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Drift instabilities of cellular patterns
S. Fauve, S. Douady, O. Thual
To cite this version:
S. Fauve, S. Douady, O. Thual. Drift instabilities of cellular patterns. Journal de Physique II, EDP
Sciences, 1991, 1 (3), pp.311-322. �10.1051/jp2:1991170�. �jpa-00247520�
Classification
Physics
Abstracts47 20 03 40G
Drift instabilities of cellular patterns
S
Fauve,
SDouady
and O Thual(*)
Ecole Normale
Supbneuie
de Lyon, 46 allbe d'Itahe, 69364Lyon,
France(Received
24April1990,
accepted mfinal form
23 November1990)
Rksulnk. Nous dbcnvons des mbcamsmes blbmehtaires qui mduisent une dbnie I
vliesse
constante d'une structure cellulaire Nous considbrons soit une structure
spatiale
statique, soitune onde stationnaire. Dans Ids deux cas nous montrons comment « l'instabilitb de dbnve » est
like I la bnsure de l'invanance par rbflexion
d'espace
Lorsque le mode leplus
instable a unnombre d'onde fim, « l'mstabihtb de dbrive peut ltre
prbcbdbe
par une instabihtb oscillatoire quiengendre
une nlodulation spatiotemporelle de la longueur d'onde de la structure mitiale Nousinterprdtons
divers rbsultatsexpdrimentaux
rdcents dans le cadre du moddle que nousproposons
Abstract. We report basic michamsms that generate a
secondary
dnft instability of a stationary cellular pattern or astanding
wave pattern In both cases, we~how how the drift bifurcation » isassociated with a
space-reflection symmetry-breaking
When the most unstable mode comes in at finite wavenumber instead of zero wavenumber, the dnft instability can bepre-empted by
anoscillatory instability
of the basic pattem wavenumber We interpret different recentexpenmental
observations within this framework1. Introduction.
Drift instabilities of cellular
patterns
have beenwidely
observed m variousexperimental
situations Convection m
binary
fluid mixtures[I],
or Couette flow between two horizontal coaxialcylinders
with apartially
filled gap[2], display
transitions fromstationary
totraveling
rolls. As
clearly
noticed m reference[2],
thetraveling
rolls are tilted and the direction of thepropagation
is determinedby
thisasymmetry.
Thetraveling-roll
state is eitherhomogeneous
m space, or there exist domains of inclined rolls with
opposite
tilt and thus oppositepropagation
direction. Similarresults_have
bden foundrecently
m a filmdraining experiment
13j.
Drift instabilities have been also observed m directional
crystal growth experiments.
Above the onset of the Mulhns-Sekerkainstability
ofliquid crystals, solitary
modespropagating along
the interface have been observed[4].
Thesesolitary
modes » consist of domains ofstretched
asymmetric
cells that connect tworegions
with symmetnc cells.Similarly,
domains of tilted lamelae movingtransversally along
thegrowth front,
have been observedduring
(*)
National Center ofAtmosphenc
Research, PO Box 3000, Boulder, C080307, USAdirectional solidification of eutectics
[5],
and therelationship
of the tilt direction to the one ofpropagation
has been alsoemphasized.
Finally,
a driftinstability
was observedrecently
for astanding
surface wave excitedparametrically
in a horizontallayer
of fluid contained m a thinannulus,
submitted to vertical vibrations[6].
It was observedthat,
as thednving amplitude
isincreased,
thestanding
wavepattem
eitherbegins
to move at a constantspeed
m onedirection,
orundergoes
anoscillatory instability
thatcorresponds
to a compression mode of theperiodic
structure(I,e.
awavenumber modulation m space and
time).
On the theoretical
side,
it isinteresting
to note that asecondary
bifurcation that transformsa stationary structure into a
traveling
one has beenpredicted by
Malomed andTnbelsky
before theexpenmental
resultsquoted
above[7]. They
used a Galerkin approximation for model equations of theKuramoto-Sivashinsky type,
andpointed
out that the dnftinstability
arises in that case from thecoupling
betwedn thespatial phase
of the basic structure with thesecond harmonic
generation. Recently
this bifurcation was understood in a moregeneral
wayfrom
symmetry
considerations[8]. Finally,
a dnftinstability
has been observedby
numericalintegration
of theKuramoto-Sivashinsky equation [9].
