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Interface dynamics and anisotropy effects in directional solidification
S. de Cheveigné, C. Guthmann
To cite this version:
S. de Cheveigné, C. Guthmann. Interface dynamics and anisotropy effects in directional solidification.
Journal de Physique I, EDP Sciences, 1992, 2 (2), pp.193-205. �10.1051/jp1:1992133�. �jpa-00246472�
Classification
Physics
Abstracts81.30 61.50 47.20
Interface dynamics and anisotropy effects in directional solidification
S, de
CheVeign6
and C. GuthmannGroupe
dePhysique
des Solides(*),
Tour23, 2 PI. Jussieu, 75251 Paris Cedex 05, France(Received 6
May
1991, revised 4 October I991,accepted
28 October 1991)Rksum4. Une 6tude de la
dynarnique
de l'interface cellulaire en solidification directionnelle d'unalliage
binaire dilu6 de CBr4 nous aperrnis
d'observer un certain nombre d'instabilit6s secondaires(propagation
de cellules incl1n6es, modesoptiques,
cellules anorrnales, etc.) dont certaines 6taient bien connues et traditionnellement attribu£es h des effets del'anisotropie
cristalline.
Cependant,
laplupart
de ces instabilitds sont observables dons uneexp6rience qui
estl'analogue hydrodynamique
de la solidification directionnelle, ladigitation Visqueuse dirig6e
ouinstabilit6 de
l'imprirneur
(M. RABAUD, S. MICHALLAND and Y. COUDER, Phys. Rev. Lent. 64 (1990) 184). Cetteanalogie
va nous perrnettre de discuter (es r61esrespectifs
del'anisotropie
cristalline et de la
dynarnique
propre auxsystbmes
uni-dimensionnels.Abstract. A
study
of thedynamics
of the cellularsolid-liquid
interface in directional solidification of a diluteCBr4 alloy
has allowed us to observe a number of secondary instabilities(travelling
states, optical modes, anomalous cells, etc.) some of which were well known andtraditionally
attributed to the effect ofcrystalline anisotropy.
However, most of these instabilitiesare also observed in a
hydrodynamic analog
of directional solidification, directional viscousfingering
(M. RABAUD, S. MICHALLAND and Y. COUDER, Phys. Rev. Lent. 64 (1990) 184). Thisanalogy
enables us to discuss theinterplay
ofcrystalline anisotropy
and of thedynamics generic
to one-dimensional systems in directional solidification.Among
the variousdynamical
systems that exhibitregular pattems
when out ofequilibrium,
those which can be considered as one-dimensional are ofparticular
interestII.
Their
dynamics
have been modelized and it has been shown thatthey
candevelop
a numberof
secondary
instabilities as well asspatio-temporal
chaos[2].
In the presentarticle,
weshali
describe some
aspects
of thedynamics
of one such system, directional solidification of thinsamples
and their relations towavelength
selection. Thequestion
which will arise is : is the behavior of thissystem generic,
identical to that of other lDsystems,
or does thecrystalline
substrate
play
a role ?(*) Associated with Universities Paris 7 and Pierre-et-Marie-Curie and with the Centre National de la Recherche
Scientifique.
In directional solidification
(DS),
asample
ispulled
at avelocity
V in a constanttemperature gradient
G set up around itsmelting temperature
in such a manner as toprogressively solidify
thesample [3].
If the material is not pure, soluterejection (or incorporation,
if thepartition
coefficient is greater thanI)
will occur at thesolid-liquid
interface. Above a critical
pulling speed,
forgiven
concentration and temperaturegradient,
diffusion is no
longer
sufficient to assure the evacuation of solute and the interfaceadopts
aperiodic
cellular pattem in which solute is accumulated in the cusps of the cells. The presentexperiments
focusparticularly
onnon-stationary phenomena. They
were carried out on thin(50
± 5 ~Lm unless otherwiseindicated) samples
of tetrabromomethane(CBr4),
a transparentorganic material, containing
a fraction of a percentimpurities.
The temperaturegradient
wasG
w loo °/cm which
gives
a thresholdV~
= 8 ~Lm/s for theplanar-cellular
front transition. Theexperiments
were observed under amicroscope
andvideo-taped. (The experimental
set-upand
previous stationary-state
resultsconceming
this material can be found elsewhere[4, 5]).
In the present work we have made extensive use of
spatio-temporal diagrams
madeby extracting
agiven
line from thedigitalized
videoimage
atgiven
time intervals(typically
0. I to Is)
andrecreating
animage (with
onespatial
dimension and onetemporal one) by
juxtaposing
these lines[6].
