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On the phenomenology of tilted domains in lamellar eutectic growth
B. Caroli, C. Caroli, S. Fauve
To cite this version:
B. Caroli, C. Caroli, S. Fauve. On the phenomenology of tilted domains in lamellar eutectic growth.
Journal de Physique I, EDP Sciences, 1992, 2 (3), pp.281-290. �10.1051/jp1:1992143�. �jpa-00246483�
J.
Phys.
I France 2 (1992) 281-290 MARCH 1992, PAGE 281Classification
Physics
Abstracts81.30F 03.40 64.70D
On the phenomenology of tilted domains in lamellar eutectic
growth
B. Caroli
(I, 2),
C. Caroli(I)
and S. Fauve(3)
(1)
Groupe
dePhysique
des Solides(*),
Universitds Paris 7 et Paris 6, 2 Place Jussieu, 75005 Paris, France(2) Facult6 des Sciences Fondamentales et
Appliqudes,
Universit6 de Picardie, 33 rue Saint Leu, 80039 Amiens, France(3) Ecole Norrnale
Supdrieure
de Lyon, 46 allde d'ltalie, 69364 Lyon Cedex 07, France(Received I
July
1991, revised 5 Npvember 199I,accepted
13 November1991)Rdsum4. Nous montrons que, du fait du
couplage
entre lesdynamiques
d'inclinaison(amplitude
de lapartie impaire
duprofil
de front) et dephase,
laph6nom6nologie
des domaines d'inclinaison delargeur
finiepropos6e
par Coullet et al.pour1e
cas d'une bifurcation d'inclinaisonhomogbne
souscritique garde
les mEmescaract6ristiques
qualitativesquand
cette bifurcation estdirecte, comme c'estle cas pour la croissance
eutectique
lamellaire.Abstract. We show that, due to the
coupling
between tilt(amplitude
of theantisymmetric
partof the front
profile)
andphase dynamics,
thephenomenology
of tilt domains of finite widthproposed
by Coullet et al. within the assumption of a subcritical homogeneous tilt bifurcation retains the samequalitative
features when this bifurcation is direct, as is the case for1ame11areutectics.
It has
recently
come tolight
that out ofequilibrium
systemsexhibiting
one-dimensionalstationary
front pattems with small deformationamplitudes undergo
ageneric parity- breaking
« tilt » bifurcation. Thisphenomenon
has been observed and studied in directionalsolidification of
liquid crystals ill,
lamellar eutecticgrowth [2]
and directional viscousfingering [3].
The basicpattem
loses its reflectionsymmetry
about the cell(or lamella)
center and the appearance of thisasymmetric
distorsion isaccompanied by
a drift of thepattem along
the front at a constantvelocity.
In eutecticgrowth,
where the frontdynamics
isregistered by
the frozen spacearrangement
of the two immisciblephases
in thesolid,
this results in the formation ofregions
ofperiodic
lamellae tilted at a constantangle
with respectto the
growth
direction.Coullet et al.
[4]
haveproposed
aphenomenological description
of thisbifurcation,
basedon a
(truncated) amplitude equation
for the asymmetryparameter A,
which can beunderstood as the
amplitude
of theantisymmetric
part of the front deformation(Qr,
(*) Assoc16 au CNRS.
equivalently,
the lamellar tiltangle).
The drift ofasymmetric
pattemsimplies
that the evolution of A isstrongly coupled
to thephase dynamics
of theperiodic
pattem.Contained in such a
phenomenology is,
of course, thedescription
ofhomogeneously
tilted states of aninfinitely
extended front. In the absence of a «microscopic
»description
of thishomogeneous bifurcation,
one has to make anassumption
about its super or subcriticalcharacter. In all
experiments reported
up to now, tilted states have been observed asinclusions of finite lateral size
[5],
limitedby
a front and a rear « wall»
traveling along
the front at constantvelocity(ies).
Recent detailed studies in eutecticgrowth
show that such domains may either grow(I.e.
increase their widthlinearly
withtime),
orshrink,
orkeep
aconstant
width, depending
on the values of thegrowth velocity
V and on thewavelength
A of the basicperiodic
structure which isbeing
swept[6].
