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Disordered porous solids : from chord distributions to small angle scattering
P. Levitz, D. Tchoubar
To cite this version:
P. Levitz, D. Tchoubar. Disordered porous solids : from chord distributions to small angle scattering.
Journal de Physique I, EDP Sciences, 1992, 2 (6), pp.771-790. �10.1051/jp1:1992174�. �jpa-00246600�
Classification
Physics
Abstracts61.10D 61.12D 61.40
Disordered porous solids
:from chord distributions to small
angle scattering
P. Levitz and D. Tchoubar
Centre de Recherche sur la Matibre Divisde, CNRS, lB rue de la Ferollerie, 45071 Orldans, France
(Received 4 March 1992,
accepted16
March 1992)Rdsumd. Les solides poreux
biphasiques
sont desexemples
de milieux interfaciauxcomplexes.
La diffusion aux
petits angles
(SAS)ddpend
fortement despropridt£s g£om6triques
de l'interfacepartitionant
le milieu poreux. Lespropri6t6s
de la d6riv6e seconde de la fonction d'autocorr61a- tion de densit6 d6flnitquantitativement
le niveau de connection entre la diffusion auxpetits
angles et les caract6ristiques statistiques de cette interface. Uneexpression
utilisable de cetteseconde d£riv6e,
impliquant
les distributions de cordes assocides h laphase massique
et au rdseau de pores, futpropos6e
parMering
et Tchoubar (MT). Mettant hprofit
lapossibilit6
actuelle d'une comparaison quantitative entre lestechniques d'imagerie
et la diffusion auxpetits
angles, cepapier
tente decompl£ter
et d'6tendrel'approche
MT. Dans unpremier
temps, nous montrons enquoi
la connaissance de ces distributions de cordes permet dedist1tlguer
certains types de d6sordres structuraux. Une relationexplicite
entre le spectre de diffusion auxpetits angles
et les distributions de cordes est alorspropos6e.
Dans une troisibmepartie, l'application
h diff6rents types de d6sordre est discut6e et lespr£dictions
du modmecompar6es
aux r6sultatsexp6rimentaux disponibles.
Par utilisation du traitementd'images,
nous nous int£ressons h trois types deddsordre : le milieu aldatoire de
Debye,
pour sespropridtds
hgrandes
distances, le ddsordre« corr616 » avec une attention
particuli~re
pour le cas d'un verre poreux (leVycor)
et enfin desorganisations complexes
ok despropri6t6s
d'invariance d'6chelle delongueur
peuvent dtre observ6es.Abstract. Disordered
biphasic
porous solids areexamples
ofcomplex
interracial media. Small anglescattering strongly depends
on the geometrical properties of the intemal surfacepartitioning
a porous system.Properties
of the second derivative of the bulk autocorrelation functionquantitatively
defines the level of connection between the smallangle scattering
and thestatistical
properties
of this interface. A tractableexpression
of this second derivative,involving
the pore and the mass chord distribution functions, was
proposed by Mering
and Tchoubar (MT).Based on the present
possibility
to make aquantitative
connection betweenimaging techniques
and the small
angle scattering,
this paper tries tocomplete
and to extend the MTapproach.
We first discuss how chord distribution functions can be used asfingerprints
of the structural disorder.An
explicit
relation between the smallangle scattering
and these chord distributions is thenproposed.
In a third part, theapplication
to different types of disorder iscritically
discussed andpredictions
arecompared
to availableexperimental
data.Using
image processing, we will consider three types of disorder : thelong-range
Debye randomness, the « correlated » disorder with aspecial emphasis
on the structure of a porousglass
(thevycor),
and,finally, complex
structures where length scale invariance
properties
can be observed.1. Introduction.
Disordered porous solids
play
animportant
role in industrial processes such asseparation science, heterogeneous catalysis,
oil recovery,glass
and ceramicprocessings [I].
The confinement and thegeometrical
disorder of these systemsstrongly
influence thedynamic
orthermodynamic
processes which can takeplace
inside the pore network[2].
This raises thechallenging problem
ofdescribing
themorphology
of these porous solids. A structuralanalysis
can be handledusing
a number oftechniques [3]
: direct observation of the massdistribution
by optical
or electronmicroscopy,
molecularadsorption,
direct energy transfer.Correlations at different
length
scales of the mass distribution aregenerally probed by
smallangle scattering (SAS).
It is well known that thedensity
fluctuations are the mainorigin
of thescattering.
