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To cite this version:
Rangasamy Mahendren, Sharan Raj
and Welemane, Hélène
and Dalverny, Olivier
and Tongne, Amèvi
Thermal conduction
properties of microcracked media: Accounting for the unilateral
effect. (2019) Comptes Rendus de Mécanique, 347. 944-952. ISSN
1631-0721
Contents lists available atScienceDirect
Comptes
Rendus
Mecanique
www.sciencedirect.com
Thermal
conduction
properties
of
microcracked
media:
Accounting
for
the
unilateral
effect
Propriétés
de
conduction
thermique
des
milieux
microfissurés :
prise
en
compte
de
l’effet
unilatéral
Sharan
Raj Rangasamy Mahendren,
Hélène Welemane
∗
,
Olivier Dalverny,
Amèvi Tongne
UniversitédeToulouse,INP/ENIT,LGP,47,avenued’Azereix,65016Tarbes,France
a
r
t
i
c
l
e
i
n
f
o
a
b
s
t
r
a
c
t
Articlehistory:Received10April2019 Accepted7October2019 Availableonline22October2019
Keywords: Microcracking Heatconduction Thermalproperties Homogenization Unilateraleffect Mots-clés : Microfissuration Conductionthermique Propriétésthermiques Homogénéisation Effetunilatéral
Studies dedicated to the homogenization approach of microcracked media are largely focused on the determination of effective elastic properties. Some works investigate other properties, but most of them consider only open cracks. This paper intends to provide effective thermal properties related to the conduction problem taking into accountthe unilateraleffect(opening/closureofcracks). Suchanalysisconsiders steady-state heat transfer within an initially isotropic media weakenedby randomly oriented cracks. Accordingto the boundary conditions,estimatesand bounds basedon Eshelby-like formalism are developed to derive closed-form expressions for effective thermal conductivityandresistivityinafixedmicrocrackingstate.
2019Académiedessciences.PublishedbyElsevierMassonSAS.Thisisanopenaccess articleundertheCCBY-NC-NDlicense (http://creativecommons.org/licenses/by-nc-nd/4.0/).
r
é
s
u
m
é
Les techniques d’homogénéisation des milieux microfissurés sont principalement em-ployéespourl’étudedescomportementsmécaniquesélastiques.D’autresapplicationssont égalementpossibles,maisellesdemeurentleplussouventlimitéesàlaconsidérationde défautsouverts.Cetravailviseàdéterminerlespropriétéseffectivesthermiquesdemilieux microfissurés dans le cadre d’une conduction stationnaire. Les matériaux étudiés sont initialementisotropesetprésententdesmicrofissuresd’orientationarbitrairepouvantêtre ouvertesoubienfermées(effetunilatéral).S’appuyantsurunedémarchedetypeEshelby, les expressions des conductivités et résistivités effectives issues de différents schémas d’homogénéisationetbornesd’encadrementsonticiprésentéesetdiscutées.
2019Académiedessciences.PublishedbyElsevierMassonSAS.Thisisanopenaccess articleundertheCCBY-NC-NDlicense (http://creativecommons.org/licenses/by-nc-nd/4.0/).
*
Correspondingauthor.E-mailaddress:helene.welemane@enit.fr(H. Welemane).
https://doi.org/10.1016/j.crme.2019.10.004
1631-0721/2019Académiedessciences.PublishedbyElsevierMassonSAS.ThisisanopenaccessarticleundertheCCBY-NC-NDlicense
Homogenization is a usefultool for the modellingand analysis of the behaviour of heterogeneous materials. One of its mainobjectives istoestimate their overall propertiesfromtheirmicrostructuralfeatures (phaseproperties,inclusions distribution andgeometry, etc.). This topic is even more interesting when there is a lack ofexperimental data. Several studies have been dedicated to the micromechanical analysis of microcracked media, especially to address their elastic behaviour(forinstance[1–3] forinitiallyisotropicmaterials).Still,manypracticalapplicationsrequirepropermodellingof otherpropertiessuchasthermal,transportandpiezoelectricproperties,whicharenotinvestigatedmuch[4–8].
