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Interface response theory of composite elastic media
L. Dobrzynski, J. Mendialdua, A. Rodriguez, S. Bolibo, M. More
To cite this version:
Interface
response
theory
of
composite
elastic media
L.
Dobrzynski,
J. Mendialdua(*),
A.Rodriguez
(*),
S. Bolibo and M. MoreEquipe
Internationale deDynamique
des Interfaces, Laboratoire deDynamique
des CristauxMoléculaires,
U.R.A. No. 801 au CNRS, U.F.R. dePhysique,
Université de Lille I, F-59655 Villeneuved’Ascq
Cedex, France(Reçu
le 2février
1989,accepté
sousforme
définitive
le 21 mars1989)
Résumé. 2014 Une théorie
générale
permettant d’étudiern’importe
quel
matériauélastique
etcomposite
estproposée.
Sonapplication
auxcomposites
lamellaires est ensuitedéveloppée.
Ces résultatsgénéraux
sont illustrés par desexemples
de nouveaux modes de vibration localisés dansdes couches fluide et solide
comprises
entre deux autres solides semi-infinis. Abstract. 2014 Ageneral theory
for thestudy
of anycomposite
elastic media isproposed.
It is thenapplied
tolayered composites.
Thesegeneral
results are illustratedby examples
of new localizedvibrations within fluid and solid slabs sandwiched between two other semi-infinite solids. Classification
Physics
Abstracts68.25 - 68.65 - 68.15 - 68.48 - 64.45
1. Introduction.
Following
thepioneering
works[1]
of I. M. Lifshitz forphonons
and J. Friedel for electronson the
study
of apoint
defect in asolid,
the surface of a solid was studied as aplanar
defect in an infinite solid[2].
Interfaces between two different media[3]
and thensuperlattices
[4]
started then to be considered in a similar manner. However thisapproach
to interfaceproblems requires
one to know first theproperties
of the free surfacepieces
of matter out of which thecomposite
material is built. It was shownrecently
[5]
that thestudy
of anycomposite
material can be undertakendirectly
from the bulkproperties
of each of itspieces
together
with theboundary
conditions at the interfaces. This interface responsetheory
[5]
deals in a unified manner with
problems
formulated within discrete and continuous spaces. Itwas
applied
tophonons,
magnons, and electrons in thetight binding
[6]
approximation
as well as toelectromagnetism
and free electrons[7].
Thepresent
paper shows how thistheory
[5]
enables anycomposite
elastic media to bestudied,
andgives
new results for localized elastic vibrations within a fluid and a solid slab sandwiched between two other semi-infinite solids.The next section of this paper
gives
thegeneral equations enabling
anycomposite
elastic material to be studied. Section 3 illustrates thisgeneral theory by
anapplication
tolayered
composite
materials.Finally,
wegive specific
new results for localized elastic vibrations withina fluid and a solid slab sandwiched between two other semi-infinite solids.
2. Général
theory
for any elasticcomposite
material.2.1 BULK AND FREE SURFACE EQUATIONS. - The
equation
of motion for thedisplacements
ua, a =1, 2,
3 of apoint
of an infinitehomogeneous
3-dimensional elastic material iswhere p is the mass
density,
the vibrationalfrequency,
T al3
the stress tensorC af3 J.L JI
are the elastic constants and’Tl J.L JI
the deformation tensorThen the bulk
equation
of motion(2.1)
can be rewritten asSuppose
now that the elastic matter is limitedby
a free surface whoseposition
in the infinite 3-dimensional space isgiven by
Then the elastic constants are
where the Heavside
step
function is such thatThe use in
equation (2.6)
of 0[X3 - f (xl, X2)]
means that the elastic mediumoccupies
thespace x3 >
[(X1,X2).
Define with the
help
ofequations
(2.4)
and(2.6)
the bulkoperator
such that
Note that after differentiation of the
right
hand side ofequation
(2.8b),
one hasDefine then a surface response
operator
A
such that its elements arewhere the bulk response function
G
is definedby
~ ~
Knowing
the bulk response function G and the surface responseoperator A,
one can obtainthe response function
gs
of thehomogeneous
elastic material boundedby
the free surface definedby equation
(2.5)
from thegeneral equation
[5]
where
Ï
is theidentity
matrix.It is useful to use the
following
notation : D for the space in which the elastic matter is defined and M for the space of its free surface. Thenequation (2.13)
provides
[5]
where 3-
(MM )
is the inverse matrix ofA useful
particular
value ofequation
(2.14)
iswhere
Us 1 (MM)
and(MM)
are the inverse matrices ofgs (MM )
andG (MM ),
respectively.