Coullet and Iooss
[7]
haveshown, by
symmetry argumentsonly,
that one-dimensionalinterfaces can be
expected
to present a series ofinstabilities,
a number of which havealready
been observed in directional solidification of
liquid crystals [8]
and eutecticalloys [9],
in one- dimensionalRayleigh-Bdnard
convection[10]
and in directional viscousfingering (DVF),
also known as theprinter's instability
it].
This last system is ofparticular
interest for us because it is ahydrodynamic equivalent
to DS thephysical
mechanismsdriving
the instabilities areequivalent
but the medium in whichthey
appear has nocrystalline anisotropy.
In theexperiment,
oil istrapped
between twonearly tangential rotating cylinders,
one inside the other. The interface observed is that between the oil and air forced into the oil as thecylinders
come apart.
(DVF
can be in fact morecomplex
than DS because thecylinders
can be co- rotated orcounter-rotated.)
A closecomparison
of our results with those obtained in DVF will lead us to reconsider the role ofcrystalline anisotropy
in DS.Travelling
waves.Tilted cells were observed in the very first
experiments
on transparent materials carried outby
Jackson and Hunt
[12]
in 1965. The effect istraditionally
attributed tocrystalline anisotropy (essentially
of the attachmentkinetics)
: for cubiccrystals
such asCBr4, growth
in the(100)
direction is faster than in others. If the direction of fastestgrowth
is notperpendicular
to the
interface,
the cells growasymmetrically.
Theimportance
of attachment kinetics increases withpulling speed
until thegrowth
is orientedalong
thepreferred direction,
as is believed to be the case for dendrites.Anisotropic
interface kinetics were indeed shown toproduce
sucheffects,
bothanalytically by
Coriell and Sekerka[13]
andnumerically (in
thecase of a low
partition coefficient) by Young
et al.[141.
However, a number of observations
bring
us toquestion
thisinterpretation.
Inclined cells,by definition,
grow at anangle
to the normal to the solidliquid
interface(Fig, la)
and appearas
travelling
waves on aspatio-temporal diagram (Fig. lb).
A similardiagram
has beenpresented by
Gleeson et al.[5]
for succinonitrile-ethanol. The lateralvelocity V~
of the cells issimply
related to theirangle
of inclination a:V/V~
= cotan a.
Figure
2 shows how the lateralvelocity V~
of thetravelling
wave increases withpulling speed
V in agiven
«grain
».(This
termnormally
refers to a zone ofgiven crystalline
orientation. We shallonly
mean herea zone of cells of a
given inclination.)
Note the presence of a well definedthreshold,
at about 25~Lm/s,
below which no lateral movement is observed, to within ourprecision
ofb)
a)
Fig.
I. a) A cellular frontpresenting
inclined cells and both a source and a sink (V= 66 ~Lm/s). b) The
corresponding spatio-temporal diagram.
Note thefollowing
features : A) anasymmetric
source(cells only divide on the upper side) ; B) the same source has become symmetric (cells divide on both sides) C) an
asymmetric
sink where altemate cells arepinched
off D) is a gas bubble.8
6
~
E
~ 2
e
0
measurement
(w0.5 ~Lm/s).
If the video camera is at allmisaligned
an apparent lateral movement will appear in thespatio-temporal diagrams.
Whenever necessary, it has been subtracted out forquantitative
measurements. In ourexperiments,
the curve was notunique
:in different
grains
andsamples,
the lateralvelocity
increased withpulling velocity
from thesame threshold but its value
beyond
this thresholdvaried, depending probably
on thecrystalline
orientation of thegrain.
A curve similar to that of
figure
2 wasreported
in succinonitrile-ethanol[13].
On the otherhand,
Trivedi[16]
has studied the effects ofanisotropy
inpivalic acid-ethanol,
a material forwhich
they
are believed to be stronger than inCBr4
or succinonitrile. In that case, nothreshold in lateral
velocity
isreported
for misorientations of thecrystal
greater than 20° and the threshold observed(at
15°misorientation)
isonly
of 0.5pm/s. Indeed,
no threshold in lateralvelocity
ispredicted by
the modelizations of the effect of cristallineanisotropy
mentioned above
[13, 14]
: the lateralvelocity
waspredicted
to beroughly
constant. So the threshold in lateralvelocity
does not seem to be related to cristallineanisotropy.
In this context, it is
particularly interesting
to consider that inclinedtravelling
states withasymmetric
cells are observed in DVF[10], although
nocrystalline anisotropy
is present.Figure 3, kindly provided by Couder,
Michalland andRabaud,
shows aspatio-temporal diagram
of such waves, on either side of a source(time
runs from top tobottom).