Taking into account the unilateral effect (opening and closure of cracks) makes the estimation of the said effective propertieschallenging,andthisevenmoreasmicrocracksare orienteddefects.Someauthorshaveinvestigatedtheelastic problemtakingintoaccountboththeinducedanisotropyandrecoveryphenomenonduetocrackclosure,throughaveraging up-scaling methods [1,9–11]. Such modelling strategy has never been applied before for a steady-state heat conduction problem. So,inthiswork, we intendtoaddress thisissuethroughan Eshelby-like approachandderive effectivethermal propertiesofmicrocrackedmedia,focusingmainlyontheunilateraleffect.
2. Theoreticalframework
Assuminglengthscaleseparation,thisstudydealswithcontinuummicromechanics.Ahomogenizationprocessproviding microstructure–propertiesrelationshipsisconductedthroughmean-fieldtheory.Presentdevelopmentsforeffectivethermal propertiesareinspiredbythemathematicalanalogybetweenelasticityandsteady-stateheatconductionproblems[12,13]:
stress
σ
⇐⇒
heat flux qstrain
ε
⇐⇒
temperature gradient g stiffnessC ⇐⇒
thermal conductivityλ
compliance
S ⇐⇒
thermal resistivityρ
Hooke’s law
⇐⇒
Fourier’s lawSimilarly to the macroscopic stress and strain under equilibrium conditions, the macroscopic temperature gradient G (respectively macroscopic heat flux Q ) corresponds to the average values of its microscopic quantity g (resp. q) under stationarythermalconditions[14]:
G
=
1Ä
Z
Ä
g d
Ä = h
gi
and Q= h
qi
(1)with
Ä
beingthevolumeoftheRepresentativeVolumeElement(RVE).Moreover,thelinearthermalbehaviourisgivenbyFourier’sheatconductionlaw:
q
= −λ ·
g and g= −
ρ
·
q (2)where
λ
(resp.ρ
)isthesymmetricsecond-orderthermalconductivity(resp.resistivity)tensor.Letus considera 3D RVEof amicrocracked media. Such materialexhibits a matrix-inclusiontypology inwhich each phase(matrix,cracks)aresupposedtoexhibitahomogeneousbehaviour.Twodifferentboundaryconditionscanbeimposed attheouter boundary
δÄ
oftheRVE,i.e.eitheruniformmacroscopictemperaturegradient(G
imposed atδÄ)
oruniform macroscopicheatflux(Q imposed at
δÄ).
Assuminganinitialnaturalstate,themicroscopicandmacroscopicquantitiescan belinkedlinearlyas[15]:g
(
x) =
A(
x) ·
G and q(
x) =
B(
x) ·
Q∀
x∈
Ä
(3)where A (resp. B)isthesecond-ordergradientlocalization(resp.fluxconcentration)tensorsuchthat
h
Ai
= h
Bi
=
I (I being the second-order identity tensor). The average temperature gradient G and heat flux Q of the heterogeneous media as obtainedby(1) canthusberelatedbyeffectivethermaltensors:Q
= −λ
hom·
G and G= −
ρ
hom·
Q (4)where
λ
hom(resp.ρ
hom)istheoverallthermalconductivity(resp.resistivity)ofthemicrocrackedmedia.Letdenoteλ
mandρ
m= λ
−m1 thematrixconductivityandresistivity,λ
c,i andρ
c,i= λ
−c,1i theconductivityandresistivityoftheith (i=
1...N) familyofparallelcracksand fc,itheirvolumefraction.Simplifyingassumptionsregardingphasedistributionallowapproxi-matinglocalfieldswithinconstituentsbytheirphaseaverages,sothattheoverallthermalpropertiesforthemicrocracked mediacanbegivenas:
Fig. 1. (a) RVE with arbitrarily oriented microcracks, (b) penny-shaped crack geometry.
λ
hom= λ
m+
NX
i=1 fc,i(λ
c,i− λ
m) · h
Ai
c,i (5)ρ
hom=
ρ
m+
NX
i=1 fc,i(
ρ
c,i−
ρ
m) · h
Bi
c,i (6)where
h·i
r=Ä1rR
Är·
dÄdenotestheaveragevalueoverthevolumeofthephaser forr= {m,
ci}.
Atthispoint,effective ten-sorsλ
hom(directly derivedfromuniformgradient-basedboundaryconditions)andρ
hom(naturallyobtainedfromuniformflux-basedboundaryconditions)strictlydescribethesameequivalenthomogeneousmedia,sothatthesetensorsareinverse ofeachother,i.e.