This paper is
organized
as follows We firststudy
asimple
model of a dnftinstability
of stationary pattems, that shows the basic structure of this bifurcation. We then propose amodel
inspired by
the mechanism describedby
Malomed andTnbelsky (see
Sect.3).
Insection 4 we show that a drift
instability
of astanding
wave can be understood as asecondary
bifurcation descnbedby
the evolution equations for theamplitudes
of theright
and leftpropagating
waves. In section5,
we consider thestability
of ahomogeneous dnftmg
patternto space
dependent perturbations. Finally
we show that when the dnft bifurcation occurs at finitewavenumber,
weget
anoscillatory instability
of the basicpattern wavenumber,
observed m convection
expenments [10]
and forparametncally
excited surface waves[6].
In all cases, we show that the basic mechanism consists of thecoupling
between thespatial phase
#
of theprimary pattern,
with the orderparameter
V associated with thespace-reflection broken-symmetry, #~
ocV,
and weidentify
thephysical significance
of V for the variousexamples
considered. The notation must be consideredindependently
in each section,except
for sections 5 and 62. A naive model.
We first consider a stationary
pattern-forming
bifurcation and thus write the fieldu(x, t)
that describes thephysical system, u(x,t)
=
iA(t)e'~~+cc.iu~+h.o.t (1)
where A
(t)
is theslowly varying amplitude
of the most-unstable wavenumber k that gives rise to thestationary penodlc
pattem.u(x, t)
stands for thevelocity
and temperature fields in aconvection expenment or for the interface
position
in the reference frame moving at the frontvelocity
in acrystal growth expenment. A(t) obeys
toleading
order a Landauequation,
A~=~IA- (A(~A (2)
where ~1is the distance from
critlcahty
we have considered asupercntical
bifurcation andsimplified equation (2) by appropriate scaling
ofamplitude.
A
periodic
pattern,dnftlng
atvelocity
Valong
the x-axis, is descnbedby
a similarequation
in the reference framemoving
atvelocity
V. We go back to thelaboratory
reference frame viathe transformation x
- x
Vt,
orequivalently
forA,
A- A exp
(i Vkt). Thus, equation (2) becomes,
A~=~IA- (A(~A-ikAV. (3)
We must at this stage give an evolution equation for V. We consider the
model,
V~ =
V(-
v +(A (~) V~. (4)
The
following
considerations have been taken into account. The space reflection symmetry,x - x,
implies
the invariance V~ V. V is
linearly damped (v ~0)
in order toget
astationary
primary
bifurcation. The term V(
v A~)
is theleading
order expansion of the resonant termVf(A,
A), compatible
with the x-translation invariance whichimplies
theinvanance under A
- A exp
I#
This model is toosimple
because acoupling
of the formV(A(~
does not exist ingeneral (it
is for instance forbidden if the system is Gahleaninvariant),
but it allows one to understandsimply
the structure of the bifurcation from thestationary
pattern
to thednfting
one that occurs when ~1= v.
For ~1
~ 0 equations
(3), (4)
have stationarysolutions,
A=
Ao,
V=
0,
withAl
= ~1, that
represent periodic patterns
of wavenumber$
We write A=
iAo
+r(tji
exp ii# (tji
,
V
= V
(tj
and
get
from(3), (4),
r~= 2 ~lr + h o. t
,
thus
r(t)
isdamped
and#~
= kV(5a)
V~= (~1- v) V-V~+h.o.t (5b)
The basic pattern bifurcates first for ~1= v, and
begins
to dnft with avelocity
±
fi
Thestructure of the «drift bifurcation is as follows. its order
parameter
Vundergoes
a x ~ xsymmetry-breaking pitchfork bifurcation,
and thecoupling
with theneutral mode
#
due to translational invariance in space, generates the dnftThis bifurcation structure was found m reference
[7]
where Vcorresponds
to the basic pattern second harmonicamplitude.
