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Mapping of (1+1) D-Crystal Growth onto a 14-Vertex Model
F. Hontinfinde, A. Levi
To cite this version:
F. Hontinfinde, A. Levi. Mapping of (1+1) D-Crystal Growth onto a 14-Vertex Model. Journal de
Physique I, EDP Sciences, 1996, 6 (7), pp.873-890. �10.1051/jp1:1996104�. �jpa-00247220�
J. Phys. I France 6
(1996)
873-890 JULY1996, PAGE 873Mapping of (I + I)D-Crystal Growth onto
a14-Vertex Model
F. Hontinfinde
(*)
and A-C- Levi(**)
Dipartimeuto di Fisica and Istituto Nazionale per la Fisica delta Materia, via Dodecaneso 33, 16146 Geuova, Italy
(Received ii January1996, received in final form 4 March 1996, accepted 19 March 1996)
PACS.02.70.Lq Monte Carlo and statistical methods
PACS.81.10.-h Methods of crystal growth; physics of crystal growth
Abstract. A restricted solid-on-solid
(SOS)
single- and double-step model is introduced and studied with Glauber dynamics. Kinetics and roughness of the growing crystal are describedin terms of a Markov process whose states are given by the crystal upper edge profile that we
map onto a 14-vertex model. We solve exactly the kinetic equation for small-size versions of the model. Extensive simulations are performed to derive the large scale properties. The present study appears as a further extension of Gates and Westcott's investigation of the single-step
model.
1. Introduction
Crystal growth, beyond
itstechnological applications,
has along
and richhistory
of studies in basic scienceill
and hasgenerated,
at a fundamentallevel, interesting problems
of non-equilibrium
statisticalphysics.
Itsstudy by
theoretical andexperimental
methods hasprovided
a
deep insight
into solid statephysics
andchemistry. Despite
the recentsignificant
progressobtained
by using
statistical-mechanical models and methods[2-4]
toclarify
cluster andcrystal growth phenomena, high-dimensional growth
models are stillcomplicated beyond
anyhope
ofan exact
solution,
even when well-known,oversimplifying approximations (such
asSOS)
areapplied.
In lowerdimensions,
the situation is less hard and some important results are available in the literatureconcerning growth
kinetics. Garrod [5] solved several two-dimensionalgrowth
models where
growth
occursessentially
at kink sites. Gates and Westcott [6,7] studiedexactly
a restricted SOSsingle-step
model defined on ahexagonal
lattice and a non-restricted SOS model defined on a square lattice,relying
on adynamic reversibility
concept valid in these models.Their results on
growth
kinetics andregimes supplement
those found in previousinvestigations
on
polymer crystallization,
island or cellular structures and 2-Dcrystal growth
[8, 9j.Recently,
Hontinfinde and Touzani introduced a kinetic four-vertex model tostudy
thesingle-step
model in d= I + I where atom
deposition, evaporation
and diffusion on the surface takeplace [lo].
The main result
they
obtained is a reentrantgrowth phase diagram similar,
butprobably
not equivalent to what is often observed
experimentally during
theepitaxial growth
of metal(*) On leave from LPT, Facultd des Sciences, BP 1014, Rabat Morocco and
IMSP(UNB),
BP 613
P/Novo
Benin(**) Author for correspondence
(e-mail: levi@vaxgea,ge.infn.it)
© Les Editions de Physique 1996
874 JOURNAL DE PHYSIQUE I N°7
surfaces
ill].
In this paper, we reconsider someimportant
features ofcrystal growth
in two dimensions. We attempt a further extension of Gates and Westcott's work [6,7]by studying,
in d = I + I, asingle-
anddouble-step
model defined on a 45°-rotated square lattice wheresingle
and double steps are allowed on the
moving
"surface" (~).
Thestudy
is made easierby mapping
the interface
profile
onto a 14-vertex model. Netgrowth
orsteady
decrescence of thecrystal
is describedby
aKolmogorov
forward equation which we solvedexactly
for smallsamples.
The present model is notdynamically
reversible(see
Refs. [6,7]); however,
asteady
state does exist and thegrowth velocity
can becomputed exactly
for very small systems. The latterhelps
us to build a precise simulationprocedure
toinvestigate larger
systems. Our results show that someasymptotic
properties of the model canalready
be obtained onrelatively
small system sizes, e.g., N= 60. We find indications in the model for a
rough-to-rough
transition [12] where thegrowth
rate orvelocity
may besize-independent.