Let us stress that in order to calculate the elements of
gs
fromequations
(2.14)
and(2.16),
one has in
general
to discretize the surface spaceM,
in order to calculate the inverse matrices defined above.2.2 THE GENERAL EQUATIONS FOR A COMPOSITE MATERIAL. - Let
us now consider any
composite
material contained in its space of definition D and formed out of N differenthomogeneous pieces
situated in their spacesDi.
Eachpiece
is boundedby
an interfaceMl, adjacent
ingeneral
to j (1, j , J)
otherpieces
through
subinterface domainsMij.
The ensemble of all these interface spacesMi
will be called the interface space M of theConsidering
first eachpiece
with its freesurface,
one can calculate fromequation
(2.16)
itsThen the
corresponding
g-1
(MM )
for thecomposite
material is obtained[5]
in thefollowing
manner
All the
boundary
conditions at the interfaces are satisfiedthrough
theseequations (2.18).
By
taking
a discrete number ofpoints
in the total interface space, one calculates then the inverseg (MM )
ofg-1
1 (MM).
Let us define hereG (DD )
as a blockdiagonal
referenceresponse function constructed out ot the elements of the bulk response functions
G(D,D,).
All the elements of the response
function g
of thecomposite
material can be obtained[5]
fromThe new interface states can be calculated from
and the total variation of the
density
of statesdN (lù 2)
between thecomposite
material and the reference one was shown[5]
to bewhere the
phase
shift ’TJ ( úJ 2)
isgiven by
For
perturbation
defects,
theequation (2.21)
reduces to that firstproposed
in 1952by
Lifshitz forphonons
aroundpoint
defects andby
Friedel[1]
for free electrons aroundimpurities
in metals and usedby
him to derive the well known Friedel sum rule. The results(2.18-2.22)
inslightly
different forms were obtainedalso,
within the Surface Green’s FunctionMatching Theory
[8]
for materials with one, two and twoperiodic
interfaces. Thegeneralization
to anycomposite
material was achieved afterwards within the InterfaceResponse Theory
[5].
Let us stress
finally
thatif
U(D))
represents
aneigenvector
of the referencesystem,
equation (2.19)
enables one to calculate theeigenvectors
1 u (D )
of thecomposite
materialIn
particular if
U(D))
represents
a bulk wave launched in onehomogeneous
piece
of thecomposite
material,
equation
(2.23)
enables to calculate all the waves reflected andtransmitted
by
the interfaces.Rather than
expanding
more on thesegeneral
results,
let us illustrate themby
a fewapplications
tolayered composite
elastic materials.3.
Layered composite
materials.Any
layered composite
material can be built out of semi-infinite and slabpieces.
We will therefore first show here how to obtain fromequation
(2.17)
thecorresponding
g;- 1 (Mi
Mi )
for a semi-infinite solid and then for a slab. Then we will indicate how these results can be also used for viscous and non viscous fluids.Finally
we will describe how to use these results for anylayered composite.
In all what follows we assume the interfaces
perpendicular
to the X3 axis. Then the functionf (xl, X2)
vanishes(see
Eq.
(2.5)).
Taking advantage
of the infinitesimal translational invariance of thislayered composite
in directionsparallel
to theinterfaces,
one can Fourieranalyze
alloperators,
and inparticular
the response functionsg
andG,
according
towhere
and
il
andi2 being
unit vectors in the 1- and2-directions,
respectively. Using
equations (2.8a)
and(2.12),
one finds that the Fourier coefficientGal3
(lq 1 X3
x3 )
of the bulk response functionG
is the solution of thefollowing
system
ofordinary
differentialequations
Let us now choose an
isotropic
elastic medium for which the bulk response functionG
can be calculated in closed form.3.1 BULK RESPONSE FUNCTION FOR AN ISOTROPIC ELASTIC SOLID. - An
isotropic
elastic medium is a medium whoseproperties
areisotropic
in all directions of space. For such amedium
The square of the
longitudinal
and shearplane
wave velocities arerespectively
Such a material is also
isotropic
within the(Xl, X2)
plane.