Inliquid crystals
and directional viscousfingering, these, usually repeated, sweepings by
« tilt waves » ingeneral
result in a decrease of thewavelength
of theemerging
untilted pattem, which relaxes towards afixed, dynamically
selected value. In
eutectics,
the same trend isobserved,
but it can becomplicated by
theoccurrence of other instabilities
[6]. Quite naturally,
the observation of finite size domains ledCoullet et al.
[4]
to assume that thehomogeneous
tilt bifurcation is subcritical.They
then build adescription
of tilt inclusions which accounts for all thequalitative
features of domainbehavior.
They find,
inparticular,
that thewavelength
selectedby
tilt wavesweeping
shouldcorrespond
to the« Maxwell
point
» of the invertedhomogeneous
bifurcation.Since then, Kassner and Misbah
[7]
have been able to solve the full «microscopic
»equations describing
eutecticsolidification,
and toinvestigate
the existence ofhomogeneously
tilted solutions.
They
thus locatedirectly
theposition
of the tilt bifurcation and show that it issupercritical.
This is also
predicted [8-11]
in the cases where the tilt bifurcation can be described from the resonant interaction of a basic mode and its secondharmonic,
close to aprimary
bifurcation of cellular type.On the other hand, tilted domains in eutectics are
qualitatively
well describedby
thephenomenology
of Coullet etal.,
which assumes a subcriticalbifurcation,
as indeedsuggested by
the intuition based onequilibrium phase
transitions.In this article, we show that this
paradox
isonly
apparent andthat,
due to the strongcoupling
between tilt andphase dynamics,
asystem
with asupercritical
tilt bifurcation can also sustaintraveling
tilt inclusions with the samequalitative
behaviour as thatproduced by
asubcritical one.
As discussed
by
Fauve et al.[12, 13],
in thevicinity
of the tiltbifurcation,
thedynamics
ofour system should be described
by
thefollowing coupled equations
A~ =
pA-aA~+pA~+A~+aitb~+eAtb~+yAA~+bitb~tb~+. (la)
tb~ =
wA+Dtb~+a~A~+b~A~+C~AA~+d~tb~tb~+. (lb)
Here A stands for the
amplitude
of theantisymmetric
part of the frontprofile
of basic wavevector qo =2
w/Ao (or, equivalently,
for the lamellar tiltangle e).
tb is thephase
of theprofile.
Forexample,
if the front deformation is(as
can be done to describe tilted cellular fronts[8-10]) approximated by
thesuperposition
of two Fourier components with wavevectorsqo, 2 qo of
respective complex amplitudes
aie~~',
a~ e~~~tb =
(2tbi+tb~)/2
and Ax(2tbi-tb~).
Equations (I)
areexpansions
in powers of A, tb~ and their spacederivatives,
the functionalform of which is chosen so as to
satisfy
the symmetryproperties
of our system,namely
translational invariance
(tb
- tb + cst. and space reflection symmetry(x
- x, tb -
tb,
A -
A).
N° 3 TILTED DOMAINS IN LAMELLAR EUTECTIC GROWTH 283
Note that the model used
by
Coullet et al.corresponds
tochoosing
a~
0, p
~ 0
and,
arbitrarily imposing
inequations (I)
ai =bi
= a~ =
b~
= c2 =d~
= 0.
The WA term in
equation (16)
describes the drift of the tiltedpattem along
the averagefront. The bifurcation towards
homogeneously
tilted pattemscorresponds
to p =0.Following
Kassner and Misbah[7],
we take it to bedirect,
so that a ~0. ThePA
~ term inequation (la)
then becomes irrelevant and wewill,
from now on,forget
it.In the
homogeneously
tilted state of wavevector qo, A= ±
(pla)~~~
andtb~
= 0. The tilt thresholdcorresponds
to V~
V~(qo) (where
V is thegrowth velocity),
and we know from references[7, 14] that,
in the usualexperimental
range,V~(qo)
ccq(,
I.e.homogeneously
tilted states occur for :
A2 v ~
(A
2v)~. (2)
So, increasing
p inequation (la) corresponds
toincreasing
thegrowth velocity
at constant qo, whileincreasing
thewavelength
at constant Vcorresponds
to the shift p- p +
etb~ (with
tb~ = q qo =cst.).
