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Finite fractal diffusion-limited aggregates

M. Arturo López-Quintela, M. Carmen Buján-Núñez

To cite this version:

M. Arturo López-Quintela, M. Carmen Buján-Núñez. Finite fractal diffusion-limited aggregates. Jour-

nal de Physique I, EDP Sciences, 1991, 1 (9), pp.1251-1261. �10.1051/jp1:1991204�. �jpa-00246409�

(2)

Classification

Physics

Abstracts 05.40 68.70

Finite fractal diffusion-limited aggregates

M. Arturo

L6pez-Quintela

and M. Carmen

Bujhn-Nfiiiez

Biodynamical Physics Group, Department

of

Physical Chemistry, University

of

Santiago

de

Compostela,

E-15706

Santiago

de

Compostela, Spain (Received

9

July

1990,

accepted

in

final form

6

May 1991)

Abstract. Particle-cluster

aggregation

has been studied

by

computer simulation. It has been observed that the fractal dimension of a diffusion-limited aggregate is

only

constant when the number N of its

elementary

units is

sufficiently

large. For small N, the fractal dimension is a function of N. The concept of a differential fractal dimension

D(N)

=

-d[logn(e/ro,N)]/

d[log (e/ro)]

allows the deviation from ideal behaviour to be

quantified

and

interpreted.

Introduction of

D(N)

in the

scattering

equations allows characterization of the deviation from

linearity

of

plots

of

log

I

against log

q, where I is the

scattering intensity

and q the

amplitude

vector.

1. Inboducfion.

The formation of

large

structures from small units is a common process of

importance

in many scientific and

technological

fields. The

discovery

that most of such structures can be described in terms of fractal

geometry [I]

has in recent years stimulated

growing

interest in these kinds

of systems. One

aspect

of this interest is the

development

of new

techniques

for research on the

growth

of these structures. In

particular,

computer simulation methods for

studying

both structural and kinetic issues have received much attention. The use of

extremely

idealized models for simulation purposes

brings

out features of fractal processes that may be obscured in real

physical examples,

and so

help develop

intuitive

understanding

of more

complex

systems

and,

in many cases,

provide

a framework for

relating apparently

unconnected processes.

The first

computer

model of an

aggregation

process was

developed by

Witten and Sander

[2,

3] in an attempt to

explain

Forrest and Witten's

[4] experimental finding

that small metal

particles suspended

in a dense gas clustered into fractal structures. In the Witten-Sander

algorithm, particles

are added to the cluster one

by

one

along

random

trajectories

to

produce

fractal structures.

Though

many

non-equilibrium

processes are not

explained by

this model

(including

the Forrest-Witten

phenomenon),

there are many for which it does

provide

the

key

to

understanding, including

fluid-fluid

displacement

in Hele-Shaw cells

[5-7]

and porous media

[8, 9],

the breakdown of dielectrics

[10], electrodeposition [11-14],

random dendritic

growths [15-18],

the dissolution of porous media

[19, 20]

and the

growth

of

biological

(3)

structures

[21]. Subsequent computer

models have either

involved,

like the Witten-Sander

algorithm,

the addition of

particles

one

by

one to clusters

[2, 3, 22-24],

or have allowed the

aggregation

of

multi-particle

clusters to each other

[25, 26]

as in the

experimental

observations of Forrest and Witten.

In this article we discuss the

particle-cluster aggregation

process

by

means of a simulation program based on Ermak and Mccammon's Brownian

Dynamics algorithm [27].

In section 2

we describe the simulation

procedure,

in section 3 we use the

concept

of differential fractal dimension

(DFD)

to characterize the

dependence

of the fractal dimension of our

aggregates

on scale when the number of units is

small,

and in section 4 we examine the influence of the DFD on the structure factors of

aggregates

with small numbers of units the introduction of the DFD in the

scattering equations explains

a curvature in

log

I vs.

log

q

plots

that is unrelated to the

non-linearity corresponding

to upper and lower cut-off

points.

Final conclusions are drawn in section 5.

2. Simulation

proceJlure.

