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Correlation of Saturation Profiles in Slow Drainage in Porous Media

C. Du, B. Xu, Y. Yortsos, M. Chaouche, N. Rakotomalala, D. Salin

To cite this version:

C. Du, B. Xu, Y. Yortsos, M. Chaouche, N. Rakotomalala, et al.. Correlation of Saturation Profiles in Slow Drainage in Porous Media. Journal de Physique I, EDP Sciences, 1996, 6 (5), pp.753-767.

�10.1051/jp1:1996240�. �jpa-00247212�

(2)

Correlation of Saturation Profiles in Slow Drainage in Porous Media

C. Du (~),

B. Xu

(I), Y-C- Yortsos (~'*),

M.

Chaouche (~),

N.

Rakotomalala (~)

and D. Satin

(~)

(~)

Department

of Chemical

Engineering

and Petroleum

Engineering Program, University

of Southern

California,

Los

Angeles,

CA

90089-1211,

USA

(~) Laboratoire

Fluides, Automatique

et

SystAmes Thermiques,

Bitiment 502,

Campus Universitaire,

91405

Orsay Cedex,

France

(Received

30

January

1995, revised 15 December 1995, accepted 22

January1996)

PACS.05.40.+j Fluctuation

phenomena,

random processes, and Brownian motion PACS.05.90.+m Other topics in statistical

physics

and

thermodynamics

PACS.06.30.Bp Spatial

dimensions

(e.g., position, lengths, volume, angles, displacements, including

nanometer-scale

displacements)

Abstract. We

study

the

spatial

correlation of one-dimensional

I-D)

saturation

profiles

ob-

tained

during

slow

drainage

in porous media, where

capillary

effects

predominate. Using

prop-

erties of Invasion Percolation in an uncorrelated

medium,

we compute the correlation structure of the

profile.

At small values of the

lag (but

for

sufficiently large systems)

the

profile

ap-

proaches

the structure of the record of a

fractional

Browman motion

(mm)

with Hurst exponent H

=

(D -1) /2,

where D is the fractal dimension of the

percolation

cluster.

Sufficiently

far from

percolation,

the

profile

is

a white noise. Noise measurements in

displacement

experiments

using

an acoustic

technique

are

reported

for the 3-D case. The

theory

is confirmed with 2-D simula- tions. An apparent mismatch in the 3-D case is attributed to finite-size effects. The

approach

is

generalized

to correlated

percolation.

R4sum4. Nous avons 6tud16,

th60riquement

et h l'aide de simulations

num6riques,

les cor-

r6lations

spatiales

des

profils

de saturation obtenus au cours de l'invasion d'un milieu poreux par une

phase

non mouillante

(drainage).

La saturation

(concentration volumique)

de la

phase

envahissante est

moyennde

dans la direction

perpendiculaire

h l'dcoulement; cette saturation est ensuite dtudide dans des conditions ok les elfets capillaires sont dominants. Ce processus est bien ddcrit par la Percolation d'Invasion. Pour un milieu sans corr41ation, on montre que la

structure des corr61ations approche un mouvement Brownien fractionnaire

(fractional

Brownian

motion

(mm))

d' exposant de Hurst H

=

(D -1)/2,

ok D est la dimension fractale de I' amas de

percolation.

Suffisamment loin du seuil de

percolation,

la structure des corr61ations du

profil

de saturation est d6crite par un bruit blanc. Des mesures de bruits au cours

d'exp6riences

de d6-

placement

1l'aide d'une

technique

acoustique ont dt6 elfectu6es. A 2-D, la th60rie est confirmde par des simulations. A 3-D, la diff6rence entre th60rie d'une part et simulations et

expdrience

d'autre part, est attribude h des effets de taille finie. Les r6sultats sont ensuite

g6n6ralis6s

au cas

de la

percolation

corr416e.

(*)Author

for correspondence

(e-rnail: yortos@euclid.usc.edu)

@

Les

(ditions

de

Physique

1996

(3)

1. Introduction

The slow

displacement

of a

wetting phase

from a porous medium

by

the

injection

of a non-

wetting phase,

immiscible to the former, has been

analyzed

in much

detail,

due to the relevance of the process to

engineering applications,

such as oil recovery and

groundwater remediation,

but also because of its interest from a statistical

physics viewpoint.

