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Submitted on 1 Jan 1990
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the multiple scattering limit
D.J. Pine, D.A. Weitz, J.X. Zhu, E. Herbolzheimer
To cite this version:
Diffusing-wave
spectroscopy: dynamic
light scattering
in the
multiple scattering
limit
D. J.
Pine,
D. A.Weitz,
J. X. Zhu and E. HerbolzheimerExxon Research and
Engineering,
Route 22 East, Annandale, NewJersey
08801(Received
on January 3, 1990,accepted
infinal form
on May 16,1990)
Abstract. 2014
Dynamic
light scattering
is extended tooptically
thick(opaque)
media which exhibita very
high degree
ofmultiple scattering.
This newtechnique,
calleddiffusing-wave
spectroscopy(DWS),
exploits
the diffusive nature of the transport oflight
instrongly scattering
media to relate thetemporal
fluctuations of themultiply
scatteredlight
to the motion of the scatterers. Asimple
theory
of DWS, based on the diffusionapproximation
for the transport oflight,
isdeveloped
tocalculate the
temporal
electric field autocorrelation functions of themultiply
scatteredlight.
Twoimportant scattering
geometries
are treated : transmission andbackscattering.
Thetheory
iscompared
toexperimental
measurements of Brownian motion of submicron-diameterpolystyrene
spheres
in aqueoussuspension.
The agreement betweentheory
andexperiment
is excellent. The limitations of thephoton
diffusionapproximation
and thepolarization dependence
of the autocorrelation functions are discussed for thebackscattering
measurements. The effects ofabsorption
oflight
andparticle polydispersity
are alsoincorporated
into thetheory
and verifiedexperimentally.
It is also shown how DWS can be used to obtain information about the mean size of theparticles
which scatterlight.
Classification
Physics
Abstracts 05.401. Introduction.
Dynamic light scattering (DLS)
has proven to be apowerful
tool for thestudy
ofdynamical
processes insimple
andcomplex
fluids.Using photon
correlationtechniques
toanalyze
thetemporal
fluctuations of scatteredlight,
DLSprovides
detailed information about thedynamics
of thescattering
medium[1,
2,
3].
Asignificant
limitation of DLS(also
calledquasielastic light scattering
orphoton
correlationspectroscopy)
has been the lack of ageneral
scheme for
applying
it tosystems
which exhibitstrong
multiple scattering.
However,
in aseries of recent
experiments,
DLS has been extended tostudy optically
thick media which exhibit a veryhigh degree
ofmultiple scattering
[4,
5,
6].
This newtechnique,
calleddiffusing
wavespectroscopy
(DWS), exploits
the diffusive nature of thetransport
oflight
instrongly
scattering
media to relate thetemporal
fluctuationsof multiply
scatteredlight
to the motion of the scatterers.Thus,
DWS can be used tostudy particle
motion in concentrated fluids such ascolloids, microemulsions,
and othersystems
which are characterizedby
strong
multiple
scattering [6, 7].
The basic features of DWS have been outlinedpreviously
in brief reportsby
several groups
[4,
5,
6].
Here,
wepresent
a more extensive report on the theoretical andexperimental
details of DWS.Before the
development
of DWS there were numerousattempts
to account for the effects ofmultiple scattering
in DLSexperiments.
Most focused onsystems
which exhibitrelatively
weak
multiple scattering.
The most successful of thesetechniques, developed by
Phillies[8]
and Dhont et al.[9] rely
on elaborate schemes which discriminateagainst multiply
scatteredlight
so thatonly
the fluctuations ofsingly
scatteredlight
areanalyzed.
Thesetechniques
arepractical,
however,
only
when asignificant
fraction of the scatteredlight
which is collected has been scatteredjust
once.By
contrast, DWS relates thetemporal
fluctuations ofmultiply
scatteredlight
to theunderlying dynamics
of thescattering
medium.Thus,
DWS extends theapplication
of conventional DLS tostrongly scattering
systems
which arecompletely
dominated
by multiple scattering,
thatis,
tosystems
which areessentially
opaque.One
important
consequence ofmultiple scattering
is that DWSprobes
particle
motion overlength
scales much shorter than thewavelength
oflight
in thescattering
medium,
A. This is tobe contrasted with DLS in the
single scattering
limit,
where the characteristic timedependence
of the fluctuations is determinedby
particle
motion over alength
scale setby
the inverse wavevectorq - 1 -,A,
where q
=(4
7r/A )
sin(0 /2)
and 0 is thescattering angle.
Inthe
multiple scattering regime,
the characteristic timedependence
is determinedby
the cumulative effect of manyscattering
eventsand, thus,
by particle
motion overlength
scalesmuch less than A.
Therefore,
the characteristic time scales are much faster and thecorresponding
characteristiclength
scales are muchshorter than
for conventional DLS. In thefollowing
section we review thetheory
of DWS based on the diffusionapproximation
for thetransport
oflight.
We thenapply
thistheory
to twoimportant
experimental
geometries, backscattering
andtransmission,
and compare thepredictions
of thetheory
toexperimental
measurements on aqueous colloidalsuspensions
ofpolystyrene spheres.
We also discuss the limitations of thephoton
diffusionapproximation
fordescribing
thetransport
oflight
within the context of ourbackscattering measurements.