λ
hom=
ρ
−hom1 .Followingthismodellingstrategy,closed-formapproximationsofeffectivethermaltensorscanbederivedwhenever lo-calizationandconcentrationtensors(denoted as
h
Ai
estc,i andh
Bi
estc,i resp.)areestimated.Worksonthesingle-inhomogeneity problem, initiated by Eshelby [16] in elasticityand extendedto thermoelasticity [13,17], provide some solutions to such issueiftheinclusionsareellipsoidal.Indeed,thetemperaturegradientandheatfluxlocalfieldsinthecrackcanbe approx-imatedbytheuniformrespectivelocalfieldsobtainedinanellipsoidembeddedinan infinitematrixsubjectedtouniform boundaryconditionsdenotedasG∞andQ∞.Assumingperfectinterfaces,severalrepresentationscanbedevelopedaccord-ingtotheremoteconditions,matrixproperties,phasevolumefractions,geometryandpropertiesoftheinhomogeneity. Forthe presentcase, theRVE iscomposed ofan initially isotropic homogeneous media,considered asthe matrix.Its thermalconductivity and resistivity tensors are given by
λ
m= λ
mI andρ
m=
ρ
mI (λ
m andρ
m are the scalar thermalconductivity andresistivity, with
λ
m=
ρ
m−1) respectively. This matrix is weakened by randomly distributed microcrackswitharbitraryorientations(Fig. 1a).A convenientwayto representsuchkindofdefectisundertheformofa flatoblate ellipsoid(meansemi-axesa andc,Fig.1b).Fortheith familyofparallelmicrocracks, nidenotestheirunitvector,
ω
i=
ci/
aitheirmeanaspectratio,anddi
= N
ia3i their scalarcrackdensityparameter(N
i isthenumberofcracksintheith family perunit volume,[18]).Thecrackvolume fractionisthus fc,i=
43π
diω
i.Undertheseassumptions,estimatedsolutionsfor localizationandconcentration tensorsh
Ai
estc,i andh
Bi
estc,i depend on the followingdepolarization tensor SEi (similarto the Eshelbytensorofelasticproblems)[19]:SEi
=
³
1−
π
2ω
i´
ni⊗
ni+
π
4ω
i(
I−
ni⊗
ni)
(7)Thelast importantpointsfortheconsidered problemdeal withthe geometryandpropertiesofthecracks.Regarding the former,theconfigurationofpenny-shaped crackscorresponds tothe limitcase
ω
i→
0,whichmustbe introducedatthe veryendofthemathematicaldevelopments.Moreover,thefactthatmicrocrackscanbeeitheropenorclosedaccordingto compressiveloadsisintroducedthroughthelatterpoint.Inbothcases,cracksareassumedtobeisotropic(λc,i= λ
c,iI andρ
c,i=
ρ
c,iI),buttheybehavedifferentlydependingonthestateofthemicrocrack:•
fortheopencase,λ
c,i=
0 andρ
c,i→ ∞,
whichcorrespondstoadiabaticconditionsonthecrackslips,•
followingthe works ofDeudé etal.[10], closedcracks are represented by a fictitious isotropic materialwith scalar conductivityλ
c,i= λ
∗ and resistivityρ
c,i=
ρ
∗, which accounts for some heat transfer continuity at the closure of cracks (frictionless contact).Takingλ
∗= λ
m andρ
∗=
ρ
m may seem natural, butwe willnevertheless continue thedevelopmentforageneralcasewhere
λ
∗ andρ
∗ arescalarswiththeconditionsλ
∗6=
0 andρ
∗6→ ∞.
3. Gradient-basedformulation
Bygradient-basedformulation,wemeantoimposeauniformmacroscopictemperaturegradientG attheouterboundary
δÄ
ofthe RVE.Such asituationcorresponds to theclassical strain-based condition ofEshelby’sproblem. Letusconsider threedifferentapproachestoderivetheeffectiveproperties.Fig. 2. Phase properties and boundary conditions at infinity: (a) imposed temperature gradient G∞, (b) imposed heat flux Q∞.