The well-known processes of Invasion Percolation

(IP) [1,

2] and of Invasion Percolation in a Gradient

(IPG) [3,4]

have

been used to describe these processes in uncorrelated random porous

media,

in the absence

or presence of an external

gradient, respectively. Recently,

the

properties

of

percolation

in correlated

media,

the correlation function of which

decays algebraically,

e-g-

C(p)

r~~

p~~/,

where

-)

<

il

< o and

v is the correlation

length

exponent, have also been uncovered

[5].

Typically, laboratory displacement experiments

in porous media are

performed

in geome- tries of a uniform cross-section in the direction of

displacement

x

(e.g.

rectilinear or

cylindrical cores).

The main

quantity

of interest is the saturation of the

non-wetting (invading) phase, Six, t),

which denotes the volumetric fraction of the pore-space

occupied by

the

non-wetting phase, transversely averaged

over the cross-section

(yz).

This

quantity

can be measured

using

various

diagnostic methods, including acoustics, X-rays,

etc., in order to infer various char- acteristics of the

displacement.

For

example,

in the case of

IPG,

the

slope

of the saturation

profile

near the front

gives

a measure of the

gradient applied [6-8].

For the case of

IP,

the fluctuation of the saturation

profile

furnishes additional information on the medium and the process. This information would be of

particular interest,

for

example,

if it indicates a cor- related pore-space

[9,10].

In an earlier

investigation using

a continuum

model,

Yortsos and

Chang [10] pointed

out that the saturation

profile

can reveal the characteristics of the

underly- ing

pore structure,

provided

that the

displacement

is controlled

by capillarity

and the process is away from

percolation.

To our

knowledge, however,

a

study

of the correlation structure of

the

profile

near

percolation

has not been

attempted.

The

objective

of this

investigation

is to

study

the structure of the fluctuation of the saturation

profile during drainage,

both near and far from

percolation. Because,

in our

context,

slow

drainage

is

equivalent

to

IP,

the

problem

is also

equivalent

to the

analysis

of the fluctuations of the

occupation profile

of IP. In this paper, we first

develop

a

theory

based on the correlation

properties

of

percolation

processes, which is

subsequently

tested ~vith the numerical simulation

of the process in 3-D and 2-D lattices.

Experiments

in uncorrelated porous media are also

conducted and

provide

a test of the

theory

in 3-D.

Theory

and simulations are then extended to correlated

percolation problems,

where the correlation function

decays algebraically.

2.

Theory

2.1. 3-D GEOMETRIES. We consider slow

drainage (invasion percolation)

in a rectilinear porous

medium, represented

as a 3-D cubic lattice of extent L x L x N

(N

>

L) (Fig. I).

No-flow

boundary

conditions are

applied

at the lateral

sides,

the

displacement being

forced in the direction x.

During

the invasion process, a front

develops

at the

leading edge

of the

displacement,

the extent of which increases until it becomes

comparable

to the lateral extent L. Within this

region,

the mean saturation varies with both

time,

t, and

position,

x,

leading

to a

non-stationary profile.

Of interest to this paper is the

spatial

fluctuation of the saturation in the

region following

the front, where the mean saturation is

approaching

a

steady-state,

and

the

profile

is closer to

being stationary.

Let

9(r)

denote an indicator

function, equaling

I or o when the site is or is not

occupied,

(4)

w MM w

w

20

15

io

~

~ 0 5 lo t5 20 25

30

Fig.

I.

Snapshot

of Invasion Percolation in a 3-D lattice.