In the case of abiphasic matrix,
these fluctuations are localizedjust
at thesharp
interface which
partitions
the system. Thesmall-angle scattering,
considered as apurely
interfacial
phenomenon [4],
is thenstrongly dependent
on thegeometrical properties
of this oriented interface. This statement can bequalitatively
understood if we consider a disordered porous medium ascompletely
defined eitherby
its mass distribution orby
the orientedinterface
separating
the « void » space from the« mass » part of the matrix.
Properties
of the second derivative of the mass autocorrelation functionquantitatively
define the level ofconnection between
small-angle scattering
and the statisticalproperties
of the interface[5, 6].
This has been known for a
long
time, almost for smooth and convexparticles.
As shownby
Guinier[7]
and Porod[8],
arelationship
between theshape
of a convexparticle
and itsscattering
can be madeusing
the concept of chord distribution. A chord is a segmentbelonging
to theparticle
andhaving
both ends on the interface. It can be considered as alinear
path
which correlates two distinctpoints
of the interface.Many
attempts have been made todevelop
thisconcept
further. Connections between small rexpansion
of the chord distribution and local or semi-localproperties
of the interface such as the curvature, theangularity
weredeveloped independently by
Porod[8], Mering
and Tchoubar[9],
Wu and Schmidt[10, 1II.
These different studies wereessentially dealing
with convexparticles
whereonly
one chord distribution was needed. Extension to abiphasic
porous solid(generally
anon-convex
structure)
is morecomplicated.
Thegeneral expression
of the second derivativeof the mass autocorrelation function involves a « delicate
» surface
integral,
as shownby
Ciccarillo et al.
[5]. Mering
and Tchoubar[12]
haveproposed
a more tractableexpression
of this secondderivative, involving
the «pore » and «mass » chord distribution functions.Several
hypotheses
are involved in theiranalysis (I)
the porous solid is considered as anisotropic biphasic
random media(it)
their derivation considers the distribution of matteralong
a random line(an
one-dimensionalanalysis)
;(iii)
aspecific
type of randomness where uncorrelation betweenadjacent
chords has to be assumed. At thistime,
in thesixties,
no attempt was made togive
anexplicit expression
of the smallangle scattering involving
chord distribution functions and able to be checkedby independent experimental
data. Based on the presentpossibility
to make aquantitative
connection betweenimaging techniques
and small-angle scattering,
this paper tries tocomplete
and extend theapproach
ofMering
andTchoubar. In section
2,
we discuss how chord distribution functions can be used asfingerprints
of the structural disorder. Asexamples,
wegive analytical expressions
andlarge
rexpansions
of chord distribution functions for two types of randombinary
media :(I)
theDebye
randomness and(it)
systems where alength
scale invariance property can be observed either for the bulk part or the interface. In section 3, the second derivative of the massautocorrelation,
involving
the « pore » and« mass » chord distributions, is
computed using
a« three-dimensional
» derivation. We also
give
anexplicit expression
of thesmall-angle
scattering
whichdirectly depends
on the Fourier transforms of chord distributions. Inpart 4,
the
application
to different types of randomness iscritically
discussed andpredictions
arecompared
to availableexperimental
data.Using image processing,
we will consider three types of disorder : thelong-range Debye
randomness, « correlated » disorder with aspecial emphasis
on the structure of the vycor porousglass, and, finally, complex
structures wherelength
scale invarianceproperties
can be observed.2.
Biphasic
random medium and chord distribution functions.2, I BACKGROUND. A
simple description
of atwo-phase
system includes twoassumptions.
First,
eachphase
is considered ashomogeneous
and is characterizedby
its averagedensity.
Second,
these twophases
areseparated by
an idealsharp
interface. As discussedby
Ciccariello
[13],
the real structure is thenprobed
with a coarsegrain
sizelarger
than the atomic scale. In this domain ofapproximation,
it ispossible
to define at least two types of chord distribution functions[14].
The chord size distribution « in number »(called
for short : chorddistribution)
is related to the conditionalprobability
ofhaving
a chord size between r and r +dr, knowing
that the chordbegins
at aspecific point
of the interface. This distribution will be notedf~(r)
orf~(r)
where the indices p and m stand for pore and mass,respectively.