Insubsequent
section,
weshow how DWS can be used for
particle sizing,
and discuss the effects ofabsorption
oflight
and
particle polydispersity.
2.
Theory.
The
key
to thetheory
of DWS is thedescription
of thepropagation
oflight
in amultiply-scattering
medium in terms of the diffusionapproximation.
Within thisapproach,
thephase
correlations of the scattered waves within the medium arignored,
andonly
the scattered intensities are considered[10].
Thus,
thepath
followedby
an individualphoton
can be described as a random walk. Whether the diffusionapproximation
is valid in agiven
system
depends
on thelength
scales over which thetransport
oflight
is described. Forlength
scales less than the mean freepath (or
extinctionlength),
f,
of the coherentfield,
the waveequation
for the electric field must be used. For
length
scaleslonger
thanl,
thephase
correlation of thewaves must be considered
only
forlimited,
specialized
cases. The mostcommonly
studiedexample
is that of enhancedbackscattering
where thephase
coherence of the scattered fieldsplays
an essential role[11, 12].
Moregenerally,
it isonly
in the case ofextremely
strong
scattering,
where theIoffe-Regel
limit isapproached,
andlight
localization ispredicted
to occur, that the use of the full waveequation
is essential[13].
However,
achieving
thiscriterion has proven elusive
and,
fornearly
all cases ofpractical
interest,
thetransport
oflight
can be described in terms of theintensity
or energydensity.
over a distance
f.
In this case thetransport
of thelight
energydensity, U(r, t ),
can bedescribed over
length
scaleslonger
thanf
by
the diffusionequation
where
De
is the diffusion coefficient of thelight.
Then, Dl
=cf/3
where c is thespeed
that thelight
travelsthrough
the effectivebackground
medium. Forparticles
which are not smallcompared
toA,
thescattering
isanisotropic,
and the mean number ofscattering
events, no,required
to randomize the direction oflight propagation
isgreater
than one. Thelength
scale over which this randomization occurs is thetransport
mean freepath, l *,
definedby
e * = no f.
Thus,
forno > 1,
the diffusionequation
is validonly
overlength
scaleslonger
thanf*
andDl
=cf*/3.
Inpractice,
this means that thetheory
for DWS basedsolely
on thediffusion
approximation
willprovide
an accuratedescription
of thetemporal
fluctuations of the scatteredlight
when thesample
dimensions aregreater
than f*
and the distance thatprotons
travelthrough
thesample
is muchgreater
thanl*.
Two theoretical
approaches
have been used to describe the fluctuations in the scattered electric field. The firstapproach
starts from the waveequation
for thepropagation
oflight
and uses a
diagrammatic expansion
to describe thescattering
from random fluctuations in the dielectric constant. The lowest order term in thisexpansion corresponds
to the diffusionapproximation.
The consequances of motion of the scatterers were first consideredby
Golubentsev
[14]
andtemporal
autocorrelation functions for differentscattering geometries
were calculated
by Stephen [ 15]. Subsequently,
MacKintosh and John[16]
refined thisapproach by considering
the effects ofanisotropic
scatterers and non-diffusive modes ofpropagation
of thelight.
The second theoretical
approach
differs from the firstby
considering
the diffusivetransport
of individualphotons directly,
rather thanstarting
from the waveequation.
Thepath
of eachphoton
is determinedby
random,
multiple scattering
from a sequence ofparticles.
Thefluctuations in the
phase
of the electric field due to the motion of the scatterers is calculated for eachlight
path.
The contributions of allpaths, appropriately weighted
within thephoton
diffusionapproximation,
are then summed to obtain thetemporal
autocorrelation function. It ismathematically simpler
andphysically
moretransparent
thandiagrammatic
methods. It canalso be more
easily generalized
tolarger particles
which scatterlight anisotropically.
Thisapproach
was firstdeveloped by
Maret and Wolf[4]
toanalyze temporal
corrélation functions oflight
backscattered from dense colloidalsuspensions.
Pine et al.[6]
extended theiranalysis
to transmission
geometries
and calculatedexplicit expressions
for the correlation functions. This work wasrecently
reviewedby
Pine et al.[17].
In section2.A,
we follow the earlierworks of Maret and Wolf
[4]
and Pine et al.[17]
and review thetheory
which leads to ageneral expression
for thetemporal
correlation function ofmultiply
scatteredlight.
Insection
2.B,
we discuss the calculation of the distribution ofphoton path lengths through
thesample using
thephoton
diffusionapproximation
and in section 2.C we discuss the method we use to calculateexplicit expressions
for thetemporal
autocorrelation functions we measure.2.A. CORRELATION FUNCTION FOR MULTIPLY-SCATTERED LIGHT. - For
simplicity,
weconsider a
suspension
of identicalspherical particles randomly dispersed
in a fluid andilluminated with laser
light
ofwavelength
À. Forspecificity,
we assume a slabgeometry,
asshown in
figure
la ;
othergeometries
will be discussed later. Thesuspension
must beoptically
thick so that all thelight entering
thesample
is scattered many times beforeexiting.
Scatteredlight exiting
thesample
is collected from a small area near thesample
surface(within
Fig.
