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Non-Homogeneous and Irregular Interfaces: Electrodes and Membranes
M. Filoche, B. Sapoval
To cite this version:
M. Filoche, B. Sapoval. A Simple Method to Compute the Response of Non-Homogeneous and
Irregular Interfaces: Electrodes and Membranes. Journal de Physique I, EDP Sciences, 1997, 7 (11),
pp.1487-1498. �10.1051/jp1:1997143�. �jpa-00247465�
A Simple Method to Compute the Response of Non-Homogeneous
and Irregular Interfaces: Electrodes and Membranes
M.
Filoche (*) and
B.Sapoval
Laboratoire de
Physique
de la MatikreCondens4e, icole Polytechnique,
91128 Palaiseau Cedex, France
(Received
23April
1997, revised 7July1997, accepted
23July 1997)
PACS.05.60.+w
Transport
processes:theory
PACS.47.53.+n FractalsPACS.82.65.Yh Other surface and interface chemical processes
Abstract. We present a detailed numerical test of the
coarse-graining
methodproposed by
Sapoval to compute the fluxthrough
anirregular
interface in the case where the local response isinhomogeneously
distributed. It isshown, through comparison
with detailed finite elementssimulations,
that this method permits to deduce the flux across anirregular
interface from itstopography only,
as forexample
in the case of non-uniformpolarizability
inelectrochemistry.
The interest of the method lies in its
computational simplicity.
It then constitutes an essential step towards theunderstanding
of the flux acrossirregular
interfaces in non-linearregimes.
Introduction
We consider here the linear
transport
acrossirregular interfaces,
a commonphenomenon
in many natural or industrial processes. Oneexample
is the electrical response of electrodes incontact with
electrolytes.
Anotherexample
is thetransport
to and across a membrane whereneutral
reacting species
arebrought
to the surfaceby
diffusion currents instead of electricalcurrents in electrochemical
systems.
The sameproblem
arises in theEley-Rideal
mechanism inheterogeneous catalysis
where reactants have to diffuse to acatalytic
porous surface in order to react. Its&equent
occurrence and itspractical importance
hasjustified
numerous studies of the influence of the interfacegeometry
on the net flux across such interfacesill.
Flactal
geometry
has beenextensively
used as a model for extremegeometrical irregularity
for several reasons. It first
provided
somehope
to better understand theubiquitous
constantphase angle
response inelectrochemistry [1,2].
Thepossible
role of the fractal structure of the interface has beenextensively
studied and several results have beenobtained, especially
in 2-dimensionalsystems.
For a review 6f theearly
works on &actal electrodes see[1,2]
and thereferences therein.
Secondly
one canhope
thatunderstanding
the behavior of fractal electrode would lead to theunderstanding
of the role ofgeometrical irregularity
ingeneral
even when it is not fractal. This secondgoal
has beenpartly
realized for the linear response of 2D-electrodes ofarbitrary geometry [3,4].
(*)
Author forcorrespondence (e-mail: marcel.filochetlpolytechnique,fr)
©
Lesiditions
dePhysique
1997The purpose of this paper is first to extend the finite scale renormalization
procedure,
pro-posed
in[3],
to the case of anirregular (self-similar)
electrode with a nonhomogeneous
distri- bution of the localtransport parameter.
This finite size real space renormalizationprocedure
was called the
"rope
walk" in reference [5]. It is called here "the landsurveyor"
method because it is based ongeometrical
measurements made on thetopography
of the electrode.Our second motive is to
explore
the use of finite elements method tocompute
numerical solutions of theLaplacian
field with mixedboundary
conditions. Thistype
of method isrequired
in order tostudy
the non-linear response ofirregular
interfaces.We
study
here situations where both thegeometry
and the localtransport properties
areirregular.
We first recallbriefly
the nature of theproblem
that we address. Consider the electrochemical cell shown inFigure
la. The response of this cell isgoverned by
theresistivity
p of the
electrolyte
andby
the rate ofcharge
transferoccurring
at the interface. We restrictour
study
to the case where the smallestgeometrical
feature I of thegeoInetry
is muchlarger
than the
Debye length. Consequently
we may use theLaplace equation
AV= 0 instead of the Poisson
equation
for the electricalpotential
in the bulk of theelectrolyte.
Thetransport
equation
in the voluIne is J= -i7V
/p
where J is the vector current in theelectrolyte.
