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HAL Id: jpa-00209768

https://hal.archives-ouvertes.fr/jpa-00209768

Submitted on 1 Jan 1984

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Diffusion limited aggregation with directed and anisotropic diffusion

R. Jullien, M. Kolb, R. Botet

To cite this version:

R. Jullien, M. Kolb, R. Botet. Diffusion limited aggregation with directed and anisotropic diffusion.

Journal de Physique, 1984, 45 (3), pp.395-399. �10.1051/jphys:01984004503039500�. �jpa-00209768�

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Diffusion limited aggregation with directed and anisotropic diffusion

R. Jullien, M. Kolb and R. Botet

Laboratoire de Physique des Solides, Université Paris-Sud, Centre d’Orsay, 91405 Orsay, France

(Reçu le 20 septembre 1983, accepté le 14 novembre 1983)

Résumé.

2014

On étudie des agrégats à structure fractale obtenus à partir d’un processus de croissance par diffusion limitée. On présente des simulations numériques bidimensionnelles faites dans le cas où un agrégat pousse sur une

ligne de base. Pour une diffusion isotrope, ce modèle se comporte comme le modèle de croissance sphérique de

Witten et Sander. On trouve qu’une diffusion directionnelle rend l’agrégat compact alors qu’une diffusion ani- sotrope semble conduire à un exposant fractal variant continûment.

Abstract.

2014

Fractal aggregates obtained from diffusion limited growth processes are studied. Numerical simula- tions are reported for a two-dimensional cluster growing on a basal line. For isotropic diffusion this model behaves

as the spherically growing model of Witten and Sander. It is found that directed diffusion renders the cluster compact while anisotropic diffusion apparently yields a continuously varying fractal dimension.

Classification Physics Abstracts

68.70

-

05.40

-

82.70R

1. Introduction.

The formation of clusters by aggregation of particles

is a quite general phenomenon occurring in many scientific areas such as physics (dendritic growth), chemistry (flocculation of colloids, formation of gels, polymerization), medicine (growth of tumors) etc...

In most cases the resulting clusters have interesting

« fractal » structures [1]. The irreversible character of the phenomenon yields peculiar scaling properties

which are probably different from those of equilibrium

systems currently encountered in statistical physics.

Many theoretical models have been developed to reproduce the main features of the experiments. In the

Eden model [2] the extra particle is added with equal probability on any neighbouring site of the cluster’s surface. The resulting cluster is always compact, i.e.

its fractal dimension is equal to the usual Euclidian dimension. This model has been invoked to describe the growth of tumors. In the diffusion limited aggrega- tion (DLA) model of Witten and Sander [3] single particles stick one by one on an immobile growing

cluster after diffusing in a purely random walk fashion.

The resulting cluster has a characteristic fractal dimension smaller than the Euclidian dimension.

Recently, it has been proposed that it can describe

two fluid displacements in porous media [4]. In the

« clustering of cluster » model of Kolb et al. [5] and

Meakin [6], clusters of particles as well as single particles are allowed to diffuse together and any kind

of clusters stick on contact. The resulting clusters are

much more stringy than in DLA and their fractal dimension is smaller. This model seems better adapted

to describe flocculation and gelation. In the last two

models the diffusion process is assumed to be always purely isotropic. Such hypothesis is clearly unphysical

and in most cases, the diffusive motion of a given particle, or cluster, is certainly influenced by the

presence of the other clusters. This effect is complex

in the clustering of cluster model. On the contrary in the DLA model the study can be done in a,simple way since there is only one diffusive particle in presence of

one dendrite. The aim of this paper is to study the effect

of directed and anisotropic diffusion for the single particle in the DLA model. By directed diffusion we mean that the particle has more probability to go in a

given direction, for example the direction of the cluster. By anisotropic diffusion we mean that the probability of moving along one axis is greater than

along the perpendicular axis; however the probabi-

lities to move in one direction and the opposite are rigorously equal on each axis. This study has been performed on a new version of the DLA model which considers a different geometry. Here, the cluster grows

on a surface instead from a single seed particle. After introducing the model (part II) we show that it gives

the same results as the Witten and Sander model in two dimensions in the case of isotropic diffusion (part III). Then we study the cases of directed and

anisotropic diffusion (part IV).

Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:01984004503039500

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396

2. A new version of the DLA model.

In the original DLA model as studied by Witten and

Sander [3] and Meakin [7] the dendritic cluster grows

spherically around an initial seed particle. Later, Meakin [8] (see also Racz and Vicsek [9]) studied the

growth of dendrites by DLA on fibres and surfaces but with the limitation that the thickness of the deposit is

much smaller than the width of the substrate, in order

to avoid significant influence of the boundary condi-

tions. On the contrary, in our model, the dendrites grow from a basal plane, as tregs on the ground, but

with a height much greater than the width of the plane,

to recover the same feature as in the Witten and Sander’s case, as explained below. Our numerical simulations are restricted to two dimensions. We consider a regular square lattice, the lattice constant

being considered as the unit of length. The basal plane on which the dendrites grow is here a line of

ordinate y

=

0. Practically, this line is finite and contains L lattice constants. Then the added particle

moves on a semi-infinite ribbon of width L with

periodic boundary conditions in the x-direction (i.e.

x

=

L is equivalent to x

=

0). At each step of the iterative growth process a single particle is released

on a site chosen at random among the L different sites of a row at ordinate y

=

yo far above the cluster.

(Practically it is enough to choose yo

=

ym + 1 where yM is the maximum ordinate of the cluster.)

Then the particle undergoes a random walk on the lattice until it reaches an unoccupied site adjacent to

a site of the cluster and becomes part of the cluster

(see Fig. 1). (By definition we consider as the cluster

or the dendrite the base line and all the particles sticking to it.) As in the Witten and Sander model the particle is lost if it goes too far away from the cluster (practically y > 5 yM is enough). After the particle sticks to the cluster a new particle is released

Fig. 1.

-

Sketch of the growth process.

and the process is repeated. In order to include the different possibilities of directed and anisotropic

diffusion we label differently the probability of jump- ing in the different directions. p is the probability to jump to a neighbouring site just below the original one.

q is the probability to jump to the right or to the left.

Then the probability to jump to a neighbouring site

above is 1

-

p - 2 q. The case of isotropic diffusion corresponds to p = q

=

1/4. We call directed diffu- sion the case when p > 1 - p - 2 q, i.e. p + q > 1/2

when the particle jumps preferentially in-the direction of the cluster. We call anisotropic diffusion the case

when p = 1 - p - 2 q i.e. p + q = 1/2 but p is

generally different than 1/4. In that case one axis is preferred but the probabilities to jump to one direction

or the opposite on each axis are the same. To determine

the speed of growth of the cluster quantitatively,

one can follow its maximum height yM or, alternatively,

its effective height ym defined by :

where the summation covers all the N occupied sites.

In the usual geometry (cluster growing from a seed particle), one has

where N ws is the number of particles in the Witten and Sander’s cluster of radius RWS and of fractal dimension D. Now if we consider the volume R r R + ym and a 0 a + Aa where yM R and Aa 1, the number of particles N in this volume is :

Fig. 2.

-

Definition of the jumping probabilities (a) and

sketch of the two cases of directed (b) and anisotropic (c)

diffusion.

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In terms of the width L - R ea of the basal plane,

one gets :

Thus, when a steady state is reached, N becomes proportional to yM, and defining A(L)

=

N/ym, one

has for given Aa 1 (1/Aoc is a measure of the curva-

ture of the basal plane) :

Thus in the spirit of finite size scaling methods one

can evaluate A(L) for different successive widths L and extract D from a log-log plot of A(L) versus L

for large L.

