PCM in the direction ma
man, n, 19199191). ). AmAmonong g ththe e vavaririouous s memeththodods s of of
of the HTF flow, as well as the thermal resistance of the HTF flow, as well as the thermal resistance energy storage, latent heat thermal energy storage
energy storage, latent heat thermal energy storage
of the PCM in the direction normal to the HTF of the PCM in the direction normal to the HTF is particularly attractive. The motivation for using
is particularly attractive. The motivation for using flo
flow, w, cacan n boboth th be be igignonorered. d. In In a a lalateter r ananalalysysisis,, ph
phasase e chchanange ge mamateteririalals s (PC(PCM) M) is is ththeieir r hihighgh Gh
Ghononeieim m (1(198989) 9) totook ok ininto to acaccocoununt t boboth th ththee energy storage density and their ability to provide
energy storage density and their ability to provide
conduction within the PCM in the direction of the conduction within the PCM in the direction of the heat at a constant temperature (Abhat, 1983).
heat at a constant temperature (Abhat, 1983).
HTF flow and the direction normal to the HTF HTF flow and the direction normal to the HTF In
In ororder der to to perperforform m a a lonlong-tg-term erm peperforformarmancence flo
flow w anand d shshowowed ed ththat at a a susubsbstatantntiaial l ererroror r inin ana
analyslysis is of of a a spespecificified ed solsolar ar heaheatinting g syssystemtem, , anan es
estitimamatiting ng ththe e sosolalar r frfracactition on ((amamouount nt of of tototatall adequate model of the heat storage unit is needed
adequate model of the heat storage unit is needed
heating load supplied by solar energy) was heating load supplied by solar energy) was intro-(Klein
(Klein et alet al.., 1976) which, naturally, depends on, 1976) which, naturally, depends on
duc
duced ed by by negnegleclectinting g the the conconduductiction on witwithin hin thethe its design. A survey of the previously published
its design. A survey of the previously published
PCM
PCM. . HowHoweveever, r, the the comcommon mon conconcluclusiosion n frofromm papers dealing with latent heat storage reveals that
papers dealing with latent heat storage reveals that
both works is that the reduction in storage volume both works is that the reduction in storage volume the most intensively analyzed latent heat energy
the most intensively analyzed latent heat energy
by using PCM is not as nearly as pronounced for by using PCM is not as nearly as pronounced for storage (LHES) unit is the shell-and-tube LHES
storage (LHES) unit is the shell-and-tube LHES
liquid-based systems as it is for air-based systems. liquid-based systems as it is for air-based systems. unit with the PCM filling the shell and the heat
unit with the PCM filling the shell and the heat It
It isis, , ththererefeforore, e, prprefefererabable le to to ususe e a a LHLHES ES ununitit tra
transfnsfer er fluifluid d (HTF) (HTF) flowflowing ing thrthrougough h the the tubtubeses
coupled with an air-based system. For that reason, coupled with an air-based system. For that reason, (Lacroix, 1993; Bansal and Buddhi, 1992; Esen
(Lacroix, 1993; Bansal and Buddhi, 1992; Esen et et
air is
air is conconsidsidereered d as as the HTF the HTF in in the subsethe subseququentent
al
al.., , 19199898; ; SoSoma ma anand d DuDutttta, a, 19199393; ; IsIsmamail il anandd
analysis. analysis. Alves, 1986) or, vice versa, PCM filling the tube
Alves, 1986) or, vice versa, PCM filling the tube
The problem of the phase change of PCMs falls The problem of the phase change of PCMs falls and HTF flowing parallel to it (Esen
and HTF flowing parallel to it (Esen et alet al.., 1998;, 1998;
into the category of moving boundary problems. into the category of moving boundary problems. Wh
When en ththe e PCPCM M chchanangeges s ststatate, e, boboth th liliququid id anandd
†
† solid phases are present and they are separated bysolid phases are present and they are separated by
Author to whom correspondence should be addressed. Tel./ Author to whom correspondence should be addressed. Tel./
the
the movimoving ng interinterface between them. face between them. TherThere e havehave
fax:
fax: 1181-44-943-7395; e-mail: fujii@isc.meiji.ac.jp81-44-943-7395; e-mail: fujii@isc.meiji.ac.jp
1 1
ISES member.
ISES member. bebeen en mamany ny didiffffererenent t nunumemeriricacal l memeththodods s de de--51
velo
veloped for deaped for dealing witling with the phase chah the phase change pronge prob- b- accoaccounted unted for for (V(Volleroller et alet al.., 1987; Lacroix, 1993;, 1987; Lacroix, 1993; lem
lem (Ban(Bansal asal and Bnd Bududdhidhi, 19, 1992; S92; Soma aoma and Dnd Duttutta, a, SomSoma a and and DutDutta, ta, 1991993). Whi3). While le in in momost st worworks,ks, 19
199393; ; MuMurrrray and Lanay and Landidis, 195s, 1959) 9) of whiof which the ch the coconvnvecectitive ve heheat at trtranansfsfer er frfrom om ththe e HTHTF F to to ththee mo
most st attattracractivtive e and and cocommommonly nly useused d are are the the so- so- PCM iPCM is cals calculculateated thrd througough the mh the mean vean valualue of the of thee cal
called led ententhalhalpy mpy methethods ods (V(Volloller aer and Cnd Crosross, 1s, 1981981; ; heaheat t tratransfnsfer er coecoefficfficienient t ((a a convconv), ), sosome me auauththororss V
Volleroller, 1985; , 1985; VVolleroller, 1990). The , 1990). The majomajor reason for r reason for solvesolved the probld the problem of phase chaem of phase change counge coupled withpled with thi
this is s is thathat the t the metmethohod does not requd does not require expire expliclicit it tratransinsient ent conconvecvectivtive e heaheat t tratransfnsfer er betbetweeween n HTFHTF tre
treatmatment of ent of the conthe conditditionions s on the on the phphase chanase change ge and PCMand PCM, , i.ei.e. . witwith the h the comcompleplete Oberte Oberbecbeck’s setk’s set bo
boundundary ary ((cf. cf. CaCarslrslaw aw and and JaeJaegerger, , 191959), 59), i.ei.e. . thethere re of of equequatiations ons solsolved ved for for the the HTF HTF (Bel(Bellecleci i andand is no