The rate of
charge
transfer at the interface is characterizedby
a resistance per unit surfacer
(known
as the Faradaicresistance) and,
if any,by
acapacitance
r~ per unit surface butwe restrict here to the
study
of the Faradaicd.c.-response.
Hence the current at the surface isJn
=
-V/r
where V is the localpotential
in theelectrolyte
at soInepoint "very
near"the interface. Here the Faradaic resistance r has a space
dependence r(s)
as a function of the curvilinear abscissa s as indicated inFigure
la. We then consider theDC-probleIn
asillustrated in
Figure
la where the outer electrode is atpotential Vo
and the inner electrode at zeropotential.
Due tocharge conservation,
the currentjn is
= -V
Iris crossing
the electrode surface Trust beequal
to the Ohlnic currentjn
=
-i7nV/p reaching
it froIn the bulk. As a consequence the d.c.boundary
condition can be written asv/v~v
~
r(s) /p
=
A(s). (i)
This introduces a local
physical length
scaleA(s)
in ourproblem.
From a mathematicalpoint
ofview,
theproblem
is to find theproperties
of theLaplacian
field on the surface with the so-called Fourier or mixedboundary
condition(I).
The role of thelength
A on the currentdistribution on
irregular
electrodes wasalready recognized
in the late forties in the case of thehomogeneous
response(with
uniformr) [6, 7].
The
equivalent
circuit of a cell like that ofFigure
la is made of two resistances in series:the resistance of the
electrolyte Ro
which isproportional
to theelectrolyte resistivity
p anddepends
on thegeometry
of thecell,
and the resistance of the electrodeZode
whichdepends
on r and on the
geometry
such thatZcell
"
R0
+Zode. (2)
Our aim here is to compute and discuss the electrode
impedance Zode.
The "Land
Surveyor"
MethodThis method
pernlits
inprinciple
tocompute Zode
from thetopography
of the electrode and the functionA(s) only.
It wasproposed
in reference [3]. We extend it tonon-homogeneous
surfaces. The idea is to substitute the
problem
ofLaplacian
transfer across the real electrode(which presents
a finite transferrate) by
aproblem
ofLaplacian
fieldobeying
the Dirichlet' j)
~~~~ ~ i~j)
~fi) ~/
s is the cu~ihnear coordinate along
this intedace
ELECTROLYTE AV =
L
V v~
a)
COARSE-GRAINING
lP ) j~
~
"
s'is the cu~ihnear coordinate along this new Intedace
L,(A 61) +-+
[~A 250
b)
Fig. 1. Top: schematic representation of the type of electrochemical cell under study. The elec-
trode has an
irregular
geometry schematized hereby
a self-similar fractal and also aninhomogeneous
resistivity r. In the example shown here the left part presents r =6pi
while theright
part presentsr =
25pi.
The curvilinear coordinatealong
the electrode geometry is s. Bottom: result of the coarse- graining procedure on the upper electrode. The curvilinear coordinatealong
this new geometry is s' and the perimeter of this new curve isL~,.
Thisfigure
isgiven
here as anexample:
thecomputations
have been carried on half of this cell.
boundary
condition(V
=
0)
but with a differentgeometry,
obtainedby
acoarse-graining
of the realgeometry
to aphysical
scale determinedby
thelength A(s).
The Dirichlet
Laplace problem (V
=
0)
onirregular
electrodes has beenthoroughly studied,
at least in d
= 2. Note that the Dirichlet
problem
is known as that of"primary
current dis- tribution" in the field ofelectrochemistry.
Morespecifically
animportant theorem,
Makarov'stheorem, describing
theproperties
of the current distribution on anirregular (possibly
frac-tal)
electrode can be used[8, 9j.
This theorem states that the information dimension of the harmonic measure(here
the harmonic measure is the normalized currentdensity)
on asingly
connected electrode in d
= 2 is
exactly equal
to I. This veryspecial property
of theLaplacian
field can be illustrated in thefollowing
manner: whatever theshape
of theworking electrode,
the size of theregion
where most of the current flows isproportional
to the overall size(or diameter)
L of the electrode under a dilation transformation.This result has a
simple
butprofound meaning
in terms of thescreening efficiency
of thegeometrical irregularity,
and this is what we use here. We consider thesimplest description
of anirregular
electrode: the ratio S=
Lp IL
of theperimeter length Lp
dividedby
its sizeor diameter L
[10].