respectively. Then,

the transverse saturation is

~j 9(r)

~~~~

~ rEAu) ~~~

L2

From

percolation theory,

we know that < 9 >r~~

L~~~,

where D is the fractal dimension of the

percolation

cluster and E is the

dimensionality

of the

system. Hence,

we obtain the

following scaling

of the saturation

< S >r~~

L~~~

<

S~

>r~~

L~l~~~l (2)

To estimate the correlation structure of this

profile,

we consider the autocorrelation function

R(h

e<

S(x)S(x+ h)

>. where all distances have been normalized with the mean pore

length,

I. To

develop

an

expression

for

R,

we use the correlation function

g(r)

=<

91r')9(r'+ r)

>

(3)

which denotes the

probability

that a site at a distance r

=

jrj

from an

occupied

site is also

occupied (it belongs

to the same

cluster). Then,

~ g(r)

<

S(x)S(x

+

h)

>" ~

~~

(4)

the sum

being

over all r that connect every

point (yo, zo)

on the

plane

x with every

point (y, z)

on the

plane

x + h

(Fig. 2a).

We know that near

percolation, g(r)

behaves as

g r~J

Crl~-~l (5)

where the

prefactor

scales as C r~~< 9 >r~~

Ll~~~)

the

exponent

iii

(5) gives

the

scaling

for an IP

problem

and differs

by

a factor of 2 from the OP exponent used in our

previous

(5)

~ h _ L

y,z

L ~Y0'~0

~---~- ~---

"

' ' '

' ' '

/ ' /

a)

~ ~ ~~~

1,o i,i

c b

yo>zo

d a

b)

0,0 1,0

Fig.

2. Illustrations of the notation used:

a)

3-D lattice,

b)

Partition of the yz plane for the

evaluation of the

integral.

publication [11]. Hence,

to evaluate the sum in this

regime

is

equivalent

to

computing £~ r~°,

where we have denoted a

#

(D 3) /2 (note

that -o.235 <

a <

o).

To

proceed,

we

replace

the sum

by

an

integral

K m

o,zo,y,z r~°dydzdyodzo (6)

and note that

r~

= p~ +

h~ (7)

where

P~ = (Y Yo)~ +

(z zo)~ [8)

Next,

we rescale all distances

by L,

the rescaled variables

varying

in

[o,I] (Fig. 2b),

and

proceed by keeping

the

previous

notation for the sake of convenience.

Then,

the

integral

in

(6)

reads

K =

L~~+~ / / / /

(p~

+

e2)"dydzdyodzo

+

L~°+~I(e) (9)

yo,zo,y,z

where we introduced the

variable,

e

= h

IL.

To evaluate the

quadruple integral

I we

partition

the

plane

yz as shown in

Figure

2. After some

algebra,

I reduces to

I(E)

= 4

/ / (1- v)(i z)(v~

+ z~ +

e~)"dydz (lo)

~ ~

(6)

Before we

proceed

with the numerical evaluation of

(lo),

we will evaluate its

asymptotic

be- havior in the limit of small e. For this we note that I consists of the sum of the

following

three

integrals

~

Ii (e)

= 4

/ /

(y~

+

z~

+

e~)°dydz (ii)

o o

12(e)

= -4

/ /

(y~

+ z~ +

e~)°dy~dz (12)

~ ~

13(e)

=

/ / ~ ~ (y~

+

z~

+

e~)"dy~dz~ (13)

the

leading

behavior of which in the limit of small e can be

readily

obtained. After some

calculations,

we find

~~~~ ~~~~

(° )

i) ~~~~~

~

~~~~~

~~~~

I~(e)

=

i~(o)

+

o(e2a+3) (is)

ere

we

1

~2a+2

where

~ ~

I(o)

= 4

(1 y)(I z)(y~

+

z~)°dydz (18)

which can be also

expressed

in terms of

incomplete

Beta

functions,

if necessary. We note

(by converting

in radial coordinates and

making

use of the result 2a +1 >

-1)

that the

integral

in

(18)

exists. Back substitution in

equations (4)

and

(9) gives

the

asymptotic

result

<

S(x)S(x

+

h)

>r~~

CL~°I(o) (I

b

~)) ~~~)

+ O

() ~l(19)

where we defined the

positive

constant

~r

j

=

(a

+

i) I(o~ (20)

Equation (19)

is

consistent,

in the limit h -

o,

with the result <

S~

>r~~

L~l~~~l

of

(2), given

the

scaling

with L of the

prefactor

C.

Typically,

one is interested in the

semi-variogram, SV,

which in terms of the

original

defini-

~~°" ~~~~~

sv +<

(s(x

+

h) s(x))2

>m~ i

j (21)

Its

asymptotic

behavior in the small e limit can be obtained from

(19).