is no need need for tfor trackiracking thng the phae phase chse change ange bounboundary dary ContConti, 1993; Trpi, 1993; Trp et alet al.., 1999)., 1999). thr
thrououghoghout ut the phase the phase chachangnge e domdomainain. . HoHowevwever, er, In the In the prepresensent t anaanalyslysis, is, the the matmathemhematiatical cal momodeldel be
besiside de ththe e fafact ct ththat at imimplplicicit it finfinitite e didiffffererenence ce fofor r phphasase e chchanange of ge of ththe e enencacapspsululatated ed PCPCM M isis dis
discrecretiztizatiation on resresultults s in in a a set set of of nonnonlinlinear ear equequa- a- derderiveived unded under the follor the followinwing assumg assumptiptionsons:: ti
tionons, the meths, the method has sevod has severeral othal other draer drawbwbacacksks. . ((AA) The) Thermrmal coal condnducuctitivivity of the PCty of the PCM in theM in the The
These se are are the the ququite ite cumcumberbersomsome e calcalculculatiation on of of dirdirectection ion of thof the HTF fle HTF flow iow is igns ignoreored.d. li
liququid id frfracactition on upupdadatetes s anand d ththe e fafact ct ththat at ththe e (B) (B) ThThe e efeffefectcts s of of nanatuturaral l coconvnvecectition on wiwiththin in ththee temp
temperatuerature fiere field wild within thin the Pthe PCM iCM is not s not calcucalculated lated melt are melt are neglinegligiblgible e and can and can be ignoredbe ignored.. ex
explplicicititly ly bubut t vivia a enenththalalpypy-t-temempeperaratuture re cocorrrrelela- a- (C) The PC(C) The PCM behM behavaves ides ideaealllly, i.y, i.e. sue. such phch phe- e-tio
tion. n. In In thithis s pappaper, er, a a sligslightlhtly y momodifidified ed ententhalhalpy py nomnomena aena as pros properperty degty degradradatiation anon and supd supercercooloolinging meth
method, wod, which ehich enablenables decos decoupliupling of ng of tempetemperaturrature e are not accouare not accounted fornted for.. an
and ld liqiquiuid fd fraractctioion fin fieleldsds, i, is ps preresesentnteded. D. Dererivivatatioion n (D) (D) ThThe e PCPCM M is is asassusumemed d to to hahave ve a a dedefinfinititee of discret
of discretizatiization equatioon equations is ns is straistraightfghtforwarorward and d and meltimelting poinng point (isothermt (isothermal phase chaal phase changenge).). th
the e memeththod od ititseself lf is is vevery ry eaeasy sy to to imimplplememenent. t. (E) (E) ThTherermomophphysysicical al prpropoperertities es of of ththe e PCPCM M araree different for the solid and liquid phases but are different for the solid and liquid phases but are independent of temperature.
independent of temperature.
2.
2. MATHEMATHEMATICMATICAL MODELAL MODEL
(F) The PCM is homogeneous and isotropic. (F) The PCM is homogeneous and isotropic. Th
The e susubjbjecect t of the of the prpresesenent t ininveveststigigatatioion n is is a a (G) Th(G) Therermamal rel resisiststanance ace acrcrososs ths the wae wall oll of thf thee sing
single cole containntainer filler filled wed with PCith PCM (Fig. M (Fig. 1). Pac1). Packing king contcontainer is neglecteainer is neglected.d. th
the e PCPCM M in in sisingngle le cocontntaiaineners rs enenabableles s momodudulalar r (H) La(H) Lateteraral sidl sides of tes of the rehe rectctanangugulalar conr contataininerer con
constrstructuction ion of of the the LHELHES S uniunit t and and is is alsalso o ververy y are are welwell inl insulsulateated, d, i.ei.e. he. heat tat tranransfesfer ocr occurcurs ons only oly onn econ
economic omic from from the vthe viewpoiewpoint oint of mass f mass prodproductiouction. n. sidessides xx550 and0 and xx55d d (cf. Fig. 1).(cf. Fig. 1).
More
Moreoverover, co, complemplete mte meltinelting og of thf the Pe PCM, CM, whicwhich is h is In oIn order rder to vto validaalidate thte the fire first assst assumptumption ion (A(A), th), thee abso
absolutellutely necessary necessary for long-tey for long-term (searm (seasonal) heat sonal) heat influeinfluence of the connce of the conductduction withion within the PCM in thein the PCM in the sto
storagrage (Zivke (Zivkoviovic and Fujc and Fujii, 19ii, 1999), is di99), is difficfficult to ult to dirdirectection ion of of HTF HTF flow flow was was numnumeriericalcally ly invinvestesti- i-ob
obtatain usiin using a ng a shshelell-l-anand-d-tutube LHEbe LHES S ununit wheit where re gagateted d in in ththe e fofollllowowining g waway. y. ReRetataininining g alall l ththee la
largrge e mamasssses es of of ththe e PCPCM M arare e ininvovolvlveded. . ababovove e asassusumpmptitionons s anand d neneglglecectiting ng ththe e cocondnducuctitionon The
There re are are sevseveraeral apl approproachaches es to tto the he matmathemhematiati- - witwithin hin the the PCM PCM in in the the dirdirectection ion nonormarmal l to to thethe ca
cal l momodedeliling of LHEng of LHES S ununitits. In soms. In some e momodedelsls, , HTHTF F floflow, w, ththe e gogovevernrnining g eqequauatitionons s fofor r heheatat con
conducductiotion within within the n the PCM in both the direPCM in both the directiction on tratransfnsfer and phaser and phase change change e can be writcan be written as:ten as: of the HTF flow and the direction normal to the
of the HTF flow and the direction normal to the
≠
≠ H H ≠≠ k k ≠≠T T
HTF flow are taken into account (Lacroix, 1993; HTF flow are taken into account (Lacroix, 1993;
]
]
≠≠t t 55]
]
≠≠ z zS
S DD
]
]
r r]
]
≠≠ z z (1)(1)Gh
Ghononeieim, m, 191989)89), , whwhilile e in in otothehers rs ththe e efeffefect ct of of natural convection within the molten PCM is also
natural convection within the molten PCM is also ≠≠T T
ai ai rr
]
]
]
]
m m cc 55a a A A T s s T 22T T dd (2)(2) f f p f p f ≠≠ z z convconv ht ht aiai rrwhere all the variables are defined in the where all the variables are defined in the nomen-clature table. Detailed description of the clature table. Detailed description of the numeri-ca
cal l sosolulutition on of of ththe e ababovove e seset t of of eqequauatitionons s isis omitted as it is described later in the paper. Here, omitted as it is described later in the paper. Here, only the results obtained are discussed briefly. only the results obtained are discussed briefly.