The chord size distribution « in
length
»g~(r) (g~(r)) gives
theprobability density
to find a pore(mass)
chordhaving
a size between r and r + dr andpassing through
apoint
Mrandomly
distributed in the pore
(mass) phase.,These
distributions are null fornegative
distances. The relation between g andf
distributions is[12, 14]
:g,(r) ~j~~
I
= m, p
(1)
with
j
=
j~ rf,(r)
dr(2)
o
and
j~ f~(r)
di =(3)
o
An
interesting question
can be asked at thislevel, conceming
thepossibility
ofusing
chord distribution functions asfingerprints
of different models of disorder. In the next twosections,
we discuss two of them :
Debye
randomness and disorderinvolving
alength
scale invariance.2.2 DEBYE RANDOMNESS. A
theory
ofsmall-angle scattering
from abiphasic
randomsystem was first
proposed by Debye,
Anderson andBrumberger [15, 16].
Asrecently
discussed
by
Ciccariello[17],
randomness inDebye's
sense is related to thetheory
ofstationary
random functions[18].
Moreparticularly,
a « lineal »analysis
of aDebye
randomsystem
isclosely
connected with the model of the randomtelegraph signal
solvedby
Rice[19].
Let
Q;(r)
denote theprobability
that no collision with the interface occursalong
a segment oflength
rstarting
from a randompoint
M located either in the pore(I
=p)
or in the massphase (I
=
m). Assuming
aDebye
random system, theprobability
that no collision occurs in the interval oflength
r + dr reads as :Qi(r
+dr)
=
Q,(r) (i
p,dr)
I= p, m
(4)
In this
equation,
twohypotheses
areimplicitly
assumed.First,
any eventoccurring
on oneside of the random line
going through
M isindependent
of any eventsoccurring
on the otherside.
Second,
theprobability densities, p~
and p~, ofhitting
the interface from the pore orthe mass part of the matrix are constant. The
probability
that the firstcrossing point
appears in the interval(r,
r +dr)
is written as :P;(r)
dr=
Q;(r)
p, dr I= p, m.
(5)
Combining equations (4)
and(5)
we get :P,(r)
= p,
exp(
p,r)
I= p, m
(6)
The chord size distribution functions in
length
arecomputed using
the convolution ofP;(r)
with itself :gi(r)
=HI
reXp(
/l,(r rl)) eXp(
/l,rl) d~l (7)
Using equation (I),
the two chord size distribution functions in number read :f,(r)
=
I exp( r/j) (8)
with
ij
=
i/p; (9)
As shown in section
3, equation (8) permits
the retrieval of theexponential
variation of thebulk autocorrelation and
consequently
the well knownDebye expression
forsmall-angle
scattering [16]. However,
thenegative exponential
form off~(r)
andf~(r)
raises somequestions conceming
the localproperties
of the interface. For acompletely
smooth(differentiable) interface,
the small rexpansion
of the two chord distributions scales as r. Thepositive slope
of this linearrelationship
isdirectly
related to the curvatureproperties
of theinterface
[10, 20]. Debye
randomness acts in a different way. Small rexpansion
ofequation (8)
exhibits apositive
value at theorigin
and anegative slope.
This type of disorder involves a strong interfacialangularity [5, 8, 9, 12].
Thisexplains why
thescattering intensity predicted by Debye
does not follow theasymptotic
behaviorpredicted by
Kirste and Porod[21]
for &mooth and curved interfaces.2,3 DISORDER INVOLVING A LENGTH SCALE INVARIANCE. We consider disordered
systems with
length
scale invarianceproperties.
Morespecially,
we will focus on thelong-
range behavior of chord distribution functions. Let us consider abiphasic
mediumhaving
aself similar interface. The intersection of this surface with a random line is also a self similar set of
points. Using
the rule of thumbconceming
intersection of sets[22],
the number ofintersection
points along
a distance R is :Ns(R)
=Fs R~~~~ (10)
where
ds
is the fractal dimension of the interface andFs,
ashape
factor. The average chordlengths
for the pore(or
themass) portion
of thismatrix, computed
on a characteristic size R, isgiven by
:(j)~
oz(~°'(~~
i = m, p(i1)
where
~P;(R)
is the average volume fraction of thephase I,
measured on thelength
scale R.From
equation (2),
we have(ij)~
R#
rf;(r)
dr(12)
0
and the
long
range behavior of chord distribution functions can be written as :d(ij)~)
f;(R)
°°#
dR " ~' ~'(13)
Let first consider the case of a matrix
having
a self similar surface and a compact(non-fractal)
distribution of the mass and the pore networks[23]. ~P~(R)
and~P~(R)
areindependent
of R and we get :f~(R)
oz i= m, p.
