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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�
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 ChemicalEngineering
and PetroleumEngineering Program, University
of SouthernCalifornia,
LosAngeles,
CA90089-1211,
USA(~) Laboratoire
Fluides, Automatique
etSystAmes Thermiques,
Bitiment 502,Campus Universitaire,
91405Orsay Cedex,
France(Received
30January
1995, revised 15 December 1995, accepted 22January1996)
PACS.05.40.+j Fluctuation
phenomena,
random processes, and Brownian motion PACS.05.90.+m Other topics in statisticalphysics
andthermodynamics
PACS.06.30.Bp Spatial
dimensions(e.g., position, lengths, volume, angles, displacements, including
nanometer-scaledisplacements)
Abstract. We
study
thespatial
correlation of one-dimensionalI-D)
saturationprofiles
ob-tained
during
slowdrainage
in porous media, wherecapillary
effectspredominate. Using
prop-erties of Invasion Percolation in an uncorrelated
medium,
we compute the correlation structure of theprofile.
At small values of thelag (but
forsufficiently large systems)
theprofile
ap-proaches
the structure of the record of afractional
Browman motion(mm)
with Hurst exponent H=
(D -1) /2,
where D is the fractal dimension of thepercolation
cluster.Sufficiently
far frompercolation,
theprofile
isa white noise. Noise measurements in
displacement
experimentsusing
an acoustic
technique
arereported
for the 3-D case. Thetheory
is confirmed with 2-D simula- tions. An apparent mismatch in the 3-D case is attributed to finite-size effects. Theapproach
is
generalized
to correlatedpercolation.
R4sum4. Nous avons 6tud16,
th60riquement
et h l'aide de simulationsnum6riques,
les cor-r6lations
spatiales
desprofils
de saturation obtenus au cours de l'invasion d'un milieu poreux par unephase
non mouillante(drainage).
La saturation(concentration volumique)
de laphase
envahissante est
moyennde
dans la directionperpendiculaire
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 lastructure des corr61ations approche un mouvement Brownien fractionnaire
(fractional
Brownianmotion
(mm))
d' exposant de Hurst H=
(D -1)/2,
ok D est la dimension fractale de I' amas depercolation.
Suffisamment loin du seuil depercolation,
la structure des corr61ations duprofil
de saturation est d6crite par un bruit blanc. Des mesures de bruits au coursd'exp6riences
de d6-placement
1l'aide d'unetechnique
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 etexpdrience
d'autre part, est attribude h des effets de taille finie. Les r6sultats sont ensuite
g6n6ralis6s
au casde la
percolation
corr416e.(*)Author
for correspondence(e-rnail: yortos@euclid.usc.edu)
@
Les(ditions
dePhysique
19961. Introduction
The slow
displacement
of awetting phase
from a porous mediumby
theinjection
of a non-wetting phase,
immiscible to the former, has beenanalyzed
in muchdetail,
due to the relevance of the process toengineering applications,
such as oil recovery andgroundwater 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]
havebeen used to describe these processes in uncorrelated random porous
media,
in the absenceor presence of an external
gradient, respectively. Recently,
theproperties
ofpercolation
in correlatedmedia,
the correlation function of whichdecays algebraically,
e-g-C(p)
r~~
p~~/,
where-)
<il
< o andv is the correlation
length
exponent, have also been uncovered[5].
Typically, laboratory displacement experiments
in porous media areperformed
in geome- tries of a uniform cross-section in the direction ofdisplacement
x(e.g.
rectilinear orcylindrical cores).
The mainquantity
of interest is the saturation of thenon-wetting (invading) phase, Six, t),
which denotes the volumetric fraction of the pore-spaceoccupied by
thenon-wetting phase, transversely averaged
over the cross-section(yz).
Thisquantity
can be measuredusing
various
diagnostic methods, including acoustics, X-rays,
etc., in order to infer various char- acteristics of thedisplacement.
Forexample,
in the case ofIPG,
theslope
of the saturationprofile
near the frontgives
a measure of thegradient applied [6-8].
For the case ofIP,
the fluctuation of the saturationprofile
furnishes additional information on the medium and the process. This information would be ofparticular interest,
forexample,
if it indicates a cor- related pore-space[9,10].