Moregenerally
it wasrecently pointed
out on symmetryconsiderations,
translational invariance m space(#
-
#
+constant)
and space reflectionsymmetry (x~
-x,#
--#,
V~V),
that when astationary pattern undergoes
asecondary pitchfork
bifurcation that breaks the reflectionsymmetry,
thecoupling
of the pattemspatial phase
isgenencally
of the form givenby
equations(5),
and generates a driftinstability [8]. Thus,
on symmetryconsiderations, equations (5)
can be considered as theleading
orderamplitude
equations that describe the dnft bifurcation ».We should
emphasize
that V does not need to be avelocity
field m order togenerate
thedrift,
which occurs because of the form of thecoupling
with thespatial phase given by
equation(5a).
V is the order parameter of the «dnftbifurcation»,
associated with thex--x broken symmetry. The
only
constraint on V is thus thesymmetry
constraint,(x
- x,~
-
#,
V-
Vi.
Differenttypes
of symmetrybreaking
bifurcation can be ofcourse considered for V. In
particular, interesting
patterndynamics
can occur if V bifurcatesat a finite wavenumber instead of zero wavenumber
(see
Sect.6)
In realisticproblems,
oneneeds to find the nature of the order
parameter
V of the « drift bifurcation ». Ageneral
modelis given in the next section for the transition from
stationary
topropagating patterns
Insection
4,
thisproblem
is solved forparametncally
excitedstanding
wavesundergoing
a dnftinstability.
3. A drift
instability
ofstationary pattems.
In their Galerkm
approximation
of a model equation, Malomed andTnbelsky
found that the dnftinstability
occurs when the second harmonic of the basicpattern
is notlinearly damped strongly enough.
We thus consider a situation where two modes k and 2 k interactresonantly,
u
(x, t)
=
[A (x, t) e'~~
+ c,c, u~ +[B(x, t) e~'~~
+ c-c u2k +(6)
From
symmetry
argument(translational
invariance mspace),
the evolution equations for A and Bread,
to1hlrd order,
A~=~IA-18-a(A(~A-p(B(~A (7a)
~B~=vB+sA~-y(A(~B-3(B(~B (7b)
The
quadratic coupling
terms describe the resonant interaction between the modes k and2k Their coefficients can be taken
equal
to e=
±I
by appropriate scaling
of theimphtudes
the coefficientof1B
can be takenequal
toI, making
the transformationu ~ u, if necessary Positive values of a,
p,
y and 3 ensureglobal stability.
The bifurcationdiagram
Ofequations (7)
have been studiedby
several authors in the context of resonant wave interaction[I1, 12, 13]
or as a model ofspatial penod doubling
bifurcation[14]
We thus refer to these papers for the mathematicalaspects
and discussequations(7)
m the restrictedcontext of the « dnft bifurcation ».
Writing
A=Re'*, B=Se'~, 3=2~-9,
we
get
from(7)
R~ = (~1 aR ~
pS~)
R RS cos 3(8a)
S~ =
(v yR~ 35~)
S +sR~cos
3(8b)
~t
-
'12
S ~l
Sin ~
(8C)
#
= s sin 3
(8d)
In the context of our
study
we must take v < 0(the
second harmonic islinearly damped)
and increase the bifurcationparameter
~1 When~1becomes positive,
the null state bifurcates to an orbit of stablestationary
patterns related to each otherby
space translation.R=Ro#0, S=So#o, 3=30=o, and#arbitrary.
A cellular pattern
dnfting
with a constantvelocity, corresponds
toR~=0, S~=o, 3~=o, ~~=constant#0.
This
implies
2 SsR~/S
=
o,
and thus s=
I. So the coefficients of the
quadratic
terms must haveopposite signs
in order to observe the dnftinstability
Note that this means that thesecond harrnonic does not enhance the stationary
instability
near onset;indeed,
for~1 m o and v <
o,
B followsadiabatically
A(B
oc A~),
and thequadratic
term of equation(7a)
contributes to saturate the pnmary
instability.
The stationary pattern is destabilized when 2 SoRj/6~
vanishes as~1is
increased. Thishappens
if the condition I +v
(2
y + 3)
m 0 is
satisfied,
whichcorresponds
to the condition that the second harmonic is notstrongly damped
( iv
not toolarge).
