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transfer problem
Grégoire Allaire, K. El Ganaoui
To cite this version:
Grégoire Allaire, K. El Ganaoui. Homogenization of a conductive and radiative heat transfer problem.
Multiscale Modeling and Simulation: A SIAM Interdisciplinary Journal, Society for Industrial and Applied Mathematics, 2009, 7 (3), pp.1148-1170. �10.1137/080714737�. �hal-00784061�
CENTRE DE MATHÉMATIQUES APPLIQUÉES
UMR CNRS 7641
91128PALAISEAU CEDEX (FRANCE).Tél: 0169 33 4600. Fax: 01 69 3346 46
http://www.map.polytehnique.fr/
Homogenization of a ondutive
and radiative heat transfer
problem
Grégoire Allaire, Karima El Ganaoui
R.I. 639 September 2008
GRÉGOIRE ALLAIRE
†
AND KARIMA ELGANAOUI
‡
Abstrat. Thispaper isdevoted tothe homogenizationof a heat ondution problem ina
periodiallyperforateddomainwithanonlinearandnonloalboundaryonditionmodelingradiative
heattransfer intheperforations. Beause ofthe onsideredritialsalingit isessentialtousea
methodoftwo-saleasymptotiexpansionsinsidethe variationalformulationofthe problem. We
obtain a nonlinear homogenized problem of heat ondution with eetive oeients whih are
omputedviaaellproblemfeaturingaradiativeheattransfer boundaryondition. Werigorously
justifythishomogenizationproess forthelinearizedproblembyusingtwo-saleonvergene. We
perform numerialsimulationsin2-d: wereonstrutanapproximatetemperature eldbyadding
tothe homogenizedtemperature aorretorterm. Theomputednumerial errorsagreewiththe
theoretial preditederrorsand provethe eetiveness ofourmethod formultisale simulationof
ondutiveandradiativeheattransferproblemsinperiodiallyperforateddomains.
Keywords.Homogenization,two-saleonvergene,radiativetransfer,heatondution.
AMSsubjet lassiations.
1. Introdution. The goal of this paper is to theoretially and numerially
study the homogenization of a ondutiveand radiative heat transferproblem in a
perforatedperiodimedia. The motivation of this problem omes from the nulear
reator industry: an alternative onept to the usual pressurized water reators is
thatofgasooledreators. Typially,agraphitematrix(playingtheroleofneutron
moderator)isperiodiallyperforatedbylonghannelsontainingeithertheuranium
fueloragasoolantwhihishelium. Reallthatthessionnulearreationsprodue
alargeamountofheatwhihshouldberemovedfromthereatororebyaoolantin
ordertoativateasteamgenerator(throughaheatexhanger)andnallytoprodue
eletriity. Herewefousonlyontheheattransferprobleminsuhanheterogeneous
medium. Tosimplifytheexposition,weassumethatthegraphiteanduraniummatrix
isalreadyhomogenizedandanbeonsideredasasinglehomogeneousmaterial. In-
sidethismatrixheat istransmittedbysimplelinearondution. Ontheotherhand,
the helium heat ondutivity is ompletely negligible with respet to the radiative
transfer taking plae inside the hannels. We therefore fae a oupled problem of
heat ondution and radiation where the number of helium hannels is very large,
typially of the order of 104. For dimensioning purposes as well as safety studies manynumerialsimulationshavetobeperformedforwhihadiretapproah(mesh-
ing all the geometri details) is impossible, orat least muh too ostly. Therefore,
homogenizationisaneessaryingredientforthestudyofsuhdevies.
Inthisproblemthegoalofhomogenizationistwofold: rst,itmustyieldalear
denition of what is the homogenized problem, and seond, it has to give expliit
formulas for the eetive parameters as well as a reipe to approximate the exat
solution. Indeed,sinetheoriginalmodel isamixtureoftwodierenttypeofequa-
tions(ondutionandradiativetransfer),thepreiseformofthehomogenizedsystem
is not lear a priori. Conerning the seond point, the original problem is posed
in aperforatedmedium whilethe homogenizedproblem is posed in ahomogeneous
∗
ThisworkhasbeensupportedbytheFrenhAtomiEnergyCommission,DEN/DM2SatCEA
Salay.
†
CMAP,(gregoire.allairepolyte hniq ue. fr) .
‡
CMAP,(ganaouimap.polytehniq ue.f r).
medium, sotaking into aount orretorterms is of paramount importane if one
wantsageometriallysoundreonstrutionofanapproximatesolution.