Our modeldepends
on a parameter n related to thespatial coupling
between two next-nearestneighbours.
We findthat,
forincreasing
n, the
growing
surface becomes smoother and we suspect that for n-cc anegligibly
smallgrowth velocity
will result. The latter appears to be consistent with the decrease of the time- exponentfl
[13] of the surface as a function of n. Wedefine,
at fixedgrowth
parameters,a
time-dependent
order parameterifi(t)
to report results about the stepdensity
fluctuationson the
growing
surface. Such parameter has been often used in theliterature,
e-g- tostudy
the
dynamics
ofstep-doubling
transitions [14]. We find that itsamplitude I(t)
is consistent with theanalytic
formproposed by Hoogers
andKing [lsj
in asimple
model introduced to interpret experiments on reaction kinetics. This order parameter has valuesindicating perfect layer growth
at low temperature andlarge driving
force onrelatively large
systems, whereas athigh
temperature, thedecay
of itsamplitude
expresses a continuous mode where thegrowing
surface exhibits ahill-and-valley
structure. Wegive
aqualitative growth phase diagram
forn = 3,
relying
on the Wilson-Frenkel [16] behaviour of thegrowth
rate in the continuous mode.We also
explore
the fundamental question of effective diffusion incrystal growth theory
wheregrowth
occursby
atomdeposition
andevaporation.
When an atom evaporates from asite,
andshortly afterwards,
in the next simulation step, another atom condenses in thevicinity
of this site, thiscoupled evaporation-deposition
process may be considered as an effective diffusion.We show
by
a statisticalanalysis
that it ispossible
to find a temperature domain where such effective diffusion follows an Arrhenius law when theevaporation
rate isproperly
chosen.In Section 2, we describe our stochastic model. Section 3
gives
its numerical solution(exact
on small
samples
andby
simulation onlarger systems).
Section 4 is devoted to results and discussion.2. The
Microscopic
ModelThe model is defined on a 45°-rotated square lattice formed
by
a stack of discs(Fig. I).
Weassume that the
growing crystal
is well-structured and thesolid-on-solid'(SOS)
condition isfulfilled.
Single
and double steps are allowed on thesurface;
therefore, the present model appears as an extension of thesingle
step model studiedexactly by
Gates and Westcott[6,7].
The essential feature of the model arises from the condition that the
height
difference between any two surface nearestneighbour
atoms can be either I or 3 in unit ofa/2,
where a is thelattice repeat distance. The numerical
analysis
of thegrowth
kinetics of modelsincluding higher
steps would beexpensive
incomputation
time. We find convenient toreplace
the stack of discsby
its upperedge profile
and we define the interface between thecrystal
and the fluidphase
as the lineconnecting
the centers of surface atoms of successive columns. Thus the(~) For short, in the following the model will be simply named the double-step model.
N°7 14 VERTICES IN
(1+1)D
GROWTH 875o~o
~
jojo~ ~o
o~o o~o~o o~o~o~o~o~o~
o~o~o~o~o~ o~o~o~o~o~o~
o~o~o~o~o~o o~o~o~o~o~o~o~
o~o~o~o~o~o~o~o~o~o~o~o~o~
Fig. I. Mapping of the surface of a two-dimensional crystal onto a 14-vertex model. Simple and double steps are present on the surface. The line connecting black discs represents the growing crystal edge profile which can be thought of
as a connection of
some 14-vertex lines.
(>2
9 >o11
f~/ ~
7 5 4
Fig. 2. The fourteen vertices used to map the crystal edge profile in Figure I. Vertices with small numbers are those shown in the figure. Vertices with big numbers are found by reversing all
arrows. At each vertex, the ice rule holds [17]. The line representation of these vertices is obtained
by replacing arrows pointing to the south-west or north-west by lines while others are deleted. In this representation, vertices 3, 4, 5 and 6 coincide with their usual line representation in the 6-vertex
model
[iii.
lateral "area" of a double step does not
belong
to the interface but to thecrystal
This line is identified to a line withcyclic boundary
conditions in aspecial
14-vertex model(Fig. 2).
Other non-used vertices of the same type are considered as
non-physical
in the model. This linemapping
establishes a one-to-onecorrespondence
between agiven
state of the system anda 14-vertex
configuration.