(14)
~ds-1
A second
interesting
situation concems abiphasic
mediumhaving
a fractal distribution ofmass as
found,
forinstance,
in diffusion limitedaggregates,
cluster-cluster structures[24],
In this case, the mass volume fraction scales with R as :~P~(R)
=
F~ R"~~~~ (15)
and
Alp(R)
=i
~P~(R) (16)
where
F~
is ashape
factor. For a massfractal,
the two exponentsd~
andds
areequal [23]
andwe obtain from
equations (10)
and(11)
:~ F~
( m)~
=~ (17)
The average « mass » chord
length
isindependent
of the scale used in thecomputation,
Themass chord distribution function has a well-defined first moment and must
decay
faster thanI/r~
to avoid alogarithmic divergence
atlarge
r, On the contrary, the pore chord distributionfunction scales as :
f~(R)
oz(18)
R~~
In the three former
examples, large
rexpansions
of chord distribution functions exhibitspecific properties
of the structural disorder. It can be observed thatequations (14)
and(18)
can be
directly
used on a random section of the matrix, In this case, the exponent, such as(1s -1), gives
the fractal dimension of the intersection of the 3D interface and a randomplane.
3. From chord distribution to
small-angle scattering.
According
to classicaltheory,
the smallangle scattering I(q)
is related to the 3D Fourier transform of the fluctuation autocorrelation function :~
ir)
=
( dro(p(ro) >) (p(ro
+
r) >) (19)
where
p(r)
is the mass(the density)
distribution and p the volume average ofp(r).
As mentioned in the
introduction, small-angle scattering
isstrongly dependent
on thegeometrical properties
of the interfaceseparating
the pore and the mass part of the matrix.Properties
of the second derivative of the mass autocorrelation functionquantitatively
define the level of connection betweensmall-angle scattering
and the statisticalproperties
of thisinterface
[5].
For anisotopic biphasic
randommedium,
anexpression
of this secondderivative, involving
the « pore » and « mass » chord distribution functions has beenproposed [12].
Thiscomputation
is based on a statisticalanalysis
of the mediumalong
a random line andgives,
for 0w r :
~ir)"
=
(G(r)
2&(r)) (20)
with
G(r)
=
f~(r)
+f~(r)
2f~(r)
*f~(r)
++
fm(r)
*fp(r)
*fm(r)
+fp(r)
*fm(r)
*fp(r) (21)
The convolutionproduct
issymbolized by
a star.Sv
is the total interfacial area per volume unit.G(r)
is null for r~ 0. The Dirac distribution on the rhs of
equation (20)
isdirectly
connected with a finite
discontinuity of1~ irl'
atr = 0
(I.e.
a finite value ofSv).
Thissingular
part ofequation (20)
determines theq~~ leading
term in thehigh
qexpansion
of the smallangle scattering (The
Porodlaw)
and the linear behaviour ofl~ir)
at very smallr.
The
regular
part of 1~~(r)",
noted [1~ir)"]
andequal
toSv G(r)/4,
can be retrievedusing
a« three-dimensional »
computation.
Let us start from the functionalexpression proposed by
Ciccariello et al.
[5]
:16'l
i~)
~l
~
~) j ~
dS~ dk~("S
k~)~ dS'( OS'
k~)
3(~SS' k~)j
(22)
w
r is
positive
or null. S is the total surface.&s
is the unit vectorperpendicular
at the surface S in thepoint
to which the differential element dS refers.&s
and&s,
lie outside the mass network.Equation (22)
ismathematically significant
if theboundary
S is such that atangent plane
canbe defined almost
everywhere,
except for a set ofsingular points having
a null measure.Looking
around a statisticalpoint Os belonging
to theinterface,
theangular
average over allpossible
directions ib can besplit
into twoequal
parts. The tangentplane
to thesurface,
atOs,
defines two half spaces: one for directionspointing
to the pore network(noted
il
+),
and one for solidangles pointing
to the massphase (noted
il~). Equation (22)
can be written :i~ir)"i
=
~j iF+ (os, r)
+
F-(os, r)> (23)
with
~~~~~°~'
~~~
~~_~ d6~(*s
~+)ids,~~
S
~''
"~
~~~SS'r6~)
~~~~The brackets stand for the total surface average, defined
by
the firstintegral
inequation (22).