3.1. Dilutescheme
In a first approach,we are going to estimate the homogenized propertiesassuming a dilute densityof cracks, which amounts to considerno interactionbetween defects.Remoteconditions onthe Eshelby problemleadin that casetothe macroscopicgradient(G∞
=
G,seeFig.2a).Hence,thegradientlocalizationtensorisgivenby:h
Ai
dilc,i=
h
I
+
PEi·
¡ λ
c,i− λ
m¢
i
−1(8)
wherePEi
=
SEi·
ρ
m isthesymmetricsecond-orderinteractiontensor(equivalenttothefirstHilltensorinelasticity).Eq. (8)canbesimplifiedas:
h
Ai
dilc,i=
h
I−
SEi¡
1− ξ
i¢
i
−1 withξ
i=
λ
c,iλ
m (9)Eq. (5) thusleadsto:
λ
dilhom= λ
m"
I−
4 3π
NX
i=1 diω
i¡
1− ξ
i¢ h
Ai
dilc,i#
(10)Wecanseethatthe
λ
dilhomdependsontheaspectratioω
i inourcase.However,weshowthatthequantityω
i¡
1− ξ
i¢ h
Ai
dilc,i tendstoalimit Ti whenω
i→
0,so:λ
dilhom= λ
m·
"
I−
4 3π
NX
i=1 diTi#
with Ti=
lim ωi→0ω
i¡
1− ξ
i¢
h
I−
SE,i¡
1− ξ
i¢
i
−1 (11)Suchexpansionincludesbothcrackconfigurations,i.e.,foropencracks
λ
c,i =0,soξ
i=
0,whileforclosedcracksλ
c,i= λ
∗6=
0,soξ
i6=
0.Takingthisintoaccount,tensorTi fortheith familyofcracksisgivenby:Ti
=
2
π
ni⊗
ni,
if cracks are open0
,
if cracks are closed(12)
Accordingly,Eq. (11) canbesimplifiedas:
λ
dilhom= λ
m·
"
I−
8 3X
i/open dini⊗
ni#
(13)inwhichonlyopencrackscontribute inan additivemanner.Asanexample,theeffectivethermalconductivityofamedia weakenedbyasinglefamilyofparallelmicrocrackswithunitnormal n anddensityd takestheform:
λ
dilhom=
λ
m−
83d
λ
mn⊗
n,
if cracks are openλ
m,
if cracks are closed3.2.Mori–Tanakascheme
In linewith the Eshelby-like approach, the Mori–Tanaka(MT) scheme [20] considerscracks embedded in an infinite media(with matrixproperties)that issubjectedto theaveragetemperaturegradient overthematrix phase(G∞
= hgi
m,see Fig. 2a). Introducing inhomogeneities inside a thermally-stressed matrix in this way amounts to account for some interactionsbetweencracks.Averagingrule(1) leadstothefollowinglocalizationtensor:
h
Ai
MTc,i= h
Ai
dilc,i·
"
fmI+
NX
j=1 fc,jh
Ai
dilc,j#
−1 (15)NowEq. (5) canbewrittenas:
λ
MThom= λ
m·
"
I+
4 3π
NX
i=1 diTi#
−1= λ
m·
"
I+
8 3X
i/open dini⊗
ni#
−1 (16) since lim ωi→0ω
ih
I−
SE,i¡
1− ξ
i¢
i
−1=
Ti also.Accordingly,thespecificconductionbehaviourforthesimplecaseofasingle familyofparallelmicrocracksaccordingtotheirstatusdescribedisasfollows:λ
MThom=
λ
m−
8 3dλ
m 11
+
8d3 n⊗
n,
if cracks are openλ
m,
if cracks are closed(17)
3.3.PonteCastañeda–Willisupperbound
Based on theHashin–Shtrikman bounds [21], Ponte Castañeda andWillis (PCW) derived explicit strain-based bounds forthe effectivestiffness of composite materials withellipsoidalinclusions [3]. Theirestimate corresponds to a rigorous upper bound for the class of cracked media in which the matrix is the stiffest phase. The PCW formulation separately accountsfortheinclusionshapeandspatialdistribution,respectively,throughfourth-orderinteraction
P
Ei andspatialcrack distribution
P
dc tensors.Usingasimilar approachforthethermalproblemwithasecond-orderspatial distributiontensor Pdc,theeffectiveconductivitycanbegivenby:
λ
PCWhom= λ
m+
Ã
I−
NX
i=1 fc,ih
¡λ
c,i− λ
m¢
−1+
PEii
−1·
Pdc!
−1·
Ã
NX
i=1 fc,ih
¡λ
c,i− λ
m¢
−1+
PEii
−1!