In an earlierinvestigation using
a continuummodel,
Yortsos andChang [10] pointed
out that the saturationprofile
can reveal the characteristics of theunderly- ing
pore structure,provided
that thedisplacement
is controlledby capillarity
and the process is away frompercolation.
To ourknowledge, however,
astudy
of the correlation structure ofthe
profile
nearpercolation
has not beenattempted.
The
objective
of thisinvestigation
is tostudy
the structure of the fluctuation of the saturationprofile during drainage,
both near and far frompercolation. Because,
in ourcontext,
slowdrainage
isequivalent
toIP,
theproblem
is alsoequivalent
to theanalysis
of the fluctuations of theoccupation profile
of IP. In this paper, we firstdevelop
atheory
based on the correlationproperties
ofpercolation
processes, which issubsequently
tested ~vith the numerical simulationof the process in 3-D and 2-D lattices.
Experiments
in uncorrelated porous media are alsoconducted and
provide
a test of thetheory
in 3-D.Theory
and simulations are then extended to correlatedpercolation problems,
where the correlation functiondecays algebraically.
2.
Theory
2.1. 3-D GEOMETRIES. We consider slow
drainage (invasion percolation)
in a rectilinear porousmedium, represented
as a 3-D cubic lattice of extent L x L x N(N
>L) (Fig. I).
No-flow
boundary
conditions areapplied
at the lateralsides,
thedisplacement being
forced in the direction x.During
the invasion process, a frontdevelops
at theleading edge
of thedisplacement,
the extent of which increases until it becomescomparable
to the lateral extent L. Within thisregion,
the mean saturation varies with bothtime,
t, andposition,
x,leading
to a
non-stationary profile.
Of interest to this paper is thespatial
fluctuation of the saturation in theregion following
the front, where the mean saturation isapproaching
asteady-state,
andthe
profile
is closer tobeing stationary.
Let
9(r)
denote an indicatorfunction, equaling
I or o when the site is or is notoccupied,
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 thepercolation
cluster and E is thedimensionality
of thesystem. Hence,
we obtain thefollowing 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 functionR(h
e<S(x)S(x+ h)
>. where all distances have been normalized with the mean porelength,
I. To
develop
anexpression
forR,
we use the correlation functiong(r)
=<91r')9(r'+ r)
>(3)
which denotes the
probability
that a site at a distance r=
jrj
from anoccupied
site is alsooccupied (it belongs
to the samecluster). Then,
~ g(r)
<
S(x)S(x
+h)
>" ~~~
(4)
the sum
being
over all r that connect everypoint (yo, zo)
on theplane
x with everypoint (y, z)
on theplane
x + h(Fig. 2a).
We know that nearpercolation, g(r)
behaves asg r~J
Crl~-~l (5)
where the
prefactor
scales as C r~~< 9 >r~~Ll~~~)
theexponent
iii(5) gives
thescaling
for an IPproblem
and differsby
a factor of 2 from the OP exponent used in ourprevious
~ h _ L
y,z
L ~Y0'~0
~---~- ~---
"
' ' '
' ' '
/ ' /
a)
~ ~ ~~~1,o i,i
c b
yo>zo
d a
b)
0,0 1,0Fig.
2. Illustrations of the notation used:a)
3-D lattice,b)
Partition of the yz plane for theevaluation of the
integral.
publication [11]. Hence,
to evaluate the sum in thisregime
isequivalent
tocomputing £~ r~°,
where we have denoted a
#
(D 3) /2 (note
that -o.235 <a <
o).
To
proceed,
wereplace
the sumby
anintegral
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 distancesby L,
the rescaled variablesvarying
in[o,I] (Fig. 2b),
andproceed by keeping
theprevious
notation for the sake of convenience.Then,
theintegral
in(6)
readsK =
L~~+~ / / / /
(p~
+e2)"dydzdyodzo
+L~°+~I(e) (9)
yo,zo,y,z
where we introduced the
variable,
e= h
IL.
