J. Fluid Mech.
(2010),
vol.
658,
pp.
188–210.
c
Cambridge University Press 2010
doi:10.1017/S0022112010001606
Single-particle motion in colloids:
force-induced diffusion
ROSEANNA N. ZIA
1
†
AND
JOHN F. BRADY
1
,
2
1
Department of Mechanical Engineering, California Institute of Technology, Pasadena, CA 91125, USA
2
Department of Chemical Engineering, California Institute of Technology, Pasadena, CA 91125, USA
(Received
7 July 2009; revised 26 March 2010; accepted 29 March 2010;
first published online 9 June 2010)
We study the fluctuating motion of a Brownian-sized probe particle as it is dragged
by a constant external force through a colloidal dispersion. In this nonlinear-
microrheology problem, collisions between the probe and the background bath
particles, in addition to thermal fluctuations of the solvent, drive a long-time diffusive
spread of the probe’s trajectory. The influence of the former is determined by the
spatial configuration of the bath particles and the force with which the probe perturbs
it. With no external forcing the probe and bath particles form an equilibrium
microstructure that fluctuates thermally with the solvent. Probe motion through
the dispersion distorts the microstructure; the character of this deformation, and
hence its influence on the probe’s motion, depends on the strength with which the
probe is forced,
F
ext
, compared to thermal forces,
kT/b
,definingaP
́
eclet number,
Pe
=
F
ext
/
(
kT /b
), where
kT
is the thermal energy and
b
the bath particle size. It is
shown that the long-time mean-square fluctuational motion of the probe is diffusive
and the effective diffusivity of the forced probe is determined for the full range of P
́
eclet
number. At small
Pe
Brownian motion dominates and the diffusive behaviour of the
probe characteristic of passive microrheology is recovered, but with an incremental
flow-induced ‘microdiffusivity’ that scales as
D
micro
∼
D
a
Pe
2
φ
b
, where
φ
b
is the volume
fraction of bath particles and
D
a
is the self-diffusivity of an isolated probe. At the
other extreme of high P
́
eclet number the fluctuational motion is still diffusive, and the
diffusivity becomes primarily force induced, scaling as (
F
ext
/η
)
φ
b
, where
η
is the vis-
cosity of the solvent. The force-induced microdiffusivity is anisotropic, with diffusion
longitudinal to the direction of forcing larger in both limits compared to transverse
diffusion, but more strongly so in the high-
Pe
limit. The diffusivity is computed for
all
Pe
for a probe of size
a
in a bath of colloidal particles, all of size
b
, for arbitrary
size ratio
a/b
, neglecting hydrodynamic interactions. The results are compared with
the force-induced diffusion measured by Brownian dynamics simulation. The theory
is also compared to the analogous shear-induced diffusion of macrorheology, as well
as to experimental results for macroscopic falling-ball rheometry. The results of this
analysis may also be applied to the diffusive motion of self-propelled particles.
Key words:
colloids, particle/fluid flow, rheology, Stokesian dynamics, suspensions
1. Introduction
The motion of active microscale particles driven through complex fluids is a physical
process central to many current scientific problems: vesicle trafficking in cells, artificial
†
Email address for correspondence: roseanna@caltech.edu
Single-particle motion in colloids: force-induced diffusion
189
nano-motors and nanotherapeutic drug delivery devices are a few important examples
(Janke
et al.
2005; Shirai
et al.
2005; Heath, Davis & Hood 2009). The increased
demand for knowledge of this small-scale behaviour has made microrheology a key
step in the understanding, use and design of such systems. Among the collection
of techniques known as microrheology, most involve tracking the movement of a
colloidal particle (or a set of particles) in order to determine the properties of the
surrounding environment (MacKintosh & Schmidt 1999). There are two main types of
particle tracking microrheology:
passive
– tracking the random motion due to thermal
fluctuations – and
active
– applying a constant or oscillatory force to the particles,
for example by using optical tweezers or magnetic fields. A detailed comparison can
be found in Khair & Brady (2006). Most microrheological work to date has focused
on passive microrheology, to obtain linear viscoelastic properties by correlating the
random thermally driven displacements of tracers to the complex modulus through a
generalized Stokes–Einstein–Sutherland relation – a process which is well understood
but limited in its scope to equilibrium systems. Yet as noted above, many systems
of practical interest are driven out of equilibrium and display (indeed, rely upon)
nonlinear behaviours. Recently a body of work has emerged focusing on this active
nonlinear microrheology regime (Habdas
et al.