The

aggregation

model used is a version of Witten and Sander's

particle-cluster

mechanism

[2, 3],

the

general plan

of which is as follows. The space in which the process occurs consists of

an inner zone bounded

by

a

sphere

B of radius r~ and an outer zone bounded

extemally by

a concentric

sphere Q

of radius

r~.

At the

beginning

of the simulation there is a

single particle

located at the centre of the

spheres,

and simulation

proceeds by releasing particles

one

by

one

from random

positions

on

B,

whence

they

describe random

paths

until

eventually they

either

al

reach some

point adjacent

to one of the

particles

of the

aggregate,

to which

they

are then

regarded

as

adhering,

or

b)

wander outside

Q,

in which case the

particle

is abandoned. In most DLA

simulations, including

the

original

Witten-Sander

algorithm, particles

move on a

lattice, usually

a square one,

by

steps of one lattice unit in a random

direction,

which restricts the

angles

between successive

path steps

and between

adjacent aggregate particles (in

the case of a square

lattice,

to

0( 90(

180° and

270).

A more realistic

approach

is to simulate

particle

motion

by

means of Errnak and Mccammon's Brownian

Dynamics algorithm [27]

because

this

algorithm

does not introduce restrictions of

angles allowing,

on the other

hand,

a very easy

incorporation

of

particle

interactions like electrostatic or

DLVO,

and then can be used to simulate the

aggregation

of

spherical

colloidal

aggregates [28-34].

This

algorithm

constructs

stochastic

trajectories

whose steps are solutions of Smoluchowski's

equation

for a short time

interval,

as follows.

From the

Langevin equations,

Errnak and Mccammon obtained the

following expression

for the

displacement

of a

diffusing particle

:

~

3Dg D( F)

r~ = r~ +

£

At +

£

At + R~

(At) (I)

J

~9

J

~B ~

where

r)

and r~ are the

positions

of the

particle

at the

beginning

and end of a time interval of duration

At,

D~~ is the diffusion tensor,

is the total external non-Brownian force on the

panicle

and R~ is a random

displacement

due to Brownian causes

(superscript

0's indicate values at the

beginning

of At and «I,

label

coordinates).

This

equation

is valid for At

large compared

with

mD(/k~

T

(where

m is the mass of the

particle,

taken as

unity

in our

work)

and small

enough

to ensure

negligible

variation of the extemal forces and the diffusion tensor

gradient.

The random Brownian

displacements Ri

are calculated as

R~

(At )

=

£ «q xj (2)

(4)

where the

%

are obtained from a random number generator with

(,)

= 0 and

(xi xj)

=

2

3q

At

(3~j being

the Kronecker

delta)

and the

weights

«~j

satisfy

Ii

-1 1/2

"11 "

~~ £ "~k (3~)

k =1

lj

-1

«~~ =

D( £

«i~. «y~

/«jj

I >

j (3b)

k=1

Equations (1)-(3) imply

that the first and second moments of the distribution of Ar~ = r~

r)

are

given by

(Ar~(At))

=

£ ~~°

+

~° ~)

At

(4a)

j

~~j

~B T

(Ari (At ) Ar~ (At))

= 2. D

~~

At

(4b)

In this work we assumed that no extemal forces were

present,

so that F

=

0 and the diffusion tensor is

given by

k~

T

Dij

=

(5)

car1~ro

where ro is the radius of the

diffusing particles,

1~is the

viscosity

coefficient of the solvent and c is a constant whose value is 4 or 6 when stick or

slip

conditions are considered

respectively.

The above n-dimensional Brownian

generalized algorithm [35]

was used to simulate the formation in two dimensions of DLA

aggregates

made up of various numbers of

particles

N for each

N,

simulations were

performed using

various values of the mean free

path

d defined

1/2 as d

=

Ar))

This value can be varied

using

a constant value of

D~ (taken

as

unity

in

,

our

work)

and

changing

the value of At.