Let us ome bak to the physial modeling of the original problem. The true
problemis three-dimensionalbut theheliumhannelsarelongparalleltubes,soho-
mogenization takes plae only in the ross setion. Therefore, it is not a severe
restritiontoonsideronlythetwo-dimensionalhomogenizationofarosssetionof
thegeometry (see Figure2.1) asweshall dobelow. Asusual in homogenizationwe
denote byε the period. The matrixperforateddomain is Ωε where energytransfer
is done by ondution. The tubes or holes are τε,i, with boundariesΓε,i whih are
grey-diuse surfaes, and are lled by helium, assumed to be a transparentmedia
withoutheat ondution norabsorption of radiation. Under these assumptions, the
radiation equation anbeintegrated inside eah hole τε,i to produe a ompliated
(non linear and non loal) boundary ondition on the wall Γε,i. Setion 2.2 gives
a preise desriptionof this boundaryondition. Let us simply gives theomplete
model when theemissivity is equalto one. Forgiven bulkand surfaeheat soure
termsf andg,thetemperatureTεisasolutionof
−div(Kε∇Tε) = f in Ωε,
Kε∇Tε·n = g on ∂Ω,
−Kε∇Tε·n = σ
ε Tε4(x)− Z
Γε,i
F(x, s)Tε4(s)dγ(s)
!
on Γε,i,
(1.1)
where F(x, s) is the so-alled view fator for the wall Γε,i. The saling ε−1 in the
righthand sideof theboundaryonditionyieldsaperfetbalane, in thelimit asε
goestozero,betweenthebulkheatondution andthesurfaeradiativetransfer. A
dierentsalingwas studiedin[7℄.
Sine the seminal paper [12℄ it is known that the use of two-sale asymptoti
expansionsinperforateddomainsissometimesdeliate,espeiallywhentheboundary
onditionsarenonlinearandnonloal ashere. Indeed,thehomogenization of(1.1)
by the formal method of two-sale asymptoti expansions(as presented in [8℄, [9℄,
[11℄,[21℄)isnotompletelyobvious,allthemoreifoneworkswiththestrongfromof
theequations. Asexplainedin Setion3itismuhsimplerto performthetwo-sale
asymptoti expansionsin the variationalformulation of (1.1), symmetriallyin the
unknownand inthetest funtion (followinganideaofJ.-L. Lions[16℄). Asaresult
we obtain that the leading term T(x) in the ansatz of Tε(x) is the solution of the
followingnonlinearhomogenizedproblem
(
−div(K∗(T)∇T) = mes(Y
∗)
mes(Y)f in Ω,
K∗(T)∇T·n = g on ∂Ω, (1.2)
whereK∗(T)istheeetiveondutivity,dependingonthemarosopitemperature
T,anddenedthroughaloalellproblem(3.3)whihisalinearizedondutiveand
radiativetransferproblemintheunit ell(seeProposition 3.1).
In Setion 4 we give a rigorous justiation of suh an homogenization result
for the linearized versionof (1.1) (see Theorem 4.6). Our main toolsare two-sale
onvergene[2℄,[20℄andsuitableTaylorexpansionsofthetestfuntion oneahhole
boundaryΓε,i inordertotakeadvantageof theviewfatorproperties.
Eventually Setion 5is onerned with numerial simulations for this problem.
Followingalassialideainperiodihomogenization,weapproximatethesolutionTε
of (1.1)bythetworsttermsofitsansatz,i.e.,thehomogenizedsolutionT plusthe
so-alledorretorterm
Tε(x)≈T(x) +ε Xd i=1
ωi
T3(x),x ε
∂T
∂xi
(x), (1.3)
whereωiarethesolutionsoftheellproblems. SineT isdenedinthefulldomain Ω while Tε is merely dened in the perforated domain Ωε, the orretor term is
ruialfor agoodapproximation. Wemakeomparisonsbetweentheexatsolution
Tε (or,at least, aonvergednumerialapproximationof it,when available)and the reonstrution(1.3). WeobtainanumerialerrorestimateoftheorderofεinL2(Ω),
as predited by homogenization theory [9℄. Of ourse, the gain in terms of CPU
timeand memorystorageis enormouswhen using (1.3)insteadofsolvingtheexat
problem(1.1)sinethehomogenizedproblem(1.2)requiresonlyaoarsemesh. Note
howeverthattheellproblemmustbesolvedfordierentvaluesof themarosopi
temperatureT. Finallyletus mentionthat aslightlysimplermodelis studiedin [6℄
andthatmoredetailsanbefoundin[14℄.
2. Setting of the problem. Thegoalof thissetion isto denepreisely the
geometry of theperforated periodi medium, to introdue the model of ondutive
andradiativeheat transferproblemandtogivesomenotations.