Even though conduction within the PCM in the Even though conduction within the PCM in the direction of HTF flow plays an important role for direction of HTF flow plays an important role for long LHES units (containers) and relatively high long LHES units (containers) and relatively high convective heat transfer coefficients (Fig. 2), its convective heat transfer coefficients (Fig. 2), its
Fig. 1.
convec-2 2
Fig. 2.
Fig. 2. TempTemperaterature variature variation within the PCM ion within the PCM in the in the diredirectioction n of the of the HTF flow forHTF flow for ll5533 mm andand a a 55300 W/m K.300 W/m K.
con convv
tiv
tive he heat eat tratransfnsfer er coecoefficfficienients ts (s(such uch are are thothose se whewhen n WitWith h the the forforegoegoing ing assassumpumptiotions, ns, the the ententhalhalpypy ai
air r is is usused ed as as ththe e HTHTF) F) anand d rerelalatitivevely ly shshorort t foformrmululatatioion n fofor r ththe e cocondnducuctitionon-c-conontrtrololleled d phphasasee con
contaitainerners s (fro(from m 20200 0 to to 400 400 mmmm). ). FurFurthethermormore, re, chachangnge e can be writcan be written as (Vten as (Volloller, 199er, 1990; 0; VVollollerer et et
com
comparparisoison n of of the the solsolutiution on obobtaitained ned usiusing ng thethe alal.., 1987):, 1987): mathematical model defined with the set of Eqs.
mathematical model defined with the set of Eqs.
≠
≠ H H k k
(1) and (2) and the solution obtained solving the (1) and (2) and the solution obtained solving the
]
]
≠≠t t 55ddiiv vS
S
]
]
r r ggrraaddT TDD
(3)(3)sa
same me prproboblelem m ususining g ththe e lulumpmped ed mamass ss memeththodod sh
showows s ththat at no no sisigngnifiificacant nt imimprprovovememenent t of of ththee
An alternative form of Eq. (3) can be obtained by An alternative form of Eq. (3) can be obtained by res
resultults s is is obtobtainained ed if if the the conconducductiotion n witwithin hin thethe
split
splitting ting the the total enthalpytotal enthalpy H H intinto o sensensibsible le andand PCM is accounted for (Fig. 4). These results are
PCM is accounted for (Fig. 4). These results are
latent heat components: latent heat components: in
in acaccocordrdanance ce wiwith th ththe e reresusultlts s obobtatainined ed byby Ghoneim (1989), who concluded that there is no
Ghoneim (1989), who concluded that there is no H H 55hh11 L L?? f f (4)(4) ll
sig
signifinificancant t chachange nge in in the the prepredicdictiotion n of of the the solsolarar fraction with reduction of
fraction with reduction of DD z z to to lesless s thathan n 20200 0 mmmm. . whewherere
2 2
Fig. 3.
Fig. 3. TempTemperaterature variature variation within the PCM ion within the PCM in the in the diredirectioction n of the of the HTF flow forHTF flow for ll550.3140.314 mm andand a a 5515.5 W/m K.15.5 W/m K.
con convv
Fig. 4.
Fig. 4. CompaComparison betwerison between the en the lumpelumped d mass methomass method and d and the case when the the case when the axiaaxial conductiol conduction is n is accoaccounted for.unted for. T T ≠ ≠ f f ≠ ≠hh ≠≠ k k ≠≠T T ll
]
]
]
]
]
]
]
]
]
]
h h55EE
ccddT T (5)(5) 5 5S DD
S
22 L L (8)(8) ≠ ≠t t ≠≠ x x r r ≠≠ x x ≠≠t t T T mm The fullyThe fully impliimplicit cit discrdiscretizaetization equation for tion equation for anan and
and T T mm is the melting temperature of the PCM.is the melting temperature of the PCM.
internal node ‘
internal node ‘ii’ can be written as (Fig. 5):’ can be written as (Fig. 5): For the problem of isothermal phase change, the
For the problem of isothermal phase change, the local liquid fraction
local liquid fraction f f ll is defined as:is defined as: ≠≠hh k k ≠≠ f f ll
ii ii
]
]
≠≠t t 55]
]
]
]
22 s s T T ii22112222T T i i 11T T ii1111dd22 L L]
]
≠≠t t (9)(9) 1 1 if if T T ..T T r r DD x x m m f f ll((T T ))55HH
(6)(6) 0 0 if if T T ,,T T m m whwherere e ththe e sesensnsibible le enenththalalpy py teterm rm anand d liliququidid Substituting Eq. (4) into Eq. (3) gives:
Substituting Eq. (4) into Eq. (3) gives: fraction term are deliberately left in the differen-fraction term are deliberately left in the differen-ti
tial al foform rm fofor r ththe e coconvnvenenieiencnce e of of susubsbseqequeuentnt
≠ ≠ f f ≠
≠h h k k ll
]
]
≠≠t t 55ddiiv vS
S
]
]
r r ggrraaddT TDD
22 L L]
]
≠≠t t (7)(7) numerical computation. It should be noted that thenumerical computation. It should be noted that thediscr
discretizaetization tion equaequations tions for for bounboundary dary nodenodes s de- de-Eq.