To evaluate thequadruple integral
I wepartition
theplane
yz as shown inFigure
2. After somealgebra,
I reduces toI(E)
= 4/ / (1- v)(i z)(v~
+ z~ +
e~)"dydz (lo)
~ ~
Before we
proceed
with the numerical evaluation of(lo),
we will evaluate itsasymptotic
be- havior in the limit of small e. For this we note that I consists of the sum of thefollowing
threeintegrals
~
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 bereadily
obtained. After somecalculations,
we find~~~~ ~~~~
(° )
i) ~~~~~
~~~~~~
~~~~I~(e)
=i~(o)
+o(e2a+3) (is)
ere
we
1
~2a+2where
~ ~
I(o)
= 4(1 y)(I z)(y~
+z~)°dydz (18)
which can be also
expressed
in terms ofincomplete
Betafunctions,
if necessary. We note(by converting
in radial coordinates andmaking
use of the result 2a +1 >-1)
that theintegral
in
(18)
exists. Back substitution inequations (4)
and(9) gives
theasymptotic
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)
isconsistent,
in the limit h -o,
with the result <S~
>r~~L~l~~~l
of(2), given
the
scaling
with L of theprefactor
C.Typically,
one is interested in thesemi-variogram, SV,
which in terms of theoriginal
defini-~~°" ~~~~~
sv +<
(s(x
+h) s(x))2
>m~ ij (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
~~
0-'
~ _- -4
a) ~°~ ~~~~~
-1
d3
-2.5 -2 -1 .5 -1 -0.5 0b)
~°~ ~~~~~Fig.
3. Numerical evaluation of thesemi-variogram plotted
vs the dimensionlesslag
hIL
for inva- sionpercolation: a)
3-Dgeometries, b)
2-D geometries. The dashed lines are the asymptotictheory predictions
withslope
2a + 2 = 1.53 for 3D and 2a +1= 0.896 for2D, respectively.
This behavior is similar to the
(self-affine)
trace of a fractional Brownian motion with Hurstexponent [12]
H =
~
~
(23)
which in the
present percolation problem (with
or withouttrapping)
reads H m 0.765. This exponent is different from the onereported
in[11],
where a differentscaling
of the correlation function was used.The numerical evaluation of
(21)
isplotted
inFigure
3a. Theasymptotic
behavior at smalle is consistent with
(22), provided
that the dimensionlesslag
is smaller thanapproximately
0.01. The rather small range of the
validity
of(22)
must be taken into consideration in theinterpretation
of the numerical simulationsreported
below.The above is
applicable
nearpercolation.
For a system away frompercolation,
thepair-
connectedness function takes thedependence,
gr~~
exp(-r If).
where the correlationlength (
is assumed much smaller than L. We can calculate the correlation functionby proceeding
asbefore and write
1(e, b)
= 4
j j ii y)ji z)
exp
(-j(y2
+ z2 +2)1/2j dydz 124)
~ ~
To derive the
asymptotic
behavior of I in the limit b e)
~ 0 we
apply
tvice theLaplace
method for theasymptotic
evaluation ofintegrals [13]
to obtain1(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 asignal
correlated over distances of order(.
For suffi-ciently large h, therefore,
theprofile
has the correlation structure of a whitenoise,
asexpected.
2.2. 2-D GEOMETRIES. A similar
approach
can beapplied
for 2-Dgeometries. Consider, first,
the behavior nearpercolation. Now,
the calculation of theintegrals
iseasier;
forexample,
theintegral corresponding
to(10)
reads1(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 theleading
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 thepositive
constanta =
/ (v~°
(v~
+i)a) dy (31)
Since a <
0,
theintegral
converges.Thus,
one arrives at thefollowing expression
for the autocorrelation function<
S(x)S(x
+h)
>r~~<S~
> I c~
l+ O(e) (32)
L
~~~~
where we introduced the
positive
constantc =
2a(20
+1)(a
+1) (33)
Equivalently,
we may write<
(s(x
+h) s(x))2
>r~~ 2c <s2
>((
~~(34)
where the Hurst
exponent
is now, H=
(D
E+1) /2
=(D -1) /2. Hence,
weexpect
H m 0.4I for IP withtrapping
and H m 0.448 forOrdinary
Percolation(OP)
or for IP withouttrapping.
As in the 3-D case, this result differs from Du et al.
ill].
Figure
3b shows aplot
of the SV for the 2-D case. Theasymptotic dependence (34)
is well satisfied for values of the dimensionlesslag
smaller thanapproximately 0.I,
which is a factor of10larger
than in the 3-D case. This behavior should also be considered wheninterpreting
the simulation results below.Away
frompercolation,
a similarapproach applies.