It ispossible
that in this system, translational symmetry
along
the air-oil interface be broken for instanceby
lateral flow of the oil. But there is no
equivalent
to themicroscopic anisotropy
of attachment kinetics.These two observations lead us to believe that
microscopic
cristallineanisotropy
may not be theonly
factorinfluencing
thegrowth morphology
of cells in directional solidificationalthough
cristalline orientationapparently
affects theirprecise angle
of inclination and thatmore
generic dynamic
instabilities alsoplay
a role. We shall see further evidence of this in what follows.Fig.
3. Aspatio-temporal diagram
with asymmetric
source observed in directional viscousfingering (kindly provided
by COUDER, MICHALLAND and RABAUD. Thespatial
coordinate is horizontal and timeincreases downward). Note that a single central cell splits altemately to one side then to the other.
Let us first examine in more detail the
spatio-temporal diagram
offigure16.
Boundariesbetween
grains
appear on thespatio-temporal diagrams
as sources where cells widen thensplit
and sinks where cells narrow andpinch
off. Sources can be more or lesssymmetric
with cells
appearing
on both sides of theboundary,
orthey
can beasymmetric
withonly
cellson one side
splitting.
In the upper part offigure
16 one can see anasymmetric
source becomesymmetric.
We haveonly
observedasymmetric
sinks : onegrain
appears to be blockedby
the other.Figure
16(feature C)
also shows aparticular
oscillation of the sink where the last cell and the second last cell arealtemately pinched
off.In
DVF,
sinks andasymmetric
sources appear to be identical to thosereported
here.Symmetric
sources,however,
are different(see Fig. 3)
: asingle
central cellsplits altemately
to the left and to the
right
whereas infigure
16 there are two central cellsclearly separated by
a continuous lineprobably
agrain boundary
and each cellsplits
to its own side. This is an illustration of onepossible
interaction betweendynamic
instabilities and thecrystal
:sinks and sources seem to lock onto a defect of the
crystal,
I-e- agrain boundary.
Asymmetric
cells andwavelength
decrease.A number of
secondary
instabilities can be described as cases where acell,
too widecompared
to the normal
wavelength
at thatvelocity, unsuccessfully attempts
totip-split (Fig. 4).
Whentip-splitting
succeeds, two new cells appear, but when itfails,
the result is anasymmetric
cell with a shoulder that is advected back towards the solid. Theinstability
canpropagate
or notalong
the interface. It has been shown[1,
7,17]
that the presence of such modes is related to thedevelopment
of the second harmonic of the interface deformation. The cellshape
goesfrom sinusoidal to « square » with a flattened center that can allow
tip-splitting.
The term
« mitten cells »,
suggested by
Cladis et al.[18],
describeslarge amplitude
cells with a thumb-like shoulder. Agiven
cellperiodically begins
totip split,
but thedip slips
off-i
x ~
$ e
~
x ~ °
_
x
m
i lo loo
vl~L1n/s)
Fig.
4. Averagewavelength
I versuspulling velocity
V for cellspresenting
optical modes (crosses) and mitten orpre-splitting
instabilities (diamonds). The line represents the averagewavelength (dispersion
is about 10fb) for normal cells [4].JOURNAL DE PHYSIQUE I T 2, N'2, FEBRUARY 1992 8
center so the deformation is advected
back, giving
the characteristic shoulder. The cell thenregains
its initialshape
and the whole process startsagain.
The samething
canhappen
to itsneighbours, slightly dephased
in time, hence theimpression
ofpropagation.
This is best seenin
figure
5b. Thephenomenon,
firstreported by Venugopalan
andKirkaldy [19]
and observed in succinonitrileby
Heslot and Libchaber[20],
can also be described as a failedtip- splitting.
The cells areabnormally
wide(here
68 ~Lm on average instead of a normal value of 50 ± 5 ~Lm)(Fig. 4).
Mitten cells can also be observed in DVF[I il.
G ""
,. "z
~' -~ 'T '$ ~~'
~ w'~
' r-L'
~~ Z '.S~_- S,
i n©' j~b ~G'
~
', ~$
"~ f .'
.I
~~ 'l '[
z ''
"
»,' M')_. t~)~.-~ ~l't
~Q~- j
~
~"~' -"-'
, .~~
&'~ ~~" -~
3 /- /.
_' ~- -~
_' ,' l-?i~
i -,,'
~
II- /,
t
b)
a)
Fig.
5. a) An interfacepresenting
« mitten cells ». Atip split
off centergives
a shoulder that is advected back (V= 10 ~Lm/s). b) The
corresponding spatio-temporal diagram.