2004; Meyer
et al.
2005; Squires &
Brady 2005; Khair & Brady 2006; Wilson
et al.
2009). In such a system, tracer
particles undergo displacements not only due to random thermal fluctuations, but
also due to the application of an external force applied directly to the tracer, or
‘probe’. The dispersion is driven out of equilibrium, and as with macrorheology,
dynamic responses such as viscosity can be measured. Since the tracer interrogates
the material at its own (micro)scale, much smaller samples are required compared
to traditional macrorheology, and localized material heterogeneity can be explored.
This is a particular benefit for rare biological materials and small systems such
as cells. Khair & Brady (2006) recently established the theory that predicts the
microviscosity of dilute systems of colloids, and defined the relationship between
micro- and macroviscosity – a critical step in the development of microrheology as
an experimental tool. Recent experiments confirm the theory (and raise additional
questions) (Meyer
et al.
2005; Squires 2008; Wilson
et al.
2009).
But in both theory and experiment, the focus thus far has been on the mean
response of the material – the viscosity – and far less work has been devoted to
particle fluctuations that occur due to collisions between the probe and bath particles.
As the probe moves through the dispersion it must push neighbouring particles
out of its way; these collisions induce fluctuations in the probe’s velocity, scattering
it from its mean path. Is this scattering diffusive? Is it isotropic? How important
is the scattering compared to the Brownian diffusion the probe simultaneously
undergoes? The answers to these questions are fundamental to understanding the
motion of an active microscale particle – important for both scientific and technology
considerations. Little work has been published on this topic (Habdas
et al.
2004), even
though it has major implications for a wide range of technologies beyond material
interrogation.
Previous study of particle fluctuations in colloidal macrorheology shows that
imposing a shearing flow on a suspension enhances particle diffusivity (Leighton &
Acrivos 1987; Morris & Brady 1996; Brady & Morris 1997; Breedveld
et al.
1998).
The imposed shear flow drives the microstructure from equilibrium, giving rise
to mechanisms of diffusion not present in a quiescent suspension: a deformed
microstructure and interparticle collisions. A forced microrheological probe also
imposes a flow that drives the suspension from equilibrium, again leading to a
190
R. N. Zia and J. F. Brady
(
a
)
–
–
+
+
+
+
–
–
(
b
)
F
γ
.
Figure 1.
Microstructural deformation under (
a
) macrorheological shear flow and (
b
)micror-
heological forcing. In simple shearing motion (
a
), bath particles accumulate along the
compressional axis and deplete along the extensional axis. A tracer at the origin (the dark
sphere) experiences both in-plane and out-of-plane bath particle gradients. In (
b
), the (dark)
tracer itself deforms the microstructure, accumulating particles on its upstream face and leaving
a wake of depletion behind, creating an axisymmetric structure with only longitudinal and
transverse components.
deformed microstructure and interparticle collisions – and hence to an analogous
force-induced diffusion, or ‘microdiffusivity’. It is the primary objective of this study
to extend the theoretical model of active nonlinear microrheology to one that is
explicit in the fluctuations of the microstructure, and thereby develop expressions for
predicting the resultant force-induced diffusion.
It is also useful to ask whether the qualitative agreement between micro- and
macroviscosity can be extended to the micro- and macrodiffusivity. Both the shear-
and force-induced diffusions grow out of fundamentally similar mechanisms: external
forcing causes the tracer to scatter off of the microstructure, rather than wander
passively through it. But the directionality and magnitude of the scattering depend
on the shape of the deformed microstructure, and this asymmetry is distinct for the
two cases, as illustrated in figure 1. The idea of whether a direct correlation between
macro shear-induced diffusion and micro force-induced diffusion is possible (or even
necessary) will be explored in this study, and a comparison is sought between the two.
To build up a physical model, we follow the example of Squires & Brady (2005)
and consider the motion of a Brownian probe driven by an externally applied force
through a dispersion of neutrally buoyant-force- and torque-free colloidal particles.