(18)Itisalsoconvenienttoobservethat:
λ
PCWhom= λ
m·
Ã
I+
NX
i=1 fc,iMc,i· λ
m·
Pdc· λ
m!
−1·
Ã
I−
NX
i=1 fc,iMc,i·
Qdc!
(19) where Mc,i=
h
¡
ρ
c,i−
ρ
m¢
−1+
QEii
−1,QEi
= λ
m·
¡
I−
PEi· λ
m¢
(equivalenttothesecondHilltensorinelasticity)andQdc=
λ
m·
¡
I−
Pdc· λ
m¢
.Forsimplicity,asphericalspatialdistributionisadoptedinthisstudy,forwhichPdc reads:Pdc
=
1
3
ρ
m (20)Eventhough,thePCWformulationisderived fromtheenergyapproach,Eq. (18) canbeinterpretedintheformofEq. (5) throughthefollowinglocalizationtensor:
h
Ai
PCWc,i= h
Ai
dilc,i·
Ã
fmI+
NX
j=1 fc,jh
I+
¡
PEj−
Pdc¢ · ¡ λ
c,j− λ
m¢
i
· h
Ai
dilc,j!
−1 (21)AsalreadyemphasizedbyPonteCastañedaandWillis,itcanbeobservedthat,whenPdc
=
PEi,thePCWschemecorresponds totheMori–Tanakaestimate(Eq. (21) comestoEq. (15))whilethecasePdc=
0 leadstothediluteapproximation(Eq. (21) reducestoEq. (8)).TakingintoaccountEqs. (18)–(19),orequivalentlyEqs. (21) and(5),thecorrespondingeffectiveconductivityreads:
λ
PCWhom= λ
m·
"
I−
Ã
4 3π
NX
i=1 diTi!
·
Ã
I+
4 9π
NX
i=1 diTi!
−1#
(22)λ
PCWhom= λ
m·
I−
8 3X
i/open dini⊗
ni·
I+
8 9X
i/open dini⊗
ni (23)whichreducesto:
λ
PCWhom=
λ
m−
8 3dλ
m 11
+
8d9 n⊗
n,
if cracks are openλ
m,
if cracks are closed(24)
forasingle familyofparallelmicrocracks.NotethatMT(Eq. (17))andPCW (Eq. (24))tendtodilute prediction(Eq. (14)) whend
→
0.4. Flux-basedformulation
Thissection considersauniformmacroscopicheatflux Q at
δÄ.
Estimatesandboundare basedonthelocalfieldsof cracks embeddedinsideamatrixsubjectedtoa uniformheatflux atinfinity( Q∞). Accordingly,thetemperaturegradientg(x) tends to
ρ
m·
Q∞ when|x|
→ ∞.
This,therefore, amounts tothe gradient boundary conditionsof theEshelby-likeproblem that provide the averagetemperature gradient
hgi
c over the cracks volume. From theaverage heat flux in thisphase
hqi
c =λ
c· hgi
c,estimatesoftensor B canbederived.4.1. Dilutescheme
Forthedilutescheme,theconditionsatinfinitycorrespondtothemacroscopicheatflux( Q∞
=
Q ,seeFig.2b),sothath
Bi
dilc,i= λ
c,i· h
Ai
dilc,i·
ρ
m=
h
I
+
QEi·
¡
ρ
c,i−
ρ
m¢
i
−1(25)
SubstitutingEq. (25) intoEq. (6),weget:
ρ
dilhom=
ρ
m·
"
I+
4 3π
NX
i=1 diTi#
(26)Aspreviouslymentioned,Eq. (26) accountsforthecracksstate.Foropencracks,
ρ
c,i→ ∞,
soagainξ
i=
0,whileforclosed cracksρ
c,i=
ρ
∗6→ ∞,
soξ
i6=
0 withtherelatedexpressionoftheTi tensorsprovidedinEq. (12).Now,ρ
dilhom=
ρ
m·
"
I+
8 3X
i/open dini⊗
ni#
(27)Takingthisintoaccount,theexpressionoftheeffectiveresistivitytensorforasinglefamilyofcracksbecomes:
ρ
dilhom=
ρ
m+
83d
ρ
mn⊗
n,
if cracks are openρ
m,
if cracks are closed(28)
Itshouldbenotedthat,accordingtotheboundarycondition,thediluteapproximationleadstoadifferentrepresentationof thethermalbehaviourintheopenstateofthecracks,
λ
dilhom6= (
ρ
dilhom
)
−1.Asimilarresultisobtainedinelasticityaswell.Yet,theeffectiveconductivityandresistivityareobviouslyinverseofeachotherfortheclosedstateofcracks,
λ
dilhom= (
ρ
dilhom)
−1, whileinthiscasestrain-basedorstress-basedformulationsofelasticitystillremaindifferent[11,22].4.2. Mori–Tanakascheme
Inthiscase,theremoteconditionscorrespondtotheaverageheatfluxoverthematrixphase( Q∞
= hqi
m,Fig.2-b)andagain,usingtheaveragerule,thefluxconcentrationtensorisgivenby:
h
Bi
MTc,i= h
Bi
dilc,i·
"
fmI+
NX
j=1 fc,jh
Bi
dilc,j#
−1 (29)IntroducingEq. (29) intoEq. (6) finallygives:
From Eqs. (16), (27) and (30), itis clearthat theMori–Tanakaapproach leads tothe samepredictions undergradientor fluxconditions,bothforopenandclosedmicrocracks,i.e.