It ispossible
to choose inequations (3.2)
and(3.4) k2
= 0. The results obtained forG(k11
x3 x3 )
can be used for anyother direction of
k¡1,
after a rotation of the Xi and X2 axes such thatk¡1
liesalong
xl. As in this
case
1 k¡, 1
=kll
=kl,
we will write them as function ofkll
rather thankl.
Let us define also
and
Another
interesting
property
due to theisotropy
in the(xl, x2)
plane
is thedecoupling
of the transverse vibrationspolarized along x2
from thesagittal
vibrationspolarized
in the(x1, x3 )
plane.
Thisdecoupling
will remain forall layered composites
and it ispossible
tostudy separately the X2 polarized
transverse vibrations and thesagittal
ones in suchcomposites.
The elements of
Let us remark that a t =
(klr- úJ2/cf)1I2
is real forúJ :ctkll
and that we choosea
t = - i
( cv
2/ cf -
kir )112
for úJ :> Ctkll.
Thenegative sign
in this last resultcorresponds
in the response functions tooutgoing
waves at x3 = ± 00. The same considerationapplies
to3.2 ONE SEMI-INFINITE SOLID. - Let
us consider now a semi-infinite solid such that x3 r 0. For the
isotropic
solid described above and forkp -
*Ikll ,
the elements of thecleavage
operator
definedby equation
(2.10)
becomeWith the
help
ofequations
(2.11),
(2.15), (2.16)
and(3.12)
one obtainsLet us note that the
gs 1 (00 )
for the same elastic medium but such that X3 -- 0 has the sameexpression
(3.14)
but with achange
ofsign
in theoff-diagonal
elementscoupling
the xi and x3polarisations.
Note also that
from
which,
with thehelp
ofequation
(2.20)
one obtains the well knownRayleigh
wavedispersion
relation.With the
help
ofequation
(2.14),
one also recovers[10]
the response functionUs
of the semi-infinite solid.3.3 A FREE SURFACE SOLID SLAB. - Let
us now consider an
isotropic
elastic slab such thatThe interface space M is now formed out of these two surfaces X3 = ± a. The
cleavage
operator
has contributionsproportional
to a(X3
+a )
and to 6(x3 - a ) ;
the coefficients of the first one areequal
to thosegiven by equation
(3.13),
thesigns
of the coefficients of the second contribution arejust changed.
Asabove,
one can calculate thecorresponding
Us
(MM).
The calculation of the
sagittal
contribution togs
1 (MM)
can be obtained moreeasily,
with thehelp
of the reflectionsymmetry
through
the middle of the slab. Thisdecouples
thecorresponding
4 x 4 matrix in two(2 x 2)
matrices:g-- ’(MM)
for thesymmetrical
coordinatesand
gsÂs
for theantisymmetrical
coordinatesrespectively.
Theirexpressions
arewhere
and
where
The above
expressions
areparticularly
useful forcomposites keeping
this reflexionsymmetry
through
the middle of a central slab. Ingeneral,
however,
we will need the(4 x 4 )
expression
of the slabg s 1 (MM )
for the normalcoordinates {I- a,
Xl)’ 1-
a, X3),
where
3.4 THE SPECIAL CASE OF FLUIDS. -
It was shown before
[11]
that the motion of a fluidgoverned by
the linearized Navier-Stokesequation
can be studied with thehelp
of theequations
that describe the motion of a solidproviding
thatand
where co is the
longitudinal speed
of sound in thefluid,
po itsdensity,
and g
and1£ ’ are
the coefficients of shear and dilatationviscosity.
A non-viscous fluid can also be studied from the above
equations, by taking
the limitct - 0 in them.
3.5 ANY LAYERED ELASTIC COMPOSITE. - We have
now all the
ingredients
necessary for thestudy
of the elasticproperties
of anylayered composite
with fluid and solidparts.
Once thes ’(Mi
Mi )
for each differentpart
isdetermined,
then theg- 1 (MM)
of thecomposite
is obtainedby
linearsuperposition
of theseJs ’(Mi
Mi),
asspecified by equations
(2.18).
Thenthe main basic
properties
of thecomposite
can be obtained with thehelp
ofequations
(2.19)-(2.23).