The size ratio of probe to bath particle is arbitrary. As the probe particle moves
through the suspension it must push neighbouring particles out of its way; a build-
up of background particle concentration forms in front of the advancing probe
and a deficit or wake trails it. The bath particles (including the probe) undergo
Brownian diffusion due to thermal fluctuations of the solvent, which acts to restore
the deformed microstructure to an equilibrium configuration. The ratio of advective
forcing to entropic restoring force is the P
́
eclet number,
Pe
=
F
ext
/
(
kT /b
), where
kT
is the thermal energy and
b
the bath particle size. In the linear-response regime
(
Pe
→
0), diffusion of the bath particles dominates. As the probe forcing increases
and
Pe
grows beyond
∼
O
(1) – the active nonlinear-response regime – advection
plays an increasingly important role in the shape of the distorted microstructure.
Since the details of this shape govern the strength and likelihood of collisions between
probe and bath particles, its determination is critical to understanding the resultant
force-induced diffusive spread of the probe’s trajectory.
Single-particle motion in colloids: force-induced diffusion
191
The spatiotemporal distribution of bath particles obeys a Smoluchowski equation.
Prior treatments of active microrheology formulated the expression for the steady
microstructure moving relative to a fixed probe. We extend this approach by
considering both the steady microstructure deformation and fluctuations in the
microstructure responsible for diffusion of the probe. The resulting Smoluchowski
equations are solved for all
Pe
by a combination of perturbation methods and
numerical computation to obtain both the steady microstructure along with a new
quantity, the probability-weighted collisional displacements of the probe relative to
the bath particles.
Scaling arguments are useful for predicting the behaviour for extreme values of the
P
́
eclet number. For random-walk processes, the diffusivity scales as
D
∼
l
2
τ
,
(1.1)
where
l
is the size of a probe step and
τ
is the decorrelation time. For very weak
forcing,
Pe
1, Brownian diffusion dominates the motion; so the time scale is
τ
∼
(
a
+
b
)
2
/D
a
, where
D
a
is the self-diffusivity of an isolated probe particle of size
a
.
In this linear-response regime,
l
∼
Pe
(
a
+
b
). The number of diffusive steps depends
on the number of bath particle collisions; thus, for very small
Pe
, the microdiffusivity
should scale quadratically in the forcing and linearly in volume fraction of bath
particles
φ
b
:
D
micro
∼
Pe
2
φ
b
D
a
,
Pe
1
.
(1.2)
For large forcing,
Pe
1, the time scale is now advective,
τ
∼
(
a
+
b
)
/U
,theprobe
can move
l
∼
(
a
+
b
) in that time and the force-induced microdiffusivity should scale
linearly with the P
́
eclet number and in volume fraction of bath particles:
D
micro
∼
Pe
φ
b
D
a
,
Pe
1
.
(1.3)
In the remaining sections of this paper, we propose and examine an extended
model for active nonlinear microrheology that is explicit in the probe fluctuations, and
explore the resultant force-induced diffusion. In
§
2, we formulate the Smoluchowski
equation that governs the evolution of the microstructure in physical space, along
with kinematic expressions for the probe flux. The latter comprises advective and
interparticle contributions, and from these the diffusive flux of the probe is extracted
and separated into Brownian and flow-induced components. To make analytical
progress an assumption of diluteness is made. In
§
3 the Smoluchowski equation is
separated into steady and fluctuating components, completing the formulation of the
problem. In
§
4.1 the case of asymptotically weak probe forcing,
Pe
1, is studied.
Regular perturbation expansions are sufficient to obtain the
O
(
φ
b
) correction to the
long-time self-diffusivity, which corresponds to passive diffusion:
D
∼
D
a
(1
−
2
φ
b
),
where
φ
b
is the (dilute) volume fraction of bath particles and
D
a
is the diffusivity
of an isolated probe (Batchelor 1976). Higher orders in
φ
b
Pe
are required in order
to find the first effect of the forcing on particle self-diffusion and we proceed to
O
(
φ
b
Pe
2
) whereupon the problem becomes singular, which requires the use of matched
asymptotic expansions. In
§
4.2 we shift focus to the opposite extreme of very strong
probe forcing, or
Pe
1, and the nonlinear response of the microstructure is exposed.
This limit is also singular with a boundary layer at the probe surface. To solve for
probe fluctuations at arbitrary values of the P
́
eclet number, a numerical solution
is required, and a finite difference scheme is employed to this end in
§
4.3. In
§
5
we present an alternative solution of the problem based upon measurements of
192
R. N. Zia and J. F. Brady
the probe’s displacements obtained by Brownian dynamics simulation, presented
juxtaposed to the Smoluchowski results. Section 6 is devoted to a comparison of
microdiffusivity to the macrodiffusivity (theory and experiments). Throughout, we
consider a simplified model that neglects hydrodynamic interactions between particles;
this simplification affords insight into the basic physics of diffusive behaviour arising
from interparticle forcing, but could be extended to include other interparticle forces
such as hydrodynamic interactions; the approach also offers a direct solution to related
problems such as self-propelled objects. The study is concluded with a discussion in
§
7, including a brief discussion of hydrodynamic interactions, self-propulsion and
non-spherical shapes.