Figure2.1. Refereneellandperiodidomain
2.1. Geometry. LetΩbeasmoothbounded opensetin Rd (d= 2or3in the
appliations). WedeneaperiodiperforateddomainΩε,whereεdenotesitsperiod,
byremovingfromΩaolletionofholes(τε,k)k=1,...,M(ε)inaperiodimanner. Eah
holeτεk isequal,uptoatranslation, tothesameunit holeτ resaledatsize ε. The
domain Ω is also subdivided in N(ε) periodiity ells (Yε,i)i=1,...,N(ε), eah of them
beingequal,uptoatranslation,to thesameunit ellY =Qd
j=1(0, ℓj). Thenumber
ofperiodiityellsisnotequaltothenumberofholessine,intheappliationtogas
ooledreators,thereareseveralholesperell(seeFigure2.1). WedenotebyY∗ the
solid partof Y, i.e., Y∗ =Y \τ, and by Γ the boundary of τ (by aslightabuseof
languagewedenote byτ anindividual holeaswellasall theholesontainedin the
unitellY). Toavoidsomeunneessarytehnialities(see[1℄fordetails),weassume that,ifaperiodiityellutstheboundaryof Ω, thenit doesnotontainanyhole.
Theholesτε,k orrespondtoheliumhannelsinourappliationwhereradiativeheat
transfertakesplae,whileΩεorrespondstothesoliddomainwhereondutiontakes
plae. Insummarywehave
Ωε= Ω\
M(ε)[
k=1
τε,k, ∂Ωε=∂Ω∪Γε with Γε=
M(ε)[
k=1
∂τε,k=
N(ε)
[
i=1
Γε,i, (2.1)
where Γε,i denotesthe boundariesof theholesτε,k inside theellYε,i. Denotingby
mesthemeasure(surfaeorvolume,dependingontheontext)ofaset,wereallthe
followingidentities
mes(Y)εd= mes(Ω)
N(ε) (1+O(ε)), mes(Γε,i) =εd−1mes(Γ), mes(Yε,i) =εdmes(Y).
Denotingbydγ(x)thesurfaemeasureonΓε,wedenetheenterofmassx0,iofΓε,i
by
x0,i= 1 mes(Γε,i)
Z
Γε,i
x dγ(x) orequivalently
Z
Γε,i
(x−x0,i)dγ(x) = 0.
Similarly, y0 denotesthe enter of massofthe unit holeboundaryΓ. Wereall the
followingobviousidentities.
Lemma 2.1. Asmoothfuntion f satises Z
Γε,i
fx ε
dx=εd−1 Z
Γ
f(y)dy, Z
Γε,i
fx ε
(x−x0,i)dx=εd Z
Γ
f(y)(y−y0)dy, Z
Γε,i
fx ε
(x−x0,i)⊗(x−x0,i)dx=εd+1 Z
Γ
f(y)(y−y0)⊗(y−y0)dy,
ε
N(ε)
X
i=1
mes(Γε,i)f(x0,i) = mes(Γ) mes(Y)
Z
Ω
f(s)ds+O(ε).
2.2. Boundaryonditions. Asalreadysaidtheholesareatuallyheliumhan-
nelswhere radiativeheat transfertakesplae. Sinehelium isassumed tobetrans-
parent(noheatondution norabsorptionofradiation),thisproessismodeledbya
boundaryonditionontheholesboundaries. Letus reallthemodelingofradiative
exhanges between grey-diuse surfaes [15, 17℄. A grey-diuse surfae emits and
absorbsradiationinthesamemannerinalldiretions. Partofthereeivedradiations
anbereeted: a surfaeisthus haraterized byits emissivity ewhih takesval-
uesbetween0(fullreetion)and1(noreetion). DenotingbyT thetemperature andbyR theradiosity,i.e. theintensity ofemittedradiation,wehavethefollowing
relationship
R(x) = eσT4(x) + (1−e)J(x), (2.2)
Figure2.2. DomainwitharadiativeavityΣ
whereσistheStefan-Boltzmannonstantand J isgivenby J(x) =
Z
Σ
F(x, s)R(s)dγ(s),
whereF(x, s)istheviewfator(ageometrialquantity)betweentwodierentpoints xand s of a avity Σ(see Figure 2.2). Thus, the radiosityis given asthe solution
ofanintegralequationintermsofthetemperature. Forourappliation,theexpliit
formulaoftheviewfatorin2-dforaonvexavityis
F(x, s) = ns·(x−s)nx·(s−x) 2|s−x|3
where nz denotestheunit normalat thepointz. However,ourmathematialstudy doesnotrelyonthisspei formulaandwesimplyneedthefollowingpropertiesof
thekernelF: forany(x, s)∈Σ2,itsatises
• F(x, s)≥0,
• F(x, s) =F(x, s),
• R
ΣF(x, s)ds= 1.