We find

<

(S(x

+

h) S(x))~

>r~~ 2b <

S~

> ~

(22)

L

~~

(7)

0-'

~ _- -4

a) ~°~ ~~~~~

-1

d3

-2.5 -2 -1 .5 -1 -0.5 0

b)

~°~ ~~~~~

Fig.

3. Numerical evaluation of the

semi-variogram plotted

vs the dimensionless

lag

h

IL

for inva- sion

percolation: a)

3-D

geometries, b)

2-D geometries. The dashed lines are the asymptotic

theory predictions

with

slope

2a + 2 = 1.53 for 3D and 2a +1= 0.896 for

2D, respectively.

This behavior is similar to the

(self-affine)

trace of a fractional Brownian motion with Hurst

exponent [12]

H =

~

~

(23)

which in the

present percolation problem (with

or without

trapping)

reads H m 0.765. This exponent is different from the one

reported

in

[11],

where a different

scaling

of the correlation function was used.

The numerical evaluation of

(21)

is

plotted

in

Figure

3a. The

asymptotic

behavior at small

e is consistent with

(22), provided

that the dimensionless

lag

is smaller than

approximately

0.01. The rather small range of the

validity

of

(22)

must be taken into consideration in the

interpretation

of the numerical simulations

reported

below.

The above is

applicable

near

percolation.

For a system away from

percolation,

the

pair-

connectedness function takes the

dependence,

g

r~~

exp(-r If).

where the correlation

length (

is assumed much smaller than L. We can calculate the correlation function

by proceeding

as

before and write

1(e, b)

= 4

j j ii y)ji z)

exp

(-j(y2

+ z2 +

2)1/2j dydz 124)

~ ~

(8)

To derive the

asymptotic

behavior of I in the limit b e

)

~ 0 we

apply

tvice the

Laplace

method for the

asymptotic

evaluation of

integrals [13]

to obtain

1(E b)

=

4(27rb)~/~ (~(i

~/)(~/~ +

E~)~/~

exP

-1(~/~

+

~)~/2)

dv

=

87rbexP 1- II (25)

The final result reads

<

S(x)S(x

+

h)

>r~~<

S~

>

exp(-

~

(26) f

which can also be rewritten as

<

(S(x

+

h) S(x))~

>r~J 2 <

S~

>

I

exp(- ()j (27)

This expresses the

semi-variogram

of a

signal

correlated over distances of order

(.

For suffi-

ciently large h, therefore,

the

profile

has the correlation structure of a white

noise,

as

expected.

2.2. 2-D GEOMETRIES. A similar

approach

can be

applied

for 2-D

geometries. Consider, first,

the behavior near

percolation. Now,

the calculation of the

integrals

is

easier;

for

example,

the

integral corresponding

to

(10)

reads

1(E)

" 2

/

(1

Y)(Y~ +

f~)°dy (28)

where a is defined as

before,

but with E

= 2. Before the full numerical

evaluation,

we consider the

leading

behavior of

(28) by writing

I(f)

-

~~a

+

/~a

+

i~

+ 2

~ (i

Y) i(Y~ +

f~)° Y~°i dY (29)

and

taking

the small e limit. The result is

~~~~

(20

+

~(a

+

1)

~~~~~~~

~

~~~~

~~~~

In the

above,

we took into consideration that 2a +1 < 1, and introduced the

positive

constant

a =

/ (v~°

(v~

+

i)a) dy (31)

Since a <

0,

the

integral

converges.

Thus,

one arrives at the

following expression

for the autocorrelation function

<

S(x)S(x

+

h)

>r~~<

S~

> I c

~

l+ O(e) (32)