2. Microdiffusivity
The theoretical framework of active microrheology begins with a simple model: a
single Brownian probe particle of radius
a
is dragged by a constant external force
F
ext
through a dispersion of colloidal particles, all of size
b
, which are immersed in
a solvent of density
ρ
and viscosity
η
. The importance of fluid inertia relative to the
viscous shearing forces is characterized by the Reynolds number,
Re
=
ρUa/η
,where
U
is the characteristic velocity of the moving probe, and for micrometre-sized probes
Re
1, so that the fluid mechanics are governed by Stokes flow. The advective forcing
of the probe acts to deform the microstructure of the bath, while the Brownian motion
of the bath particles counteracts it in an attempt to restore equilibrium. This interplay
drives fluctuations in the probe’s velocity that give rise to diffusive behaviour. The
primary goals of this section are to examine the dispersive contributions to the probe’s
flux relative to the bath, formulate the expression for the force-induced component
and show that the force-induced dispersive motion is indeed diffusive.
We begin by defining the hard-sphere model for the interactive potential
V
(
r
)
between a particle of size
a
and a particle of size
b
located at positions
x
1
and
x
2
,
respectively; they are separated by
r
=
x
2
−
x
1
. Thus defined, the particles exert no
force on each other until their surfaces touch,
r
=
a
+
b
, at which point an infinite
repulsive potential is exerted to prevent their overlap:
V
(
r
)=
{
∞
,r<a
+
b,
0
,r>a
+
b.
(2.1)
In general, the radii
a
and
b
at which particles exert the hard-sphere force are not the
same as their hydrodynamic radii,
a
h
and
b
h
, the surface at which the no-slip boundary
condition is obeyed. Various physical conditions of the colloids or the solvent can
extend the effective size of the particle beyond the hydrodynamic radius, e.g. steric
hindrance or an ionic screening layer; two particles may then experience a hard-sphere
repulsive force at overlap of their increased effective or ‘thermodynamic’ radii.
Following the excluded annulus model of Morris & Brady (1996) and Bergenholtz
et al.
(2002), the ratios
λ
a
=
a/a
h
and
λ
b
=
b/b
h
give the relative importance
of hydrodynamic interactions between particles (figure 2). When
λ
a
,
λ
b
∼
O
(1),
hydrodynamic interactions strongly affect the particle configuration; as
λ
a
,
λ
b
→
1,
the particles get close enough that short-range lubrication forces become important.
We shall assume a system of particles for which
λ
a
,
λ
b
1, where hydrodynamic
interactions are negligible compared to interparticle and thermal forces. This model
captures the essential features of the dispersive process while keeping the analyses
Single-particle motion in colloids: force-induced diffusion
193
z
θ
a
h
b
h
b
a
r
F
ext
y
Figure 2.
Pair interaction for the probe and bath particle.
as simple as possible; the effect of hydrodynamic interactions are discussed briefly
in
§
7.
We consider the probe amid a dispersion of
N
−
1 bath particles in a configuration
x
N
. The distribution of particles is given by an
N
-particle probability density,
P
N
(
x
1
,
x
2
,...,
x
N
;
t
), which obeys a Smoluchowski equation
∂P
N
∂t
+
N
∑
i
=1
∇
i
·
j
i
=0
,
(2.2)
where the sum is over all particles in the dispersion, and the flux of particle
i
is given
by
j
i
=
U
i
P
N
(
x
N
;
t
)
−
N
∑
j
=1
D
ij
·∇
j
(ln
P
N
(
x
N
;
t
)+
V
N
/kT
)
P
N
(
x
N
;
t
)
.
(2.3)
Here,
kT
is the thermal energy,
D
ij
=
kT
M
ij
is the relative Brownian diffusivity
between particles
i
and
j
and
M
ij
is the mobility tensor relating the velocity of
particle
i
to the force exerted on particle
j
. The first term on the right-hand side of
(2.3) is the advective flux of particle
i
with velocity
U
i
, the second term is the flux
due to entropic gradients in the microstructure and
D
ij
·
(
∇
j
V
N
/kT
)
P
N
gives the flux
of particle
i
due to the forcing of interactive potential with particle
j
.