Since p must increase with thewavelength,
this at once indicates thate ~ 0.
Finally,
D is thephase
diffusion coefficient in the untilted state, which we assume to be Eckhaus-stable(D
~ 0
).
Following
references[12, 13],
it can be checkedimmediately by linearizing equations (I)
about thehomogeneously
tilted solution :Ao
= ±(pla
)~'~tbo
=
wtAo (3)
that the
stability
of this solutionagainst long wavelength perturbations (oz
exp(
at + ikx))
isgovemed by
thedispersion
relation :«~
+«
(2
pikAo(y
+b~)
+tJ(k~))
ikAo(2 pb~
+em)
+d(k~)
=
0.
(4)
The term ikA
o(2 pb~
+ em isdestabilizing
: itgives
rise to an unstable mode with :Re «
(k )
= ~
~ j e2 w2
+o(» )j (5)
So,
due to thecoupling
between tilt andphase, immediately
above the bifurcation(where
pm
I),
notonly
is the non-tilted stateunstable,
but sois,
aswell,
thebifurcating
homogeneously
tilted one. This poses thequestion
of the nature of the(time-dependent)
structure into which the system then
restabilizes,
and inparticular, again,
of the existence oftraveling
tilt inclusions.1. Tilted domains of constant width,
We first want to examine whether the
phenomenological coupled equations
for tilt andphase
can sustain, below the
homogeneous
tiltbifurcation,
I.e. for p~ 0, solutions
corresponding
to
drifting
domains oflarge
but finite width : A=
A
(x
vt)
; ~b~ =
~b~(x vt) (6)
with :
A(Qc)=A(-Qc)=o; ~x(Qc)=o. (7)
JOURNAL DE PHYSIQUEI T 2, N' 3, MARCH 1992 12
Equations (I)
contain 12 parameters, among whichonly
one, the« distance » from the
homogeneous
bifurcation p, isnecessarily
small. On the otherhand,
from the directstudy
ofhomogeneously
tilted states[7, 14],
it ispossible
to deduce the values of the three parametersa, e, w.
Moreover,
on the basis ofapproximate
calculations[15]
of thephase
diffusion coefficient in untilted structures, one canreasonably
expect that, foreutectics,
D « I(in
units of the chemical diffusioncoefficient),
due to the smallness of the relevant Peclet numbers.However, equations (I)
contain seven more coefficients aboutwhich,
up to now, noinformation is available I.e. neither their
signs
nor their orders ofmagnitude
are known.We will see that an
analytic
treatment of tilt inclusions is validonly
underquite
restrictiveconditions
(namely,
accidental smallness of some combinations of coefficients of theA
tb~ coupling terms). So,
such a calculation canhelp
to elucidatequalitatively
how tilt inclusions can coexist with thesupercritical bifurcation,
but it cannotyield quantitative predictions.
In this
situation,
and for the sake ofsimplicity,
we choose toperform
theanalysis
on the truncated version ofequations (I)
usedby
Coullet et al. Thequalitative
effect ofreinserting
non-zero values for ai,
...,
d~
will bebriefly
discussed at the end ofparagraph
2.The truncated
equations
read[4]
:A~= pA-aA~+A~+eAtb~+yAA~ (8a)
~~
= WA +Dtb
~
(8b)
and we choose to look for a domain
moving
towardsincreasing
x(v
~0).
Formal
integration
of the x-derivative ofequation (8b) yields
:i w
A~,(x', t') (x x')~
~~~~'~~
~°_w ~'~-w
~~~~'
[4 wD(t t')]~'~~~~ ~~(~ ~'~
The infinite limit in the time
integration implies
that initial conditions(details
of the nucleationevent)
have beenforgotten,
I.e. that the domain has beenexisting
for a time muchlonger
than theappropriate phase
diffusion time-hereD/v~.