Eq. (7) r(7) reprepreseesentsnts, t, togogethether er witwith h EqsEqs. (5) . (5) and and (6) (6) pend pend on on spespecificific c bouboundandary ry conconditditionions s and and areare an
and d ththe e apapprpropopririatate e ininititiaial l anand d bobounundadary ry cocon- n- dedeririveved d frfrom om an an enenerergy gy babalalancnce e on on bobounundadaryry dit
ditionions, s, the the matmathemhematiatical cal modmodel el of of conconducductiotion n concontrotrol l vovolumlumes.es.
cconontrtroolllleed d isisooththerermamal l pphahase se chchanangge. e. TThhe e kkey ey ffeaeatuturre e oof f ththe e pproroppososed ed mmetethhod od is is ththee fact that for an isothermal phase change (which is fact that for an isothermal phase change (which is the case for most salt hydrates), the temperature the case for most salt hydrates), the temperature
3.
3. NUMERNUMERICAL SOLUTIICAL SOLUTIONON
o
of f ththe e PCPCM M wiwiththin in a a gigivven en coconntrtrool l vovolulummee For the problem of one-dim
For the problem of one-dimensioensional isothenal isothermal rmal remaremains conins constant astant and eqnd equal to itual to its meltis melting temng tempera- pera-ph
phase chanase change of ge of the PCM encathe PCM encapsupsulatlated withied within n a a turture e untuntil the PCM il the PCM has melhas melted comted complepleteltely. Con-y. Con-re
rectctanangugulalar r cocontntaiainener r (Fi(Fig. g. 1), 1), ththe e gogovevernrnining g sisideder first thr first the case whe case when coen contntrorol volul volume ‘me ‘‘i‘i‘ is‘ is eq
equauatition on fofor tr the he PCPCM fM folollolows fws frorom Em Eq. q. (7): (7): fufulllly soy solilid or fd or fulully lly liqiquiuid. Id. In thn that cat casase, fe, frorom thm thee
Fig. 5.
definition of sensible enthalpy, Eq. (5), and the
definition of sensible enthalpy, Eq. (5), and the k k DDt t
ol ol dd
]
]
]
]
liquid fraction, Eq. (6), it follows that:
liquid fraction, Eq. (6), it follows that: f f l l 55 f f ll 11 22 s s T T ii 2222T T 11T T dd (18)(18)
2 211 m m ii1111 i i ii r r L L DD x x ≠ ≠hhi i ≠≠T T ii wh
whicich h is is ththe e eqequauatition on fofor r upupdadatiting ng ththe e liliququidid
]
]
≠≠t t ;; cc]
]
≠≠t t (10)(10)fra
fractiction on fielfield d witwithin hin the the concontrotrol l volvolumume e thathat t isis undergoing a phase change. As Eq. (15) shows, undergoing a phase change. As Eq. (15) shows, and
and
liquid fractions are updated from the temperature liquid fractions are updated from the temperature
≠ ≠ f f
llii field field anand d nonot t frfrom om ththe e sesensnsibible le enenththalalpy py fiefieldld
]
]
≠≠t t ;; 00 ((1111)) (V(Volleroller, , 19901990; ; LacrLacroix, oix, 1993). 1993). The The temptemperatueraturereand
and the the liqliquid uid frafractiction on fielfield d are are decdecououplepled, d, thethe where
where cc is the specific heat of the solid or liquidis the specific heat of the solid or liquid
temperature field within the PCM being calculated temperature field within the PCM being calculated phase, depending on state of the control volume.
phase, depending on state of the control volume. in
indedepependndenentltly y frfrom om EqEq. . (13) (13) foforcrciningg aa 55 ii2211
Af
Afteter r inintrtrododucucining g EqEqs. s. (10) (10) anand d (11)(11), , EqEq. . (9)(9)
a
a 550,0, aa 551 1 aanndd bb 55T T fofor r ththe e cocontntroroll ii1111 i i i i mm
reduces to ordinary heat diffusion equation: reduces to ordinary heat diffusion equation:
volumes which are undergoing the phase change. volumes which are undergoing the phase change.
≠
≠T T k k Furthermore, on the basis of Eq. (18), it can beFurthermore, on the basis of Eq. (18), it can be ii
]
]
≠≠t t 55]
]
]
]
22 s s T T ii22112222T T i i 11T T ii1111dd (12)(12) inferred that for an isothermal phase change, allinferred that for an isothermal phase change, allr r ccDD x x
the heat supplied to the control volume the heat supplied to the control volume undergo-Backward differencing of the left side term gives,
Backward differencing of the left side term gives, ining g a a phphasase e chchanange ge is is usused ed fofor r chchanangiging ng ththee after rearran
after rearrangingging, , the the fully implicit finite fully implicit finite diffdiffer-er- amamouount nt of of lalatetent nt heheat at cocontntenent t of of ththat at cocontntroroll ence equation of the form:
ence equation of the form: volume.volume.
At this point it is worthwhile to describe the At this point it is worthwhile to describe the
a
a ??T T 11aa ??T T 11aa ??T T 55bb (13)(13)
ii2211 ii2211 i i i i ii1111 ii1111 ii imimplplememenentatatition on of of ththe e cocompmpututatatioionanal l momodedel,l,
which is as follows: which is as follows: where coefficients
where coefficients aa 55aa 55 22Fo,Fo, aa 551111 ii2211 ii1111 ii
ol
ol dd (a) Coefficients ‘(a) Coefficients ‘aa’ of Eq. (13) are formed. For’ of Eq. (13) are formed. For
2
233Fo andFo and bb 55T T are introduced for the sakeare introduced for the sake i
i ii
nodal points where the liquid fraction
nodal points where the liquid fraction f f is strictlyis strictly of
of comcompuputattationional al simsimpliplicitcity. y. SupSuperserscricript pt ’ol’old’d’ lili
in the interval [0,1], 0
in the interval [0,1], 0 ,, f f ,,1, the coefficients of 1, the coefficients of
refers to the previous time step and Fo is a finite
refers to the previous time step and Fo is a finite lili
Eq. (13) are set to:
Eq. (13) are set to: aa 55aa 550,0, aa 551 and1 and
difference form Fourier number:
difference form Fourier number: ii2211 ii1111 ii
b
bi i 55T T mm..
a a ?? DDt t
(b
(b) ) ThThe e seset t of of lilinenear ar alalgegebrbraiaic c EqEqs. s. (13) (13) isis
]
]
]
]
Fo
Fo55 22 (14)(14) D
D x x solved using the Gauss-Seidel iterative procedure.solved using the Gauss-Seidel iterative procedure.