Thesystem
ofequations (8a), (8b), (8c)
thenundergoes
asupercntical pitchfork
bifurcation. The two bifurcatedstationary
states "are such thatR(=25(,
3= ±
3r#
0 Above theinstability
onset,~
increaseslinearly
in timeaccording
toequation
(8d)
As notedearlier,
this staterepresents traveling
waves.The bifurcation from the stationary pattern to the
traveling
one has all the charactenstics of the « dnft bifurcation described in section 2. Its orderparameter, 3
= 2
~ 9, undergoes
a
pitchfork
bifurcation that breaks the basicpattern
reflectionsymmetry
Thecoupling
with the basicpattern spatial phase ~
induces the dnft motionaccording
toequation (8d),
and the direction ofpropagation
is determinedby
the sign of 3. Thus the mechanism descnbedby
Malomed and
Tnbelsky [7]
for their modelequations
appears to be ageneral
oneAlthough
the drift bifurcations observed in the experiments of reference
[1, 2]
near codirnension-two bifurcations are not describedby
thismechanism,
we expect that our k- 2k interaction mechanism is relevant for the expenments of references[3, 4, 17]
4. The drift
instability qf
aparametrically
excitedstanding
wave.We have observed
recently
a driftinstability
of astanding
surface wave,generated by
parametric excitation in a horizontallayer
of fluid contained in a thinannulus,
submitted to vertical vibrations[6].
It was observedthat,
as thedn~lng amplitude
isincreased,
thestanding
wave
pattem
eitherbegins
to move at a constantspeed
in onedirection,
orundergoes
anoscillatory instability
thatcorresponds
to a wavenumber modulation in space and time. We first describe the dnft bifurcation and discuss theoscillatory instability
in section 6Close to the onset of
instability,
we wnte the surface deformation in the formf(x,t) =Aexpi (wt-kx)+Bexpi (wt+kx)+cc +h.o.t, (9)
where A and B are the
slowly varying amplitudes
of thenght
and left waves atfrequency
w =
w~/2,
where w~ is the extemaldnving frequency.
The equations for A and B are atleading
order[6],
A~+cA~= (-A +iv)A+~lfi+aA~~+ (p(A(~+y(B(~)A (10a)
B~-cB~= (-A +iv)B+~11+aB~~+ (p(B(2+y(A(2)B, (10b)
where is the
dissipation (A
~0),
vcorresponds
to thedetuning
between the surface wavefrequency
wo andw~/2, ~1is proportional
to the externalforcing amplitude
Theimaginary
parts of
fl
and y describe the nonlinearfrequency
variation of the wave as a function of theamplitude,
whereas the real partscorrespond
to nonlineardissipation.
The real part of c, c~, is the groupvelocity
Note that theimaginary part
c, is non-zerohere, contrary
to the caseof waves
generated by
aHopf
bifurcation in an infinite system, and describes asa~
does,
wavenumberdependent dissipation.
a,corresponds
todispersion
When ~lm
0,
astanding
wave regime is observed Toanalyze
itsstability
wewrite,
A= exp
(S
+R)
exp 1(
& + 4~)
and B= exp
(S R)
exp 1(
& 4~)
,
and get from
equations (10)
forspatially homogeneous
wavesS~ = + cosh 2 R [~1 cos 2 & +
(p~
+y~)
exp 2S] (I la)
8~ = v + cosh 2 R
~1 sin 2 & +
(p,
+ y,)
exp 2S] (I16)
R~ = sinh 2 R
[-
~1 cos 2 & +(p~ y~)
exp 2S] (I lc)
4~~ = sinh 2
R[~1
sin 2 & +(p, y,)
exp 2S] (lid)
& and 4i are
respectively
thetemporal
andspatial phases of,
the pattem Note that theequation
for 4~decouples,
because of the translation invariance of thesystem
in space. Thestanding-wave
solutionscorrespond
to(So,
&o, R =0).