In DLA simulations it is

usual,

for each new

particle

released from

B,

to

update

B and

Q

so that

r~/2

ro

= J1~~~~/2 ro + 5 and

r~

=

3

R~~~,

where

l~~~

is the

length

of the

longest

radius of the

aggregate

at this stage of the simulation. In the work described here we chose to

update

B and

Q

with reference to the radius of

gyration

of the

aggregate, 1§,

which as a random

variable

parametrized by

the number of

particles

in the aggregate fluctuates less than l~~~~, I-e- is a more stable index of the

relationship

between the size of the aggregate and the

number of

particles

in it.

Specifically,

the initial values of r~ and r~ were

51ro

and

71ro respectively,

and as the aggregate grew, r~ and

r~

were

updated

to

keep (r~ R~) Id, (r~ r~)/d

and

d/R~

constants at the same time l~~~~ was checked to make sure it did not exceed r~

(since

it never

did,

we refrain from

describing

the

adjustment

to be made in this

event).

When the

previous

relations are constants the mean number of steps for

trajectories

obtained with a

given

value of At is constant. This means

[36-38]

that we obtained

trajectories

with a fractal dimension

d~

constant

during

the

growth

of an aggregate.

In

particular,

in this paper we will focus our

study

on two

aggregates

obtained with the conditions

(r~ R~) Id

= 25 with

d/R~

m I

(d~

m 1.9

)

and

(r~ R~)/d

=

5 with

d/ll~

m 5

(d~ m1.6).

It has been checked that the value of the constant d/11~ does not have any influence on the results

obtained,

at least in the range 0.5 «

d/ll~

< 5 we have

performed

the

simulations. A value of ro

=

0.51

was used.

(5)

3. Fractal

analysis

of swan

aggregates.

The fractal dimension of each aggregate constructed was

computed by

the box

counting

method

[39].

This method consists of

covering

the aggregate with a lattice of side e

(in

units of

ro), counting

the number

n(e, N)

of cells

occupied by

the aggregate, and

repeating

this

procedure

for

successively

smaller values of e. The fractal dimension is defined as

Figure

I

shows,

for a two-dimensional aggregate, the linear

scaling

behaviour of

log

n

(I.e.

the existence of a

scale-independent Di)

for each of several values of N. For an ideal fractal

aggregate,

the fractal dimension

given by equation (6)

should be

independent

of N. Our simulation results

show, however,

that this situation should

only

be attained for

sufficiently large

N. For small

N,

the fractal dimension is

N-dependent

the lines of

figure

I have different

slopes. Analogous

behaviour has also been observed in other fractal processes,

including

Brownian

trajectories [36, 37].

To characterize such

behaviour,

we use a differential fractal dimension

(DFD) [36, 37],

I-e- a fractal dimension defined

locally

with respect to the scale

parameter.

In the present context we can define the DFD as

~ p~

d

log

n

(

e

fro,

N

)

dlog (e/ro) (7a)

6 N=isoo

/~

~S

~

~

=200

4

4

» ,

'

O~

log

e

Fig. I.- Log n(e,N) (number of occupied boxes) versus Loge (e is the side of the box) for bidimensional aggregates

composed

of different numbers N of

elementary particles.

The aggregates

were obtained

using trajectories

with the initial simulation condition

(rs R~)/d

= 25. The simulation results (A) have been fitted to a

straight

line

(lines).

(6)

in which we have

explicitly

stated that e is

expressed

in units of ro.

Alternatively,

an

analogous

definition of the DFD can be introduced as :

d

log M(r/ro,

N

)

~ ~~'~°~ ~

d

log r/ro ) ~~~i

where

M(r/ro,

N

)

is the number of

particles

within a radius r of the centre of the

aggregate (ro

~ r ~

R~~~).

We have found that these DFD functions defined for clusters formed

by

diffusion-limited

aggregation

can be fitted

by

similar

equations

to those

proposed by Takayasu [36],

Tsurumi

[38]

and the own authors

[37]

to random motion

D(N)

=

Di

~

(8a)

+

k~.