LetJbetheoperatorgoingfromLp(Σ),1≤p≤+∞,intoitselfdened by J(f)(x) =
Z
Σ
F(x, s)f(s)dγ(s). (2.3)
DenotingbyEtheoperatoronsisting ofmultiplyingbytheemissivityvaluee,(2.2)
anberewritten
R= (Id−(Id−E)J)−1EσT4.
Ontheavitywalltheenergybalanereads
q−R+J = 0, (2.4)
whereq istheheat uxtransmittedbyondutionfrom thesolid Ωto theavityΣ,
fromwhihwededue
q= G(σT4),
whereGisalinearnon-loaloperatordened by
G(ϕ) = [Id−J] [Id−(Id−E)J]−1E(ϕ) ∀ϕ∈Lp(Σ). (2.5)
LetusreallsomepropertiesofJdenedby(2.3)(see[22℄).
Lemma 2.2. The operatorJ going fromLp(Σ) toLp(Σ),1≤p≤ ∞,satises
• J(c) =c,∀c∈R;
• kJk ≤1;
• J isnonnegative: ∀f ∈Lp(Σ), f≥0 ⇒ J(f)≥0;
• J issymmetri(self-adjoint for p= 2)inthe sense that Z
Σ
J(ϕ)ψ= Z
Σ
J(ψ)ϕ, ∀ϕ∈Lp(Σ), ψ∈Lp′(Σ), with 1 p+ 1
p′ = 1.
We easily dedue from Lemma 2.2 that (Id−ςJ), 0 ≤ς < 1, is invertible (for ς = 1,(Id−ςJ)isnotinvertiblesineker(Id−J) =R). Inpartiularwededuethat G is well dened, symmetriand non negative (this is lear for 0 <e ≤ 1 and for e = 0wendG≡0).
Remark 2.3. The operators dened by (2.3), (2.5) will be denoted by Jε, Gε
respetively,ifating onΓεinsteadof Γ.
2.3. Governing equations. Let Kbethe ondutivity tensorof the unit ell Y∗. We assumeKto be symmetri,uniformlyoeriveand bounded (innorm L∞),
i.e.,thereexist twopositiveonstants0< α≤β suhthat
∀v∈Rd, fora.e. y∈Y∗, α|v|2≤ Xd i,j=1
Ki,j(y)vivj≤β|v|2. (2.6)
Asusual,K(y)beingaY-periodifuntion,wedeneitsYε-periodiextension
Kε(x) = Kx ε
.
For given bulk and surfae soure terms f and g, we onsider the following mixed
problemofondution andradiativeheattransferfortheunknowntemperatureTε
−div(Kε∇Tε) = f in Ωε, Kε∇Tε·n = g on ∂Ω,
−Kε∇Tε·n = 1εGε(σTε4) on Γε,
(2.7)
where G is the operator dened by (2.5). For non-negativesoures, the boundary valueproblem(2.7)admitsauniquepositivesolutionaswasprovedin[22℄. Themain
diultyin(2.7)isthenon-linearandnon-loalboundaryonditiononΓε. Notealso
theε−1 salingin theboundaryonditionwhihinsuresthat theradiativeondition
will notdisappear when passingto the limit ε → 0 and will be represented in the homogenizedmodel.
2.4. Notations. Thesubsript # in thedenition of funtional spaes on the
unitellY indiatesthatweonsiderY-periodifuntions. WedenotebyL2(Ω;C#(Y))
thespaeofmeasurableandsquaresummablefuntionsofx∈ΩwithvaluesintheBa-
nahspaeofontinuousandY-periodifuntionsofy. WedenotebyL2(Ω;H#1(Y∗))
thespaeof measurableand squaresummablefuntions ofx∈Ωwithvaluesin the
Sobolev spae H#1(Y∗) of Y-periodi funtions dened only on Y∗. We all ell-
problemaproblemthatwesolveonlyontheelementaryelloftheperiodidomain.
Cell-problemsusually takeinto aountthe mirostruturebehaviorand ontribute
totheeetiveparametersalulation. WedenotebyO(εp), p∈Rafuntionofε >0
suhthatthereexistsaonstantCnotdependingonεsothatwehave|O(εp)| ≤Cεp
forallε >0.