λ
MThom= (
ρ
MThom)
−1.Thesameconclusionhasbeendrawnforelasticpropertiestoo[11,22].
4.3.PonteCastañeda–Willislowerbound
Asinspiredby[3],DormieuxandKondo[11] derivedavariationalstress-basedlowerboundfortheeffectivecompliance usinganenergyapproach.Similarlytothiswork,thethermalresistivitycanthusbegivenas:
ρ
PCWhom=
Ã
I−
NX
i=1 fc,iMc,i·
Qdc!
−1·
Ã
I+
NX
i=1 fc,iMc,i· λ
m·
Pdc· λ
m!
·
ρ
m (31)FromEqs. (19) and(31),wecanobservetheequivalencebetweentheupperandlowerPCWbounds,since
λ
PCWhom= (
ρ
PCWhom)
−1. Asforthegradient-basedbound,theaboveestimatecanbeinterpretedthroughthefollowingconcentrationtensor:h
Bi
PCWc,i= h
Bi
dilc,i·
Ã
fmI+
NX
j=1 fc,jh
I+
¡
QEj−
Qcd¢ · ¡
ρ
c,j−
ρ
m¢
i
· h
Bi
dilc,j!
−1 (32)Takingintoaccount thespatial distributionadoptedinEq. (20),theflux-basedPCW boundleadstothefollowingeffective thermalresistivity:
ρ
PCWhom=
"
I+
Ã
4 3π
NX
i=1 diTi!
·
Ã
I−
8 9π
NX
i=1 diTi!
−1#
·
ρ
m (33)AfterintroducingEq. (12),weget:
ρ
PCWhom=
"
I+
Ã
8 3X
i/open dini⊗
ni!
·
Ã
I−
16 9X
i/open dini⊗
ni!
−1#
·
ρ
m (34)Forasinglefamilyexampleconsideredthroughoutthestudy,theaboveequationcomesto:
ρ
PCWhom=
ρ
m+
8 3dρ
m 11
−
16d9 n⊗
n,
if cracks are openρ
m,
if cracks are closed(35)
whichagaintendstothedilutecase(Eq. (28))ford
→
0.5. Discussion
We propose to highlight the consequences of microcracks on thermal properties through the case of a matrix with a single familyofparallel cracks, forwhichclosed-form expressions of diluteandMori–Tanaka estimatesandvariational boundshavebeenprovidedinthetext.