Let us consider a local
orthogonal
coordinate systemspecified by
the tangentplane
at thepoint Os (x
and yaxis)
and the direction&s (the
zaxis). Using
standard differential geometryone gets :
ds'(&s<
6~)=
do'dw'P(o', w', o~, w~) (25)
and
3(rss, r")
= ~ ~
3(8'
8w)3(w'
w w)3(rss, r) (26)
where
(rss<, W', o')
and(p~, o~)
are thespherical
coordinates ofOs,
and &respectively.
P is a
lengthy
functioninvolving partial
derivatives of rss, with respect to o' and W"However for o'
=
o~
andp'=
p~, we have :P(o~,
w~,o~, w~)
= sgn (&s<6~)R$
sin(o~). (27)
The second
integral
ofequation (24) gives
a series of contributionsrespectively
associated with each intersection of the interface with a linehaving
the direction &. For il + half space, the first intersection fromOs
involves a porechord,
the second a pore chord followedby
amass
chord,
and so on.Using equations (24), (26)
and(27),
we get :F~ (Os, r)
=
ld&(ds &)
x~+
x
~-
~(~~
3(R~~p~ r)
+~~~
~~3(R~~p
m~
r) ~~~~l'~ 3(R~~~
~ ~~
r)
+(28)
r r r
R~~~~ is the
length
of the pore chord which goes fromOs
to the first intersectionalong
the direction &. Related to the secondintersection,
R~~~,~~ is the total
length, along
the direction&,
of the pore chord followedby
a masschord,
and so on.The next step consists in
averaging equation (28)
over allpossible positions
ofOs.
There is nosimple
andgeneral
way ofobtaining
this average. Ifadjacent
pore and mass chords arestrongly correlated,
thecomputation
has to take into account distribution functionsinvolving
two,three,...
consecutive chords.Following Mering
and Tchoubar[12],
we have toconsider a
specific
type of randomness where statisticalisotropy
of the matrix anduncorrelation between
adjacent
chords are assumed. This is a stronghypothesis
which must be checked for each system. in this case, we have :ld&(&s n+ &)
~r~
~~~8(R
~~~~r)
=2 w w/2
~2
=
dp~ do~
sin(o~)
cos(o ~) duf~(u)
j
3(u r)
= grf~(r) (29)
o o
r
and
Ii da(&s.
6~)~~)
~'~
3(R~~~,
~~r)
=grf~(r)
*f~(r) (30)
n+ r
Finally
weget
:(F~ (os, r))
=
gr( f~(r)
+f~(r)
*f~(r) f~(r)
*f~(r)
*f~(r)
+) (31)
JOURNAL DE PHYSIQUE i -T 2, N' 6.JUNE t992 31
and
IF- (Os, r))
=
«(
+fm(r) fm(r)
*fp(r)
+fm(r)
*fp(r)
*fm(r) (32) l~ ir)"I
=
( ~fm(r)
+fp(r)
2f~(r)
*f~(r)
++
fm(r)
*fp(r)
*fm(r)
+fp(r)
*fm(r)
*fp(r) (33)
This result is similar to the
regular
part ofequation (20).
Let us now try to connect the chord distribution functions to an
explicit expression
of thesmall-angle scattering, I(q).
For anisotropic
medium we have :I(q)
=
l~
4grr~l~ ir)
~~~ ~~~~ dr(34)
~ qr
l~ir) being
an even
function,
the formerequation
can be written :i(q)
=
~ "
) (Real ( I 2(q))
(35)
with the
general
notation :+ w
@(q)
=
w(r) exp(iqr)
dr(36)
-
w
Using
the standardproperties
of the Fourier transform of distributions andknowing
thatl~ir)"
is also an evendistribution,
we get fromequation (20)
~
sv i (q)
= j Real
(I G(q)) (37)
2 q with
~~~~ l~~ ~~~~ ~~~~~~~~
~~II
°~G(r) exp~iqr~
~~ ~~~~The modulus of
/~(q)
or
/~(q)
ranges between 0 and I.Looking
at the Fourier transform of the rhs ofequation (21),
we find aconverging geometrical
series andd(q)
reads~ fm(q)
+fp(q)
2f~(q) f~(q)
~ ~~~~
l
fm(q) fp(q)
Finally using equations (35), (37)
and(39),
thesmall-angle scattering
can be written as :grsv
dIi (l /m(q)) (1 fp(q)) (40)
~~~~ ~
i dq q2~~~ f~(q) /p(q)
The well known
Debye expression
can be recoveredusing
the chord distribution functionsgiven
inequation (8)
:8
gr@~(l
@~)d~
I(q)
=
(41)
(1
+f q~~
where basic
stereology gives
twogeneral
relations : I~
l
(42)
d
i~ ip
and
4
@p(I
~bp)Sv
"(43)
4.