N ~

D

(r fro i

= D

f ~

(8bi

+

k~. (r/rot

'

where

Di

is the

limiting

value for

large aggregates,

and k~,

k~, fl

~

and

fl

~ are

parameters

that

depend

on the conditions of the

aggregation

process

(I.e. aggregation model,

fractal dimension of

trajectories

and interactions between reactive

particles

and

cluster). Likewise, Dr depends

on the conditions of the

aggregation

process : for

example,

for the two limit cases,

when the

trajectory

is a two-dimensional ballistic motion

(d~

=

I

Di

=

2

[40],

while for two- dimensional ideal Brownian motion

(d

-

0, d~

=

2) Di

- 1.6

[2, 3].

With our

algorithm large

clusters with any fractal dimension between these two limits can be obtained.

So,

for

example,

in

figure

2 the fractal dimension

Di

for different

large

clusters

(N

m

10~)

is

plotted

versus the value of

d/(r~ R~)

used in the

simulation,

I-e- ; for different values of the fractal dimension of the

trajectories, d~.

It can be seen that for

d/(r~ R~)

S 0.01 the usual DLA fractal is

obtained.

For a

specific aggregation

model

(for example particle-cluster, cluster-cluster, etc.)

it is assumed that the parameters

fl~, k~ (or fl~, k~)

must have the same values when the fractal

dimension of the reactive

trajectories

and the eudidean space,

d~

in which the aggregate is

embedded,

are the same, I-e-

they

are universal parameters like the fractal dimension

Di,

which has been studied

by

other authors

[41] showing

that it

depends

on

both,

2,I

Di

2,o

,""

l 9 ~,"

l, 8

,~

;i

1.7

"

1.6

o-i

d/(rB.Rg)

Fig.

2.-Fractal dimension

Dr

for

large

aggregates versus the relation

d/(r~-R~)

used in the simulation. The

symbols

are the simulation results, The dashed lines are to

guide

the eye,

(7)

d~

and

d~. So,

for

example,

Honda et al.

[41]

have studied this

dependence

for a

particle-

cluster model

showing

that

Di

=

(d(

+

d~

I

)/(d~

+

d~

I

).

In

figure

3

we have

plotted,

for

aggregation

processes with two different values of the fractal dimension of the reactive

trajectories,

the

N-dependence

of the fractal dimension of the

aggregate

;

symbols

indicate fractal dimensions obtained

using equation (6),

and the continuous curve is the result of

fitting equation (8a).

The results of

k~, fl~

and

Di

are summarized in table I for the two

aggregates.

This table shows that

flN

decreases when

Di

decreases and that

k~

has the inverse behaviour.

However,

more studies are

required

to obtain a definite relation between the behaviour of these parameters

(k~, fl~

or k~,

fl~)

and the fractal dimension

Di.

1.8

m

D(~/)

m

m

m

1,6

a

, a

1.5 a

1.4

O

N

Fig. 3. Box

counting

fractal dimension D

(N)

of two bidimensional aggregates obtained by computer simulation,

plotted against

N.

Aggregates

were obtained

using

reactive

trajectories

with

(rs R~)/d

=

25

(A)

and (rB

R~)/d

= 5

(.).

Solid lines are the results of

fitting equation (8a).

Table I. Values

of p~, k~

and

Di

obtained

by fitting of

the simulation results to

equation (8a).

Aggregate flN ~N ~f

0.350 ± 0.010 0.285 ± 0.005 1.79 ± 0.01

II 0.462 ± 0.005 0.121 ± 0.002 2.00 ± 0.01

The small-N

N-dependence

or small-r

r-dependence

of the fractal dimension of diffusion- limited

aggregation

clusters also arises with other methods of measurement, such as the radius of

gyration

method

(log R~

= const. +

D(N). log N)

or the correlation function method

(log

g

(r/ro)

= const. +

(D (r/ro) d~). log r).

As an

example,

in

figure 4,

in which

log

N is

(8)

2~7

2.3

»

. »

* »

. 4

* 4

* »

»

«

1.9

O.7 1-O

log Rg

Fig. 4.- Log N (number of

particles

of the

aggregate)

vs.