Theirstability
with respect tospatially homogeneous perturbations
issimple
toinvestigate
fromequations (11)
We assumep~
+yr10
and thedetuning
smallenough (
v <p~/p, ). Then, perturbations
in S and& are
damped
Perturbatlons in R and 4~obey
theequations,
4~~=2[v+2p,exp2So]R+h.o.t (12a)
R~=2[-A +2prexp2So]R+h.o.t. (12b)
When the
standing
wave patternamplitude
exp 6~ issmall,
R isdamped
and thestanding
wave pattern is stable As thednving amplitude
isincreased,
5~ increases and R becomes unstable forexp2 So
=
A/2pr, provided
thatpr~0
A non zero value of R breaks the x~x symmetry
(see Eq (9)
and the expressions of A and B versusS, R, &, al.
Thus R is the orderparameter
of the « dnft bifurcation » for thisstanding
waveproblem.
Thecoupling
with thespatial phase
4~ generates the dnft(Eq (12a)).
The structure of the « drift bifurcation is again similar to that descnbed in section 2(Eqs. (5)). However, higher
order terms inequations (12)
show that the dnft bifurcation is subcntical in this case. One caneasily
check this
by
noting that thednfting
solution ofequations(11), S~=R~= &~=0,
4l~, 0,
exists for exp 2So
<A/2 pr,
i-e-only
before the onset of the dnft bifurcation But additional terms of the form(A
(~A, (B(~ B,
can stabilize thednfting solution,
and even make the dnft bifurcationsupercntical
5.
Instability
of tbehomogeneous drifting pattern.
The
experiments
of references[3, 4] usually
do notdisplay
stablehomogeneous dnfting patterns,
but often localizeddnfting
regions. This was describedby
assuming that thepanty breaking
bifurcation is subcntical[8].
We show here that even if the bifurcation issupercritical,
thehomogeneous dnfting
solution isgenerally
unstable in thelong wavelength
limit. To wit, we
generalize
equations(5)
to take into accountspace-dependent
pertur-bations :
4t
" V
(13a)
Vt=AV- V~+a#xx+bvxx-C4xxxx-dvxxxx+fV#x+gvvx+h#x#xx+h.o.t.
(13b) Equations (13)
are agradient expansion,
the form of which is givenby
symmetry arguments,translational invanance in space
(#~ #+ constant),
and space reflection symmetry(x
- x,#
~
#,
V-
V). Higher-order
terms in equation(13a)
canalways
be removedvia a nonlinear transformation
[15]. (The
coefficient k ofEq (5a)
has been scaled inVl.
If thecoefficients,
a,b,
c,d,
are positive, the V=
0 solution first bifurcates when vanishes and
becomes
positive
Thehomogeneous drifting
pattern,Vo
= ±
$ #o
=
Vot,
bifurcatessupercntically,
itsstability
toinhomogeneous
disturbances of the formexp(~t
+iqx),
isgoverned by
thedispersion relation,
~~+ (2
>iqgvo
+bq2j
~
iqfvo
+aq2
=
o(q2j, (14j
that shows that the term
f VW
~
can destabilize the
homogeneous
patternindependently
of the signoff
thusleading
tospatially inhomogeneous
patterns without assuming a subcntlcalbifurcation for V
The observation of such a
pattern
in thevicinity
of a drift bifurcation wasrecently reported [19]
in theexpenment
described in reference[3],
where an oil film is drained between twocylinders.
When onecylinder
is at rest, say the outer, astationary
cellularpattern
of the oilmeniscus is created above a cntical rotation
velocity
of the innercylinder
Aslight
counter-rotating motion of the outer
cylinder
thengenerates
a dnft of thispattern,
that consists of manydnfting
domains movingerratidy
Thehomogeneous
dnft is stabilizedonly
forlarger
counter-rotation velocities
[19].
Anotherexpenmental
observation that can be understood withequations (13)
is the stationary pattem wavenumber selection withincreasing
rotationvelocity
of the innercylinder,
when the outercylinder
is at rest. It is observed that anabrupt
increase of the inner
cylinder velocity
leads to a pattern wavenumber modificationby
nucleation of a transient
dnfting
domain. As noted in reference[8]
thisdnfting
domaingenerates
aphase gradient,
say q, that leads to a newpenodic pattern
of wavenumber k+ q.Indeed,
V=
0, #
= qx, is, a
particular
solution ofequations (13),
for which thedamping
rate ofperturbations
in V is A +fq. Consequently
the dnft of this newpattern
is inhibited iffq
<
0,
for q~
Al f.