(c) Liquid fractions are updated from the (c) Liquid fractions are updated from the tem-where
where a a 55k k / / r r cc is the thermal diffusivity of theis the thermal diffusivity of the
perature field using Eq. (18). perature field using Eq. (18). PCM. The thermophysical properties in Eq. (14)
PCM. The thermophysical properties in Eq. (14)
(d) A check for the ‘start’ and for the ‘end’ of (d) A check for the ‘start’ and for the ‘end’ of depend on the state of the control volume. Those
depend on the state of the control volume. Those
phase change is performed. Explicitly, if the state phase change is performed. Explicitly, if the state of the solid phase should be inserted if the control
of the solid phase should be inserted if the control of
of ththe e liliququid id frfracactition on fiefield ld chchanangeges s wiwiththin in ththee volume is in the solid state and those of the liquid
volume is in the solid state and those of the liquid
given time step, i.e. a finite volume commences or given time step, i.e. a finite volume commences or phase if the control volume is in the liquid state.
phase if the control volume is in the liquid state.
terminates with the phase change, the coefficients terminates with the phase change, the coefficients No
Now, w, coconsnsidider er ththe e cacase se whwhen en memeltltining g ((oror of
of EqEq. . (1(13) 3) neneed ed to to be be upupdadateted d anand d ststepeps s ((aa)) freezing) occurs around a certain node ‘
freezing) occurs around a certain node ‘ii’. In that’. In that
through (d) repeated for the same time step. through (d) repeated for the same time step. cas
case, e, the the liqliquid uid frafractictionon f f lili lilies es ststririctctly ly in in ththee
In
In prpracactiticece, , fofor r momost st titime me ststepeps s ononly ly ononee interval [0,1]. Recognizing that for an isothermal
interval [0,1]. Recognizing that for an isothermal
iteration is needed per time step. The only time iteration is needed per time step. The only time phase change:
phase change:
when two iterations are needed is when the phase when two iterations are needed is when the phase change boundary moves from one control volume change boundary moves from one control volume
T
T ;i i ; T T mm (15)(15)
to the next one. to the next one. and from Eq. (5):
and from Eq. (5):
3.1.
3.1. ChecChecking king for start for start / / end of the phase changeend of the phase change
≠ ≠hh
ii
]
]
≠≠t t ;; 00 ((1166)) At the end of each time step, the check for startAt the end of each time step, the check for startand/or end of the phase transition is performed and/or end of the phase transition is performed Eq. (9) becomes:
Eq. (9) becomes: ththrorougughohout ut ththe e enentitire re dodomamainin. . FoFor r ththe e cacase se of of melting, checking for the ‘start’ and ‘end’ of the melting, checking for the ‘start’ and ‘end’ of the
≠ ≠ f f
llii k k phphasase e chchanange ge is is peperfrforormemed d in in ththe e fofollllowowiningg
]
]
]
]
]
]
L L 55 s s T T 2222T T 11T T dd (17)(17) 2 2 ii2211 m m ii1111 ≠ ≠t t r r DD x x fashion:fashion: 3.1.1.3.1.1. START of meltingSTART of melting. For a given time step,. For a given time step, Backward differencing of the liquid fraction term
Backward differencing of the liquid fraction term
ol ol dd
g
giivveess:: iiffT T $$ T T whilewhile T T ,,T T , it indicates that within, it indicates that within i
this time step, the finite volume in question begins
this time step, the finite volume in question begins 3.1.2.3.1.2. END of meltingEND of melting. For a given time step, if . For a given time step, if
ol ol dd
with melting. In that case, the coefficients of Eq.
with melting. In that case, the coefficients of Eq. f f llii$$1 while1 while f f llii ,,1, it indicates that within this1, it indicates that within this
ti
time me ststepep, , ththe e cocontntrorol l vovolulume me in in ququesestition on hahass (13)
(13) arare e upupdadateted d as as dedescscriribebed d ababovove e anand d ththee
melted completely. In that case coefficients of Eq. melted completely. In that case coefficients of Eq. cal
calculculatiation on for for thathat t stestep p is is perperforformed med agaagain. in. ItIt (1
(13) 3) arare e agagaiain n seset t toto aa 55aa 55 22Fo,Fo, aa 55
should be noted, however, that in the time step
should be noted, however, that in the time step ii2211 ii1111 ii
ol ol dd
1
1112233Fo andFo and bb 55T T and the calculation forand the calculation for
wh
when en a a cocontntrorol l vovolulume me hahas s jujust st bebegugun n wiwithth i i ii
that time step is performed again. In the time step that time step is performed again. In the time step melting, Eq. (18) has the form:
melting, Eq. (18) has the form:
in which the phase change boundary moves from in which the phase change boundary moves from
k
k DDt t the control volume in question to the next one,the control volume in question to the next one,
ol ol dd
]
]
]
]
f f 55 f f 11 s s T T 2222T T 11T T dd ll i i llii 22 ii2211 m m ii1111 coefficientcoefficient bb has the following form:has the following form:
ii r r L L DD x x cc olol dd LL olol dd
]
]
2 2s s
T T 22T Tdd
(19)(19)]
]
b b 55T T 22 1122 f f (20)(20) m m ii i i m ms s
lldd
L L cc iiwhere the last term on the right hand side can be where the last term on the right hand side can be The last term on the right-hand side of Eq. (19)
The last term on the right-hand side of Eq. (19)
described as the amount of heat needed to described as the amount of heat needed to com-re
reprpresesenents ts ththe e amamouount nt of of sesensnsibible le heheat at ththat at isis
pletely melt the control volume in question within pletely melt the control volume in question within ne
neededed ed to to raraisise e ththe e tetempmpererataturure e of of ththe e cocontntroroll
the time step and which consequently can not be the time step and which consequently can not be volume from the temperature in the previous time
volume from the temperature in the previous time
ol
ol dd used to raise the temperature of the PCM.used to raise the temperature of the PCM.
sstteep p ((T T i i ) ) to to ththe e mmeleltitinng g tetemmppereratatuure re ((T T mm).).