Application
to diwerenttypes
of disordered media.From the
experimental point
ofview,
twoquestions
can be raised.First,
are the chord distributions efficient togive specific
information on the structural disorder ?Second,
is the connection withsmall-angle scattering really
describedby equation (40)
? In otherwords,
canwe find different types of disordered structures where uncorrelation between
adjacent
chordscan be assumed ? Based on the
present possibility
to makequantitative
connections betweenimaging techniques
andsmall-angle scattering,
wecritically
discusspossible applications
to differenttypes
of randomness.4,I EXPERIMENTAL PROCEDURE AND IMAGE PRocEssiNG. For an
isotropic
andbiphasic
random
medium,
the fluctuation autocorrelationfunction,
defined inequation (19),
is one ofthe few characteristics that remain
unchanged
whether you observe them two- or three-dimensionally [25, 26].
In thefollowing, digitized
sections of different porous structures arenumerically analyzed.
Directcomputation
ofl~ir)
isperformed along
several bundles ofparallel
lines. These areuniformly
distributedalong
different random directions. To minimizesize
effect,
the maximal value of r is less than 1/3 of the average size of thepicture.
The small-angle scattering I(q)
iscomputed
fromequation (35).
The chord distribution calculation isperformed
in four steps :(I)
definition of a random direction ;(it) localization, along
this direction, of apair
of nearestneighbor pixels having
different values(0
for the pore, I for themass).
Thispair
defines the first end of a chord(iii)
estimation of the chordsegment along
the direction chosen. This chord can
belong
to the pore or to the mass network and(iv)
computation
of the sizehistogram by
iteration of the former steps. Thisalgorithm gives
the chord size distribution in numbers and was checked on basicfigures (the
cerde forexample)
where
analytical expressions
are known. Agood
agreement is obtained except for the firstpixels
where the discrete nature of thedigital image
inducesslight
artefarcts.4.2 LONG-RANGE DEBYE RANDOMNESS.
Figure
I shows adigitized
section of dolomiteadapted
from[27].
The evolution of the pore and the mass chord distributions follows two successiveregimes (see Fig. 2).
As is the case for a smooth and curvedinterface,
these distributions scale with r at small distances. Just after the maximum of eachdistribution,
anegative exponential
form is observed. This is agood example
oflong-range Debye
randomness. Infigure 3,
we compare the directcomputation
ofI(q)
from theimage
with the chord distribution formalism(Eq. (40)).
On the samescale,
one observes agood
agreement.4.3 « CORRELATED
» DISORDER. The
small-angle scattering
of some porous solids showsa
peak corresponding
to the existence of arelatively
well defined correlationlength.
We discuss how a chord distribution model can succeed or fail topredict
thescattering properties
of these correlated structures.
Let us first consider the case of a porous
glass (Vycor 7930,
lot742098,
TrademarkComing).
The matrix isprepared by leaching
aphase separated
borosilicateglass
and appearst,~" ~~
~*f ~
W,
-~,,
,
~ ~
'
a~ j
O
w ,
4#°,
*
#~ ~
', ~
',
o*«
j~ ~
4
~
~~
f~'~ f . ~'~~
''
~
# °~/
#'
.
'
,
.
~w fl~ ~'~j t~
~ ~
,
~','
,
,~ _,_ ~p~
'j
'
", ~z ~ '~'~W~
»
.,'~ ' "~$
Fig,
I.Digitized picture
of a thin section of dolomite,adapted
from reference [27]. The pore network is shown in black, The horizontal bargives,
inpixels,
the numerical resolution.io'~
P
~E
~~
"
o~
, lo'~
0
200'
o~ °
~3 1(Q)
~i
1 0'
o
~,3
o'~
io'~
io'~
i o° i o~QlPixel
'~)
Fig.
3. Smallangle scattering
of a porous solidhaving
a random section as the one shown infigure
I, The open circles are the directcomputation
from theimage
and the solid line is the calculatedscattering using
the chord distribution model(Eq,
(40)),t, ~£ jj~l~ ~t~~
~
' '
,
~
, - .
,
«
'
. -
j..
£ ~
,
, .
- ,
~
, T,, .,,
, »
~ h'q~.