Log

R~

(radius

of

gyration)

for the bidimensional aggregates of

figure

3. Symbols as figure 3. Solid fines represent ideal fractal behaviour (behaviour at large

scales).

plotted against log R~

for the same

aggregates

as in

figure 3,

the

N-dependence

of the dimension measured

using

the

gyration

radius is shown

by

the deviation from the

straight

lines

corresponding

to the ideal behaviour of

large

aggregates. A similar deviation from

linearity

is observed in

plots

of

log g(r) against log

r.

4.

Scattering

from swan diffusion limited

aggregates.

For an

aggregate

of fractal dimension

Di,

the correlation function

g(r)

is

given by [42]

g

(r)

cc r~~ ~~

(9)

which leads

[43]

to the

following expression

for the

scattering

structure factor

S(q)

:

i(q)

cc

s(q)

cc

q~f (lo)

where q is the

scattering amplitude

vector, and

I(q)

is the

scattering intensity.

In real systems

equation (10) only

holds over a finite range ro ~ r ~

f (f

is the size of the

aggregate).

Several modifications have been

proposed

to model the effect of an upper cut-off at the

aggregate size,

the most

widely

used

being [43-45]

g(r)

= A r ~~~~~

exp

(- r/f) (I I)

which leads

[43]

to

S(q)

=

~~ ~~~~

~

sin

i(Df

I arctan

(q, f

)1

(12)

(1

+

1/(q, f )~)~~~~

~~'~

(q ro)

~

(9)

where r is the gamma function. The lower cut-off at ro can be

largely

taken into account

by introducing

an additional form factor

f~(q)

=

exp(-q~r(/6)

in the

expression

for the

scattering intensity I(q)

:

1(q)

= P

VI (Ps

Po)~

f~(q S(q) (13)

where p is the

panicle

number

density

of the

aggregate, (p~ po)

is the contrast in

scattering length density

and

Vo

is the volume of the

elementary particles.

When

Di,

in

equation (11),

is

replaced by

the

scale-dependent

fractal dimension

D(r/ro)

so as to model the behaviour of non-ideal

fractals,

it becomes difficult to obtain a

correspondingly

sensitive

expression

for

S(q)

unless it is assumed that q cc

I/r.

With this

assumption, equation (8b)

can be written

D(q)

=

Di

~

(14)

+

k~.

q 9

Ignoring

the upper cut-off and

assuming

further that

D(q)

varies

slowly

with q,

S(q)

cc

(ro.

q

)~~l~l,

and the

scattering intensity

will be

given by

the

equation

I(q) CCf~(q)(ro. q)~~~~ (15)

for I

If

~ q ~ l

fro.

For observations at a

large

scale

(q

« I

fro),

D

(q

-

D~

and

equation (15) predicts

the

usually

assumed linear

dependence

of

log

I on

log

q ; but for small r this is not so,

Figure

5 shows calculated

scattering

data for the

computer-simulated

fractal aggregates of

figure

3.

4

~~

i~

3

'._ '>._

° ""

-1,5 -1.I -O.7 -O.3

log q

Fig.

5.-

Log

I

(scattering intensity)

vs.

Log

q

(scattering

vector

amplitude)

for the aggregates of

figure

3.

Symbols

as

figure

3. The dotted fines are the results of

fitting equation (15) ~f~(q)

=

constant)

and the

straight

lines

correspond

to ideal fractal behaviour.

(10)

It should be realized that the non-linear behaviour reflected in

figure

5 has

nothing

to do with the non-linearities associated with the upper and lower cut-offs. The upper cut-off effect

occurs for r

>

f(q

~ l

If ) (even

in the linear

region

of

log

I vs.

log

q

plots,

so

long

as

f

is

finite),

and the lower cut-off effect occurs r

~

ro(q

> I

fro)

; the effect shown in

figure

5 occurs in the range ro ~ r ~

f.