For a
stationary
domain as definedby equations (6)
and(7), equation (9)
becomes :~~~~~ l~~
~'~~'~ ~~~ ~~ ~'~if~ ~'~
=
) ~- A(X~
+j~
dX'j'~
exp
~ ~'
( lo)
-w
where X
= x vt and
f~
= D/v is the diffusion
length of
thephase
in the basic state.From
equations (8)
and(10),
we see that the spacedependence
of A isgovemed by
twolength parameters, namely
theLandau-Ginzburg length [p[~~'~,
whichdiverges
at thebifurcation,
andf
~, which remains finite. This entails that the local wavevector tb~ is
spatially
slaved
by
the tiltamplitude.
The lowest order of thecorresponding multiple
scaleexpansion gives
:~bx(X~ =
) (- A(S~
+f~ @ (i1)
Such a truncation is valid
only
if :f~
= ~ « p ~'~(12)
v
N° 3 TILTED DOMAINS IN LAMELLAR EUTECTIC GROWTH 285
Equation (8a)
becomes :~~~+~v+(y+@)A)~+~~=0 (13)
dX v dX &A
where
U(A )
=~ )
A ~(
A~(14)
That
is,
thecoupling
to thephase gives rise,
in the«
potential
»U(A),
associated with astationary
domaindrifting
atvelocity
v, to av-dependent
cubic term : the initialpitchfork
bifurcation of
homogeneous
structures becomes an effective transcritical one.In the
region
:~2 ~2
~ < ~1 ~ 0
(15)
4 au
U(A)
has three extrema, among which a maximum at A=
0,
U=
0.
As usual in such
problems,
and since we areonly looking
forqualitative behaviours,
we will treat the «dissipative
» term(proportional
todA/dx)
inequation (13) perturbatively.
A wide
stationary
domain(I.e.
a domain withnegligible
interaction between itswalls)
is a mechanicaltrajectory
of theparticle
ofposition
A at time X inpotential U(A) ending
at A= 0 for X
= + oa after
having
started from some A at X= oa and
having
spent anarbitrarily long
time at some finite A* Theonly
way for such a process to bepossible
is that :(I)
the two maxima of U have the sameheight,
I.e.U(A*)
= 0
(16)
where A* is the second maximum of U.
(ii) A(x- oa)
= 0 and the total
dissipation integrated along
any half of thetrajectory joining
A=
0 with A
=
A* vanishes.
Calling A(X~
=A*Z(X~
thishalf-trajectory,
thiscondition reads :
v
j~ dX(~ )~+ (y+@)A* j~ dXZ(~)~=0. (17)
_w
dX v -w dX
Conditions
(16)
and(17) provide
two relations betweenthe,
stillfloating,
parameters p andv, the solution of
which,
if itexists,
defines both the location inparameter
space,p
*,
of an « effective Maxwellpoint
» and the daftvelocity
v* of tilt domains of constant width.It is
immediately
seen that condition(16)
entails that~~~~
~
~.
~*=
~ ~ ~
(j8)
w2 ~2 9'
3 auso that the
corresponding potential
:U*(A
=
flA ~(l ~~
~
(19)
The
half-trajectory joining (A*,
X=
oa)
to(A
=
0,
X= +
oa)
is :z(x)
=
((~
=
ii
+ exp x11 (20)
so that condition
(17) yields
:~~
~il
~~~~~j~~
~ ~~~~which
always
has(whatever
thesign
ofyw)
thesingle
solution :*2 W~ E~ Y
y~
+ 12 aD'2j
~ "
~ £j
+ ~ ~(22)
w e
and the
corresponding
values of p*, A*,
are related to v*by equations (18).
This result can be
expressed
as follows :given
awavelength Ao
of the basic untilted frontpattern,
there exists agrowth velocity
V*(Ao)
such that :A(V*(Ao)
~
(A~V)~
at which the system can
support drifting
tilted domains of constantwidth,
I.e. « tilt waves » withparallel
walls. In thissituations,
sincetb(X
-oa)
=
0,
thewavelength
of the untiltedpattem
is unaffectedby
the passage of the tilt wave.Conversely (since adding
a constant totb~ simply
shiftsp),
thisdefines,
for eachgrowth velocity Vo,
a basicwavelength A*(V~)[A*~(Vo)Vo~(A~V)~]
for thepropagation
ofstationary
tilt waves.Moreover,
fromequation (10),
the wavevector q~ inside the tiltedregion
is such that :
q~-qo=~x=-ii* =lllli«0.