Forthe open cracks, we note that the material exhibits a damage-induced anisotropy, irrespective of the scheme or boundaryconditions.Tobeprecise,theeffectivethermalpropertiesaretransverselyisotropicaroundaxisn ofcracks(see Eqs. (14),(17),(24) and(28),(30),(35)).Especially,conductivity(respectivelyresistivity)ismostlydegraded(resp.enhanced) alongthedirectionorthogonaltothesurfaceofthecracks,whichisconsistentwiththeadiabaticconditionsonthelipsof thecracks. Asan illustration, Fig. 3presentsthe rosediagramsofthe generalizedscalarconductivity
λ(
v)
andresistivityρ
(
v)
inthedirectionoftheunitvectorv definedby:λ(
v) =
v· λ
hom·
v andρ
(
v) =
v·
ρ
hom·
v (36)Onthecontrary,wenotethatclosedcracksdonotcontributetothedegradationorenhancementofthermalconduction properties.This resultis true regardlessof the scheme,boundary conditions,fictitious properties(λ∗,
ρ
∗) or considereddirectionv.Indeed,inallcases,effectiveconductivityandresistivityinanydirectionrecovertheirinitialvalue(ofthevirgin material)attheclosureofmicrocracks,i.e.:
λ(
v) = λ
m andρ
(
v) =
ρ
m,
∀
v, if cracks are closed (37)Thismeansthatthe continuityofheat transferisfullyensuredwhenmicrocracksare closed,witha conductionresponse equaltothatinsidethehomogeneousisotropic(virgin)matrix.Suchaconclusionclearlydiffersfromtheresults microme-chanicallyestablishedforelasticproperties.Indeed,underfrictionlessconditions,crackclosureleads topartialrecoveryof
Fig. 3. Generalizedthermalconductivityλ(v)andresistivityρ(v)normalizedbytheirinitialvaluesforamaterialweakenedbyasinglefamilyofparallel microcracksofunitnormaln (cracksdensityd=0.1).
Fig. 4. Predictionsofhomogenizationestimatesandboundsforthegeneralizedthermalconductivityλ(n)andresistivityρ(n)foramaterialweakenedby
asinglefamilyofopenparallelmicrocracksofunitnormaln.
mechanicalproperties.Considering,forinstance,theYoungmodulusE
(
v)
= [
v⊗
v: S :
v⊗
v]
−1(resp.theelongation modu-lusL(v)
= [
v⊗
v: C :
v⊗
v])
withS
thecompliancetensor(resp.C
thestiffnesstensor)forastress-basedformulation(resp. forastrain-basedformulation),ithasbeendemonstratedthatclosedcracksdonotinfluencetheYoungmodulusE(
n)
(resp. theelongation modulus L(n))
inthedirection n normaltothecracks,butstill remainactiveforothersdirections[23,24]. Thecompletedamagedeactivationforheat-conductionpropertiescanbeattributedtothelessercomplexityoftheproblem itselfandalsotothesimpledefinitionofthedepolarizationtensor.Comparedtoelasticcase,theEshelby-liketensorSE forconductionbehaviour(Eq. (7))contains onlybasicinformation,asitis ofthesecondorder, symmetric,anddependsonly ontheaspectratio
ω
andtheorientation n ofthecrack(no dependencyonthematrixproperties,liketheEshelbytensor doesintheelasticcaseforinstance).Atlast,itseemsrelevanttocomparethehomogenizationestimatesaccordingtothemicrocrackdensityparameter. Con-clusionsfortheclosedstateofmicrocracksareobvioussinceinallcasesthermalpropertiesarenotaffectedbythedefects. Ontheotherhand,theopenstateshowssomesignificantdifferencesbetweendiluteandMori–TanakaestimatesandPCW variationalboundsofconductivity,especiallyascrackdensityincreases(Fig.4(a)).Yet,similarlytocomplianceinelasticity, theMori–Tanakaformulationcoincideswiththedilutecaseforresistivity(Eq. (30)).Thisisduetothecombinationofboth thespatialcrackdistributionconsideredby MT(correspondingtoEshelby distribution)andthespecificthermalresistivity oftheopencrack(
ρ
c→ ∞).
Suchpointisconfirmedbytheevolutionofthelowerboundestablishedin[11],whichclearlydiffersfrombothpreviousschemes.Fig.4(b)illustratesthesignificantroleofinteractionsinresistivityprediction.
6. Conclusion
Thisnoteprovides homogenization-basedestimatesandboundsofsteady-stateheatconductionpropertiesfor microc-racked media. Especially,the influenceof unilateraleffects (accordingto the open orclosedstatus ofthe cracks)on the effectivethermalbehaviour istakenintoaccount.Results showthatcrackclosureleads toatotalrecoveryofthethermal conductivityandresistivityofthematerial,irrespectiveofthehomogenizationmethods(takingintoaccountornot interac-tionsbetweenmicrocracks)orboundaryconditions.Thisthusprovidesrelevantinformationforfurtherworksthatwillbe dedicatedtothethermo-mechanicalmodellingofmaterialswithevolvingdamage.
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