. ,
, -
~
'
~~~~
,f
, . .~
'
,jiff
,
' f,~
i ,@
',>
t ~. ~db~~<G
«-
Fig.
4,Digitized
pore network of a very thin section of the porous vycorglass
obtained from a transmission electronmicrograph
[3],corresponding
to alength
of3001.
The two chord distribution functions are shown infigure
6. Aspecific
mode(a peak)
can be observed for each ofthem,
followedby
aexponental
tail,
Computation
of thesmall-angle scattering
fromequation (40)
is ingood
agreement with a direct estimateusing image processing (see Fig, 5).
Morover, the « chord distribution» model
4 10~
co
3 10~
1(a)
o
i
io~
0
10°
0 0.02 0,04 0.06 0.08 0.1
~~~.i~
Fig.
5.Small-angle scattering
of the porous vycorglass.
The open circles are the direct computation from theimage.
The solid line is the calculatedscattering using
the chord distribution model(Eq.
(40)).The full circles are the measured
small-angle
Xscattering.
This curve is normalized to the calculated scattering usingequation
(40).o'~
,
/
P8
10'~ '_
11
j~E 6 10"~
(
if
:
~" 4 10' ~
m
,~ exponential tails
2 10
o
io°
0 200 400 600 800 1000
R(A)
Fig.
6. Pore and mass chord distribution functions calculated from thedigitized
image 4 (the porous vycorglass),
Full squares : the pore(p) Open
circles the solid (m).fits the
experimental
correlationpeak
observedby small-angle
X rayscattering. However,
two
discrepancies
can be observed. The modelslightly
underestimates the left part of the correlationpeak
and exhibits a q~ ~dependance
in thehigh
qregime (above
0.Ih~').
For thismaterial,
theexperimental asymptotic
behaviour is characterizedby
apower-law dependence
of the form q~ ~.? The resolution of the
digitized
porenetwork, typically
15-201,
is in fact toolow to handle
possible
localroughness
of the interface[3]. Nevertheless,
thehypothesis conceming
the uncorrelation betweenadjacent
chords appears to beacceptable
in this« correlated » porous medium.
Another
interesting example
isdisplayed
infigure
7showing
a thin section of agranular material,
built from smooth and almost convexparticles.
The mass chord distribution exhibitsa
peak
around 100pixel,
followedby
anexponential
tail(see Fig. 8).
The pore distributionFig.
7.Digitized picture
of a section of a granular material,adapted
from reference [31]. The pore network is shown in white. The horizontal bar gives, inpixels,
the numerical resolution.io'~
P
0'~
~
~E
i~
i
o' ~ °
0 100
Fig.
section of granular porous medium. Full squares : the pore (p)
; Open
rcles:
the
continuously
decreases from theorigin
and veryrapidly
evolves as anegative exponential
function. This trend recalls some
geometrical properties
of a randompacking
of identical hardspheres.
It is known that such a randomsystem
exhibits strong correlationsspreading
onseveral shells of coordination. Morover the pore chord distribution is shown to have an
exponential
form[28, 29].
Infigure 9,
we compare the directcomputation
ofI(q)
from theimage
with the chord distribution formalism(Eq. (40)).
The chord model does not fit thescattering
curvecorrectly
andgives negatives
values at small q Thisexample
showsclearly
the limitation of the chord distributions in
predicting
thesmall-angle scattering
of astrongly
correlated
system.
7 10~
6 0~ °
5 o~
4 0~ °
3 10~ °
'(Q)
2 10~ °
1 1o~
o io°
-i i o~
-2 10~
0 0.05 0.1 0,15 0.2
Q(Pixel'~)
Fig.
9. Small angle scattering of a porous solidhaving
a random section as that shown infigure
7. The open circles are the directcomputation
from the image and the solid line is the calculated scattering using the chord distribution model(Eq.
(40)).4.4 COMPLEX STRUCTURES WITH LENGTH SCALE INVARIANCE. Let us first consider the
bidimensional structure shown in
figure
10 and known as the diffusion limited aggregate[24, 30].
This is a mass fractalhaving
a fractal dimension of 1.7. The mass chord distribution showsa maximum followed
by
anexponential
tail(see Fig.
IIA).
Atlarge distances,
the pore chord distribution exhibits aI/q" form,
with a between 1.65 and 1.70(see Fig.
IlB).
These resultsare in a
good
agreement withanalytical expressions
andlarge
rexpansions
of chord distributions of a mass fractal(See
Sect. 2 whered~
Igives
the fractal dimension of the intersection of a 3D mass fractal and a randomplane).