~23~So,
thewavelength
islarger
in the tiltedregion
than outside of it. Thisprediction
agreesqualitatively
withexperimental
observations.However,
in order for thecorresponding
solution to bevalid,
v* mustsatisfy
condition(12).
Moreover, the truncation of theamplitude expansion leading
toequations (I)
or(8) implies that,
for p ~'~= O (1~ «
1,
A*= O (1~
). Using equations (18)
and(22),
oneeasily
checks that this
imposes
:we=o(~2)=o(i»i);
D«1(24)
together
withewy~0,
I.e., foreutectics,
sincee<0,
my ~0.(When ewy~0, v*,
asgiven by equation (22)
cannotsatisfy
the condition forslaving
of thephase
to theamplitude, fw
« »~~.
Note that condition
(24)
on how thecoupling parameter
we should scale with p can also be obtained if oneimposes
that all terms inequation (8a) (resp. (8b))
scalecoherently
as 1~~(resp. 1~~.
Thisimposes
thatw =
d(1~)
and e=
tJ(1~).
As mentioned
above,
if the condition on D is mostprobably
satisfied foreutectics,
it is notnecessarily
so for the otherphysical systems
where tilt has beenobserved,
and in whichphase
diffusion is known not to be very slow. We believe that the condition on the «off-diagonal coupling
parameter » we can besatisfied,
in real systems,only accidentally.
2.
GroM4ng
andshrinking
domains.In order to decide whether
non-stationary
tilt inclusions may exist for values of p different from p*,
as well as to check whether these cangive
Rse todynamical selection,
we now look for solutionsdescribing
tilted domains which grow or shrink at a constant rate, I.e, we assumeN° 3 TILTED DOMAINS IN LAMELLAR EUTECTIC GROWTH 287
that as is observed in
experiments
the front(right)
and rear(left)
walls of a domainpropagating
towards x ~ 0 move at constant but different velocities v~, v~.The
positions
at time t of these walls are :x~
(t)
= x~ + v~ t ; x~
(t)
= x~ + v~ t
(25)
and x~ x~ » p ~'~
A~
is therefore a sum of two(quasi)
nonoverlapping
termspeaked
around x~,x~, so
that,
in the formalexpression
oftb~ (Eq. (9)),
the spaceintegration
can beseparated
into the two
regions (R)
and(L) corresponding respectively
to x ~x~(t)
and x <x~(t),
wherex~(t)
lies far from both walls(I.e.
at a distance muchlarger
than p ~'~) inside the tilted domain. Then :for x e
(R ),
A and tb~ are functions ofX~
= x x~
(t) only
and, fromequations (9)
and(lo) together
with A(X~
- oa
)
= 0 :
tb~ =
I ~-
A + ~ ~(26)
VR VR
dXR
with oa
<X~
< oafor x e
(L),
A andtb~
are functions ofX~
= xx~(t)
with :tb~ =
wA*( +i (-A
+ ~ ~(27)
VL VR VL
VLdXL
(-
oa <X~
~ oa and A * is the(quasi constant)
value of A inside the domain.Equations (26)
and(27),
whenplugged
intoequation (8a),
define two disconnected mechanicalproblems
withpotentials
U~(A )
=U(A iv
=v~) (28a)
u~(A )
=
u(A iv
=
v~)
+ °~j
*) (
A2(28b)
where
U(A iv)
is definedby equation (14).
For
(- w~ e~/4 avj)
~ p ~
0, UR
andU~
both have three extremacorresponding
to thesame values of A. The common
position
of their second maximum is :~ ~
4 p a
vi
1'2A*
= +
~ ~
(29)
2 a v~ w e
A tilted domain with wall velocities
(vR, v~) corresponds
to a set of twotrajectories TR, T~
of theparticle
inUR
andU~ respectively,
such that :T~
connects A=
0 at
X~
= oa with A* at
X~
= + oa
TR
connects A=
A* at
XR
= oa with A
=
0 at
XR
= + oa.