This is evident in

figure 6,

which

shows,

for an ideal aggregate of

constant fractal dimension

Di

and for an aggregate with a

q-dependent

fractal dimension

given by equation (15),

the

(log

q

)-dependence

of

log I(q)

over a range of q

including

both cut-off

points (the

values of

D~, k~

and

fl~

used are those obtained for the

aggregate

with the smaller fractal dimension in

figure 5,

and

f

has been chosen

large enough

for ideal fractal

behaviour to have been reached before

cut-ofo.

Note that the ideal and the non-ideal fractals behave

identically

in both cut-off

regions.

4.9

~_ q_

v- ~-

3.O

f )

~ u

~

i I

Q+

~$

' ~

~

bo

I

'

° ~ ~

v fi

I-I tr ., t~

-O.8

-3.2 -22 -1.2 -O.2 O.8

1/j

i~~ ~

i/r

Fig.

6.

Log

I vs.

Log

q for an ideal fractal aggregate of constant fractal dimension

Dr (solid line)

and a non-ideal fractal aggregate

(dotted line),

with the upper and lower cut-offs

given by

the

equations (12)

and

(13). (It

is used the values of p, k and

Dr

obtained

by

fitted of the aggregate with smaller fractal

dimension,

fis assumed

large enough

that for some value of q

D(N)

=

Dr.)

The

region

into the square

corresponds to figure 5.

S. Conclusions.

In this communication we have shown that aggregates

produced by

diffusion-limited

aggregation only

possess a definite fractal dimensiod

D~

if

they

are

sufficiently large.

When

N,

the number of

particles making

up the

aggregate,

is

small,

the fractal dimension of the aggregate increases with N

approaching D~

in the limit. This behaviour has been observed

experimentally

in the

growth

of ammonium chloride

crystals [46].

Deviation from linear

scattering

behaviour in the

region

between the upper and lower cut-off

regions

is also

predicted

for small N and should be taken into account to

interpret experimentally

observed deviations

[47].

(11)

Acknowledgments.

This work has been

supported by

the

Spanish

Direcc16n General de

Investigac16n Cientifica

y Tkcnica under

Project

No. PB86-0651-C03-03. M-C-B-N- thanks the Ministerio de Educac16n y Ciencia for the

fellowships

awarded.

References

[Ii MANDELBROT B. B., The fractal Geometry of Nature (San Francisco, W. H. Freeman & Co.,

1985).

[2] WITTEN T. A. and SANDER L. M.,

Phys.

Rev. Leit. 47

(1981)

1400.

[3] WITTEN T. A. and SANDER L. M.,

Phys.

Rev. A 27 (1983) 5686.

[4] FORREST S. Q. and WITTEN T. A., J. Phys. A12

(1979)

L109.

[5] NITTMANN J., DACCORD G. and STANLEY H. E., Nature 314 (1985) 141.

[6] DACCORD G., NITTMAN J. and STANLEY H. E., Phys. Rev. Lett. 56

(1986)

336.

[7] VICSECK T,,

Phys.

Scr. T19

(1987)

334.

[8] PATTERSON L.,

Phys.

Rev. Lett. 52

(1984)

1621.

[9] MALOY K. J., FEDER J. and JOSSANG T,,

Phys,

Rev. Lett. 55 (1985) 2688.

[10] NIEMEYER L., PIETRONERO L. and WIESMANN A, J.,

Phys.

Rev. Lett. 52 (1984) 1033.

[I

Ii

BRADY R. M. and BALL R. C., Nature 309

(1984)

225.

[12] MATSUSHITA M., SANO M., HAYAKAWA Y., HONJO H. and SAWADA Y.,

Phys.

Rev. Lett. 53

(1984)

286.

[13] SAWADA Y., DOUGHERTY A., GOLLUB J. P.,

Phys.

Rev. Lett. 24

(1986)

1260.

[14] KAUFMAN J. H., BAKER C. K., NAzzAL A. I., FLICKNER M., MELROY O. R. and KAPITULNIK A., Phys. Rev. Lett. 56 (1986) 1932.

[15] ELAM W. T., WOLF S. A., SPRAGUE J., GUBSER D. V., VAN VECHTER D., BARz G. L. and MEAKIN P.,

Phys.

Rev. Lett. 54

(1985)

701.