1. - Transmissiongeometry for a
point
source.(a)
Apoint
source oflight
is incident on thesample
on the left side and is collected from apoint directly opposite
theinput
point
on theright
side. Pinholeapertures
(A)
collimate the scatteredlight. (b) 1 (t)
vs t for transmission of a delta functionpulse,
& (t), through
a slab of thickness L Theplot
can also beinterpreted
asP (s) vs s
since the fraction ofphotons travelling
a distance sthrough
thesample
in a time t =s/c,
where c is thevelocity
oflight
in thesample.
Here, L = 1mm, f * =
100 im, and c = 2.25 x10’° cm/s (the speed
oflight
inwater).
Note thatP (s ) decays exponentially
forlarge
s.the fluctuations of the scattered
light.
In DLSexperiments,
these fluctuations areusually
characterizedby
the normalizedtemporal
autocorrelationfunction,
where
E(T )
is the electric field of the scatteredlight
collectedby
the detector and T is thedelay
time. To calculateg1(,r),
we follow theapproach
of Maret andWolf [4]
and firstconsider a
single light path through
thesample.
For agiven
sequence ofscattering
events atpositions
rl, ..., r 11 and withcorresponding
successive wavevector transfers qi =ki - ki _ 1,
theproduct
of the scattered electric field at time T with that at time 0 will bewhere
Ar i (,r )
=ri ( T) - r i (0)
is the distance the i-thparticle
moves in a time T. Theargument
of the
exponential,
represents
theaggregate
phase
shift of the scatteredlight
due to the motion of all n scatterersHere
P (n)
is the fraction of the total scatteredintensity, Io, in
the n-th orderpaths
and( )
denotes averages over both theparticle displacement, Or ( T ),
and the distribution ofwavevectors q. For
large
n, thatis n » n (),
thetransport
of light through
asample
isaccurately
described within the diffusion
approximation.
This allowsP(n)
to beeasily
evaluated.Furthermore,
thelarge
number ofscattering
events in eachpath greatly
simplifies
the evaluation of the averages inequation
(2.5).
For
large
n, we can relax the condition that the sum of the intermediatescattering
vectorsn
must
equal
the difference between the incident andexiting
wavevectors, ¿
qi =kn - ko.
Ini
addition,
we also assume that successivescattering
events are uncorrelated.Thus,
thedistribution of the qi is determined
solely by
thescattering
form factor of asingle sphere.
Then,
theright
hand side oféquation (2.5)
becomesP (n) (exp [- iq -Ar (T ) ] > n.
For Brownianmotion,
the distribution of Ar(T )
is Gaussian and the average overparticle
motionis
readily performed yielding
where >q
denotes the form-factorweighted
average over q. Forsimple
diffusion,
(âr2( T) =
6 DT where D is the diffusion coefficient of theparticles.
The average over q can be
performed explicitly
forpoint-like
scatterers which scatterlight
isotropically ;
thisgives
where
To - (Dk))
andA;o=27r/A.
However,
forlarger particles
which scatterlight
anisotropically,
the average over q is more difficult toperform.
Thus,
we restrict ourselves tosmall
delay
times,
r T o, and retainonly
the first term in a cumulantexpansion,
We can compare this more
general approximation
with the exactexpression, equation (2.7),
for
point-like
scatterersby evaluating
(q2)
for a flatdistribution,
where dn denotes the solid
angle.
Thisgives,
Expanding
the exactexpression
inequation
(2.7)
gives
so that the cumulant
expansion gives
the correct results toleading
order inT / T o.
Furthermore,
the effectivedecay
time isTo/2 n,
so that forlarge
n,(E(n)(T)E(n)*(O»
Nevertheless,
forlarge
T / To
the cumulantexpansion
must fail since the exactexpression
inequation (2.7) decays
as a powerlaw,
( T / T o )- n,
due to the contributionsof scattering
at smallq. We note,
however,
that at theselong
times low orderscattering
events dominate. For smalln
n, the distribution
of ql
is not random but mustsatisfy
the conditionthat £
qi =kn - ko.
Thisi
will
modify
the average inequation (2.8)
and could have the effect of at leastpartially
offsetting
the error introducedby
the cumulateexpansion.
Equation
(2.8)
can bereadily generalized
to treat theanisotropic
scattererstypically
used inexperiments.
Here,
thesingle particle scattering intensity
ispeaked
in the forward directionand q2>
is less than2 ko.
Using
therelation 1 - cos
0 ),
[10,
18]
we haveWith this result and the cumulant
expansion
inequation (2.8),
we can evaluate the average over q inequation (2.6)
and obtain asimple expression
for the contribution of then-th order
scattering paths
to the autocorrelationfunction,
For
isotropic
scatterers,f
=l*,
and we recoverequation (2.10),
theapproximate
result forpoint-like
scatterers. We note that the accuracy ofequation (2.13) improves
as thescattering
becomes more
anisotropic.
The second cumulant ofe- Dq 2 r) q is
e - ! 2 (Dr )2(
q4) - q2)
2
. Fortypical single-particle
formfactors,
F (q ),
weexpect q4) -- q2) 2 --
(f 1 f * )2,
so that theleading
order correction to the cumulantexpansion
inequation
(2.8)
is0 [( TITo)
(f If
* )2].