This number S has a directphysical significance:
itreally
measures thescreening efficiency
of theirregularity
of the structure for DirichletLaplacian
fields. Whatever thegeometry,
if the active zone has a sizeL,
then as L=
Lp IS
the factor IIS
can be considered to be the"screening efficiency"
of theprimary
current distribution due to thegeometrical
irregularity.
This is thephysical significance
of Makarov's theorem.This result cannot be
applied
as such to an electrochemical cell because theboundary
condi- tion on the electrode is not V= 0 but V
li7nV
=
A(s).
We are then in the situation known as thesecondary
current distribution inelectrochemistry.
The realboundary
condition introduces thephysical
scale A in theproblem.
Theprocedure
that wasproposed
in [3] is to switch from the realgeometry obeying
the realboundary
condition to acoarse-grained geometry obeying
the Dirichlet
boundary condition,
with thecoarse-graining depending
on A. In a secondstep
one can use the
screening efficiency
of thecoarse-grained geometry
to find the active zone of theelectrode,
hence itsimpedance.
The discussion that wegive
now is ageneralization
of thisprocedure
as it wasproposed
in references[3-5].
We allow for the
general
situation where the surfaceresistivity
r is a functionr(s)
of the curvilinear coordinate s. This is what we call thenon-homogeneous
linear case. In order to obtainquantities
which can becompared
to measurements made on real electrochemical cellsill]
we introduce b whichrepresents
the thickness of the cellalong
the third d1nlension.We consider a
region
ofperimeter
ds around the curvilinear coordinate s. Itpresents
anelementary
admittancel§urf_
= 16
/r(s)]ds
which is snlaller than the "local access admittance"of order
b/p.
We call "local access admittance" the admittance of the small bulk area which is in front of thispart
of the interface. The value of this local access admittance does notdepend
on the area size since the admittance of a square of
electrolyte
with thickness b isequal
to Ya~~_ =b/p
whatever its size.One can then consider a
larger region
between curvilinear abscissa si and s2.Depending
onsi and s2 there exist two situations: if the curvilinear distance between si and s2 is
small,
thecurrent is limited
by
the surfaceimpedance.
On thecontrary,
if this distance islarge enough,
the current is limited
by
the bulk resistance to access the surface. But in the latter situationwe are, in a first
approximation,
back to the case of a pureLaplacian
field with theboundary
condition V= 0 since it is the access to the surface that limits the current.
The idea then consists in
coarse-graining locally
the realgeometry
to a scale such that theperimeter Lpi
in aregion
of size(or diameter) L~g,i
isgiven by
the condition that theintegral
of[b/r(s)]ds along
thatpart
of theperimeter
isequal
to the access admittance Ya~~=
b/p.
Equivalently
theintegral
ofds/A(s)
over that sameregion
should beequal
to I. Since such a definition of thecoarse-grained
diameter is difficult toimplement computationally,
we use instead the "local" chord between the curvilinear coordinates si
" s
A(s)/2
ands2 = s +
A(s)/2.
The chordlength Lc(s)
is thus defined as the distance between si and s2 in real space. In the case where r is aconstant, independent
of s, the above relation ex-presses
simply
that the curvilinear distance(or perimeter length)
between si and s2 isequal
to A
=
r/p.
Because of its
definition,
such aregion
can be considered asworking uniformly.
At thesame
time,
in the newcoarse-grained geonletry,
we aredealing
with a pure DirichletLaplacian
field. We then shift from the real
geometry
to thecoarse-grained geometry
which is made of successive chordsL~(si, s2), L~(s2, s3), L~(s3, s4).
In thecoarse-grained geometry
the curvi- linear coordinate is nameds',
as indicated inFigure
16. Theperimeter
of thecoarse-grained
electrode is named
Lp,.
Each element orgrain
of thecoarse-grained system
presents an ad- mittance which isequal
tob/p
so that the differential adnlittance of an element ds' isequal
to[b/pL~(s')ids'.
If there was noscreening,
the totalcoatse-grained
electrode would beworking uniformly
and its admittance would bellg,no
screening" 16
/pLc(8')jd8' (3)
~g
where the
integral
is takenalong
thecoarse-grained geometry.
But due to electricscreening
there exist an active zone, where most of the current arrives and apassive
zone with receivesonly
little current[11,12j
so that theintegral
can besplit
in:~~'~°
~~~~~~~~~
g,
active
~~~~~~~~'~~~~'
~~'
P"~~~~
~~~~~~~~'~~~~'
~~~The electrode admittance
(de
issimply
(de
"g, (b/pLc(s')ids'. (5)
active
Note that the
integrand
isonly
a function of the distribution ofr(s).