In the dilute limit, only pair interactions are important, and the probability
P
N
in
(2.2) and (2.3) reduces to the pair probability of finding the probe at position
x
1
and
a bath particle at position
x
2
. To analyse the relative flux between probe and bath, it
is convenient to change to a frame of reference moving with the probe, placing the
probe at
z
=
x
1
, and a bath particle at
r
=
x
2
−
x
1
. The pair Smoluchowski equation
becomes
∂P
2
(
z
,
r
;
t
)
∂t
+
∇
z
·
j
a
+
∇
r
·
(
j
b
−
j
a
)=0
.
(2.4)
Here, the subscripts
a
and
b
refer to the probe and the bath particle, respectively. We
are interested in the flux of the probe relative to any other particle, and so we integrate
P
2
(
z
,
r
;
t
) over all possible positions of a bath particle, to obtain the single-particle
Smoluchowski equation for the probe particle. Applying the divergence theorem and
194
R. N. Zia and J. F. Brady
noting that relative flux is zero at contact and at infinity, we have
∂P
1
(
z
;
t
)
∂t
+
∇
z
·
j
a
=0
,
(2.5)
where
j
a
≡
∫
j
a
d
r
. The unbounded domain of the probe makes a transformation
to Fourier space convenient. Taking the Fourier transform, denoted by
̂
,ofthe
Smoluchowski equation (2.5) yields
∂
ˆ
P
1
(
k
;
t
)
∂t
+i
k
·
ˆ
j
a
=0
,
(2.6)
where the average flux
ˆ
j
a
from (2.3) has also been transformed to Fourier space:
ˆ
j
a
=
(
U
a
−
i
k
D
a
)
ˆ
P
1
(
k
;
t
)+
D
a
∫
∇
r
ˆ
P
2
(
k
,
r
;
t
)d
r
.
(2.7)
Here,
U
a
=
F
ext
/
6
π
ηa
is the probe velocity due to the imposed constant external
force,
D
11
≡
D
a
the probe self-diffusivity, i the imaginary unit and the angle brackets
denote an ensemble average over all possible suspension configurations.
ˆ
P
2
(
k
,
r
;
t
)
and
ˆ
P
1
(
k
;
t
) are the Fourier transforms of
P
2
(
z
,
r
;
t
)and
P
1
(
z
;
t
), respectively.
The last term in (2.7) explicitly preserves the effect of bath particles on the probe.
In order to determine the average probe flux, the distribution of the bath relative to
the probe must be determined. To this end we define the structure function
g
(
k
,
r
t
):
ˆ
P
2
(
k
,
r
;
t
)
≡
n
b
g
(
k
,
r
;
t
)
ˆ
P
1
(
k
;
t
)
,
(2.8)
where
n
b
is the undisturbed number density of bath particles far from the probe.
Expression (2.8) is similar to the familiar definition of the pair-distribution function
in physical space,
P
2
(
z
,
r
;
t
)=
n
a
n
b
g
(
z
,
r
;
t
)(since
z
is the origin, it is typically omitted).
But
g
(
k
,
r
;
t
) is not simply the Fourier transform of
g
(
z
,
r
;
t
). Rather, we have
defined in Fourier space the microstructure
g
(
k
,
r
;
t
) where the
k
-dependence explicitly
preserves fluctuations of the probe relative to the origin.
Also note that
g
(
k
,
r
,t
) is not to be confused with the structure factor,
S
(
z
,
q
,t
)=
F
r
[
P
2
(
z
,
r
,t
)], corresponding to a Fourier transform with respect to the
separation vector
r
between the probe and the bath particle. Indeed, we solve for
the distribution of bath particles relative to the probe in physical (real) space
r
.The
Fourier transform variable
k
is with respect to the absolute position of the probe,
z
. To determine the diffusive motion of the probe one imagines a concentration
gradient of a dilute collection of probes; these physical-space gradients correspond to
algebraic multiples of the wave vector,
k
, in Fourier space. The probe flux down this
concentration gradient is influenced by the interaction with bath particles distributed
according to
g
(
k
,
r
,t
), a distribution that must be determined for all
r
.
Combining (2.7) and (2.8) we obtain the following for the steady average probe
flux:
ˆ
j
a
=
[
U
a
−
D
a
i
k
+
n
b
D
a
∫
∇
r
g
(
k
,
r
)d
r
]
ˆ
P
1
(
k
)
.