L

~~~~

where we introduced the

positive

constant

c =

2a(20

+

1)(a

+

1) (33)

Equivalently,

we may write

<

(s(x

+

h) s(x))2

>r~~ 2c <

s2

>

((

~~

(34)

(9)

where the Hurst

exponent

is now, H

=

(D

E

+1) /2

=

(D -1) /2. Hence,

we

expect

H m 0.4I for IP with

trapping

and H m 0.448 for

Ordinary

Percolation

(OP)

or for IP without

trapping.

As in the 3-D case, this result differs from Du et al.

ill].

Figure

3b shows a

plot

of the SV for the 2-D case. The

asymptotic dependence (34)

is well satisfied for values of the dimensionless

lag

smaller than

approximately 0.I,

which is a factor of10

larger

than in the 3-D case. This behavior should also be considered when

interpreting

the simulation results below.

Away

from

percolation,

a similar

approach applies.

We consider an

exponential pair-

connectedness function as before.

Then,

the behavior of the

integral

1(e, b)

= 2

~ (1 y)

exp

(-b~~(y~

+

e~)~/~j dy (35)

is

sought

in the limit b

=

( IL

« I. Its evaluation is

straightforward using Laplace's

method

[13]

leading

to the result

I(e, b)

=

2(2~rbe)~/~

exp

(- )) (36)

The end result is identical to the

previous equation (27).

2.3. CORRELATED PERCOLATION. The

previous approach

can be

generalized

to correlated

percolation

[5]. We will restrict our attention to

percolation

in lattices with a correlation function of

algebraic decay, C(p)

r~~

p~~,

where

-)

<

k

<

0,

and v is the correlation

length exponent

of uncorrelated

percolation.

In such cases, results are available for the

ordinary

per-

colation

problem,

but not for the

corresponding

invasion

percolation problem.

The correlation function still scales as in

(5),

where the fractm dimension is obtained from D

= E

(,

where

)

and P

are

percolation

and correlation

length exponents, respectively,

of the correlated per- colation

problem.

Isichenko [5] has shown that

exponent j

is identical to that of uncorrelated

percolation

in the

corresponding dimension, j

=

fl,

but that exponent P is not, if

)

<

fl

< 0,

where it is

given by

P

=

). Nonetheless,

the

previous approach

is still

applicable. Proceeding

as

above,

we find that the exponent H

describing

the

early

part of the SV for this

problem

is

H =

~~

+ l

(37)

in 3-D and

H

=

~~

+

l/2 (38)

in

2-D, respectively. Therefore,

in the correlated

percolation

case, H varies in the interval

[0.765, lj

in 3-D

geometries,

and in the interval

[0.41, 0.5j

in 2-D

geometries.

This

suggests

the

possibility

that at least in the

appropriate

range, the trends of the 3-D

profile (where

H >

0.5)

are

persistent,

while those of the 2-D

profile (where

H <

0.5)

are

anti-persistent [2j.

This conclusion was also reached in

[I ii, although

with different values of the

exponent. Away

from

percolation,

we

expect

the correlation structure of the

underlying

lattice to emerge.

3. Simulations

To test the

theory,

numerical simulations of

ordinary

and invasion

percolation,

in

2-D,

un-

correlated or

correlated,

lattices and in 3-D uncorrelated lattices were conducted. For the case of correlated

percolation,

the correlated lattice was created

using

the method of

Midpoint

Displacement

and S~ccessive Random Additions

[14].

The various results are summarized in

(10)

Table I. Hurst

exponent (H ) for

various processes near

percolation

Process

Dimension/Type Fieldk

Latticesize Simulation

Theory

random 100 x 100 x 500

l10 x l10 x 500 0.55

site random x x

300 x

site x

2D x

IP 300 x 600 0.30

2D random x

500 x 0.410

2D

/

site

(no trap) k

= 0.0 400 x 800 0.51 fBm 0.500 fBm

2D

/

site

(no trap) k

= -0.2 400 x 800 0.47 fBm 0.486 fBm

2D

/

site

(no trap)

H

= -0.5 400 x 800 0.40 fBm 0.465 fBm

300 x 300 x 300 0.57 fBm 0.765 fBm

x x

2D

/

site

k

= 0.0 512 x 512 0.54 fBm 0.500 fBm

OP 2D

/

site

k

= -0.2 512 x 512 0.48 fBm 0.486 fBm

2D

/

site

k

= -0.2 1024 x 1024 0.49 fBm 0.486 fBm

2D

/

site H

= -0.5 512 x 512 0.45 fBm 0.465 fBm

2D

/

site

k

= -0.8 512 x 512 0.40 fBm 0.448 fBm

Table II. Hurst

exponent (H ) for

vartous processes

far from percolation

Process Dimension Field

k

Lattice Size < S > Simulation

Theory

3D

lo x 10 x 500

~~~d°m x x

x 40 x 500

°.50 fGn

x

IP x

2D random 300 x 600 0.5 fGn

50 x x 500

x x 0.49

~

o_50 fGn

random 9°° ~~

°'~°

Tables I and II.