The admittance doesdepend
on theLaplacian
field distributiononly through
the determination of the active zone.Calling La~t.
thelength
of the active zone of thecoarse-grained electrode,
the aboveintegral
can be written
(de
"La~t.
lb/p] /
[I /L~(s')] (ds'/La~t ). (6)
cg, active
The
integral represents
the harmonic mean ofL~(s') along
the active zone. We define(L~)a~t.
as:
Our ypothesis,
using
an abrupt form of akarov'stheorem, is that the
active zone
have
a size
very
simple
expression
(de
~ (8)
This expression is
universally
valid. Atthis
stage the problem has been mplifiedwithoutany loss of generality
but
stillrequires to
in order to compute(L~)a~t. from quation (7).
One can go one step further
for
the wide ariety of systems forwhich one can
approximate
harmonic
namely
Lc)Q].
cg <
Due
to the fact that the harmonic mean is dominatedby
the small valuesof
~(s'), thisapproximation
is
validunless the allestvalues
ofthe
hord length L~ are foundonly
non-active egion
of the
electrode. A counter-example toequation (9) could then
be the
pecialcase
of
deep fjords withnarrow
ccess annels and small values of Lc only~
~~~
n= I
/
n=3
Fig.
2. Fractal mesh used in the finite element computation. Thefigure
presents the hierarchical construction of the mesh skeleton at a givengeneration.
This mesh skeleton will be the basis of a set of meshes at this generation. Here thebuilding
of a third generation mesh skeleton is shown.In all other cases the harmonic mean of the chord
length
will be the same if takenalong
the active zone oralong
the totalcoarse-grained
structure. The admittance is nowlGde
=ib/P)iL/iLc)). (lo)
We then obtain a very
simple
statement: theimpedance
of anirregular
electrode in d= 2 is
simply
the squareimpedance p16
of theelectrolyte
dividedby
the number of chords needed tomeasure the size
(or diameter)
L of the electrode. Thisapparently simple
result is not trivial.It expresses how the resistance of the electrode
depends
on theelectrolyte resistivity
and an average chordlength corresponding
to aperimeter
oflength A(s).
Thegeometry
enters herethrough
the relation between aperimeter
oflength A(s)
and its associated chord.As there exists an exact
mapping
between s ands',
such thatds'/L~(s')
=
ds/A(s),
the average chordlength given by equation (9)
can be writtenalso, working
on the initial noncoarse-grained geometry
/ Lcls)dS/AIS)
~~~~
f ds/Ajs)
~~~~I
#
I
g
g
o.
o. ~ to
Fig.
3. Example of different meshes at a given generation(here
thethird).
The initial skeleton is refinedby splitting
eachtriangle
in 4 identicaltriangles (by joining
the middle of the sides of theinitial
triangle).
Each mesh represents a new iteration of this operation.Note that in the case of a flat but
non-homogeneous
electrode, the local chordlength L~
isequal
toA(s)
=
r(s)/p
andequations (8, 9) give:
lGde
=(b/P)lL/Lp) /d8/AIS)
= b/dS/rls) l12)
since L
=
Lp
for a flat electrode. We then recover the known value of the electrode admittance for p= 0. In the
following
we will test thevalidity
of thisapproach
in different cases.Numerical Method
The electrode
impedance Zode
is obtainedby Zode IT)
=
Zceii IT) -Z~eii
IT =0)
whichcorresponds
to the
quantity
measured inimpedance spectroscopy.
Nunlerical solution of theLaplacian
problem
isperformed by using
a finite element method rather than a finite difference schemefor
efficiency
and accuracy purposes. This method will allow us also to extend later thisstudy
to non-linear
regimes.
The standard variational formulation of theproblem
is discretized witha
triangular
mesh andPi-Lagrange interpolation.
The linearsystem
obtained in such a way is solvedby using
theCholesky
method. To this end we use the Finite ElementLibrary
Modulef
[13].
In order to
compute
theimpedance
of theirregular
electrode with thegreatest
accuracy,we created a "fractal"
triangular
mesh of the structure(Figs.
2 and3)
which allows at thesame time a detailed discretization of the
boundary
and an economicmeshing
in the bulkareas where the variations of the electrostatic
potential
are smaller. The mesh of the structureat
generation
n + I uses five times the mesh atgeneration
n and atriangular
mesh of the squareplaced
under these five meshes(Fig. 2).
