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https://hal.archives-ouvertes.fr/jpa-00212428

Submitted on 1 Jan 1990

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Direct simulation of a permeable membrane

U. Brosa

To cite this version:

(2)

1051

Short Communication

Direct simulation of

a

permeable

membrane

U. Brosa

HLRZ c/o KFA, Postfach 1913, D-517 Jülich, F.R.G.

(Reçu

le 27 mars 1990,

accepté

le 3 avnil 1990) Abstract. 2014 Cellular automata are used to

compute flow thru a

permeable

membrane.

Scattering

centers constitute the membrane. This is in marked contrast to the

approach

of classical

hydrody-namics which represents a membrane

by

a

boundary

condition. With the

scattering

centers we obtain

different, but more

plausible

results

indicating

that

simple

diffusion is the

dominating

process in a

porous

layer.

We have thus a case where cellular automata show

superiority

over the classical meth-ods of theoretical

hydrodynamics.

1

Phys.

France 51

( 1990)

1051-1053 1 er JUIN 1990,

Classification

Physics

A bstracts 05.50-7.SSM

LE

JOURNAL

DE

PHYSIQUE

Tome 51 N° 11 1 er JUIN 1990

Several

investigations

on the

applicability

of cellular automata on viscous

hydrodynamics

have been done

meanwhile,

see e.g.

[1 - 4].

In these

studies,

solutions of the Navier-Stokes

equation

available from other sources were

compared

with

output

of cellular automata. It is clear now that cellular automata can

give

a truthful

picture

of

liquid

reality

as

long

as certain limits are not

transgressed

[5].

However,

at

present

those automata are

relatively

inefhcient so that their main

advantage

consists in

being

foolproof.

Probably

cellular automata will find their most relevant

applications

in the

microscopic-macro-scopic

research. From the

viewpoint

of hydrodynamics,

cellular automata are based on a schematic model of the molecular motion. Hence one can

study problems such as

fluctuations and local

equi-libration,

and one can check now much these

microscopic

properties

show up in the

macroscopic

behavior of the fluid.

For this an

example

shall be

given right

now. It is flow

through

a porous membrane. For a

microscopic

theory,

a membrane is a

layer

of

scattering

centers which the

liquid

has to

wriggle

thru. The

applications

of

membranes,

however,

are

macroscopic.

We became aware of the

problem

in a

previous study

[6].

The

geometry

is shown in

figure

1: 1Bvo channels conduct Poiseuille

flow,

each on its own. The

problem

would be trivial if it were

not for a membrane that connects the channels. The maximum velocities are v"zax at the inlets

of both channels but vmax -f-

Ovmax

and Vm02: -

wmax

at the outlets of the upper and the lower

(3)

1052

channel,

respectively.

A

part

of the

fluid, therefore,

must pass the membrane. It turned out in

[6]

that the

computed velocity

field

V(r)

depends

much on the way in which the membrane is taken into account. The

boundary-value

problem displayed

in

figure

1 is hence a sensitive indicator of the treatment of

porosity.

Fig.

1. - Flow thru two channels connected

by

a membrane. All parts show flows with

Reynolds

number 500. The truput is

50%,

i.e.

làvmo:a:/vmo:a:1

= 0.5. We have solid walls in the middles, indicated

by

the full

lines, and mirror

planes

above and below,

depicted by

the dashed lines. See the text for the

meaning

of the four parts and the papers

[6, 8]

for details

concerning

the geometry and the

algorithms.

In classical

hydrodynamics[7],

the behavior of the membrane is described

by

the

boundary

con-dition

meaning

that the membrane allows

only

for fiow

perpendicular

to its surface.

Equation (1)

is to

hold on the dotted line in

figure

1.

However,

its correctness may be doubted.

First, experts

in

hydrodynamics

notice at once that

(1)

is

just

the

slip

boundary

condition on a vertical wall as used in the

theory

of idéal

liquids.

The

application

of

slip

boundary

conditions to

problems

with viscous flow

along

solid bodies is known to

give

misleading

results.

Second,

there is no reason

why

the fluid should not cross the membrane in an

oblique

direction.

With cellular automata we can

easily

look into this

problem.

All we have to know is that a cellular automaton

opérâtes

on a

grid.

Then we select some of the nodes in the

vicinity

of the dotted line and let them become

points

at which the molecules

experience

backward reflections.

(4)

1053

The essence of the results is distilled in

figure

1. Part

(a)

shows

unhampered thruput.

Instead of the

membrane,

there is

just

a hole. Due to inertia effects the fluid passes the hole

preferentially

at its downstream

edge.

In Part

(b)

the

boundary

condition

(1)

is

put

into force. It

only

makes the velocities vertical. As mentioned

already

above,

(1)

is an

equation

for idéal

liquids.

Hence we cannot

expect

a real

impediment

of the flow. Part

(c)

shows what

happens

when every second node on the dotted line is made a

scattering

center. We see now a much broader distribution of the velocities over the membrane. This is

expected

since the

scattering

centers induce diffusion. In

addition,

the velocities pass the membrane

obliquely.

For the results exhibited in Part

(d), only

every third node was used as

scattering

center. The

only point

to be noticed here is the small difference with Part

(c).

In addition 1 have modelled the porous membrane in several different

ways. For

example,

1 took nodes not

only

from the dotted line but from a

strip

around that line. I

composed

nodes to form small

hexagons,

and so forth.

Invariably pictures

as shown in

figure

1

(c)

and

(d)

were obtained. This is an almost trivial result as it is

always plain

diffusion which features the flow in the porous

layer.

It is nevertheless remarkable that it takes so few

scattering

centers

to

get

full diffusion.

Part

(b)

of

figure

1 shows results

presented

first in

[6].

The

juxtaposition

with Part

(c)

exhibits that we have in fact a

significant

modification.

Finding

the same results

by

computational

methods of classical

hydrodynamics

seems to be

possible.

However,

one has to discard the

boundary

condition

(1)

and must model the membrane

by

a

layer

of small but finite thickness. In this

layer,

inertia is

damped

so that the Navier-Stokes

equation

can be

replaced

by

a diffusion

equation.

As a

boundary

condition between the porous

layer

and the free

flow,

continuity

of the

velocity

field

ought

be

stipulated.

Such an

arrangement

complicates

the

application

of classical methods like finite elements so that cellular automata have an

edge.

Acknowledgements.

l’m

grateful

to C. Küttner for

suggesting

the

problem

to me.

Encouragement

by

D. Stauffer is

appreciated.

Part of this work was done

using

the new interactive facilities at the HLRZ.

References

[1]

D’HUMIERES D. and LALLEMAND P.,

Complex Systems

1

(1987)

599.

[2]

LIM H.A.,

Phys.

Rev. A. 40

(1989)

968;

LIM H.A.,

Complex Systems

2

(1988)

45.

[3]

HAYOT E and RAJ LAKSHMI M.,

Physica

D 40

(1989)

415.

[4]

DUARTE J.A.M.S. and BROSA U., J. Stat.

Phys.

59

(1990)

501.

[4]

DAHLBURG J.P., MONTGOMERY D. and DOOLEN G.D.,

Phys.

Rev. A 36

(1987)

2471.

[6]

BROSA U., KÜTTNER C. and WERNER U., Flow thru a porous membrane simulated

by

cellular automata

and finite elements, submitted for

publication

in J. Stat.

Phys.

[7]

BERMAN A.S., J.

Appl. Phys.

24

(1953)

1232.

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