We consider anexponential pair-
connectedness function as before.Then,
the behavior of theintegral
1(e, b)
= 2~ (1 y)
exp(-b~~(y~
+e~)~/~j dy (35)
is
sought
in the limit b=
( IL
« I. Its evaluation isstraightforward using Laplace's
method[13]
leading
to the resultI(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 begeneralized
to correlatedpercolation
[5]. We will restrict our attention topercolation
in lattices with a correlation function ofalgebraic decay, C(p)
r~~
p~~,
where-)
<k
<0,
and v is the correlationlength exponent
of uncorrelatedpercolation.
In such cases, results are available for theordinary
per-colation
problem,
but not for thecorresponding
invasionpercolation problem.
The correlation function still scales as in(5),
where the fractm dimension is obtained from D= E
(,
where)
and Pare
percolation
and correlationlength exponents, respectively,
of the correlated per- colationproblem.
Isichenko [5] has shown thatexponent j
is identical to that of uncorrelatedpercolation
in thecorresponding dimension, j
=
fl,
but that exponent P is not, if)
<fl
< 0,where it is
given by
P=
). Nonetheless,
theprevious approach
is stillapplicable. Proceeding
as
above,
we find that the exponent Hdescribing
theearly
part of the SV for thisproblem
isH =
~~
+ l
(37)
in 3-D and
H
=
~~
+
l/2 (38)
in
2-D, respectively. Therefore,
in the correlatedpercolation
case, H varies in the interval[0.765, lj
in 3-Dgeometries,
and in the interval[0.41, 0.5j
in 2-Dgeometries.
Thissuggests
thepossibility
that at least in theappropriate
range, the trends of the 3-Dprofile (where
H >0.5)
are
persistent,
while those of the 2-Dprofile (where
H <0.5)
areanti-persistent [2j.
This conclusion was also reached in[I ii, although
with different values of theexponent. Away
frompercolation,
weexpect
the correlation structure of theunderlying
lattice to emerge.3. Simulations
To test the
theory,
numerical simulations ofordinary
and invasionpercolation,
in2-D,
un-correlated or
correlated,
lattices and in 3-D uncorrelated lattices were conducted. For the case of correlatedpercolation,
the correlated lattice was createdusing
the method ofMidpoint
Displacement
and S~ccessive Random Additions[14].
The various results are summarized inTable I. Hurst
exponent (H ) for
various processes nearpercolation
Process
Dimension/Type Fieldk
Latticesize SimulationTheory
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
/
sitek
= 0.0 512 x 512 0.54 fBm 0.500 fBm
OP 2D
/
sitek
= -0.2 512 x 512 0.48 fBm 0.486 fBm
2D
/
sitek
= -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
/
sitek
= -0.8 512 x 512 0.40 fBm 0.448 fBm
Table II. Hurst
exponent (H ) for
vartous processesfar from percolation
Process Dimension Field
k
Lattice Size < S > SimulationTheory
3D
lo x 10 x 500
~~~d°m x x
4° 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
saturationprofiles
near and far frompercolation
for the 3-D IP caseare shown in
Figures 4top
and4bottom, respectively.
Because the abovetheory
is based on theassumption
of awell-developed percolation
state, in all IPproblems
weanalyzed
thepart
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)
atbreakthrough
of theinvading phase, (bottom)
at conditions away frombreakthrough.
of the
profile
away from theinvading
front and from the inlet to minimize finite-size effects.In an
analogous study [8],
alength-to-width
ratio of two wasused,
and the middlepart
of theprofile
wasanalysed.
The fluctuations wereanalyzed
in various ways,by constructing
thespectral density,
thesemi-variogram
or theR/S
curve[2,9]. However, consistently
reliable results were obtainedonly
from thesemi-variogram,
the other two indicators oftensuffering
from
large
local correlations.Figure
5 shows theplot
of thenumerically
determined exponentHn~m
vs its theoretical value for aprofile
nearpercolation.
The raw data used are described in detail in Table I. The datareported
are ensemble averages over 10 realizations(in
the standardcase).
It is apparent thattheory
and simulation agreereasonably
well for the 2-D case, theagreement being
better for the OP case(where
theprofile
of thelargest
cluster atpercolation
wasanalysed).