If Ah denotes the absolute value of theheight
difference between two surface next-nearest(NN) neighbours,
the energy ev of agiven
vertex v is defined as:e~ =
ji/2)e~jih)n
11)816 JOURNAL DE PHYSIQUE I N°7
where e has the dimension of an energy, ~ is a coefficient which introduces a difference between vertices
by depending
on the vertex"length" (in
the linerepresentation)
as follows:~ =
12)~/~l/2a.
12)Vertices 3,
4,
5 and 6 whichbelong
to the 6-vertex model(two-dimensional
version of the icemodel) II?]
have ~= l. Even if n
= I, the relation
(2)
does not favour double step formation at low temperature. In theremaining
of the article, ~depends
on unless otherwisespecified. Expression ii
describes thespatial coupling
between NNneighbours
whereas nearestneighbours
interact with infinite energy. n=
1/2
maycorrespond
to thestandard/Gaussian
SOS model. The energy e is defined as positive and assumed not to
depend
on the temperature.The relation
ii)
insures:ES " e6 " e7 = e8 = 0
(3)
Hence,
thecompletely
flatsurface, corrugated
on atomic scale with NNneighbours lying
in the samelayer
has zero energy. Theground
state of the system is twicedegenerated
with fourground configurations,
since relationii) gives
to the "reconstructed" surface(787878...)
and the non-reconstructed surface(565656...)
the same energy.However,
the surface(787878...)
has
larger
interface width and may evolve at low temperature to the structure(565656...).
The 14-vertex energy of aconfiguration
a isgiven by:
E
=
~j
N~e~(4)
J
where N~ is the number of vertex of type
j
in theconfiguration.
Possibleconfigurations
of a system of linear size N areparted
into time-conserved classes characterizedby
S:S=Ni+N3+2Nio+N12+2N13-(N2+N4+2Ng+Nii+2N14) (5)
related to the mean
slope
of the surface. A class will be named "active" if thecorresponding configurations
canchange according
to thegrowth
rules(see below), "passive"
otherwise.The case S
= o
implies
that the two ends of the interface haveheight
differenceequal
toa/2
or3a/2 (see Fig. I).
For N even, S E[-2N,
-2N + 2,.., 2N 2,2N],
whereas for N odd, S E[-2N
+1,-2N + 3,..,2N-1].
Theconfiguration
a and its mirrorimage (with
respect to an horizontalaxis)
-a,belong
toopposite
classes. Puregrowth
on acorresponds
to pure decrescence on -a, but both classes have the samesteady
state distributionprobability.
Accordingly,
the presentstudy
will be restricted to systems with linear size N > 3 and topositive
and activeclasses,
I.e, S Elo,..
,
2N 2] for N even and S E
[1,..
,
2N 3] for N odd.
N =1 and N
= 2 correspond to trivial cases.
Classes in the model are associated to surfaces with well-defined Miller indices.
They
arenaturally
divided into subclasses whoseconfigurations
differonly by translations;
e-g-, for N= 2, class
lo),
we have ns= 2
subclasses,
eachcontaining
twoconfigurations: (78, 87); (56, 65)
whereas for N= 4, ns
= 11 and for N
= 8, ns = 567. For N
= 7, class
(I),
ns= 187.
We find also
possible
to describe the interfaceusing
thefollowing procedure.
We label as in references[6,7],
unit steps of the interfaceby
az,Ii
= 1, 2,
.,
N)
from the left to theright
and set azequal
to1/3
if I is asingle /double
up step and azequal
toII
3 if I is asingle /double
down step.Therefore,
the surfaceconfiguration
ofFigure
I which is, in the 14-vertex formulation,a =
(8, 7,14,
6,13, lo,..,
II)
is
represented
as:? "
(+3,
-3, -1, +1,+3, +1,
-3, +1,..N°7 14 VERTICES IN 11 +
1)D
GROWTH 877C~~E
5 6 5,», -~
Cl
E~~
b)
~ ~ ~c
I)
E 6 5 6,; - c
I j
E~)
~~
d)
~~~Fig. 3. Example of two
depositionlevaporation
events on a flat surface(a,c)
and their correspon- dence in the 14-vertex formulation(b,d).
Vertex numbers correspond to those listed in Figure 2.The allowed surface
configurations
are such that two consecutive values of a~equal
to 3or -3 are
forbidden; otherwise,
the model would become atriple
step model and much moreN
complicated.