The newpenodic
pattern thus remainsstationary
because of wavenumber modification(see Fig I).
Within the framework of the model of section3,
this stabilization mechanism is associated to the increase of the second harmonicdamping
rate when the pattern wavenumber is increased(Fig. I).
R
,,
k k+q ,'
,
o
,«
x x'
2k 2(k+q)
k
Fig.
I Sketch of the wavenumber selection mechanism when the control parameter R isabruptely
increased above themarginal stability
curve(solid line),
the pattem of wavenumber k(o)
becomes unstable to the drift bifurcation because its second harmonic is notsuffciently damped.
However, thehomogeneous dnfting
solution is unstable and the propagation ofdrifting
inclusions increases the wavenumber to k + q(.),
thusstabilizating
a new static pattern because thedamping rate
of the second harmonic increases. The dashed curve represents the selected wavenumber of the static'cellular pattern(Note
that in the model equations (7), the lineargrowthrates
Jz and v of the modes k and 2 k are notindependent)
6.
Oscfllatory phase
modulation ofperiodic
patterns.As said
above,
anoscillatory phase
modulation ofpenodic pattems
has beenrecently
observed as a
secondary instability
of convection rolls[10]
or surface waves[6]
After thisinstability
onset, theposition
of the rolls(or
of the wavecrestsrespectively)
is modulated in space and timeby
astanding
wave In the surface wave expenment[6],
thisoscillatory
instability
was observed close to the dnft bifurcation in theexpenmental parameter
space.The numencal
integration
ofequations (10)
has shown that thisoscillatory instab1llty corresponds
to astanding
wave modulation of the basicpattern spatial
andtemporal phases,
in agreement with the
expenmental
observations[6] (see Fig. 2).
We show that the
coupling
that generates the «drift bifurcation» is also apossible
mechanism to describephase
modulation ofpenodic patterns,
if the orderparameter
V isdestabilized at a finite wavenumber. We consider equations
(13),
that govem the spacedependent perturbations
of the basic-periodic
pattem, with Am
Ao,
Ao ~0.Thus,
thestanding pattern
is stable withrespect
tohomogeneous perturbations.
Thegrowth
rate of aperturbatioi
of the formexp(~t
+iqx),
isgovemed by
thedispersion relation,
~~+ ~(-A +bq~+dq~)+aq~+Cq~=O(q~). ('5)
Stability
at shortwavelength implies
d ,~ 0. For a
~ 0 and b
< 0 an
oscillatory instability
occurs first for A
o =
b~/4 d,
with a finite wavenumber qo =(A
o/d~~'~, and afrequency
at onsetiio
=
(aqj+ cq)~'~, provided
that a +cqj~0. lifhen Ao
issmall,
i-e- close to the «dnft(a) (b)
(C)
tl(d)
aJ
o x lo o x lo
Fig 2 Numerical observation of the
oscillatory
mode The control parameters used in the numerical simulation of theamplitude
equations(10)
are A= 2.5, v
= 3, Jz
= 4, a, I, a,
=
I, p~
=
0.I,
p,
= I, y, = 02, y, = 0.I, c,= 35, c, = 2 5, L
=
10.
Temporal
evolution of the moduhprofiles (A(x, t)
and(B(x, t) [respectively a)
andb)],
of thespatial phase ~P(x, t)
=
(argA
2
arg
B)
[c)] and of thetemporal phase
8(x,t)
=
(arg
A + argB) [d)] Twenty
one successiveprofiles
2
ale
displayed
on the samefigure
with anarbitrary upward
shift, for a time interval t e [0,Ii
,' ,
,,'
,"
(rTlT~
, ,
,,
,0
h
Re~
Fig. 3 -Perturbation
growthrate
as a function of the wavenurnber of the oscillatoryinstability (a~0,
b<0)bifurcation»,
qo is small and thus we expect thegradient expansion
to bejustified.