Thus,
forlarge
scatterers, where$ * > Q,
the rangeof validity
ofequation (2.13)
may extend up to T --T o.
The total field autocorrelation
function,
g1(,r),
is obtainedby summing
overscattering
paths
of all ordersIf we rescale n
by defining
n * - n/no
=(f/f*)
n, theexponential
term in thisequation
isidentical to
equation (2.10)
forisotropic
scatterers.Furthermore,
for n > n 0,P (n )
can bewritten as a function of n* rather than n.
Physically,
this reflects the fact that overlength
scales
longer
thanl*,
thescattering
appears to beisotropic
and thephoton
diffusionequation
should beadequate
to describe thetransport
oflight.
As aresult,
in thisapproximation,
This reflects a renormalization of the mean free
path
foranisotropic
scatterers, so that thelight
may be viewed asundergoing
anisotropic
random walk with an averagestep
length
f*.
We note that the
decay
rate of agiven path depends critically
on itslength. Long paths
reflect theaggregate
contribution of manyscattering
events.Thus,
eachparticle
need moveonly
asmall distance for the total
path length
tochange by
awavelength.
This occurs in a shorttime,
leading
to arapid decay
rate.By
contrast, shortpaths
reflect the contribution of a small number ofscattering
events.Thus,
eachparticle
mustundergo
substantial motion for the totalThe
key
to the solution ofequation (2.15)
is the determination ofP(n*).
This task isgreatly simplified
if we pass to the continuum limit.Thus,
weapproximate
the sum over n*by
anintegral
over thepath lengths,
s = n * f * ( = ni ),
and obtainIn this case, P
(s)
is the fraction ofphotons
which travel apath
oflength s through
thescattering
medium.Physically, equation (2.16)
reflects the fact that alight path
oflength s
corresponds
to a random walk ofslf*
steps
and thatg1( T ) decays,
on average,exp (-
2T /To)
perstep.
Now we can use the diffusionapproximation
to describe the random walk of thelight,
andP (s)
can be obtained from the solution of the diffusionequation
for theappropriate experimental
geometry.
Weemphasize,
however,
that the continuumapproxi-mation to the discrete
scattering
events will break down whenever there aresignificant
contributions from short
light paths.
2.B. BOUNDARY CONDITIONS AND CALCULATION OF
gl ( T )
FROMP (s).
- Our method fordetermining P (s)
can be illustratedby considering
asimple experiment.
An instantaneouspulse
oflight
is incident on the face of asample
whichmultiply
scatters thelight.
The scatteredphotons
will execute a random walk untilthey
escape thesample.
Here,
we focus onthose
photons
which exit thesample
at somespecified point,
rd, on theboundary
wherethey
are detected. The flux ofphotons reaching
rd is zero at t =0,
then increases to amaximum,
and
finally
decreases back to zero atlong
times when all thephotons
have left thesample
(see
Fig.
1 b).
At time t, thephotons arriving
atpoint
rd are those that have traveled apath length
s = ct
through
thesample.
Thus,
the flux ofphotons arriving
atpoint
rd at agiven
time isdirectly proportional
toP(s).
The details of this timedependence,
and hence theshape
ofP(s),
willdepend
on theexperimental
geometry.
To obtain
P (s)
for agiven experimental
geometry
we use the diffusionequation
forlight
equation (2.1),
to determine thedispersion
induced in a delta functionpulse
as it traverses thescattering
medium. We denote thedensity
ofdiffusing photons
within the mediumby
U(r ).
For initialconditions,
weexploit
the fact that the direction of the incidentlight
israndomized over a
length
scalecomparable
tof*
and therefore take the source ofdiffusing
light intensity
to be an instantaneouspulse
at a distance z =zo inside the illuminated
face,
where we
expect
that zo -f *,
that isIn sections 3 and
4,
where we calculateexplicit expressions
for thetemporal
autocorrelation functions for transmission andbackscattering geometries,
we discuss the consequences ofapproximating
the source term with a delta function. ’In addition to the initial
conditions,
theboundary
conditions must ensure that there is noflux of
diffusing photons entering
thesample
from theboundary.
Thus,
outside asample
consisting
of a slab of thickness L between z = 0 and z =L,
where J+
(z)
and J(z)
are the fluxes ofdiffusing photons
in the + z and - zdirections,
respectively.
In theappendix
we showthat,
within the diffusionapproximation,
the fluxes ofwhere J±
are taken to bealways positive.
TheUc/4
term will dominate the total flux in agiven
direction in the interior of thesample
where thedensity
ofphotons
ishigh.
However,
the netflux in a
given
direction will be dominatedby
thegradient
term, consistent with Fick’s lawTo obtain the
boundary
conditions,
we consider thesample
interface at z = 0 whereJ+ =
0 and J isgiven by equation (2.19).
Hence,
J(z
=0) = 2013
J_(0)
and the net flux isdirected out of the
sample.
Inside thesample,
adistance £*
away from theboundary,
the totalflux is
given by equation (2.20).