Figure
6a shows twopairs
of « anomalous cells».
Again,
these cells are also observed in DVFby
Rabaud et al.[I II
and in DS ofliquid crystals [2 II.
The cells areabnormally
wide and each one is flattened on the sidefacing
the other. Differentaspects
of theirdynamics
areillustrated in
figure
6b. Thepair
can remain stable forquite long periods,
in which case it hasapproximately
the width of three normal cells. It can beprogressively squeezed
out(feature C).
If it is too wide it candisappear through
thesplitting
of both cells(feature D).
In these two cases, thepair disappears
withoutleaving
any trace. But another type ofinstability
can also be observed thepair
widens and the wall between the cells appears to oscillate until one of the twosplits (feature E,
orFig. 6c).
In fact the two cellsaltemately undergo
a series of unsuccessfultip-splittings
the oscillation of the middle wall is due to the advection back ofthe shoulder on altemate sides until one of them
finally
succeeds. This canhappen
repeatedly.
In this case thepair
seems to be locked onto agrain boundary (we
have checked thisby examining
thesample
at rest :grain
boundaries form cusps wherethey
reach the solid-liquid interface).
Rabaud et al.[22]
observe a similarlocking phenomenon
in DVF on a scratch made on one of theirrotating cylinders.
A-
C)
a)
w-
b)
Fig.
6. a) A frontpresenting optical
modes (A) and 4pairs
of anomalous cells (B). The lower cell of the lowestpair
is splitting. b) Thecorresponding
spatio-temporal diagram, with : A)optical
modes B)a
pair
of anomalous cells C) apair
becomesprogressively
normal D) apair disappears
after both cellssplit
; E) apair
thatregularly splits
afterpresenting
«pre-splitting
» oscillations. c) Ablow-up
(x 2.5) of a «pre-splitting
» oscillation(T~~
w 0.6 s) and anoptical
mode(T~~~ w 1.8 s).
Figure
7 shows thepropagation along
the front of asingle
cell deformation on a low-amplitude
cellular front. These deformations areanalogous
to the mittens that are observedon
higher amplitude cells,
in thatthey
appear to be unsuccessfultip,splits. They
are also observed in DS ofliquid crystals [81,
but above about 3 times the thresholdvelocity
for thetransition from a
planar
to a cellular front. Herethey
can be observed much closer tothreshold,
due no doubt to the fact that the bifurcation is subcritical: the interface deformation is neverpurely sinusoidal, higher
harmonics are present from the start and thecells look square. This can also be seen on the
marginal stability
curve forimpure CBr4
(critical velocity V~
vs. wavenumberq),
that isparticularly
flat-bottomed[4]
: modes at 2 q(and beyond)
are accessiblepractically
at threshold.Fig.
7. A sequence ofpictures
of the interface taken every 5.7 sshowing
thepropagation
of a solitary mode (V= 14 ~Lm/s).
The
periods
of these «pre-splitting
»oscillations,
I.e. those of the central cell wall of anomalous cells and of the mitteninstability,
decrease as thepulling speed increases, approximately
asT~~~ oc
V~~ (Fig. 8).
This is also the timescaling
of the diffusion time(D/V~w
los for V
= lo
~Lm/s),
as remarkedby
Gleeson et al.[15].
Theperiodicity
ofdendrite
side,branching
in DS ofCBr4
falls on the same curve[23] (in
succinonitrile-acetone[24]
the order ofmagnitude
of theperiodicity
is the same but it decrease as V~i.
Onecan
speculate
that the same type of fluctuation of thetip
can(a) split
aflat-tipped (rich
in secondharmonic) cell, (b)
be a little off center, fail tosplit
it and be advected back or(c)
in the case ofsufficiently pointed cells,
wheretip-splitting
is blocked[5],
form side-branches I.e.high frequency
shoulders that have room todevelop laterally.
Optical
modes andwavelength
increase.In
regions
of thesample
where the cellularwavelength I
is too small(Fig. 4),
either because of a recent localadjustment
of cell widths a cell hassplit
in thevicinity
or because theloo
lo
]
w
~~4
o
~I
T
i io
8. -
of
oscillation ceases and the
adjustment
thenspreads
out over theneighboring
cells. Even incases where the cell walls do not touch at the
interface,
a rearrangement can takeplace
behindthe interface
causing
the cells topinch
offalternately, producing
the checkered pattem seen inthe middle of
figure
6a[26].