The number of nodes of thismeshing (which
represents
the number ofdegrees
of freedom and thus thecomplexity
of theproblem)
increases like 5" where n is thegeneration
of the fractalelectrode,
instead of 9" in the case of aregular
square mesh.
This method allowed us to
compute accurately
theimpedance
up to a sthgeneration
elec-trode on a standard Unix workstation
(Hewlett-Packard C160).
Thecomputation
time wasfrom I second to a few minutes for a
given
value of the surfaceresistivity
r.Results
We compare now the land surveyor method with direct numerical simulation of the
Laplacian
field in the electrochemical cell. Severalphysical
situations have beeninvestigated.
The
geometry
of the electrode isgiven by
the Viczek fractal(half
of the domain described inFig. I).
The bulkresistivity
p is takenequal
to Itogether
with the smaller cut-off I. A surfaceresistivity
requal
to 1corresponds
then to A= I
= I. The
geometry
of the bulkelectrolyte
under the electrode is
roughly
a square and it has beennumerically
verified for various cases that thecomputation
results do notdepend
on the distance between both electrodes as soonas it is
greater
than a few I.We first
compute
the response of the 4thgeneration
electrode with a uniform surface resis-tivity
r. In thishomogeneous
case it is well known that there exist twoasymptotic
behaviors for very small A(the
Makarovregime
for A <I))
and for verylarge
A(the
trivial uniformregime
for A »Lp).
In bothregimes
the electrodeimpedance
isproportional
to the surfaceresistivity
r. Between theseregimes,
theimpedance
of a "fractal" electrode follows a power law whoseexponent
isapproximately equal
to the inverse of the interface dimension.The results are shown in
Figure
4. Thegeneral
behavior of the land surveyor methodreproduces
the threeregimes.
Thediscrepancy
that we observe for A=
r/p
smaller than I is due to anexpected
flaw of the finite elements simulation consecutive to insufficient mesh at the interface. Thisregime (the
Makarovregime)
would need a much finer mesh in order to be studiedaccurately.
In this work we focus on theregime
where A=
r/p
> I which is the situation ofpractical
interest. As shown inFigure 4,
the "land surveyor method" is ingood agreement
with the nunlerical s1nlulation. Notonly
it follows both power law for I < A <Lp
and A >
Lp regimes
but itgives
also the crossover between theseregimes
without morecomplex computation
eventhough
these crossovers extend over alarge
range of A. Note that the small oscillations in the land surveyor criterium are due to apeculiarity
of ourspecific geometry:
two
points
which are faralong
the electrode can be very near in the real space(this
is(he
case
for
example
when A isequal
to theperimeter
of a square, forexample
A= 4i and A
=
20i)
leading
to an artificial small value of(L~).
Thisdivergence
is notmeaningful
and could be avoidedby using
the diameter of the"grain"
instead of the chordlength.
For all other tests~2
-numerical simulation
~ l
~ t C
~
~ w
#I
i "
~
.-
)
~
o'lo°
surface esistivity yin units of px? )
Fig.
4.Comparison
between the result of the "land surveyor method" and the numerical values of Z~de for the 4th generation electrode. One candistinguish
between threeregimes (Makarov regime
where A <
I,
intermediate regime where I < A<~L~,
andpurely
ohmicregime
whereLp
«A),
connected
through
two crossovers: one around A= I and the other around A
=
Lp.
Here I= 1 and
Lp
= 625.and due to
computation
timeconsiderations,
thegeometry
of theirregular
electrode will be a 3rdgeneration
Viczek fractal.The second test case is a
study
of a deterministicinhomogeneous
distribution of the localresistivity r(s).
Theresistivity
r varies from rmin to rmax=
10rmin along
the curvilinear coordinate s of the interfacegoing linearly
from the minimum value(on
the leftedge
of theinterface)
to the maximum value(in
the middle of theinterface)
and thendecreasing
until theopposite edge.
Thecomparison
between the exact numerical simulation results and the land surveyor method is shown inFigures
5 and 6. In this case, the results of the land surveyor method match almostexactly
the numerical simulation in allparts
of the curve. Theapproximation (7)
isextremely good
since the harmonic mean of the chordlength
is dominatedby
the smallest values which are found in the activeregions
of the electrode.We then
study
theopposite non-homogeneous
case, where the minimumresisitivity
is located in the least accessibleregions,
here the upperregion
of the electrode. The ratio between rmjnand rmax has been
kept
constantequal
to 10. Asexpected,
the land surveyor method fitsthe numerical simulation better in the
large resistivity
area of the curve. In the "fractal" or"power
law"regime, tfie
land surveyor method overestimates the admittance contribution of the lowresistivity part
of theinterface,
since thisportion
ispartly
screened. Nevertheless theratio between both methods never exceeds a factor 2 which means that our criterium can still be used to determine the order of
magnitude
of the electrodeimpedance
without any furthercomputation.