Ingeneral.
however,
the numerical resultsunderpredict
the theoretical value. In3-D, only
random latticeswere used. For this case, there is a noticeable difference between theoretical and numerical
predictions.
We attribute this mismatch to finite-sizeeffects,
which appear to diminishslowly
with increased size
(compare
the first three entries in Tab.I).
Finite-size effects are alsopresent
in2-D,
the trendbeing
in theright 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 showstypical plots
of the SV of the numerical simulation results in 3-D and 2-Dgeometries.
Because ofcomputational
lim-itations, the 3-D simulations are restricted to
generally
smallsizes,
hence thecorresponding
dimensionless
lag,
hIL,
istypically larger
than 0.01. In that range,however,
the behavior of the theoretical SI~ does notstrictly
follow(22),
as shown inFigure
3a. As aresult, attempting
~ 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 anmm
signal
for a system nearpercolation ((x)
denotes 2-Dresults, (+)
denotes 3-Dresults).
to
interpret
these simulations with apower-law scaling
leads to a value smaller thanexpected,
as indeed shown in
Figure
5. On the otherhand,
in 2-Dgeometries
the lattice sizes arelarger (Fig. 6b),
and the dimensionlesslag
is within theregion
where theasymptotic
behavior(34)
holds
(compare Fig.
3b andFig. 6b).
A closeragreement
is thusobtained,
as shown inFigure
5.Table II shows results
corresponding
to asystem
away frompercolation.
Agenerally good agreement
was found betweentheory
andsimulation, although
results are better for OP rather than IP. The transition from fBm to fGntype
noise as we move away frompercolation,
isclearly
observed in all cases studied(compare
Tab. I andII). However,
the rate ofapproach
to an fGnsignal
as thepercolation probability
increases was found to be muchslower, namely
tooccur at
higher
mean saturationvalues,
in IPcompared
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 thepercolation regimes,
theexperiments
wereconducted in the presence of a small amount of
gravity, corresponding
to Invasion Percolation in a Gradient. Inprevious
studies[4-8],
it was shown that IPG shares many of the features of GradientPercolation, namely
it contains aleading
front of width aftr~~
Bj"/l~~"I,
where theproperties
of IP areexhibited,
followedby
acompact
pattern. The correlation structure isexpected
tocorrespond
to IP atpercolation conditions,
near thefront,
and to IP far frompercolation,
upstream from thefront,
thus weanticipate
the twoprevious scalings
to emergenear and far from the
front, respectively.
In the
experiments,
alighter density non-wetting
fluid(nonane)
wasinjected
at very lowrates
(with
thecapillary
number, Ca=
qp/~i, equal
to10~~,
where q denotes the flowvelocity,
p the
viscosity
and ~i the interfacial tension between thefluids)
todisplace
a heavierwetting
-1 .5
~.5
-2 -1.5 -1 -0.5 0a)
~°~~~~~~> 0
$
G-1
~~3
-2.5 -2 -1 .5 -1 -0.5 0log (h/L) b)
Fig.
6.Typical semi-variograms
of saturationprofiles
from numerical simulations:a)
3-D Invasion Percolation in a lattice 200 X 200 X 400,b)
2-D Invasion Percolation ina lattice 1000 X 2000. Solid lines denote fitted
straight
lines withslope
1.19 for 3D and 0.896 for 2Drespectively,
where slope = 2H.fluid
(water)
in the direction fromtop-to-bottom.
The porous medium consisted ofglass
§eads
of diameter a= 100 pm
(permeability
5Darcy) packed
in a rectilineargeometry
of dimensions 4 x 2 x 30cm~ corresponding
to a 400 x 200 x 3000 network.Hence,
the effective size for theanalysis
of theexperimental
correlations is about 200. This should be taken into consideration in theinterpretation
of theexperiments.
Care was takenduring packing
to ensuregood mixing
of the beads in order to avoidlong-range
correlations. Thecorresponding gravity
Bond
number, Bg
=
~~~~~,
whereAp
is thedensity
difference andg the acceleration of 'f
gravity,
was estimated atBg
=10~~
Saturation data were obtainedby
an acoustictechnique
described elsewhere[15],
which allows for aspatial
resolution of1 mm with an accuracy of10~3
in saturation. The far frompercolation regime
is ensuredby
acapillary barrier,
whichallows a
large
increase in the saturation up to S= 0.60.