Of course, it is also possible to evaluate D from the particle-particle correlation function [3, 7] given by :

where the density function p(r), defined on each lattice

site, is equal to one if the site is occupied, zero if not.

In practice, we have calculated C(r) along the x and y-directions. It is known that in a fractal structure

C(r) must behave as

This is obviously valid only for r L.

3. Results in the case of isotropic diffusion.

In order to determine D precisely we have estimated the coefficient A(L) by waiting until ym reaches 20 L and by averaging over twenty samples. Figure 3

shows the top of a typical cluster obtained by this

method for L

=

48. The quantitative results as a plot

of log A versus log L for L

=

3, 6, 12, 24, 48 are given

in figure 4. The error bars have been estimated from the calculated standard deviation of the results. The dashed and full curves correspond respectively to ym and ym. From the asymptotic slope of both curves

one can estimate :

This result is very similar to Witten and Sander [3]

and Meakin [7]. One can conclude, as expected, that

the geometry (a seed or a basal plane) does not change

the fractal dimension of the structure.

In figure 5 one gives the results for the correlation functions Cx and Cy for L

=

12, 24, 48. Cx and Cy are quantitatively different, since considering a finite length L in the x-direction artificially introduces an

anisotropy. However, when L -> oo the difference

disappears gradually. Moreover, log Cx goes through

a maximum at r

=

L/2 as expected from the periodic boundary conditions. The scaling regime is better

defined for Cy where log Cy shows a quite linear

behaviour as a function of log r up to r > L where it reaches a constant value. In order to estimate the

Fig. 3.

-

The top ten rows of a typical cluster of total

height yM

=

20 L where L

=

48 is the width of the strip,

obtained in the case of isotropic diffusion p = q

=

0.25.

Fig. 4.

-

Plot of log A (L) versus log L in the isotropic case.

The continuous and dashed lines correspond to the case

where A(L) is calculated from the effective height and the

maximum height, respectively. For comparison the slope

0.66 is indicated.

exponent a

=

d - D one must extrapolate the slopes

to the infinite L limit. This is done in figure 6 where

we report the slopes estimated from log Cx and log Cy

as a function of 1/L. The slopes extrapolate quite well

to the common value :

which gives :

a value consistent with, but less precise, than the value

extracted from figure 4.

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398

Fig. 5.

-

The correlation function in the isotropic case : log C(r) is plotted versus log r for L

=

12, 24, 48. The

continuous and dashed lines correspond to the y and x directions, respectively.

4. Results in the case of directed and anisotropic dif-

fusion.

We have learned from the preceding sections that the finite size results from log A versus log L give a better

estimate of D than the correlation function. Therefore

we will only report the results for log A versus log L

in the case of directed and anisotropic diffusion.

Let us first discuss the case of directed diffusion.

We have studied the case where the probability to

diffuse to the bottom is larger than the others. A typical example obtained for q

=

0.25, p

=

0.3 (L

=

48) is

shown on figure 7. When comparing this figure with figure 3, it is really difficult to appreciate the differences.

However, when looking at the quantitative results,

the conclusion is clear. In figure 8, we report the log A

versus log L plot in the cases q

=

0.25 and p

=

0.3, 0.4.

One can see that, after a finite L crossover, the asymp- totic slopes become equal to one for all p values different from 0.25. For p

=

0.3, the crossover bet-

ween the isotropic regime and the directed regime

occurs around L - 12 while for p

=

0.4, the directed

regime is already reached for L - 6. From these results

one concludes that directed diffusion always yields a

compact structure, i.e. a structure in which D

=

d.

This is confirmed by calculations done for other p values and not reported here : even if the directional character of the diffusion is small, the resulting cluster

is always compact if we look at sufficiently large scale.

This is very similar to the conclusion of a recent work

by Meakin [10] who studied the effect of particle

drift in the original DLA model. Even if the geometry

Fig. 6.