Notethat,
for thistype
ofsituation,
it ispossible
to compute theLaplacian
fieldon the new
coarse-grained geometry
to obtain the location of the activeregion
and then useonly
the firstpart
ofequation (7).
This wouldgive
a verygood approximation
of the electrodeimpedance
at a minimum cost(solving numerically
aLaplace equation
with Dirichletboundary
conditions in a
simplified geometry).
In the third case,
Figure 7,
we studied thevalidity
of our method in the case of a ran- dom distribution of theresistivity along
theinterface,
a most common case in real devices.o~
ff
-numerical simulation~f
~2 land sUrveyor method
_C
[
0'~i li
f
0° surface rests>iviw~ mini mum on<heedgesof ~eirreguia< elecfnDde
d~ and maximum in(he cenfe< pan
TJfl
~
,
dD 0
dD
lo~
10'~ lo° lo' lo~ lo~ 10~ 10~
minimum surface resistivity (in units of p x?
Fig.
5.Comparison
between the "land surveyor method" and the numerical simulation results foran
inhomogeneous
distribution of theresistivity along
the electrode: the local resistivity is small on the lateraledges
of the electrode and large in the middle part of the electrode. Note the perfectmatching
due to the
good
quality of approximationii).
~3
< -numerical simulation
k ~2 land surveyor method
3 e
j
< 10'
wI li
~ surface <esisovi~ is maximum on>he edges
( 0 of >hei«eguier erec><ode
~ andminimumin~ecenterpafl
w
13 10'
w w
,2
0° 0' O~ 0~ 0~ 0~ 0~
minimum surface resistivity in units ofp x I)
Fig.
6.Comparison
between the " land surveyor method" and the numerical simulation results foran
inhomogeneous
distribution of theresistivity
along the electrode: the local resistivity islarge
at theedges
and small in the middle part of the electrode. In this case the poorvalidity
ofapproximation ii)
leads to asignificative discrepancy
between bothmethods,
but even in this casethey
never differby
more thana factor 2.
The ratio between maximunl and minimunl
resistivity
iskept equal
to 10. As in the homo- geneous case, results show verygood agreement
between numericalcomputation
and the land surveyor method. This result wasexpected
since the smallest values of the chordlength
arehomogeneouslj
distributedalong
theinterface,
in both active andpassive regions.
o~
~p ~~3 -numerical simulation
j land surveyor method
(
oo
#I
I E
) ."
f
o~
10'~
inimum
surface esistivity (in units of p x I)
Fig.
7.Comparison
between the land surveyor method" and the numerical simulation results for aninhomogeneous
and random distribution of the resistivity along the electrode: as in thehomogeneous
case, the repartition of small resistivity values between active and
passive
regions of the electrode leads to a good matching between both methods.Conclusions
In summary we have
developed
a new method ofcomputing
the transferproperties
ofirregular
interfaces such as electrodes or
rough absorbing
membranes.Apart
from the interfacegeometry,
all that is needed are the values of themicroscopic transport
coefficients(here
for instance theelectrolyte resistivity
and the Faradaicresistance).
We have tested this method for variousnon-homogeneous
distributions of the surfaceresistivity.
The
general
conclusion that one can draw from this work is that the measurement of the electrodeimpedance
is agood approximate
measurement of the harmonic average of the chordlength corresponding
to aperimeter A(s).
Thesimplicity
of the method makes it agood
candidate for the
study
of the response ofirregular
interfaces in non-linearregimes
for instance when the local current across the electrode is related to the localvoltage by
a non-linearrelation
j
=
f(V).
All these results can beapplied
to thestudy
ofparticle
transfer acrossinhomogeneous
andirregular
porous membranes orcatalysts
as indicated inill.
Acknowledgments
The authors wish to
acknowledge
useful discussions with W.Dieterich,
B. Mandelbrot and M.Rosso. This research was
supported by
N-A-T-O-grant
C.R.G.900483. The Laboratoire dePhysique
de la MatiAre CondensAe is "UnitA de recherche associAe du Centre National de la RechercheScientifique
No. 1254".References
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