Rather thanexpanding
thesegeneral
results,
let us illustrate themby
anapplication
to the vibrations of a fluid and a solid slab sandwiched between two semi-infinite solids.4. A few
applications.
4.1 THE FLUID SANDWICH VIBRATIONS. - Let
us consider a non-viscous fluid slab of thickness 2a sandwiched between two identical semi-infinite solids. The
application
of thelocalized within the fluid slab. Note first that there are no transverse
polarized
modes in the fluid slab.The
expression giving
thesymmetrical sagittal
sandwich modes was found to beand those for the
antisymmetrical sagittal
oneswhere the p o and p are the mass densities of the fluid and of the solid
respectively ;
« 1 and « t are the
outgoing
atinfinity penetration
coefficients of the solidgiven by
equations
(3.8)-(3.9)
and ao is theequivalent
of afor
thelongitudinal
wave in theliquid.
Remark that in the limit a - oo , coth ao a and th a 0 a --+
1,
bothequations
(4.1)
and(4.2)
reduce to theexpression
for the localized vibrations at aplanar
fluid-solid interface[12].
Figure
1represents
the firstsymmetrical
andanti-symmetrical
modes localized within the fluid slab.Defining
thespeed
of these modesby
c, werepresented
clct
=f (kp a)
for theparameters
characteristic of an acousticPerot-Fabry
interferometer[13].
In connexion withthis
experiment, using equations
(2.23)
we also calculated the reflected and transmitted wavesdue to an acoustic wave launched in the solid. These results are
given
in theappendix.
Fig.
1. - Localized waves in a thin fluid slab of thickness 2 a sandwiched between two identicalsemi-infinite solids. The
figure
displays
the ratio of thespeed
ofpropagation
c of these waves to the transversespeed
of sound c, in the solid as a function ofakl.
The parameters used in this calculation are those of anacoustic
interferometer, namely :
p o = 1010kglm 3,
, co = 1 900 mis for the
liquid
(N2H4, H20)
and p = 2 200kg/m 3,
Ct = 3 750 m/s and cl = 5 900 m/s for the solid(Si02).
4.2 THE SOLID SANDWICH VIBRATIONS. - Let
us now consider a solid slab of thickness 2a
sandwiched between two different semi-infinite solids.
Using
the results(3.14), (3.19)
and(2.18),
one obtains a(4
x4 )
matrixexpression
for thesagital
part
of theg-1 (MM )
associated with thiscomposite
andusing
equations (3.17), (3.14)
and(2.18)
one obtains a(2
x2)
matrixfor the transverse
part.
Thenequation
(2.20)
enables us to calculate the localized vibrations within the 5folid slab. Such localized modes were studied before with another method butonly
Let us label the two semi-infinite solids
by
thesubscripts
1 and 2 andkeep
for the solid slab the same notation withoutsubscript
as in section 3.3. The closed formexpression giving
the localized transverse modes waseasily
found to beFigure
2represents
the first of theinfinity
of modes localized within a slab of W sandwiched between Ni and Al. Theinput
parameters
aregiven
in the table I. Thespeed
c of theselocalized modes lies in between the transverse
speeds
of sound of Al and W. Note that these localized modes existonly
when the material sandwiched between the two others has atransverse
speed
of sound ct such that Ct Cll ct2. Otherwise one obtainsonly
resonantmodes,
also calledleaky
waves[12].
Fig.
2. -Speed
c of transverse localized waves in a Ni-W-Al sandwich.Table 1. -
Input
valuesfor
the calculationof
the velocitiesgiven
infigures
2,
3 and 4.where the
parameters
without index aregiven by equations
(3.20)
and for i = 1 and 2In order to discuss the different
possible
localizedsagittal
modes in such asandwich,
let usdistinguish
four casesdepending
on therespective
values of the transversespeeds
of sound of the three different materials and on the existence or non-existence of a localizedStoneley
wavehaving velocity
c, at asingle
interface between the central material and one of theothers.