Thecorresponding growthrate
isdisplayed
onfigure
3 it shows that theoscillatory instability
results from the interaction of the neutral
mode,
because of the translation invanance in space, with theslightly damped,
reflectionsymmetry-breaking
mode associated with the drift bifurcation before its onset value. Aninstability leading
to astationary
modulation of the basicpattem wavelength
can occur for a< 0 and b
~ 0. A convective
pattern
with rolls ofirregular length
has been observedexpenmentally,
but the relevance of this mechanism inthat case remains to be checked
[18].
In the
vicinity
of theoscillatory instability
onset, we write#(x,t) =A(t)expt(wet-qox)+B(t)expt(wet+qox)+cc +C(t)+h.o.t. (16)
The fields A
(t)
andB(t)
describe theslowly
varyingcomplex amplitudes
of the waves that propagate to theright
and to theleft,
whereas the real fieldC(t)
takes into account the existence ofmarginal
modes for q- 0.
Taking only
into account theleading
ordernon-lineanty, f VW
~
we obtain with standard
asymptotic
methods(see Appendix),
(Ao- iii)
~ ~
A
"
~
~ + (tY
IA
+P (B( )A ('7al
fi= ~~° ~~~~B+ (p(A(~+a(B(~)B (17b)
©
=
~~"°~°
((A (~- (B(~), (17c)
Ao
with
~
~)~ ~
~ 9
~c/dwo
'
~
~)~
~~~~
Thus,
theleading
ordernonhneanty
does not saturate theoscillatory instab1llty.
In thelong wavelength limit,
the effect of other nonlinear terms is ofhigher order,
and theinstab1llty
isJOURNAL DE PHYSIQUE II -T I, M3, MARS <WI is
subcntical If we discard terms which
depend exphcitely
onV,
theleading
order term ish#~ 4~~
We obtain C = 0 and s1rnllarequations
for A and Bwith,
~ dh ~
~~
~ ~~~~
~
~~~
~ ~
Id)
~~
~ ~~~The bifurcation is
supercritical
andstanding
waves((A(
=
(B( )
are the stablepost-
bifurcation state, whatever thesign
of h Thlscorresponds
to theexperimental
observations[6, 10]. However,
we have nogeneral argument
to discard the termsV4~ VV~
andV~
inequation (13b).
We have thus shown in this paper that a
vanety
of recentexpenmental
observations ofperiodic pattern secondary instabilities,
can be understood in asimple
framework: thecoupling
of the neutral mode associated with translational invanance in space, with a reflectionsymmetry-breaking
bifurcation. Note that a similarsingularity,
with two, zeroeigenvalues
at asecondary instab1llty
onset, occurs for theoscillatory instability
of convection rolls and leads totraveling
waves thatpropagate along
their axis,although
theunderlying physical
reasons are different[15].
Let usfinally
mention that thesecondary
instabilitiesdescribed here
obviously
fit in thegeneral classification, proposed recently
on the basis of symmetryarguments [16],
but thepresent approach
givessimple physical
mechanisms that dogenerate
thesesecondary
instabilities.Acknowledglnents.
We
acknowledge
theAspen
Center forPhysics
where part of this paper has been written We thank J.Bechhoefer,
Y.Couder,
S.Michalland,
M. Rabaud and H Riecke for discussions.This work has been
supported by
a EEC contract SCI-0035-C.Appendix
: Dedvation of theamplitude equation (17)
fromequations (13).
Taking
into accountonly
the nonlinear termf#~ #~
equations(13)
read£# =f#t#x,
where
£#
=
#
tt A
#
t
a#
xx
b#
xxt +
C#
xxxx
+
d#
xxxxt
The
dispersion
relation is£(~,tq)
= o,
W~~~~
r(~, iq)
=
~2+ ~(> +bq~+d~~) +~~~+~~~
for a
~
0,
b< 0 and d
~
0,
anoscillatory instability
occurs when A= A
o = b
~/4 d,
with afinite wavenumber qo =
(Ao/d)"~
and afrequency
at onset wo =(aq(
+cq)~'~ provided
thata +
cqj
~ 0.
Close to the
instability
onset,following
standart asymptotic methods[21],
weexpand
=
-Ao+ s~A~+...