The flow chart for the computational procedure The flow chart for the computational procedure Consequently, that amount of heat can not be used
Consequently, that amount of heat can not be used
is given in Fig. 6. is given in Fig. 6. for melting the PCM.
for melting the PCM.
4.
4. VERIFVERIFICATIICATION OF ON OF THE MATHEMATTHE MATHEMATICALICAL MODEL
MODEL
4.1.
4.1. Test problemTest problem
Th
The e perperforformanmance ce of of the the prepresensented ted metmethod hod isis first verified with a one-dimensional phase change first verified with a one-dimensional phase change test problem explained in Voller (1990). A pure test problem explained in Voller (1990). A pure liq
liquid uid iniinitiatially lly at at 2288C C occuoccupies pies the the semi-semi-infininfiniteite
space
space xx$$0. At time0. At time t t 550 the surface at0 the surface at xx550 0 isis
fix
fixed ed at at ththe e tetempmpererataturure e of of 22101088C, C, whwhicich h isis
bel
below ow the the frefreeziezing ng popoint int of of the the subsubstastancence T T 55 m m
0
088C. As time proceeds, a solid layer builds up onC. As time proceeds, a solid layer builds up on
the surface
the surface xx550 and moves out into the liquid.0 and moves out into the liquid.
Simply stated, the problem is to determine how Simply stated, the problem is to determine how the
the solsolid–liquid–liquid id sursurfacface e momoves ves witwith h timtime. e. ThThee thermal properties of the material in question are thermal properties of the material in question are assumed to be constant and equal for both solid assumed to be constant and equal for both solid
6 6
and
and liqliquid uid phphasease:: k k 552 2 [W[W// mKmK],], r r cc552.52.5331010
3
3 8 8 33
[[J / m J / m KK] a] anndd r r L L55110 0 [J/m [J/m ]]. . IIn n nnuumemeririccalal
4 4
analysis 50 time steps of
analysis 50 time steps of DDt t 554.324.3233110 0 [[ss] ] (1/2(1/2
days) and 20 space increments of
days) and 20 space increments of DD x x550.125 [m]0.125 [m]
were used. were used.
The position of the phase front after 25 days The position of the phase front after 25 days (i.e. 50 time steps) obtained with proposed (i.e. 50 time steps) obtained with proposed meth-od is
od is xx550.8405 [m]. The difference between this0.8405 [m]. The difference between this
result and the result of
result and the result of xx550.8415 [m] obtained by0.8415 [m] obtained by
Voller (1990) is merely 0.12%. Therefore, it could Voller (1990) is merely 0.12%. Therefore, it could be
be conconclucluded that ded that the the accaccurauracy cy of of the the proproposposeded comp
computatutational ional modmodel el for for condconductiouction n contcontrollerolledd isothermal phase change is satisfactory.
isothermal phase change is satisfactory.
4.2.
4.2. Experimental verificationExperimental verification
As was discussed in the previous paragraph, the As was discussed in the previous paragraph, the
Fig. 6.
Tabl
Table e 1. 1. ThermThermophysiophysical propertical properties es of of CaC1CaC1 ??6H 6H OO
2
2 22 sides. A thermocouple was placed in the centre of sides. A thermocouple was placed in the centre of
Melting point [
Melting point [88CC]] 2299..99 the container in the manner indicated in Fig. 7.the container in the manner indicated in Fig. 7.
L
Laatteennt t hheeaat t [[KKJJ // kkgg] ] 118877
3
3 ThThe e cocontntaiainener r wiwith th ththe e sosolilid d PCPCM M wawas s ththenen
D
Deennssiitty y [[kkgg // m m ]]: : SSoolliid d 11771100
placed vertically in the constant temperature bath, placed vertically in the constant temperature bath,
L
Liiqquuiid d 11553300 S
Sppeecciifific c hheeaat t [[kkJJ // kkggKK]]: : SSoolliid d 11..44 where the temperature was set towhere the temperature was set to T T 55606088C.C.
` `
L
Liiqquuiid d 22..22
Th
The e cocompmpututatatioionanal l momodedel l wawas s seset t up up to to re
re--T
Thheerrmmaal l ccoonndduuccttiivviitty y [[WW/ m/ mKK]]: : SSoolliid d 11..0099
prod
produce uce expeexperimerimental ntal condconditionitions s withiwithin n the the con-
con-L
Liiqquuiid d 00..5533
stant temperature bath. The convection heat stant temperature bath. The convection heat trans-ver
very y satsatisfisfactactory ory resresultults s for for the the conconduductiction-on-concon- - fer coeffer coefficificient betwent between the air een the air and the contand the containainerer tro
trollelled d oneone-di-dimenmensiosional nal phaphase se chachangnge e testest t proprob- b- walwall l was detewas determirmined usinned using g the corrthe correlaelatiotion n givgivenen le
lem. m. HoHowewevever, r, memeltltining g of of ththe e PCPCM M in in sesealaled ed in Inin Incrcropoperera and Da and DeeWiWitt (19tt (1985)85), and w, and was caas calclcu-
u-2 2
con
contaitainerners s is is gengeneraerally lly mumultilti-di-dimenmensiosional (nal ( botboth h latlated to bed to bee a a 5516 16 [W/m [W/m K]. FurthK]. Furthermermorore, e, aa
co co nnvv
radi
radial and al and axial axial condconductiouction exisn exist) and at) and also nalso natural tural time time stepstep DDt t 555 s and space increment5 s and space increment DD x x552 2 mmmm
co
convnvecectition on ococcucurs rs wiwiththin in ththe e memeltlted ed PCPCM. M. ThTherere- e- wewere re usused ed in in ththe e cacalclcululatatioion. n. In In FiFig. g. 8 8 ththee for
fore, e, an an expexperierimenment t was was perperforformed med in in ordorder er to to varvariatiation ion witwith tih time me of nof numeumericrical aal and nd expexperierimenmentaltal inve
investigastigate the inte the influenfluence of thce of the assume assumptionptions of the s of the valuvalues of the es of the tempetemperaturrature at e at the centrthe centre of e of the testthe test ma