Thedependence
of theperiod
onpulling velocity
is aboutT~~~ oc
V~~'~ (Fig. 9),
I-e- it decreases moreslowly
thanT~~~. The reason for this different
dependence
is not clear.Combined instabilities.
In another type of
secondary instability,
known as a tilt wave, a zone of inclined cells propagatesthrough
normal ones, as has beenclearly
observed in eutectic solidification[9].
Tilt waves are not
frequent
in theexperiments
describedhere,
but we have observed threecases.
Figure
lo shows a tilt wave associated with anoptical
mode. This is onceagain
verysimilar to a
phenomenon reported
in DVF[27].
The cases we observed were all at lowvelocities
(6
to lo~Lm/s)
and the inclined cells were at 7 ± 1° off the normal to the interface.We sometimes observe
spatio-temporal diagrams (Fig. ii)
with anapparently
chaoticmixture,
in time and space, of anomalouscells,
mitten instabilities andoptical
modes. Similardiagrams
can be observed in DVF[I ii
when thecylinders
are co-rotated. « Chaotic »grains
can coexist with
quite
stable ones at the same velocities so the orientation of thegrain
mayplay
a role assuggested by
Heslot and Libchaber[24].
A properspectral analysis
of the time evolution of theinterface,
such as has been carried out on convectionexperiments [28],
is be needed to be able to say if it is true« chaos » we
observe, and,
if so, of whattype.
Fig.
10. -Aspatio-temporal diagram presenting
a «tilt wave». The tilted cells are affected by oscillations of theoptical
mode type (V=
20 ~Lm/s).
Tip-splitting
in dendrites.To
complete
this discussion of therespective
roles of cristallineanisotropy
anddynamic
instabilities in
DS,
we wish to mention someexperiments
carried out on dendriticgrowth
in very thinsamples (e
it ~Lm). Thestability
of dendrites is a case in which cristallineb)
a)
Fig.
ll.-a) A «chaotic» interface, b) Thecorresponding spatio-temporal diagram showing
amixture of anomalous cells,
optical
modes, etc. (V= 80 ~Lm/s).
anisotropy,
either of attachment kinetics or of interfacialtension,
is essential. This has been establishedby
numerical simulations[29-34], analytical
calculations[35, 36], experiments
in viscousfingering [37, 211,
where « cristalline »anisotropy
is introducedlocally by scratching
to
plates
of the Hele-Shaw cell and in solidification[38, 391
andphase
transitions inliquid crystals [40, 411.
Moreindirectly,
dendriteinstability
has been observed when the effect ofcristalline
anisotropy
isthought
toweaken,
I.e. whengrowth
slows down[42, 43]
or inhomeotropic liquid crystal samples [44].
In the absence ofanisotropy,
or under conditions wherecrystalline
and surface tensionanisotropy, aligned along
differentdirections,
cancel eachother,
dendrites are unstable totip-splitting
and the result is a densebranching morphology (DBM).
Inexperiments [181
onsamples
of the order of I ~Lmthick,
oneeasily
obtains dendritic structures at velocities of the order of a few micrometers per second
(Fig. 12)
because the criticalvelocity
for the transition from aplanar
to a cellular interface decreasessharply
assample
thicknessdecreases,
due to meniscus effects.Therefore, simply by decreasing
the thicknessalong
thesample,
one increases the constraint. These dendritesare unstable to
tip-splitting
andproduce
a structure similar to DBM. We suppose that a suchvelocities, anisotropy
effects inparticular
kineticanisotropy
are too weak to stabilizedendritic
growth.
Conclusion.
We have observed a number of
secondary
instabilities of cellular fronts in DS. Theseinstabilities
(optical modes,
anomalouscells, solitary modes,
mittencells, travelling waves)
a) b)
Fig.
12.Tip-splitting instability
of dendrites in very thinsamples
(= I ~Lm) : a) V= 3 ~Lm/s b) V
=
6 ~Lm/s.
appear
quite
similar to those observed inDVF,
thehydrodynamic analogue
of DS.Crystalline anisotropy
is not therefore essential to theirapparition although
thecrystalline
structure of the material affects inclinationangles
and locksparticular
structures(anomalous cells,
sourcesand sinks of
travelling waves).
Whengrowth
becomesdendritic, crystalline anisotropy
isnecessary to stabilize the dendrite
tips against tip-splitting
and we have shown that in ourexperiments
it is notstrong enough
at low velocities.Acknowledgments.
It is a
pleasure
to thank Y. Couder, C.Misbah,
S. Michalland and M. Rabaud for very fruitful discussions and forallowing
us use their resultsprior
topublication.
This work wassupported by
the Centre National d'EtudesSpatiales.
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