Thecyclic boundary
conditionsimpose
aN+i= ai. When
~j
az = o, we recover
z
our usual class
(o).
Dynamics
is introduced in the modelthrough deposition
and evaporation of atoms on the surface considered as Markov processes. Vertices8/6, 1/3, 2/4, 13/lo, 14/9, 6/5, 3/12, 4/11
and
5/7
show the presence ofgrowthlevaporation
sites. Condensation(C)
andevaporation (E)
at these sites
modify
the interface line on three sites which definegrowth
and evaporation kinksubconfigurations.
The different eventswhereby
atomsjoin
or leave thecrystal edge
areexpressed
in terms of transitions between these three-site kinks as follows:X A Y
ci jE
V B M
where
A/B
denotes thepreviously
enumerated vertices. At eachposition X,
Y, V, M, several vertices may lie. In the presentmodel,
we get loogrowth
kinks(X
AY)
and loo evaporation kinks(V
BM).
Asexamples
of theprevious
transitions, wegive
inFigure
3 two eventsleading
to an adatom creation
levaporation
on an assumedinitially
flat surface(5656...6).
If AE represents the
change
in the surface energyduring
thesetransformations,
there exist, for ~ = l and n = I, z transitions with AE= +2e, z transitions with AE
= -2e and 2z
transitions with AE
= o, where in this case, z = 25. In the
single
stepmodel,
the situation is rathersimple
with z= I, since
only
vertices 3, 4, 5 and 6 are needed to describe themoving
surface.An
important ingredient
of anymicroscopic growth
model is the definition ofdynamical
rules. We model theexchange
between thecrystal
and the fluidphase by
a non-conservedGlauber-type
kinetics [18]. The transition rates are considered in thefollowing
forms where a bias isapplied
in favour of thedeposition:
~a
~
~~PIA~/kT)
j~j
I +
exp(AE/kT)
878 JOURNAL DE PHYSIQUE I N°7
for
deposition
andj~a ~
j?)
I +
exp(AE/kT)
for
evaporation
of the kink of type(a),
where a can take loo differentvalues;
T is the temper- ature, k the Boltzmann factor andA~
thedriving
force. These ratessatisfy
forA~
= o the
detailed balance condition:
caja-a')
E~l-a- a')
~~~with respect to the 14-vertex energy at the temperature considered. When
A~
= o, the model describes
equilibrium
ofcrystal
andfluid,
whereas forA~
> 0, netgrowth
occurs.If we denote
by q(a; a')
a transition out of a and
q(a)
=
~jq(a; a'),
it appears that the~, relation
q(a)
=
q(-a)
relevant for thedynamic reversibility
of the model in the sense definedby
Whittle [19] does not hold for all a. Our results show that there may be no reasonablegeneral
condition for the model to be so. Suchdynamically
non-reversible model is noteasily
tractable
analytically. Therefore, finding
anexpression
for thegrowth
ratedepending
ongrowth
parameters at thethermodynamic
limit is not trivial. The above does not howeverimply
the non-existence of asteady
state for the system. We check that any initial distributionprobability tends,
when t-cc, to asteady
state distribution. The system isnormally
driven to statisticalstability
and this results from the stochastic nature of the transition rules. Themodel shows that for ~
= l and n
= I, the property:
~j C~(AE#o)
=
~j C~(AE
=
o) (9)
holds.
This relation is also valid in the
single
step model and coincides with one of Gates and West- cott's conditions for the existence of asteady
state distributionprobability
of the system [6,7].When e = o, all surface
configurations
areground configurations
and we recover a randomdeposition
model whereonly
the restriction on Ah could limit thecrystal growth.
This caseobviously
isequivalent,
whene#o,
to the infinite temperature limit of the model.3. Numerical Solutions of the Model
3.I. EXACT STEADY GROWTH RATE CALCULATIONS.
They
areonly possible
on verysmall
samples
since the number ofconfigurations
and subclasses increasesrapidly
with system size.In the
model,
theprobability
ofadding
orremoving
more than one disc in a small intervaltime dt is set to zero. Let us assume e-g- pure
deposition.
If P~it)
is theprobability
of a attime t,
q(a; a')
theprobability
of a transition out of a,g(t)
the unconditionedexpected
total number of discs at time t,given
a, then [6]:glt
+dt)
=
glt)+
<qla)
>t dt.(lo)
The
expected growth
rateG(t)
per surface site is:Glt)
"N~~(glt)
"N~~
<ql?)