TR
is a solution of :~~+~v~+ (y+@)A~~ +(=0. (30)
dXR
VR RIn order to be able to solve our
problem analytically,
we assume that :(H H*)/H*'
~
(~H/H*(
~ l(VR,L V*)/V*(
=(BVR,L~~*'
"1where p
*,
v* are the valuescorresponding
tostationary
domains obtained inparagraph
I.We then
expand UR
and A inequation (30)
to first order aboutU*(A)
and A* Z(XR) respectively,
and also treat,again, dissipation
to first order. Thecorresponding
Fredholm condition
(see
forexample
reference[4])
then reads :l~ ~j~ ~dZ
we ~~&VR~2dZ
H
@+q q @+
+v~(~)~+(y+@)A*Z(~)~)=0. (31)
dX vR ~~°
Using
the fact that p*, v*,
A *satisfy
conditions(17)
and(18),
as well asexpression (20)
forZ(X),
we can rewrite(31)
as :2[~* ~~
6
*~~*[
i12
l~
~ * +Y~ *1
° ~~~~An
analogous
calculation fortrajectory T~ yields
:~j~*j ~~~
~~ ~
~
~j
~~jI/2
~
~~ ~~~~~
~' ~~~~
From
equations (32)
and(33)
we then find :av~ a ~
/
~ 21» *
(1
+P )
~~~~~3v~ 3vR
2p
(34b)
3VR
p
+where :
p =
~
- i
+
w~e~ j"~~ )~/~
~ 0.(35)
12av*[p*[
' 3 w eSo
3v~
and(3v~ 3v~)
both have the samesign
as3p.
Thatis,
close inparameter
space to the « Maxwellpoint
» p *(I.e., equivalently,
for A~ V close to (A~V) *)
we can state that : ifthe basic untilted
pattern
is stable with respect tohomogeneous
tilt but such thatA~V ~(A~V)* (resp. ~(A~V)*)
agrowing (resp. shrinking)
domain with auniquely
definedopening angle
can propagate into the untilted state. Its forward wall moves faster(resp. slower)
than that of thestationary
tilt waveexisting
forA2V
=
(A~V)*
Inside the
domain,
fromequation (26), tb~~ 0,
I.e. thewavelength
isalways larger
than that of the pattem which isbeing
invaded. Thesymmetric pattem emerging
after thesystem
has been sweptby
such a tilt wave has :tbj~~
= f 3p(36a)
N° 3 TILTED DOMAINS IN LAMELLAR EUTECTIC GROWTH 289
where :
~
2 w~
e
P
(36b)
3£YV*~j~*j(i+p) ~2 ~+fl
is
(since
e ~0)
apositive
number.So, provided
that conditions(24)
aresatisfied,
we can conclude that thewavelength
of untiltedpattems evolves,
under the action of tilt waves, in the same way as when the tilt bifurcation is subcritical : asanalyzed by
Coullet et al.[4], equations (36)
entailthat,
whatever thesign
of3p
for the initialpattem, repeated sweepings by
tilt domains should result in therelaxation of the
emerging symmetric pattem
towards the « Maxwellpoint
»p*, I.e.,
atconstant
growth velocity V~
in a relaxation of thewavelength
towards the«
dynamically
selected
» value A *
(Vo).
The
question
now arises of whetherusing
thecomplete amplitude expansion (I)
rather than the truncateddynamics (Eqs. (8))
leads toqualitative
modifications of the above results. Theanalysis
ofparagraph
I can berepeated,
eitherby using
theexpansion
methodleading
toequation (11)
or with thehelp
of the non-linear transform used in references[12, 13].
Thestudy
of inclusions of constant width follows the same lines as that ofparagraph I, yielding
forv*,
instead ofe@uation (21),
theequation
:v~
Ai
v~A~
= 0(37)
where
Ai
and A~ are combinations of the 12parameters appealing
inequations (I)
thesign
ofwhich remains unknown.
So,
two cases may occur[16]
:I) Equation (37) has, formally,
one or twopositive
roots forv*~.
Ingeneral, only
one of them isacceptable,
andthis, only
when someappropriate
smallness conditions on thecoefficients of the
amplitude expansion
are satisfied. These in fact reduce to conditions(24)
derived above on the truncated model.Indeed,
if w=
tJ(1~),
e =d(1~),
D «I, retaining
only
terms d (1~ ~) inequation (16)
amounts toneglecting
a~ A~, c~ AA
~
and
d~ tb~ tb~.