SinceÎ*
is the minimum distance over which theintensity
canchange
within the diffusionapproximation,
these twoexpressions
for the flux near theboundary
must beequal :
Simplifying
thisexpression,
we obtain theboundary
condition,
Alternatively,
thisboundary
condition can be obtaineddirectly by setting
theexpression
forJ+
inequation (2.19) equal
to zero[19].
Similarprocedures
can be used to derive aboundary
condition at z = L. In
general,
theboundary
conditions at either interface aregiven by
where n is the outward normal
[10].
Weemphasize
theapproximate
nature of theseboundary
conditions which were obtained
by
requiring
that the net inward flux ofdiffusing photons
bezero
[20].
Moregenerally,
the flux must be zero for allincoming
directions.However,
thismore
stringent
condition canonly
be met begoing beyond
the diffusionapproximation
to a moregeneral
transport
theory [10, 21].
Using
theboundary
conditions inequation (2.23),
we can solve the diffusionequation
forU(r, t )
for agiven experimental
geometry
[22]
and then calculate thetime-dependent
flux oflight emerging
from thesample
at time t fromequation (2.19)
evaluated at the exitpoint.
Alllight emerging
from thesample
at time t has traveled a distance s = ct.Thus,
the fraction oflight, P(s),
which travels a distance sthrough
thesample
issimply proportional
to the flux oflight emerging
from thesample
at time t =sic:
where rd denotes the exit
point
of thelight
and,
again,
n is the outward normal. The lastequality
inequation (2.24)
follows from theboundary
condition,
equation (2.23). Having
determined
P (s )
for agiven
geometry,
équation (2.16)
can be used to calculateg1( T ) .
2.C. DIRECT CALCULATION OF
g1( T ) .
- The calculation ofg1(T)
can begreatly simplified
by noting
thatequation (2.16)
isessentially
theLaplace
transform ofP (s).
Thus,
instead ofdiffusion
equation
and obtaing1(T) directly.
To thisend,
we introduce asimple change
ofvariables in
équation (2.1)
and lett = s/c.
Recalling
thatDt
=cl*/3,
equation (2.1)
becomes,
Multiplying
both sidesby exp (- ps )
andintegrating
with resect to s from 0 to oo, we obtainthe
Laplace
transform of the diffusionequation,
where
Û
=U(r,
p )
is theLaplace
transform ofU(r, s ),
and
Uo(r )
= limUo(r,
t )
= à(z -
zo, t ) [22]. Equation (2.26)
can be solvedsubject
to thet -> 0
Laplace
transform of the sameboundary
conditions usedpreviously equation (2.23), using
Green’s function
techniques.
This method iscarefully
discussedby
Carslaw andJaeger
[22]
where
explicit
solutions to the diffusionequation
and itsLaplace
transform aregiven
for mostgeometries
ofexperimental
interest. The solution toequation (2.26)
can be relateddirectly
tog1(,r) by taking
theLaplace
transformof P (s )
andusing equation (2.24)
to writeComparing equations
(2.16)
and(2.28),
we see thatwhere we have made the
identification, p
=(2
T/To)/l*,
andU(r,p)
has been normalizedso that
g1(0)
= 1.Thus,
by solving
theLaplace
transform of the diffusionequation
we canobtain the desired autocorrelation function
directly.
We illustrate this method of solution in sections 3 and 4 withexplicit
examples
for transmission andbackscattering geometries.
Finally,
forcomparison
to ourexperiments,
we note that weusually
measure normalizedintensity
autocorrelationfunctions, (/(T) /(0) / (/(0)2 =
1 +/3g2(T),
where/3
is deter-minedprimarily by
the collectionoptics
and is defined so thatg2(o)
= 1. For mostsystems
ofexperimental
interest,
the scattered electric field is acomplex
Gaussian random variable andthe
intensity
autocorrelation function is related to the field autocorrelation function calculated aboveby
theSiegert
relation,
Wolf et al.
[18]
haveexperimentally
verified that there is no observable deviation from Gaussian statistics forstrong
multiple scattering
insamples
similar to ours. Inaddition,
by
measuring g1(T) directly
inheterodyne experiments,
we have verified thevalidity
of3. Transmission.
The first
experimental
geometry
we consider is transmissionthrough
a slab of thickness L andinfinite extent
[6,
15].
Thelight
is incident on one side of theslab,
and is detected after it has diffused a distance L across thesample.
The incidentlight
beam can either be focused to apoint
on theface,
as illustrated infigure
la,
orexpanded
touniformly
fill the face of theslab,
as illustrated in
figure
2. The autocorrelation functions for these twoexperimental geometries
are different and can be calculated
by solving
theLaplace
transform of the diffusionequation
as
previously
discussed. In both cases,wc
take the source ofdiffusing intensity
to be adistance z = zo inside the illuminated face where we
expect
thatzo - 1 *.
Fig.
2. - Transmissiongeometry for an extended source. An extended source of
light (plane wave)
is incident on thesample
on the left side and is collected from apoint directly opposite
the center of theinput
beam on theright
side. A -pinhole
apertures.We first consider the case of uniform illumination of one side
by
an extended source so thatU(x, y, z, t ) = & (z - zo, t ).
The solution of the diffusionequation using
theLaplace
transform isgiven
in Carslaw andJaeger
[22] (§ 14.3)
for thisgeometry
and for theseboundary
and initial conditions.They
obtainwhere
a2 ~ 3 p /Q * = 6
" 1"0 f *2 and
Di
=cf*/3.