>tIll)
N°7 14 VERTICES IN (1+1)D GROWTH 879
In the I4-vertex
model, G(t)
has theexpression:
G(t)
=N~~ ~j C~p[Pm(t) (12)
where
p[
is themultiplicity
of the kink of type(a)
in the m~~ subclass Sm whoseweight
Pmit)
is defined
by:
Pmlt)
=
~j P«lt). l13)
Pm
it)
is obtainedby solving
theKolmogorov
forwardequation:
d
(i~~
=~
L~~,ji~, T, e)p~, it) j14)
where Lmm, =
£~ C~(M(~, p[6mm>)
denotes the elements of the transition matrix L of surfaceconfiguration
between subclasses(M(~, being
the number of ways aconfiguration
ofsubclass m'
can
change
to aconfiguration
of subclass m via processestaking
place at a kink of type(a)).
Thesteady
state solutions are used to compute thesteady growth
rate on whichwe will
mostly
focus in thefollowing.
3.2. MONTE CARLO SIMULATION The simulation avoids the difficult
problem
of subclassclassification. It is based on the
ergodicity
of the model within a class and makes thestudy
ofrelatively large
systemspossible
and even easy. Theroughness
of thegrowing
surface in the presence ofdeposition
andevaporation
processes may be studiedusing
thefollowing algorithm.
All active
subconfigurations
arelisted, together
with theircoordinates;
then the total evolutionprobability
of the surface iscomputed:
Qla)
=£IC~P$
+E~q$) lis)
a
Let r =
£~ C~p$ /Q(a)
denote the total condensationprobability.
At each simulation step,r must be
compared
to a random number rouniformly
distributed over the interval[o,I].
If r > ro, condensation is
tried;
otherwise, evaporation is chosen. Theattempted
move isaccepted
withprobability:
pmc " uJ
/Q(a) (16)
where uJ is
equal
to C~/E~
forcondensationlevaporation
on the kink of type(a).
Concerning
thegrowth
kinetics, sites where inprinciple
bothdeposition
andevaporation
events are
possible
are treated as puregrowth
sites. Such avoided evaporation sites are morestrongly
linked to theirneighbours
than those considered. Westudy essentially
the kinetics underdeposition
and evaporation in this restricted butphysical
case. For thisstudy,
the abovealgorithm
needs some modifications beforeyielding
precise results. One activesubconfiguration
must be selected among those listed and its evolution
accepted according
to the Monte Carloweights
inexpression (16).
The meangrowth
rate per surface site of agiven
active class after K simulations steps is defined as:K
G =
N~~t~~ ~j(2r 1) (17)
~=i
880 JOURNAL DE PHYSIQUE~I N°7
7000
6000
sooo
4000
S=12
3000 S=2
2000
N " 8
IOOO ~ ~/
/
~~= j oS=O
~
0.5 1.5 2 2.5 3 3.5 4 4.5 5
Temperature (kT/E)
Fig. 4. Dependence of the exact growth rate of a system of linear size N
= 8 on the mean slope
6 of vicinal surfaces (see text) and temperature. The supersaturation is kept constant:
Ap/kT
= 10
and we use
~y = I and n =1.
where t is the total real simulation time defined
by:
t =
f I/Qla) l18)
The number K needed to reach the
steady
state increases withincreasing
system size anddecreasing
values of thesupersaturation.
4. Results and Discussions
4.I. CASE r
= I. The results
reported
in this section are obtained infar-from-equilibrium
conditions where atom
desorption
from the surface isneglected.
We aremostly
interested in sometime-dependent
quantities which could characterize thegrowing
surfacemorphology (roughness,
stepdensity fluctuations)
and which areexperimentally
measurabletogether
with the averagevelocity
of the interface between the twophases, commonly
calledgrowth
rate.Steady
decrescence andtemperature-programmed multilayer desorption
could be studiedusing
the same
procedure.
Surfaces with odd size arenecessarily sloped
surfaces and we do not consider themexplicitly
in ourstudy.