Typical

saturation

profiles

near and far from

percolation

for the 3-D IP case

are shown in

Figures 4top

and

4bottom, respectively.

Because the above

theory

is based on the

assumption

of a

well-developed percolation

state, in all IP

problems

we

analyzed

the

part

(11)

0 50 100 150 200 250 300 350 400 450 500 Position X

50 loo 150 200 250 300 350 400 450 500

Position X

Fig.

4. Saturation profiles from Invasion Percolation in a 3-D lattice:

(top)

at

breakthrough

of the

invading phase, (bottom)

at conditions away from

breakthrough.

of the

profile

away from the

invading

front and from the inlet to minimize finite-size effects.

In an

analogous study [8],

a

length-to-width

ratio of two was

used,

and the middle

part

of the

profile

was

analysed.

The fluctuations were

analyzed

in various ways,

by constructing

the

spectral density,

the

semi-variogram

or the

R/S

curve

[2,9]. However, consistently

reliable results were obtained

only

from the

semi-variogram,

the other two indicators often

suffering

from

large

local correlations.

Figure

5 shows the

plot

of the

numerically

determined exponent

Hn~m

vs its theoretical value for a

profile

near

percolation.

The raw data used are described in detail in Table I. The data

reported

are ensemble averages over 10 realizations

(in

the standard

case).

It is apparent that

theory

and simulation agree

reasonably

well for the 2-D case, the

agreement being

better for the OP case

(where

the

profile

of the

largest

cluster at

percolation

was

analysed).

In

general.

however,

the numerical results

underpredict

the theoretical value. In

3-D, only

random lattices

were used. For this case, there is a noticeable difference between theoretical and numerical

predictions.

We attribute this mismatch to finite-size

effects,

which appear to diminish

slowly

with increased size

(compare

the first three entries in Tab.

I).

Finite-size effects are also

present

in

2-D,

the trend

being

in the

right direction,

as the size increases

(Tab. I).

The reason for the difference between theoretical and numerical results becomes clear when

we compare the

corresponding semi-variograms. Figure

6 shows

typical plots

of the SV of the numerical simulation results in 3-D and 2-D

geometries.

Because of

computational

lim-

itations, the 3-D simulations are restricted to

generally

small

sizes,

hence the

corresponding

dimensionless

lag,

h

IL,

is

typically larger

than 0.01. In that range,

however,

the behavior of the theoretical SI~ does not

strictly

follow

(22),

as shown in

Figure

3a. As a

result, attempting

(12)

~ x

~ +

fl

xx

x

0 O-1 0.2 03 04 0.5 06 07 0.8 09

H

Fig.

5.

Comparison

of numerical

(Hnum)

and theoretical

(H)

values of the Hurst exponent for an

mm

signal

for a system near

percolation ((x)

denotes 2-D

results, (+)

denotes 3-D

results).

to

interpret

these simulations with a

power-law scaling

leads to a value smaller than

expected,

as indeed shown in

Figure

5. On the other

hand,

in 2-D

geometries

the lattice sizes are

larger (Fig. 6b),

and the dimensionless

lag

is within the

region

where the

asymptotic

behavior

(34)

holds

(compare Fig.

3b and

Fig. 6b).

A closer

agreement

is thus

obtained,

as shown in

Figure

5.

Table II shows results

corresponding

to a

system

away from

percolation.

A

generally good agreement

was found between

theory

and

simulation, although

results are better for OP rather than IP. The transition from fBm to fGn

type

noise as we move away from

percolation,

is

clearly

observed in all cases studied

(compare

Tab. I and

II). However,

the rate of

approach

to an fGn

signal

as the

percolation probability

increases was found to be much

slower, namely

to

occur at

higher

mean saturation

values,

in IP

compared

to OP processes.

4.