Typical
saturationsprofiles corresponding
to the tworegimes
are shown inFigure
7 with thecorresponding
power spectra shown inFigure
8.Here,
we relied onspectral analysis
todetermine the
scaling
of the correlation of the fluctuations. We recall that the powerspectral density
function scales as [16]S(f)
r~~
f~~~~~
for an fBmsignal
and asS(f)
r~~
f~~~~
for an fGnsignal.
The data away from the threshold(open
circles inFig. 8)
show aslope
close tonearly
zerocorresponding
to uncorrelatednoise,
inagreement
with thetheory.
These results0.8
0.6 S 0.4
0.2
0 0.2 0.4 0.6 0.8
x~
Fig.
7T- Saturationprofile
fromdisplacement experiment:
bottom curve atbreakthrough
of theinvading
fluid; top curve away frombreakthrough.
",,
~,~~
~
',i~ ",
~ ',
4J .,.
't3 o
- o
t4 '<,
b
° ° QjIn°~
Q
4~ '.
+ ~
o.oi o.i
wave vector
Fig.
8.Log-Log plot
of thespectral density
of the saturation versus thespatial
wave-vector. Full squarescorrespond
to data in thevicinity
of thepercolation threshold,
open circlescorrespond
to theregime
away frompercolation.
The dashed line of slope -2corresponds
to H m 0.5 mm. Thehorizontal line corresponds to H m 0.5 fGn.
tend to confirm the uncorrelated structure of the
underlying glass
beadpack.
On the otherhand,
nearpercolation,
thelogs log f
data(squares
inFig. 8)
can be fitted with astraight
line of
slope
m -2(dashed line) corresponding
to an fBmsignal
with H m .5. This is incontrast to the 3-D theoretical
prediction
of H m .765(although
in betteragreement
withthe
simulations).
As in the latter case, we attribute this difference to finite-size effects. As a result of the small size of theexperimental
crosssection,
the dimensionlesslag
in theanalysis
of theexperiments
varies in a rangeexceeding 1/200,
which is notsufficiently
small to allow for a critical test of theasymptotic prediction (compare
withFig. 3a). Thus, interpreting
the available data with a power law leads to anunderprediction
of theexponent,
much like in the numerical simulation case.Experiments
in correlated media were not conducted due to lack ofa model porous medium of a controlled correlation structure.
Progress
in this direction would bedesirable,
as many natural porous media are correlated at various scales.5. Conclusions
In this paper, a
theory
wasdeveloped
thatpredicts
the correlation structure oftransversely averaged
saturationprofiles during
slowdrainage,
wherepercolation
processes are involved.The
theory
indicates that nearpercolation,
theasymptotic
behavior of thesemi-variogram
at small values of the dimensionlesslag
has thegeneral
characteristics of the record of an fBmsignal,
with trends that arepersistent
for the case of 3-Dgeometry
andanti-persistent
for the2-D case,
regardless
of the correlation of theunderlying
lattice. Thetheory
_was confirmedwith numerical simulation in 2-D lattices. Simulations and
experiments
in 3-Dlattices,
how- ever,underpredicted
theasymptotic exponent.
This difference was attributed to the small network sizesused,
which result in dimensionlesslags
that are notsufficiently
small for the trueasymptotic
behavior todevelop.
Assuming
thatexperiments
inlarger
systems can beconducted,
the results should be useful to the identification of the correlation structure of the pore-space in porousmedia,
based on saturation measurements under conditions of slowdrainage,
wherecapillary
effectspredom-
inate. The results near
percolation
in this papercomplement
those of reference [10] in the continuumregime,
far frompercolation.
Acknowledgments
The work of
C-D-,
B-X- and Y-C-Y- waspartly supported by
DOE Contract No. DE-FG22- 93BC14899. The collaboration between the two groups was facilitatedby
NATO Grant No.CRG 901053 and
by
a limitedappointment
of Y-C-Y- as Associate Researcher of the CNRS.All these sources of
support
aregratefully acknowledged.
We would also like to thank J.-F.Gouyet
forpointing
out animportant
ommission in theoriginal
draft of themanuscript.
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