The coefficients A and B are chosen sothat the
boundary
conditions,
equation (2.23),
are satisfied at z = 0 and z = L. Aftertedious,
but
straightforward algebra,
we obtainwhere the second
expression
holds for r « T o. The characteristic time scale in theseFor the second
geometry,
we considerlight
incident from apoint
source on axis with thedetector so that
U(x,
y, x,t )
= 8(x,
y, z -z0, t).
The solution for thisgeometry
and theseboundary
and initial conditions canagain
be found in Carslaw andJaeger
[22]
(§ 14.10) :
where q
_ 2 + a 2,
a 2 == 3 p / f *
= 6’T / ’T 0 f *2,
and R = 0 when the source is on axis withthe detector. The coefficients A and B are
again
foundby
applying
theboundary
conditions. Weobtain,
where
and e =
2 f*/3
L.Again,
the characteristic time scale for thedecay
of the autocorrelationfunction in
equation (3.4)
isTo(f * / L )2.
This time scale reflects the diffusive nature of thetransport
of thelight,
which introduces a characteristicpath length,
sc = n, n c * i *,
wheren c
(L/f*)2
is the mean number ofsteps
for a random walk of end-to-end distance L and averagestep
length
f*.
Physically,
this characteristic time scalecorresponds
to the time taken for the characteristicpath length
tochange by - k,
so that the totalphase
shift isroughly
unity.
Thus,
we can estimate thetypical
distance an individualparticle
has moved from nc(q2) (âr2)
.--1,
whichgives âr rms
=k f
*/2
TT’ L. Sincef
*IL «
1,
thetypical length
scaleover which
particle
motion isprobed by
D W,S in transmission is much smaller than thewavelength.
This reflects the fact that thedecay
of the autocorrelation function is due to the cumulative effect of manyscattering
events, so that the contribution of individualparticles
tothe total
decay
is small. This is instriking
contrast toordinary dynamic light
scattering
where,
by
varying
q,length
scales greater than orroughly equal
to thewavelength
areprobed.
Similarly,
the time scale over whichparticle
motion isprobed
with DWS is much shorter than with DLS.Thus,
by adjusting
thesample
thickness L in transmission measurements, DWSprovides
a means forvarying
the range oflength
and time scales over whichparticle
motioncan
be measuredusing dynamic light scattering techniques.
Another
significant
difference between DLS and DWS is thedependence
onscattering
angle.
InDLS,
varying
theangle changes
thescattering
vector, q, thusvarying
thelength
scale over which motion is
probed. By
contrast, inDWS,
the diffusive nature of thetransport
ensures that the transmitted
light
has noappreciable dependence
onangle
and we do indeed find that the measured autocorrelation functions areindependent
of detectionangle
intransmission.
Autocorrelation functions measured in transmission are shown in
figure
3. Thesample
consisted of an aqueous
suspension
of0.605-jjLm-diam.
polystyrene
latexspheres
at a volumefraction
of .0 =
0.012 in a 1.0 mm thick cuvette. There is no unscatteredlight
transmittedthrough
thesample, insuring
that thestrong
multiple scattering
limit is achieved. The data in the lower curve were obtained when thesample
was illuminateduniformly by
al-cm diameter beam from an argon ion laser with À o = 488 nm.Imaging optics
collected the transmittedFig.
3.- Intensity
autocorrelation functions vs time for transmissionthrough
1-mm thick cells with0.605-fJ.m-diameter polystyrene spheres and 0
= 0.012. The upper curve is for apoint
source(see
Fig. la)
and the lower curve is for an extendedplane
wave source(see Fig. 2).
Smooth lines are fits tothe data
by equations (3.2)
and(3.4)
with f * = 167 ktm for the extended source and f* = 166 ktm forthe
point
source.beam was focused to a
point
on one side of thesample
and transmittedlight
was collectedfrom a
point
on axis with the incidentspot.
These dataclearly decay
moreslowly
than the data obtained with an extended source illumination.Physically,
this difference reflects the fact thatfor the extended source there is a
larger
contribution fromlong paths, resulting
in a fasterdecay
than for thepoint
source.To compare these data to the
expression
for the autocorrelation function derivedabove,
wetake zo =
(4/3)
f*,
but note that the solutions are insensitive to the exact value usedsince,
ingeneral,
zo - f *
andf*/Z.
1. The value chosen for zo affectsonly
the first fewsteps
of arandom walk which
typically
consists of agreat
number ofsteps.
Thus,
the relative contribution of the first fewsteps
is small. Infigure
3,
the solid linesthrough
the data are fitsto the
appropriate equations
above. The time constant To -(Dkô)-1
1 is setequal
to 4.52 mswhere D was obtained from a DLS measurement in the
single scattering
limitusing
.0 =
10-5.
The diffusion coefficient D remainsindependent
of concentration for theparticle
concentrations used in these measurements. For both cases, excellentagreement
is found between the data and thepredicted
formsof g2 ( T ) .