Experiments

Slow

drainage experiments

were next conducted. To allow for the simultaneous determination of the correlation structure near and far from the

percolation regimes,

the

experiments

were

conducted in the presence of a small amount of

gravity, corresponding

to Invasion Percolation in a Gradient. In

previous

studies

[4-8],

it was shown that IPG shares many of the features of Gradient

Percolation, namely

it contains a

leading

front of width aft

r~~

Bj"/l~~"I,

where the

properties

of IP are

exhibited,

followed

by

a

compact

pattern. The correlation structure is

expected

to

correspond

to IP at

percolation conditions,

near the

front,

and to IP far from

percolation,

upstream from the

front,

thus we

anticipate

the two

previous scalings

to emerge

near and far from the

front, respectively.

In the

experiments,

a

lighter density non-wetting

fluid

(nonane)

was

injected

at very low

rates

(with

the

capillary

number, Ca

=

qp/~i, equal

to

10~~,

where q denotes the flow

velocity,

p the

viscosity

and ~i the interfacial tension between the

fluids)

to

displace

a heavier

wetting

(13)

-1 .5

~.5

-2 -1.5 -1 -0.5 0

a)

~°~~~~~~

> 0

$

G-1

~~3

-2.5 -2 -1 .5 -1 -0.5 0

log (h/L) b)

Fig.

6.

Typical semi-variograms

of saturation

profiles

from numerical simulations:

a)

3-D Invasion Percolation in a lattice 200 X 200 X 400,

b)

2-D Invasion Percolation in

a lattice 1000 X 2000. Solid lines denote fitted

straight

lines with

slope

1.19 for 3D and 0.896 for 2D

respectively,

where slope = 2H.

fluid

(water)

in the direction from

top-to-bottom.

The porous medium consisted of

glass

§eads

of diameter a

= 100 pm

(permeability

5

Darcy) packed

in a rectilinear

geometry

of dimensions 4 x 2 x 30

cm~ corresponding

to a 400 x 200 x 3000 network.

Hence,

the effective size for the

analysis

of the

experimental

correlations is about 200. This should be taken into consideration in the

interpretation

of the

experiments.