-

The slopes extracted from the log-log plot of the

correlation functions as a function of 1/L. The large error

bars for the correlations in the x-directions are due to the

difficulty in defining the scaling regime in that case.

Fig. 7.

-

The top ten rows of a typical cluster of total height

yM

=

20 L, where L

=

48 is the width of the strip, obtained

in the case of directed diffusion with p

=

0.3, q

=

0.25.

Fig. 8.

-

Plot of log A(L) versus log L in the case of directed diffusion with q

=

0.25 and two values of p, p = 0.3 and p

=

0.4. The case p = q

=

0.25 is shown on the same figure

and the slopes 0.66 and 1 are indicated.

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is completely different, there is also a crossover from

a fractal structure on short length scales to a uniform

structure (D

=

d ) on longer length scales. One can

conclude very generally, using the renormalization group language, that the DLA is unstable with respect

to any directional perturbation.

The case of anisotropic diffusion appears to be much

more tricky. We have not reported the figure of a typical cluster in that case because it always looks like figure 3. In figure 9 we plot log A versus log L in the

case p + q

=

0.5 and p

=

0.1, 0.2, 0.3, 0.4. Instead of a clear crossover as in figure 8, we observe here a

slow continuous variation. The results for D, with

error bars, estimated from the asymptotic slopes are I reported in figure 10. D varies smoothly with p. There i

are three special cases : for p - 0.5 the horizontal

motion is practically suppressed and the cluster becomes compact. For p - 0, on the contrary, the diffusive particle moves primarily horizontally and prefers to stick to the top of a cluster so that we must

recover D

=

1. Finally for p

=

0.25, the previously

studied isotropic case is recovered. Figure 10 strongly suggests a continuously varying exponent (like a line

of fixed points in the renormalization group language)

but we cannot really exclude a constant exponent with finite size crossover effects to the different limiting

cases p

=

0 and p

=

0.5. (This could be due to syste- matic errors due to size effects different from the statistical errors reported in the figure.)

5. Conclusion.

This work presents a new version of the DLA model in which the cluster grows on a surface. We have shown that in two dimensions this model behaves as ’ the original DLA model. Then we have studied the i influence of modifications in the diffusion process.

We have shown that directed diffusion has a dramatic effect on the fractal properties yielding a compact cluster, while anisotropic diffusion apparently changes i

the fractal dimension continuously though we cannot

exclude a jump of the exponent D. It would be really

Fig. 9.

-

Plot of log A(L) versus log L in the case of ani- sotropic diffusion with p + q

=

0.5 and for the following

values of p : p = 0.1, 0.2, 0.3, 0.4.

Fig. 10.

-

Plot of the estimated extrapolated fractal expo- nant D as a function of p in the case of anisotropic diffusion.

interesting to extend such kind of study to the case of

the clustering of clusters models [5, 6] and try, also,

to include more realistic interactions between clusters.

This will be the subject of future work.

References

[1] MANDELBROT, B. M., The fractal geometry of nature (Freeman) 1982.

[2] EDEN, M., Proc. Fourth Berkeley Symp. Math. Stat.

and Prob., J. Neyman (ed.) vol. 4, p. 233 (U.C.

Press) 1961.

[3] WITTEN Jr., T. A. and SANDER, L. M., Phys. Rev. Lett.

47 (1981) 1400.

[4] PATERSON, L., preprint.

[5] KOLB, M., BOTET, R. and JULLIEN, R., Phys. Rev.

Lett. 51 (1983) 1123.

[6] MEAKIN, P., Phys. Rev. Lett. 51 (1983) 1119.

[7] MEAKIN, P., Phys. Rev. A 27 (1983) 604.

[8] MEAKIN, P., Phys. Rev. A 27 (1983) 2616.

[9] RACZ, Z. and VICSEK, T., preprint.

[10] MEAKIN, P., preprint.

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