Theonly
fitting
parameter
is f*
and valuesof f*
= 167 )JLm for the extended source andf*
= 166 tm for thepoint
source are obtained.This excellent
consistency
forthe fitted
values off*
confirms that the differentdecay
rates infigure
3 are duesolely
togeometric
effects. The values obtained from the fit to the data are in reasonableagreement
with Miescattering
theory,
f*
=180 ktm. Nevertheless,
there is adiscrepancy
of about 7%,
with the measured values lower thanpredicted.
This in notexperimental
error, as a similardiscrepancy
is found for otherpolystyrene
latexsamples
with different sizes and different volume fractions. The values obtained from DWS measurementsin transmission are
consistently
lower than thepredicted
values,
typically by
about 10 %. Thisdiscrepancy
isprobably
not due to the consequences ofparticle
correlation on the value off*.
The
particle
interactions in thesepolystyrene samples
can beapproximated
as hardsphere
repulsion, allowing
theparticle
correlations to be determined[4].
These arerelatively
weakfor çb 0.1,
leading
tonegligible
effect onf*. Instead,
we believe that thediscrepancy
arises from theapproximate
nature of theboundary
condition that we use,equation (2.23).
Incondition and will result in a renormalization of the value of
f*
obtained from DWS transmission measurements. If this effect is notincluded,
theapparent f*
measured will be less than the correct value.While the autocorrelation functions shown in
figure
3 areclearly
notsingle exponentials,
their curvature in the
semi-logarithmic plot
is notlarge.
This reflects the existence of adominant characteristic
path length
and time scale for thesedata,
asexpected.
This alsosuggests
thesuitability
ofanalyzing
the databy
means of the first cumulantFI,
or thelogarithmic
derivative at zero timedelay.
Forequation (3.2),
the first cumulant isgiven by
For
equation (3.4),
the first cumulant must be evaluatednumerically.
Measurements offl
as a function ofsample
thickness are shown infigure
4 for several volume fractions.These data were obtained
using polystyrene
latexspheres
with a diameter of 0.497 jjbm. The incident beam was focused onto the face of awedge-shaped
cell,
allowing
the thickness to be variedby translating
the cell in the beam. Theangle
of thewedge
was about3 ;
so the cellshape
had very little effect on the form of the autocorrelation function. The data infigure
4 show theexpected
lineardependence
ofT
1 over a broad range of concentrationsconfirming
the diffusive nature of thetransport
oflight.
It isapparent
that the data do notextrapolate through
theorigin
but that theL-intercepts
are amonotonically decreasing
function
of particle
concentration and consistent withequation (3.5),
to withinexperimental
uncertainty.
The differentslopes
are dueprimarily
to the concentrationdependence
of f*,
which isexpected
to scaleinversely
withparticle density
for the volume fractions used here.Fig.
4. -Square
root of the first cumulantFi
1 of theintensity
autocorrelation function vssample
thickness L. The data were obtained
using
thepoint-source
transmission geometry for 0.497-fJ.m-diameterspheres
with volumes fractions of 1 %, 2 %, 5 %, and 10 %. The lineardependence
shown in theplot
confirms the diffusive nature of the transport oflight.
4.
Backscattering.
The second
geometry
we consider is that ofbackscattering [4,
5, 6,
15].
Here,
thelight
isfrom the same
face,
as illustrated infigure
5a. Inderiving
a functional form for theautocorrelation
function,
we would like to maintain thesimplicity
andelegance
of theLaplace
transformapproach
used in the case of transmission.However,
we must beextremely
cautious inusing
thisapproach
forbackscattering.
Inobtaining
theLaplace
transform inequation (2.16),
we have used a continuumapproximation
tochange
the summation overpaths
inequation
(2.15)
to anintegral.
However,
since s =nf
and we must have at least onescattering
event, werequire n -- 1 ;
thus,
the lower bound on s mustbe f
rather than 0.Equivalently,
forisotropic
scatterers, wheref
= f*,
thedecay
time for apath
oflength s
isexp[-
(2 7-/70) sli].
Allowing
s Q
leads tounphysically long decay
times,
sinceTo/4
represents
the shortestdecay
timepossible, corresponding
tolight singly
scatteredthrough
180°.Similarly,
foranisotropic
scatterers, wheref * > f,
werequire
s >1*
to obtainphysically meaningful decay
times.However,
in order to maintain thesimplicity
of theLaplace
transform,
the lower bound on theintegral
must be zero. Fortransmission,
this doesnot
present
aproblem
since the shortestpossible paths
are s =L,
so that n > 1.By
contrast,for
backscattering,
shortpaths
do contribute andthus,
inusing
the diffusionapproximation,
we must ensure that the contribution of the
unphysically
shortpaths
issuppressed.
A
simple
way ofachieving
this is to solve the diffusionequation using
an initial condition of a source a fixeddistance,
zo, in
from the illuminated face at z = 0. This ensures that there are no contributions frompaths
shorter than zo.Physically
we canregard
this as the source of thediffusing intensity,
which weexpect
to bepeaked
atzo - f *.
Thus,
for the initial condition wetake
U(r, t = 0)
= 5(x, y,
z -Z 0, t)
and for theboundary
conditionsagain
we useequation (2.23).