maththememataticical al momodedel. l. ThThe e PCPCM M usused ed fofor r exex- - cocontntaiainener r is is shshowown.n. pe
peririmementntal anaal analylysis is casis is calclciuium chlm chlororidide hexe hexahahy- y- FrFrom the reom the resusultlts s shshowown n in Figin Fig. . 8, it can be8, it can be dr
dratate e (Ca(CaClCl ??6H O) 6H O) witwith h the the thethermormophphysiysical cal conconclucluded ded thathat tht the age agreereemenment bet betwetween en nunumermericaicall
2
2 22
pro
properpertieties s as as lislisted ted in in TabTable le 1 1 (Fuj(Fujii ii anand d YYanoano, , and and expexperierimenmental dtal data iata is wels well witl within ehin expxperierimenmentaltal 1
1999966)). . uunncceerrttaaiinnttiiees s ((ii..ee. . ppoossiittiioonniinng g oof f tthhe e tthheerrmmooccoou u--A re
A rectangctangular ular contacontainer, iner, made made of sof stainltainless sess steel, teel, ple’ple’s s tip exactly in tip exactly in the centre of the centre of the containthe container iser is with dimensions of
with dimensions of ll55bb55100 mm and100 mm and d d 5520 20 mm mm ququitite e didiffifficucult lt anand d exexpeperirimementntal al dadata ta wewere re rereadad
(Fig
(Fig. . 1), 1), was was fillfilled ed witwith h the the calcalciucium m chlchlorioride de frofrom cm charharts, ts, whiwhich ch redreduceuces as accuccuracracy). y). ThThe he highigherer hex
hexahyahydradrate te and and welwell l insinsulaulated ted on on the the latlateraeral l sloslope pe of of the the thetheoreoretictical cal curvurve in e in the the liqliquid uid regregionion
Fig. 7.
Fig. 7. Test contaTest container.iner.
Fig. 8.
is du
is due to the fe to the facact that that the Grt the Grasashohof numf numbeber was r was veveststigigatated ed fofor r ththe e rerectctanangugulalar r anand d cycylilindndriricacall calculated for the temperature difference of
calculated for the temperature difference of T T 22 containers.containers.
` `
T
T ¯mm¯30 K, whil30 K, while e in rein realalitity y ththis diis diffffererenence bece be- - ThThe e mamaththememataticical al momodedel l fofor r ththe e isisotothehermrmalal com
comes es smasmalleller r as as the tempethe temperatraturure e of of the liquithe liquid d phaphase chanse change of the PCM fillge of the PCM filling thing the cyline cylindridricalcal PCM
PCM incincreareasesses. C. Consonsequequentently, ly, the the conconvevectictive ve heaheat t concontaitainer ner (Fig(Fig. . 9) 9) was was derderiveived d undunder er the the samsamee tr
tranansfsfer er cocoefefficficieient nt bebetwtweeeen n ththe e aiair r anand d ththe e asassusumpmptitionons s as in as in ththe e cacase of se of ththe e rerectctanangugulalarr con
contaitainer wall used in ner wall used in the calcthe calculaulatiotion n is is highigher her concontaitainerner. . HowHoweveever, r, the the gogoververninning g equequatiation on forfor tha
than n the the ‘re‘real’ al’ onone. e. FurFurthethermormore, re, it it can can be be obob- - the the two two momodeldels is s is difdifferferenent ant and fd for or the the cascase oe of thf thee serv
served froed from Fig. 8 thm Fig. 8 that in theat in theory PCory PCM reacM reaches its hes its cylincylindricadrical l contcontainer it has ainer it has the followthe following form:ing form: melting temperature faster than in the experiment.
melting temperature faster than in the experiment.
≠
≠ H H 11 ≠≠ k k ≠≠T T
This is assumed to be due to the basic assumption This is assumed to be due to the basic assumption
]
]
≠≠t t 55]
]
r r]
]
≠≠r rS DD
S
]
]
r r]
]
≠≠r r (21)(21)made in the mathematical model that the made in the mathematical model that the conduc-tion resistance of the container wall is neglected. tion resistance of the container wall is neglected.
In
In ththe e ababovove e eqequauatitionon,, H H reprepresresentents s the the tottotalal Mo
Morereovoverer, , frfrom om ththe e sasame me figfigurure e it it cacan n be be ob
ob--enthalpy, which can be split into its sensible and enthalpy, which can be split into its sensible and served that the calculated PCM’s melting time is
served that the calculated PCM’s melting time is la
latetent nt cocompmpononenent t ((cfcf. . EqEq. . (4)(4)). ). ThThe e sosolulutitionon slightly longer than the experimental one, which
slightly longer than the experimental one, which
met
methohodoldology ogy and and numnumerierical cal proprocedcedurure e for for EqEq.. may be due to the fact that the natural convection
may be due to the fact that the natural convection
(21) is the same as for Eq. (3). (21) is the same as for Eq. (3). within the liquid PCM is ignored. However, it can
within the liquid PCM is ignored. However, it can be seen that neglecting both the natural be seen that neglecting both the natural
convec-5.1.
5.1. Results and discussionResults and discussion
tio
tion n witwithin hin the the liqliquid uid PCM PCM and the and the conconducductiotionn wit
within hin the the PCM PCM in tin the dhe direirectiction oon of thf the HTe HTF floF flow w ThThe dimee dimensinsionons of the cos of the contantaineiners werrs were choe chosensen do n
do not inot introtroducduce sige signifinificancant errt error in tor in the prhe prediedictiction on in such in such a a manmanner that the ner that the vovolumlume e as as welwell l as as thethe of the
of the PCM’PCM’s s temptemperatuerature re variavariation during melt- tion during melt- convconvectivective heae heat trant transfer sfer area area for bfor both toth the cyhe cylindlindri- ri-iinngg. . ccaal l aannd d rreeccttaanngguullaar r ccoonnttaaiinneerrs s wweerre e eeqquuaall. . TThhee fixed dimensions were chosen to be the length of fixed dimensions were chosen to be the length of the cylindrical container
the cylindrical container ll 550.2 m (cf. Fig. 9) and0.2 m (cf. Fig. 9) and c
c
5.