In
Figure
4, wegive
exact results(by solving
the masterequation)
on thedependence
of thegrowth
rate forinitially
flat andsloped
surfaces with linear size N= 8 at constant
deposition
rate. The
growth
rate decreases with the macroscopic inclination b(tan
b=
SIN)
of vicinal surfaces athigh
temperature, a consequence of the decrease of the number of active sites withincreasing
b. At low temperature,preexisting
steps onsloped
surfaces inducehigher growth
rate than on a flat one. In this case, the
growth proceeds layer-by-layer
on vicinal surfacesby
steppropagation
as inspiral growth
[20]. This mode isdestroyed
athigh
temperatureby
N°7 14 VERTICES IN
(1+1)D
GROWTH 88140
16
35 14 ~"8, C(CSS
(0)
12
30 lo
a
25 6
Rate 4
20 2
~
~
2 2.22.42.62.8 3 3.23.43.63.8
4~
~
*
lo , ~
*
~ N = 600
e '
~ ~$i-a,,~~
.
~ ~
~ ~ *
~
l 1.5 2 2.5 3 3.5 4 4.5 5
Disequilibrium Aq/kT
Fig. 5. The simulated growth rate m. supersaturation at different temperatures. The inset curve
compares simulation results
(open circles)
and exact calculations(lines)
for a system of linear sizeN = 8, class (0) at four temperatures: T
=
2.5e/k,
T=
1.5e/k,
T=
elk
and T=
0.5e/k
from the top to the bottom. Calculations are performed for~y = I and n
= 1.
nucleation events on terraces. Surfaces with no terraces
(S
= 14;
12)
may then showessentially
lateral
growth
at constantvelocity.
The above results are consistent with those foundby Krug
andSpohn
[12] from the behaviour of thegrowth velocity
as a function of the localgradient
T7h of the surface. For b small, the
following
relationapproximately
holds for a system of linear size N:G(b, N)
=
G(b
= 0,
N)
+ ~tb~(19)
It has been
suggested
[4] that the temperature where p vanishes andchanges sign
maycorrespond
to arough-to-rough (RR)
transition temperature where a suddendrop
of theearly-
time
scaling
exponent fl(defined below)
of the surface isexpected.
Inmicroscopic growth
models, the effects of achange
ofphysical
parameters on thegrowth velocity provides
the bestunderstanding
of thegrowth
mechanisms of real materials.Figure
5(inset curve), displays
the dependence of thegrowth
rate onsupersaturation
at different temperatures. Simulation resultsperfectly
agree with exact calculations up to severaldigits.
Suchprecise
results areexpected
since the simulation
procedure
relies on the basic ideas of the kinetic Monte Carlomethod;
therefore it may
obviously provide
ahigh-accuracy
solution of the masterequation (14).
The mainfigure gives
simulation results for N= 600, class
(o).
At low temperature and smalldriving force,
thegrowth
rate Gnearly
behaves as:G
+~
bA~/kT (20)
where the coefficient b, which
plays
the role ofmobility (corresponding
to the kinetic coefficient forA~/kT
-o),
increases withincreasing
temperature and saturates around T +~1.5e/k.
WhenT-o,
other results indicate that b tendscontinuously
to o without anynon-linear nucleation
behaviour,
in agreement with the zeroroughening
temperature of the one-dimensional substrate. Withincreasing
temperature, thegrowth
raterapidly
saturates and882 JOURNAL DE PHYSIQUE I N°7
BOOO
7000
h'9h
T11
6000
~'~~ ~ ~
0,12 ~
4000
o.oa 3000
~~~~ Q ~'~~ 5 lo 15 20 25 30
Q ~
AH/kT
~~~~
low T ~
o
Fig. 6. Dependence of the simulated growth rate on system size at low temperature
(T
=
0.5e/k)
and high temperature
(T
=
4e/k)
forAp/kT
= 10. The high-temperature growth rates are given in arbitrary units. Inset: behaviour of the coefficient K
m. the supersaturation at T
=
4e/k;
C=
exp(Ap/kT).
Calculations were performed for~y = I and n
= 1.
depends exponentially
on thesupersaturation
atlarge A~, following
the Wilson-Frenkel [16]law: G
+~
exp(A~/kT)
I. In order to getplausible
estimates of the infinite-sizelimits,
weexplore
finite-size effects in our calculations.Figure
6displays
thedependence
of thegrowth
rate on system size at low and
high
temperature under a constant andlarge supersaturation
of the fluidphase.
The results ensure that these effects are rather weak for N > 60 at any super-saturation. One can describe the fast convergence of the
steady growth
rate to itsasymptotic
valueby
thescaling
form [21]:G(N)
=G(cc)
+KIN" (21)
where K and uJ depend on the
growth
parameters. For N > 60, the curves areapproximately
linear and uJ+~ I as in the
single
step model [21]. For small sizesand/or
low temperature,important
deviations from thescaling
relation(21)
are obtained due tohigher
order terms in IIN.