An
infinity
of localized sandwich modes exist. Theirspeed
is ct. The variation of thespeed
c as a function of 2
akll
of the first of these modes isgiven
infigure
3 for the Ni-W-Al sandwich. When 2akll
--> oo, thevelocity
of this sandwich mode goes to thevelocity
of theStoneley
waveexisting
at thesingle
W-Al interface. The other modes(not
shown in thefigure)
come out of the bulk band of Al forhigher
values of 2akll
and when 2akll
--+ oo, theirvelocity
tendsasymptotically
to thevelocity
ct of W.ii)
Ct ctl ct2 with no existence of aStoneley
waveOne
expects
similar results asabove,
apart
that all localized mode velocities c will tend to ct for 2akll
--+ oo.Only
one localized mode exists below ct1 and itsvelocity
c - cs for 2akll
--+ oo. Thevelocity
of such a mode is
represented
infigure
4 for a W-Al-Ni sandwich.iv)
ctl Ct ct2 and ctl ct2 ctThere is no
truly
localized mode within the sandwich.5. Discussion.
Let us first mention here two other
problems
which were solvedrecently
with the sameformalism.
(i)
Closed formexpressions
for bulk and surface transverse elastic waves insuperlattices
made of 3 and 4 different
layers
were obtained[16].
(ii)
Analytic expressions
for the elastic energy of interaction of apoint
defect with aplanar
defect,
aplane
of dilatation and half aplane
of dilatation in aplane
defect have beencalculated
[17].
Theimplications
forsegregation
ofimpurities
nearhigh angle grain
boundaries are also discussed in this work.
Many
otherproblems
related inparticular
to the static and vibrationalproperties
oflayered
Fig. 3.
Fig.
4.Fig.
3. -Speed
c of the firstsagittal
localized wave in a Ni-W-Al sandwich.Fig.
4. -Speed
c of thesagittal
localized wave in a W-Al-Ni sandwich.Explicit expressions
of the elastic response functions were obtainedonly
for a fewlayered
systems :
free surfaces and aplanar
interface between two static solids[19]
with conventional solutions of the differentialequations.
The formalism described in this paper enables one to consider morecomplex layered composites mostly
because the doubleboundary
conditions(continuity
of stresses anddisplacements
at eachinterface)
are combined(see
Eqs.
(2.18))
into asingle boundary
condition.Let us
finally
stress that thetheory
outlined in this paper and illustratedby
twosimple
examples
oflayered composites applies
to any elasticcomposite
without any restriction as to the number and the form of the constituents. Of course in such cases andespecially
if onedeals with
non-isotropic
constituents,
the whole theoreticalprocedure
described in Section 2 becomes numerical and should becompared
with the finite element method.Advantages
were
[20]
found in the use of the interface responsemethod,
mostly
because manyphysical
Appendix
The fluid sandwich :
localized,
reflected and transmitted waves.Consider a
sagittal
bulkpropagating
wavecoming
from X3
= + oo . Thecorresponding
eigenvector
has ascomponents
where
Using
this incident waveas
1 U(D»
inequation
(2.23),
one obtains from the second andthird term of this
equation
the reflected and transmitted waves. Let us recall that the a i and a, to be used in the response functionappearing
in thisequation
were defined asand
provide
then the reflected and transmitted wavescorresponding
to the incident wave(Al).
In what follows wegive
the finalexpressions
of these waves, where the ci, and cit take the valuesgiven by equation
(A2).
Let us define alsoand
With these
notations,
the reflected(in
the solid at X3 «--a)
wave has thefollowing
components
The wave transmitted in the fluid slab
(- a «
X3a )
isThe wave transmitted in the solid at X3 «-- - a was found to be
The above results
(A.7)-(A.9)
also contain the wavescorresponding
to the localizedsymmetrical
andantisymmetrical
modes whosedispersion
relation isgiven by Dl
= 0(Eq. (4.1))
andD2
= 0(Eq. (4.2))
respectively.
The unnormalized wavecorresponding
to thesymmetrical
modes(Dl = 0)
and theantisymmetrical
ones(D2 = 0)
is obtainedby
multiplication
of theexpressions
(A.7)-(A.9)
by Dl
andD2, respectively,
andtaking
respectively
the limitDl -->
0. Note thatB
is in this case a common normalization factor andthat for these modes localized within the fluid
slab,
Remerciements.
L’un d’entre nous
(L. D.)
voudraitexprimer
ici saprofonde
reconnaissance au ProfesseurJacques
Friedel pourl’inspiration
dedépart
et son intérêt constant et souriant. En effet leprésent
travail etplus particulièrement
la théoriegénérale
deréponse
des interfacespeut
être considéré comme unegénéralisation logique
des travaux initiaux du ProfesseurJacques
Friedel sur les défautsponctuels.
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