5. COMPCOMPARISON OF THE ARISON OF THE MELTIMELTING TIMENG TIME
the width of the rectangular container
the width of the rectangular container bb550.1 m0.1 m FOR RECTANGULAR AND CYLINDRICAL
FOR RECTANGULAR AND CYLINDRICAL
(cf. Fig. 1). The air velocity was assumed to be (cf. Fig. 1). The air velocity was assumed to be
CONTAINERS CONTAINERS
w
w555 5 m/m/ s s anand d itits s tetempmpereratatururee T T 55606088C. C. ThThee
ai ai rr
The
The melmeltinting g timtime e of of the the incincapsapsulaulated ted PCM PCM is is thethermormophyphysicsical pal proproperterties oies of thf the aire air, as w, as well aell as ths thee on
one e of of the the essessentential ial parparameameterters s for deterfor determinmining ing conconvecvectivtive e heaheat t tratransfnsfer er coecoefficfficienient t betbetweeween n thethe the
the sizsize ane and thd the she shapape of e of the the concontaitainerner, as , as it mit must ust air air and and the the concontaitainerner’s ’s walwalll a a coco nnvv, , wewere re tatakekenn cor
corresrespopond nd to to the the tottotal al amoamoununt ot of df dailaily iy insonsolatlationion. . frofrom m InIncrocroperpera a and and DeDeWitWitt t (198(1985). 5). The The PCMPCM To
To be be spspececifiific, c, ththe e cocontntaiainener r cocontntaiainining ng PCPCM M filfilliling the conng the contataininerers s wawas s chchososen to en to be calbe calciciumum sho
should uld be dbe desiesignegned in sd in such uch a waa way thy that aat at tht the ene end d chlchlorioride de hexhexahyahydrdrateate, , witwith h the the thethermormophphysiysicalcal of
of ththe e daday, y, cocompmplelete te memeltltining g of of ththe e PCPCM M is is prpropoperertities es as as liliststed ed in in TaTablble 1e 1.. ac
achihieveveded. I. In tn thahat wt wayay, t, the he mamaxiximumum em effifficicienency cy of of FiFig. g. 10 10 shshowows s ththe e vavaririatatioion n wiwith th titime me of of ththee the
the LHELHES S uniunit t is is achachievieved. ed. FurFurthethermormore, re, comcompleplete te PCMPCM’s ’s temtemperperatuature re in in the the cencentretres s of of boboth th thethe mel
meltinting og of thf the PCe PCM is M is a nea necescessarsary coy condinditiotion fn for or recrectantangugular lar and and cylcylindindricrical al concontaitaineners rs for for thethe lon
long-tg-term erm (s(seaseasononal) al) thethermarmal l eneenergy rgy stostoragrage. e. In In difdifferferent diment dimensensionions s of the contof the containainersers. For small. For small li
lighght t of of ththatat, , ththe e ininflufluenence ce of of ththe e cocontntaiainener’r’s s vavalulues oes of f d d (cf. Fig. 1) and(cf. Fig. 1) and r r oo (cf. Fig. 9), the(cf. Fig. 9), the dim
dimensensionions s and and its its shashape pe werwere e numnumeriericalcally ly in- in- difdifferferencence in e in melmeltinting tg time ime betbetweeween tn the rhe rectectangangulaularr
Fig. 9.
Fig
Fig. . 10. 10. ComComparparisoison n of of the variathe variatiotion n witwith h timtime e of of the PCM’s the PCM’s temtemperperatuature re at at the centrthe centre e of of the rectathe rectangungular and lar and cylcylindindricricalal containers.
containers.
and cylin
and cylindridrical cal concontaitainerners s is is not not so so propronounouncenced. d. PCM fillPCM filling thing the contae containeiner on the meltir on the melting time of ng time of How
Howeveever, r, on on incincreareasinsing g the the masmass s of of the the PCM PCM PCMPCM. I. It cat can bn be oe obsebserverved td that hat for for larlarger ger ququantantitiitieses filling the container, i.e. with increasing
filling the container, i.e. with increasing d d for thfor the e of thof the matee material filrial filling ling the cothe containntainer, ther, the dife differeferencence recta
rectangulngular ar contacontainer iner andand r r oo for for the the cylcylindindricrical al in the mein the meltilting timng time betwe between theen the recte rectangangulaular andr and co
contntaiainener, r, ththe e didiffffererenence ce in in ththe e memeltltining g titime me cycylilindndriricacal l cocontntaiaineners rs is is vevery prory prononoununceced, withd, with inc
increareases ses conconsidsideraerablybly, , witwith h the the recrectantangulgular ar the the melmeltinting g timtime e of of the the cylcylindindricrical al concontaitainer ner beibeingng con
contaitainer ner shoshowinwing g a a mucmuch h shoshorterter r melmeltinting g timtime e neanearly trly twicwice thae that of tht of the rece rectantangugular olar one. Ine. It shot shoulduld tha
than thn the cye cylinlindrdricaical col contantaineiner of r of the the samsame ve voluolume me be be popointinted ed ouout t thathat t in in ordorder er to to makmake e the the com com--aannd d hheeaat t ttrraannssffeer r aarreeaa. . ppaarriissoon n bbeettwweeeen n tthhe e ttwwo o ggeeoommeettrriiees s ssiiggnniifificcaanntt,,
A
A serseries ies of of numnumerierical cal expexperierimenments ts werwere e perper- - the numthe numerierical anacal analyslysis was perfois was performermed under thed under the for
formed and med and thetheir ir resresultults s are summaare summarizrized ed in in FigFig. . conconditdition of equion of equal volual volume and heame and heat transt transfer arefer areaa 11
11 which shows which shows the the influinfluence of ence of the the amouamount nt of of for for both both the the rectarectangulngular ar and and cylincylindricadrical l contcontainerainers.s.
Fig. 11.