The linearregion
increases with thesupersaturation.
A carefulanalysis
of the resultsreveals that there is a critical temperature To at which K vanishes and
changes sign;
atTo,
thegrowth
rate is almostsize-independent.
Such result indicates a possible RR transition[4,6,12,21].
A best estimation of To should be obtained atlarge deposition
rate. In the inset of thefigure,
we show the isothermal behaviour of the coefficient K with the supersaturation;it emerges that Ii is an
increasing
function of thedeposition
rate and no RR transition isexpected.
Wetherefore,
argue that in the(A~/T,T) plan,
the RR transition line may benearly straight
and normal to the T-axis.Another
interesting
result concerns the difference ingrowth speed
between thesingle
step and the double step models that wedisplay
inFigure
7. At lowdeposition
rate andhigh
temperature, thegrowth
rates arepractically
the same, a consequence of anearly
identical behaviour of all surface activesubconfigurations. Hence,
thesingle
and double step models have the sameasymptotic growth
rate per active site: thecorresponding
formula isgiven by
the relation
(3.18)
of reference [7]. At low temperature, most convex activesubconfigurations,
N°7 14 VERTICES IN
(1+1)D
GROWTH 883i~oo N =64
n=1
1200
iooo
4.5
800 4
* 3.5
* 3
600
~
2.5 2
400 1.5
o.5
200 °
O.5 1.5 2 2.5 3
tem~erat/re (k)le)
~ ~Fig. 7. Comparison between simulation growth rates per active site for the single
(lines)
and double(stars
orcircles)
step models for a system of linear size N = 64, class (0) at large supersaturationAp/kT
= 20
(main figure)
and low supersaturationA~/kT
= 3.5
(inset curves).
absent in the
single
stepmodel,
are less active than the concave ones since their evolution is notenergetically favoured; accordingly,
most of them arerejected during
the simulations. Suchsituation
obviously
leads toslightly
lowergrowth
rate per active site than in thesingle
step model. The double step nature appears atlarge deposition
rate andhigh
temperature. There, the double ortriple probability
of some sites to increasesuccessively
theirheights,
influences thegrowth speed
which becomeslarger.
We havechecked, using
the relation(21)
and theasymptotic growth
rate of Gates [7], that the latter feature remains valid in thethermodynamic
limit. It exists a well defined temperature
(main figure)
at which the two models arestrictly
identicalkinetically.
This temperatureslowly
increases with thedeposition
rate.Below,
thegrowing
surface in thesingle
step model appearsrougher
than in the double step model since alower
growth
ratecorresponds
to lesspotential
kink sites on the surface. The situation remainedunchanged
forincreasing
n as shown inFigure
8. Our results reveal that for any n, there is a temperature domain where almost nogrowth
occurs at smalldriving
force. We found that the width of thisregion
increases with n whereas it decreases forincreasing A~.
The latter feature has been also observed in d= 2 +1 [4] where a real metastable state exists. A
sloped
surface in thisregion
may however grow fast andcontinuously
whereas aninitially rough
surface willshow
extremely
slowgrowth
once becomecompletely
flat. In d= 2 +1 or
higher dimensions,
fractal or dendriticgrowth
may occur if the nucleation barrier isartificially
overcome. The trivial randomdeposition
modelcorresponds
to e= o. There is no correlation between surface sites and
particles
are launched atrandomly
selected positions above thedeposit.
Thefigure
shows that at low temperature, this model
yields
veryrough
surfaces.The
growth
rate at constantdriving
forceA~
andvarying
temperature shows the Wilson- Frenkel [16] behaviour above a well defined temperature. The latter is often considered ina crude
approximation
as a transition point from thelayer growth
to the continuous one.Although
this criterion isquestionable,
we use it todisplay
aqualitative growth phase diagram
884 JOURNAL DE PHYSIQUE I N°7
o.6
~~ random
deposition
A/£/c=0.5
O.4 sing
~~~ ~
n =
O.3
O.2
n=
oi
~
0 0.5 1.5 2 2.5 3
temperature (kTle)
Fig. 8. Comparison between simulation results on the growth rate defined per active site for different models. The random deposition model is obtained by taking e = 0.