(2.9)
For the long-time self-diffusion of the probe, we consider the short wave vector (long
length scale) limit and expand
g
(
k
,
r
)forsmall
k
, corresponding to a weak gradient
in the ‘concentration of probes’:
g
(
k
,
r
)=
g
0
(
r
)+i
k
·
d
(
r
)+
···
,
(2.10)
Single-particle motion in colloids: force-induced diffusion
195
which immediately yields the two terms governing the scattering of the probe: the
steady microstructure,
g
0
(
r
), and the probability-weighted displacement of the probe,
d
(
r
) – i.e. the likelihood of a collision and the strength and direction of the probe
displacement upon collision, respectively. Substituting this into the expression for
probe flux yields
ˆ
j
a
=
([
U
a
+
n
b
D
a
∫
∇
g
0
(
r
)d
r
]
−
D
a
i
k
·
[
I
−
n
b
∫
∇
r
d
(
r
)d
r
])
ˆ
P
1
(
k
)
,
(2.11)
where
I
is the identity tensor. Examination of (2
.
11) reveals the effect of the bath
particles on both the mean (
O
(1)) and fluctuating (
O
(
k
)) response of the overall
suspension. The first bracketed term gives the probe’s average speed through the fluid:
U
a
is reduced by the entropic reactive force of the microstructure, as given by the
integral term. This reduction in probe speed due to the suspended particles was used by
Squires & Brady (2005) to define the microviscosity. Recalling that i
k
terms represent
diffusion, the second bracketed group gives the effective diffusivity of the probe; the
third term its free Brownian diffusion, plus an increment due to interactions with the
bath. This increment corresponds to hard-sphere interactions between the probe and
bath that scatter the probe’s mean path. From a phenomenological perspective, the
effect of the bath particles is to reduce the mean velocity of the probe and increase
the diffusive spread of its trajectory – the effective diffusivity. Defining the second
bracketed group as the effective diffusivity of the probe and integrating by parts we
obtain
D
eff
≡
D
a
[
I
−
n
b
∮
r
=
a
+
b
nd
d
S
]
,
(2.12)
where
n
is the unit surface normal pointing outwards from the probe.
In the limit
Pe
→
0, the entropically hindered diffusion of a particle in a
dilute suspension without hydrodynamic interactions must be recovered,
D
eff
=
D
s
∞
=
D
a
(1
−
2
φ
b
) (Batchelor 1976), for
a/b
= 1. Motivated by this fact, we denote the
corresponding displacement field for the unforced probe
d
entropic
≡
d
(
Pe
= 0). Hence,
we express the total displacement field as a sum of entropic and mechanical
contributions:
d
=
d
entropic
+
d
,
(2.13)
where
d
is the probe fluctuation over and above that for hindered passive diffusion.
As we show below,
d
entropic
contributes
−
2
φ
b
D
a
to the effective diffusivity; so we write
D
eff
=
D
a
I
(
1
−
2
φ
b
)
+
D
micro
,
(2.14)
where we have defined
D
micro
≡
n
b
D
a
∮
nd
d
S.
(2.15)
The effective diffusivity of a tracer particle is its bare diffusivity,
D
a
I
, minus the
entropic hindrance of the bath, 2
φ
b
D
a
I
, plus an enhancement due to mechanical
scattering by the other bath particles,
D
micro
. The force-induced microdiffusivity is
proportional to the number density of bath particles, the isolated probe self-diffusivity,
and to the first moment of the hard-sphere deflections.
It remains only to obtain the steady microstructure
g
0
(
r
) and the first fluctuation
correction,
d
(
r
).
196
R. N. Zia and J. F. Brady
Pe
= 0.01
Pe
= 1
Pe
= 5
Pe
= 20
Figure 3.
(Colour online) Theoretical predictions for the deformed microstructure around a
moving probe particle in the absence of hydrodynamic interactions at the pair level. The test
particle is moving to the right and there is a build-up of background particle density in front
(red) of the probe and a deficit (dark blue) in the trailing wake (Squires & Brady 2005).