~
=~~(i) ~~2 ~(2)
~___and introduce the slow time scales
Ti
= Et, T~ =
s~
t,..To
leading
order we have £o4
~'~= 0
(to
=
£(A
= A
o)),
thatimplies
~ ~'~(x,
t,Tj, T~,.
=
I(Tj, T~, )
expt
(wo
t qox)
++
1i(Ti, T2, )
eXP1("0
t + ~0X)
+d(Tj, T2,
+ C-C-
We
get
at the next order£
~
~~~f ~
~~~~
~~~ ~~~
° ~
aTj
The
solvability
condition gives the evolution equation ford
ad
2fwoqo
~ ~
i
=>~ (lA (B( )
Then,
~
~~~=
~"°
~°[l~
exp 2 I(wo
t qox)
+
ji~
exp 2 I
(wo
t + qoxii
+ c-c-£o(21wo,
2iqo)
We get at the next order
£
#
(3)~
~j ~
(i) ~ (2) ~~
(2)~ (i)j
The
solvability
conditionsgives
~~ =~~l+ (a(1(~+p(fi(~)l
3T2
2~~
=
~~h+ (p(1(~+a(fi(~)h (17b)
3T2
2with a and
p given by equation (18).
Afterrescahng
toonginal vanables,
A=
El,
B
=
Ed
and C=
Ed,
we get theamplitude
equation(17).
The same method can be used whenconsidenng
the other nonlinear terms of(13).
References
[1] WALDEN R W, KOLODNER P, PASSNER A and SURKO C M
,
Phys
Rev Letters 55(1985)
496- 499.[2] MUTABAzI I
,
HEGSETH J J
,
ANDERECK C. D. and WESFREID J E
,
Phys
Rev. A 38(1988)
4752- 4760[3] RABAUD M, MICHALLAND S and COUDER Y,
Phys.
Rev Letters 64(1990)
184[4] SIMON A J, BECHHOEFER J. and LIBCHABER A,
Phys.
Rev. Letters 61(1988)
2574-2577[5] FAIVRE G, DE CHEVEIGNt S, GUTHMANN C and KUROWSKI P,
Europhysics
Letters 9(1989)
779-784
[6] DOUADY S, FAUVE S and THUAL O.,
Europhysics
Letters 10(1989)
309-315[7] MALOMED B A. and TRIBELSKY M I,
Physica
14D(1984)
67-87[8] Using these symmetry considerations,
pointed
outby
G. Iooss, P Coullet, R E. Goldstein and G H Gunaratne have wnttendirectly
equations similar to our equations(5),
and have considered the case where Vundergoes
a subcntical bifurcation, COULLET P., GOLDSTEIN R E and GUNARATNE G H.,Phys
Rev Letters 63(1989)
1954-1957(See
also Ref[17])
[9] THUAL O and BELLEVAUX C, Fifth Beer-Sheva Semlnar on MHD Flows and Turbulence, AIAAProgress m Astronautics and Aeronautics l12
(1988)
332-354[10] DUBOIS M, DA SILVA R., DAVIAUD F, BERGt P and PETROV A, Europhysics Letters 8 (1989) 135.
[ll] DANGELMAYR G, Dyn Stab Syst
1(1986)159-185
[12] ARMBRUSTER D, GUCKENHEIMER J. and HOLMES P,
Physica
29D (1988) 257-282[13] PROCTOR M R E and JONES C., J Fluid Mech 188
(1988)
301-335.[14] PAAP H G and RIECKE H.,
Phys
Rev A41(1990)
1943[15] FAUVE S, BOLTON E. W and BRACHET M.,
Physica
29D(1987)
202-214[16] COULLET P and IOOSS G,
Phys
Rev Letters 64(1989)
866[17] FAUVE S, DOUADY S and THUAL O,
Phys
Rev Letters 65 (1990) 385, thek 2k mechanism has been also
proposed by
H Levine, W JRappel
and H Riecke,submitted to
Phys.
Rev Letters (1989)[18] BERGt P, DAVIAUD F and DUBOIS M, pnvate communication
[19] COUDER Y, MICHALLAND S and RABAUD M, private communication
[20] See'for instance, GUCKENHEIMER J and HOLMES P, Nonhnear Oscillations,
Dynamlcal Systems
and Bifurcations of Vector Fields,