a
7
6
(~ continuous
~
~4
~
N=64 2
n=3
layer-by- layer
o
~ ~ ~ ~ ~ ~~
temperature (kTle)
Fig. 9. Growth phase diagram of a system of linear size N
= 64, class (0) obtained by taking as
transition point to the continuous mode, the temperature which gives the maximum growth rate at fixed driving force.
in
Figure
9.Sufficiently
below the transitionline, layer growth
occursby
birth,spread
and coalescence of lD islands orby
the one-cluster mode. Wellabove,
thecrystal
growscontinuously
without any nucleation barrier. As discussed in reference [4], the one-cluster mode is
expected
to
disappear
withincreasing
temperature,driving
force or system size. The one-cluster modeprevails
when the time between two consecutive nucleation events(adatoms
formation on theterrace)
islarger
than onemonolayer completion
time tby
extension from the first nucleus [22].N°7 14 VERTICES IN
(1+1)D
GROWTH 885A
simple
calculationusing
~= l and the relations
(1), (6), (17)
and(18),
shows that at low temperature(double
steps are notrelevant)
andrelatively large driving force,
thegrowth
rate per site behaves asN~~t~~,
I-e-:~ '~
N(N ~l~~i(~e/kT))'
~~~~One can
easily
check that G isapproximately proportional
to the nucleation rate, I-e-, to the rate of fixation of new adatoms on a flat surface:exp(A~/kT)/(I
+exp(2"e/kT)).
Suchproportionality however,
to ourknowledge,
has never been provenexperimentally,
except inelectrocrystallization
[23]. This modeusually
exhibitsundamped
oscillations of the interface width W withgrowth
time.To get more
insight
into thegrowth
modes androughness
of themoving
surface, we definean order parameter
ifi(t)
to monitor stepdensity
fluctuations on thegrowing
surface:ifi(t)
=~J ~~P(llrh~ (t))
~
(2~)
where h~
(t)
is asingle-valued
function which denotes the surfaceheight
at substrate coordinatej.
A similar order parameter has been considered in the literature to map thedynamics
ofstep-doubling
transitions [14]. Let us denoteby ((t)
thequantity
I(ifi(~(t),
andby I(t)
the
amplitude
of (ifi(~(t). From an assumed initialheights configuration (I,o,
I,o,..,o)
of thesurface,
one finds(~l(~(t)
= o. To avoid suchsituation,
we consider that all the flat surfacesites have the same initial
height.
Thisassumption
does not, of course, affect thephysics
ofour results. The behaviour of
((t)
isdisplayed
inFigure
lo for different temperatures. WhenI(t)
= I, lateralgrowth prevails
and the surface evolves whileremaining
flat(pure
one-cluster mode onaverage)
and thishappens
in thefigure
for T=
o.3e/k.
Alayer
is finished to be formed before a new one is started on it. Theprobability
that a second nucleation occurs in thegrowing layer
or above thegrowing
island is of the same order asA(t)
= I
I(t).
WhenI(t)
isjust
constant after one or twoperiods
of oscillation of((t),
thegrowth
islocally perfect
and takesplace
in a very fewlayers.
A constant increase ofA(t)
may indicate aprecontinuous
mode where thegrowth
is neithercompletely
continuous norlayer-by-layer.
At veryhigh
temperature, no oscillation is observed for
((t)
and thegrowth
mode is continuous, even in theearly-stage
of thegrowth.
Theamplitude
ofA(t)
is well fittedby
the functional form [15]:x(t)
=x(~x~) 1 j
~~ ~~
(24)
where
X(cc)
= 0.90 and to is fitted to 8 MCS at T
=
e/k.
In our calculations, to is approxi-mately
the time for((t)
to reach the valueo.5,
which seems not to have aparticular physical meaning. Although
the oscillationperiods approximately
coincide in Monte Carlo time at all temperatures iii thelayer
orquasi-layer mode, they strongly
differ in real time which of coursedepends
onphysical
parameters. We alsoanalyze
the influence of n on((t)
at fixed temper-ature. We find for
n = 1, 2,3 a fast
damping
of the oscillations. However, it turns out thatincreasing
n makes the surface smoother; which results are consistent with thosereported
inFigures
8 and 9. A furtherinvestigation
of the surfacemorphology
isperformed by studying
the behaviour of the interface width
Wit)
definedby:
W~(t)
=