The solution for thisgeometry
is the same as for the case of transmission withan extended source, but here we evaluate it at the incident face and
obtain,
For a
sample
of infinitethickness,
equation (4.1) simplifies,
We note that the initial condition of a source at zo appears
explicitly
in thesolution,
reflecting
the
importance
of the contribution of the shortpaths.
Infact,
weexpect
there to be a distribution in theposition
of theapparent
source, zo. Thus we mustintegrate equation (4.2)
over a distribution of sources,
f (zo).
While the exact formof f (zo)
isunknown,
we do knowthat f (zo)
goes to zero aszo «-c f *
and for zo >f *. Furthermore,
weexpect f (zo)
to bepeaked
near
zo - f *.
Thus,
toleading
order in-B/ 7- / 7- 01
g 1 (r)
isgiven by equation (4.2),
withZo/f*
replaced by
(zo)
/f*,
the average over the source distributionf (zo).
The first ordercorrection is
[(zJ) / (zo) 2 - 1] TITO,
which is small for a narrow distributionf (zo).
Physically,
we can think of(zo)
as the averageposition
of the source ofdiffusing intensity,
and we
expect
that the exact form of the distributionf (zo),
and therefore(zo),
willdepend
on the
anisotropy
of thescattering
as reflectedby f */Î.
In contrast to
transmission,
inbackscattering
there is no well-defined characteristicpath
length
setby
thesample
thickness. Infact,
sincepaths
of alllengths
contribute inFig.
5. -Backscattering
geometry for an extended source.(a)
An extendedplane
wave source oflight
is incident on thesample
from the left side and is collected from apoint
near the center of the illuminated area.(b) 1 ( t ) vs t
forbackscattering
of a delta functionpulse,
8( t ),
from a semi-infinite slab of thickness L. Theplot
can also beinterpreted as P (s)
vs s since the fraction ofphotons travelling
adistance s
through
thesample
in a time t =s/c,
where c is thevelocity
oflight
in thesample.
Here,L = 1
mm, f*=100
JLm, and c = 2.25 x10 10 cm /s
(the speed
oflight
inwater).
Note that,P (s)
decays
ass-3/2
forlarge
s.multiple scattering.
As a consequence, there is a much broader distribution of time scales in thedecay.
Thelonger paths
consist of alarger
number ofscattering
events and thusdecay
more
rapidly, probing
the motion of individualparticles
over shorterlength
and time scales.By
contrast, the shorterpaths
consist of a smaller number ofscattering
events thusdecaying
more
slowly
andprobing
the motion of individualparticles
overlonger length
and time scales.This feature is
particularly advantageous
forexploring
thedynamics
ofinteracting
systems,
which can have a broad distribution of relaxation rates associated with motion over differentlengths
scales.An autocorrelation function
measured
inbackscattering
is shown infigure
6. Thesample
consisted of an aqueoussuspension
of0.412-J-Lm-diam.
polystyrene
latexspheres
at a volumefraction
of 0
= 0.05 in a 5 mm thick cuvette. It was illuminatedby
a uniformbeam,
1 cm indiameter ;
light
from a 50 tm diameterspot
near the center of the illuminated area wasimaged
onto the detector. Thescattering angle
was -175°,
although
we foundvirtually
nodependence
of the results onscattering angle
when it was varied - 20° from that usedhere,
asexpected
fordiffusing light.
Aftersubracting
thebaseline,
thelogarithm
of the normalized autocorrelationfunction,
isplotted
as a function oftime,
infigure
6a. Thelarge
amount ofcurvature exhibited
by
the data reflects the contributions ofpaths
with a wide range oflength
scales,
leading
to a wide range ofdecay
times. Assuggested by equation (4.2),
theexpression
for
g 1 (,r )
for DWS inbackscattering,
wereplot
the data infigure
6b as a function of thesquare root of
time,
in units of To. We use To = 3.01 ms, as measuredexperimentally
in thesingle scattering
limit,
and consistent with the value calculated from the Stokes-Einstein relation. The solid line is a fit to the functional formgiven by equation (4.2),
and is inreasonably good
agreement
with the data.However,
to within theprecision
ofexperiment,
the data shown infigure
6 is linear overnearly
three decades ofdecay
whenplotted
Fig.
6.- Intensity
autocorrelation function forbackscattering
from a 5-mm thick cellcontaining
0.412->m-diameter polystyrene spheres with *
= 0.05.(a)
Data isplotted
as a function of reduced time. Alarge
degree
of curvature is evident.(b)
Data isplotted
as a function of the square root of reduce time. The dotted linethrough
the data is a fit to the more exact form inequation (4.2).
The dashed linethrough
the data is a fit to thesimpler
form ofequation (4.3).
The residuals are shown above as afunction of the square root of the reduced time. The
simpler exponential decay
with square root of timeprovides
an excellentdescription
of the data.where y =
(zo > /f *
+2/3.
This result was obtainedpreviously using
thesimpler,
but lessrigorous, boundary
condition,
U(z
=0)
= 0[6, 23].
The behavior of the autocorrelation function shown in
figure
6 is in factquite general.
Forparticles
with diameterscomparable
to orgreater
thanÀ,
wherei * / f »
1,
thesimple
exponential
formgiven
inequation (4.3)
is observed. For smallparticles,
where f
*/i -
1,
there is some curvature for data