On theother
hand, since,
inequation (16), b~
=
?°'~~~
,
in
general d(b~)
=d(w ),
and theaq
q =q~b~Atb~
term isnegligible. Finally,
the(ai
+bi tb~) tb~
terra isgenerated by
the samediffusion processes which contribute to
Dtb~,
soassuming
that D«I entails thatai,
bi
« I as well.So,
in the limit definedby
conditions(24),
the fullequations (I)
canlegitimately
be reduced to the truncated model.ii)
It may alsohappen,
in some range of values of thecoefficients,
thatequation (37)
has no solution. In this case we are left with twopossibilities
: either tilted domains of constant width do not exist(and
the systemprobably
evolves into aquasi-chaotic behavior),
or such domainsexist with a
velocity
v * which doessatisfy
thephase-slaving
condition. A conclusion about this couldonly
be reached with thehelp
of acomplete time-dependent
numericalstudy.
From the
foregoing analysis,
we can thus draw thefollowing qualitative
conclusion : in systemssusceptible
of spontaneoussymmetry breaking
of their frontprofile
via asupercritical bifurcation, (which
seems to be the case in all systems studiedexperimentally
up tonow)
thenature of the structures to be
expected
in thevicinity
of thehomogeneous
tilt bifurcationexhibits unusual features due to the
couplings
between the tilt orderparameter
andwavelength
modulations. It is thiscoupling
which isresponsible
for thepossible long wavelength instability
of thehomogeneously
tilted state. Itis, also,
the samecoupling
whichallows
(in
the extented spaceincluding configurations
with variabletb~)
for the existence ofdrifting
tilted domains of finite size below the bifurcation threshold. Ouranalysis
does notpermit
to concludedefinitely
about whether such domains exist whatever the value of the coefficients in theamplitude expansion.
It is not excluded that systemsmight
exist inwhich,
close tothreshold,
frontprofiles
would restabilize into a morecomplicated time-dependent
structure.
References
[ii SIMON A. J., BECHHOEFER J., LIBCHABER A.,
Phys.
Rev. Lent. 61(1988) 2574 ; FLESSELLES J. M., SIMON A. J., LIBCHABER A. J., Adv.Phys.
(to bepublished).
[2] FAIVRE G., DE CHEVEIGNt S., GUTHMANN C., KuRowsKI P., Europhys. Lett. 9 (1989) 779.
[3] RABAUD M., MICHALLAND S., COUDER Y., Phys. Rev. Lent. 64 (1990) 184.
[4] COULLET P., GOLDSTEIN R. E., GUNARATNE G. H.,
Phys.
Rev. Lent. 63(1989)
1954 GOLDSTEIN R. E., GUNARATNE G. H., GIL L.,Phys.
Rev. A 41 (1990) 5731.[5]
Only
veryrecently
havespace-filling
tilted states been observed in eutecticgrowth
(FAIVRE G., MERCY J. :private
communication).j6] FAIVRE G., MERCY J. : submitted for
publication
toPhys.
Rev. A.[7] KASSNER K., MISBAH C., Phys. Rev. Lett. 66 (1991) 522 and 65 (1990) 1458.
[8] PROCTOR M. R. E., JONES C., J. Fluid Mech. 188 (1988) 301.
[9] DANGELMAYR G., Dyn. Stab.
Syst,
1(1986) 159.[10] ARMBUSTER D., GUCKENHEIMER J., HOLMES P.,
Physica
29D (1988) 257.[I Ii LEVINE H., RAPPEL W. J., RIECKE H.,
Phys.
Rev. A 43 (1991) l122.[12] FAUVE S., DOUADY S., THUAL O., J.
Phys.
II France1(1991)
311.[13] FAUVE S., DOUADY S., THUAL O.,
Phys.
Rev. Lent. 65 (1990) 385.[14] KASSNER K., MISBAH C.,
Phys.
Rev. Lent. 66(1991)
445 and to bepublished.
[15] CAROLI B., CAROLI C., FAIVRE G., MERCY J., to be
published
in J.Cryst.
Growth.[16] Note that,