The DLA shown infigure
10 does not match any bidimensional cut of a 3D matrix. In that sense, we will focus our attention on the bulk autocorrelation function. As shown infigure12,
the chord model fits the functionl~iq)
whichwas
computed directly
from theimage.
Two distinct parts can be observed : a Porodregime,
athigh
q,running
asq~~
and a self similarregime,
at small q, in agood
agreement with the mass fractal dimension of 1.7.
A more
complex organization
is exhibited infigure
13 where thedigitized image
of a thin section of cement(Hydrated
calciumsilicate)
is shown[31].
Atlarge
distances, the mass and pore chord distributions evolve in a similar way(See Fig. 14)
andapproximately
decrease asI/r"~~
Thesmall-angle scattering computed
fromequation (40)
is shown infigure15.
The400P
Fig,
10. Bidimensional DLAadapted
from reference [30]. The solid is shown in black. The horizontal bargives
the numerical resolution inpixels.
0'
°°°o~~~~~~~~~~~~~~ @fl
f R
~~~~~°°°o~~
~
l 0"~ °°°°o~
10'~
~ ~0 25 50 75
~ ~~~
~~
~00
R(Pixel)
Fig.
ll, A) The mass chord distribution functions calculated from thedigitized image
10 (the 2D DLA). B) The pore chord distribution functions calculated from thedigitized image
10. The solid line has aslope
of 1,7.0'~
@
l
0'~
".,",.
Slope = 1.7
f~(R)
~',
~~h~
0'~
1o'~
~
i i o 100 1oo0
R(Pixel)
Fig.
ll (continued).o~
~
-0.73
o°
io'~
2
o"~
l o'~
i
o'~
Io'~
Io'~
i o°I o~
Q(Pixel'~)
Fig.
12.Computation
of the Fourier transform of the fluctuation autocorrelation function~~(r)
in thecase of the DLA shown in
figure
10. The full squares are the directcomputation
from theimage,
using lD Fourier transform of equation (19). The solid line is the calculated scattering using the chord distribution model(Eq.
137)).curve scales as
I/q~.~
for small q and exhibits a Porod law above q =0,6
pixel~'
It can be observed that the chord distribution modelgives
a lessnoisy
result than a directcomputation
of
I(q)
from theimage, According
to the literature[32, 33],
thesmall-angle scattering
appearsto be related to a surface fractal
having
a fractal dimension of 2.7. An the otherhand,
the similaralgebraic
evolution of the two chord distributions can be describedby equation (14)
whichgives
a fractal dimension of 2.65. A different way to check thepossibility
of a fractal~
~W
; ,
;'
(<
i
Fig.
13.Digitized picture
of cement,adapted
from reference [31]. The pore network is shown in white. The horizontal bargives
the numerical resolution inpixels,
0'~
~
o
°
- 1
£
°
~~
m
$~ ,
~
i
i '~
10 loo 1000
R(Pixel)
Fig,
14. Pore and mass chord distribution functions calculated from thedigitized
image 13. Full squares : the pore (p)Open
circles : the solid (m).surface is to
analyse
theproperties
of the hullseparating
the mass and the pore network, On thepicture,
this interfacialregion
is defined as the set ofpixels belonging
to the pore(the mass)
network andhaving
one nearestneighbor pixel
inside the mass(pore)
distribution. This set can be describedby using
adensity
which is one in the interfacialregion
and 0everywhere
else.
Figure
16 shows the conditional autocorrelation function of thisdensity.
This function~
« »~
°
Q~'~ Q'~
0~
10~
1(a)
~i
10"~
~.
i
o'~
i o~~ i
o'~
io'~
i o° i o~Q(Pixel'~)
Fig.
15.Small-angle scattering
of a porous solidhaving
a random section as that shown infigure
12.The open circles are the direct
computation
from theimage
and the solid line is the calculatedscattering using
the chord distribution model(Eq,
(40)).i o°
j°
(R)~. i
"""..,~
sloper -0.24
0~~
10 100 1000
R(Pixel)
Fig.
16. « Interracial» conditional autocorrelation function calculated from the
digitized image
shown infigure13
(see text for definition).gives
the averagedensity
of interfacial sites at agiven
distance r of anorigin point
located inside the interfacialregion.
Atlarge distances,
one observes aI/r°.~~ dependence
related to a fractal dimension(in 3D)
of 2.76. This result is in a reasonableagreement
with the other twodeterminations.