Care was taken

during packing

to ensure

good mixing

of the beads in order to avoid

long-range

correlations. The

corresponding gravity

Bond

number, Bg

=

~~~~~,

where

Ap

is the

density

difference and

g the acceleration of 'f

gravity,

was estimated at

Bg

=

10~~

Saturation data were obtained

by

an acoustic

technique

described elsewhere

[15],

which allows for a

spatial

resolution of1 mm with an accuracy of

10~3

in saturation. The far from

percolation regime

is ensured

by

a

capillary barrier,

which

allows a

large

increase in the saturation up to S

= 0.60.

Typical

saturations

profiles corresponding

to the two

regimes

are shown in

Figure

7 with the

corresponding

power spectra shown in

Figure

8.

Here,

we relied on

spectral analysis

to

determine the

scaling

of the correlation of the fluctuations. We recall that the power

spectral density

function scales as [16]

S(f)

r~~

f~~~~~

for an fBm

signal

and as

S(f)

r~~

f~~~~

for an fGn

signal.

The data away from the threshold

(open

circles in

Fig. 8)

show a

slope

close to

nearly

zero

corresponding

to uncorrelated

noise,

in

agreement

with the

theory.

These results

(14)

0.8

0.6 S 0.4

0.2

0 0.2 0.4 0.6 0.8

x~

Fig.

7T- Saturation

profile

from

displacement experiment:

bottom curve at

breakthrough

of the

invading

fluid; top curve away from

breakthrough.

",,

~,~~

~

',

i~ ",

~ ',

4J .,.

't3 o

- o

t4 '<,

b

° ° Q

jIn°~

Q

4~ '.

+ ~

o.oi o.i

wave vector

Fig.

8.

Log-Log plot

of the

spectral density

of the saturation versus the

spatial

wave-vector. Full squares

correspond

to data in the

vicinity

of the

percolation threshold,

open circles

correspond

to the

regime

away from

percolation.

The dashed line of slope -2

corresponds

to H m 0.5 mm. The

horizontal line corresponds to H m 0.5 fGn.

tend to confirm the uncorrelated structure of the

underlying glass

bead

pack.

On the other

hand,

near

percolation,

the

logs log f

data

(squares

in

Fig. 8)

can be fitted with a

straight

line of

slope

m -2

(dashed line) corresponding

to an fBm

signal

with H m .5. This is in

contrast to the 3-D theoretical

prediction

of H m .765

(although

in better

agreement

with

the

simulations).

As in the latter case, we attribute this difference to finite-size effects. As a result of the small size of the

experimental

cross

section,

the dimensionless

lag

in the

analysis

of the

experiments

varies in a range

exceeding 1/200,

which is not

sufficiently

small to allow for a critical test of the

asymptotic prediction (compare

with

Fig. 3a). Thus, interpreting

the available data with a power law leads to an

underprediction

of the

exponent,

much like in the numerical simulation case.

Experiments

in correlated media were not conducted due to lack of

(15)

a model porous medium of a controlled correlation structure.

Progress

in this direction would be

desirable,

as many natural porous media are correlated at various scales.

5. Conclusions

In this paper, a

theory

was

developed

that

predicts

the correlation structure of

transversely averaged

saturation

profiles during

slow

drainage,

where

percolation

processes are involved.

The

theory

indicates that near

percolation,

the

asymptotic

behavior of the

semi-variogram

at small values of the dimensionless

lag

has the

general

characteristics of the record of an fBm

signal,

with trends that are

persistent

for the case of 3-D

geometry

and

anti-persistent

for the

2-D case,

regardless

of the correlation of the

underlying

lattice. The

theory

_was confirmed

with numerical simulation in 2-D lattices. Simulations and

experiments

in 3-D

lattices,

how- ever,

underpredicted

the

asymptotic exponent.

This difference was attributed to the small network sizes

used,

which result in dimensionless

lags

that are not

sufficiently

small for the true

asymptotic

behavior to

develop.

Assuming

that

experiments

in

larger

systems can be

conducted,

the results should be useful to the identification of the correlation structure of the pore-space in porous

media,

based on saturation measurements under conditions of slow

drainage,

where

capillary

effects

predom-

inate. The results near

percolation

in this paper

complement

those of reference [10] in the continuum

regime,

far from

percolation.

Acknowledgments

The work of

C-D-,

B-X- and Y-C-Y- was

partly supported by

DOE Contract No. DE-FG22- 93BC14899. The collaboration between the two groups was facilitated

by

NATO Grant No.

CRG 901053 and

by

a limited

appointment

of Y-C-Y- as Associate Researcher of the CNRS.

All these sources of

support

are

gratefully acknowledged.

We would also like to thank J.-F.

Gouyet

for

pointing

out an

important

ommission in the

original

draft of the

manuscript.

References

[1] Wilkinson D. and Willemsen

J-F-,

J.

Phys.

A: Math. Gen. 16

(1983)

3365.

[2] Feder

J., Fractals, (Plenum,

New

York, 1988).

[3] Wilkinson

D., Phys.

Rev. A 30

(1984)

520.

[4]

Sapoval B.,

Rosso M. and

GouyetJ.F.,

J.

Phys. (Parts)

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Rosso M. and

Sapoval B., Phys.

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Halperin B-I-, Phys.

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961 and references therein.

[6] Hulin

J-P-,

ClAment

E.,

Baudet

C., Gouyet

J-F- and Rosso

M., Phys.

Rev. Lett. 61

(1988) 333; Gouyet J-F-,

Rosso

M.,

ClAment

E.,

Baudet C. and Hulin

J-P-, Hydrodynamics

of

Dispersed Media,

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Hulin,

A-M-

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and F.

Carmona,

Eds.

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Birovljev A., Furuberg L.,

Feder

J., Jossang T., Maloy

K-J- and

Aharony A., Phys.

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[8] Chaouche

M.,

Rakotomalala

N.,

Salin D. and Yortsos

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N.,

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Xu B. and Yortsos

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T-A-,

paper SPE 15386

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at the 59th Annual Technical Conference and Exhibition of the

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of Petroleum

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J. and Yortsos

Y-C-, Transport

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J. and Yortsos

Y-C-,

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Du

C.,

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B.,

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Carrier

G.F.,

Krook M. and Pearson

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New York

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R-F-,

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Algorithms

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Eamshaw, Ed., (Springer-Verlag,

Berlin

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W.,

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Bacri

J.-C., Hoyos M.,

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