[16] HONDO H., OHTA S., SAWADA Y., Phys. Rev. Lett. 55

(1985)

841.

[17] HONDO H., OHTA S. and MATSUSHITA M., J.

Phys.

Sac.

Jpn

55

(1986)

2487.

[18] HONDO H., OHTA S. and MATSUSHITA M.,

Phys.

Rev. A 36

(1987)

4555.

[19] DACCORD G.,

Phys.

Rev. Lett. 58

(1987)

479.

[20] DACCORD G. and LENORMAND R., Namre 325 (1987) 41.

[21] MEAKIN P., J. Theor. Biol. l18

(1986)

101.

[22] VOSS R. F.,

Phys.

Rev. 830

(1984)

334.

[23] MEAKIN P., DEUTCH J. M., J, Chem.

Phys.

80

(1984)

2115.

[24] MEAKIN P., J.

Phys.

A18

(1985)

L661,

[25] KOLB M., BOTET R. and JULLIEN R., Phys. Rev, Lett. 51

(1983)

1128.

[26] MEAKIN P.,

Phys.

Rev. Lett. 51 (1983) II19.

[27] ERMACK D., MCCAMMON J. A,, J. Chem.

Phys.

69

(1978)

1352, [28] DICKINSON E. and PARKER R., J. Colloid Interface Sci. 97

(1983)

220.

[29] ANSELL G. C., DICKINSON E. and LUDVIGSEN M., J. Chem. Sac. Faraday Trans. 2 81 (1985) 1269.

[30] ANSELL G. C. and DICKINSON E,, J. Chem. Phys. 85

(1986)

4079.

[31] ANSELL G, C. and DICKINSON E,,

Faraday

Discuss, Chem. Sac. 83

(1987)

167.

[32] ANSELL G, C, and DICKINSON E,,

Phys.

Rev. A 35 (1987) 2349.

[33] DICKINSON E., J. Colloid

Interface

Sci. l18 (1987) 286.

[34] DICKINSON E. and ELVINGSON C,, J. Chem. Sac.

Faraday

Trans. 2 84

(1988)

775, [35] DICKINSON E., Chem. Sac. Rev. 14

(1985)

421.

[36]

TAKAYASU H., J.

Phys.

Sac, Jpn 51

(1982)

3057.

[37] LOPEz-QUINTELA

M. A., ToJo C. and BUJhN-N0flEz M, C,, Mol.

Phys.

65

(1988)

1195.

[38] TSURUMI S. and TAKAYASU H.,

Phys,

Lett. A 53

(1986)

1965.

[39]

PFEIFER P, and OBERT M., The fractal

Approach

to

Heterogeneous Chemistry (John Wiley

&

Sons. Ed. D, Avnir,

1989),

(12)

[40] SUTHERLAND D. N,, J. Colloid

Interface

Sci. 226 (1974) 1241.

[41] HONDA M., ToYoKi H. and MATSUSHITA M., J.

Phys.

Sac. Jpn 55

(1986)

707,

[42] SCHAEFFER D. W. and MARTIN J. F., Kinetics of

Aggregation

and Gelation, F.

Family

and D. P, Landau Eds.

(Elsevier,

Amsterdam,

1984).

[43] TEIXEIRA J., On Growth and Form, H. E.

Stanley

and N. Ostrowski Eds. (Martinus

Nijhoff

Publ.

Dordrecht, 1986).

[44] SINHA S. K., FRELTOFT T. and KJEMS J. K., Kinetics of

Aggregation

and Gelation, F.

Family

and D. P. Landau Eds.

(Elsevier,

Amsterdam,

1984).

[45] CANNELL D. and AUBERT C., On Growth and Form, H. E.

Stanley

and N. Ostrowski Eds.

(Martinus Nijhoff

Publ. Dordrecht, 1986).

[46] OHTA S. and HONJO H.,

Phys.

Rev. Lett. 60

(1988)

611.

[47l

KJEMS J. K., FRELTOFT T., RITCHER D. and SINHA S. K.,

Physica136B (1986)

285.

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