3. Non-equilibrium microstructure
The goal of this section is to formulate an expression governing the evolution of
the microstructure
g
(
k
,
r
). The Smoluchowski equation governing the pair probability
in Fourier space gives the evolution of the fluctuating microstructure:
∂
ˆ
P
2
∂t
+
∇
r
·
[
U
r
−
D
r
∇
r
]
ˆ
P
2
+
D
a
i
k
·∇
r
ˆ
P
2
+i
k
·
ˆ
j
a
=0
,
(3.1)
where we have defined the relative Brownian diffusivity between the probe and the
bath particle,
D
r
≡
D
a
+
D
b
and
U
r
≡
U
a
−
U
b
. With the definition of
g
(
k
,
r
) in (2.8)
and substituting (2.6) into (3.1) we have leading order in diluteness, at steady state:
∇
r
·
[
U
r
−
D
r
∇
r
]
g
+2
D
a
i
k
·∇
r
g
=0
,
(3.2)
n
·
[
U
r
g
−
D
r
∇
r
g
+
D
a
i
k
g
]=0 at
r
=
a
+
b,
(3.3)
g
∼
1as
r
→∞
,
(3.4)
in which conservation requires a no-flux boundary condition at contact and there is
no long-range order. The equations are made dimensionless by scaling quantities as
r
∼
a
+
b, U
∼
F
ext
/
6
π
ηa, D
∼
D
a
+
D
b
=
kT
6
π
η
(
1
a
+
1
b
)
,
(3.5)
and together with of the expansion (2.10) of
g
(
k
,
r
), the steady microstructure obeys
∇
2
g
0
−
Pe
u
·∇
g
0
=0
,
(3.6)
n
·
[
∇
g
0
−
Pe
u
g
0
]=0 at
r
=1
,
(3.7)
g
0
∼
1as
r
→∞
,
(3.8)
where
u
is the unit vector parallel to probe forcing. Squires & Brady (2005) have
solved this problem analytically for all
Pe
=
F
ext
/
(
kT /b
). A contour plot in figure 3
shows the perturbed steady microstructure
g
0
for a range of
Pe
.
The expression governing the probability-weighted displacement also forms an
advection–diffusion equation, but is forced by gradients in the steady microstructure:
∇
2
d
−
Pe
u
·∇
d
=
β
∇
g
0
,
(3.9)
n
·
(
∇
d
−
Pe
ud
)=
1
2
β
g
0
at
r
=1
,
(3.10)
d
∼
0as
r
→∞
,
(3.11)
Single-particle motion in colloids: force-induced diffusion
197
where
β
≡
2
/
(1 +
a/b
). Hence, the displacement field
d
is coupled to
g
0
. In the next
section the coupled system is solved analytically in the limit of small and large
Pe
,
and numerically for arbitrary values of the P
́
eclet number.
4. Results
4.1.
Low-Pe limit
For small P
́
eclet number, Brownian diffusion of the bath particles easily repairs the
deformation of the microstructure caused by the probe’s motion. Since the bath is
hardly displaced from equilibrium, we approach the solution with a perturbation
expansion in small
Pe
. Recalling (3.6)–(3.8), however, it is apparent that the problem
is singular: at some distance
ρ
∼
r
Pe
from the probe, advection is as important as
diffusion. The domain is divided into two regions, and matched asymptotic expansions
yield the expression for the steady microstructure
g
0
to
O
(
Pe
2
):
g
0
(
r
;
Pe
)=1
−
1
2
u
·
r
r
3
Pe
+
1
4
(
1
r
−
1
3
uu
:
[
I
r
3
−
3
rr
r
5
]
−
uu
:
rr
r
3
)
Pe
2
,
(4.1)
which agrees with the solution that Squires & Brady obtained to
O
(
Pe
), which we
have extended here to
O
(
Pe
2
).
A similar method is applied to (3.9)–(3.11) to obtain the fluctuation field. The
Pe
0
term of the expansion of
d
yields the solution
d
entropic
≡
d
(0)
=
−
1
4
β
r
r
3
,
(4.2)
which gives
D
eff
(
Pe
=0)=
D
a
[
1
−
1
2
(
1+
a/b
)
2
φ
b
]
,
(4.3)
which, for equal probe and bath particle size, recovers the long-time self-diffusivity
of an isolated sphere in a quiescent solvent reported by Batchelor (1976),
D
eff
(
Pe
=0)=
D
s
∞
=
D
a
(1
−
2
φ
b
). Since there is no flow at
Pe
=0,this
O
(
φ
b
) correction
is due to the entropic hindrance of the bath.
It is interesting to note that the
O
(1) solution for
d
is the same as the
O
(
Pe
)
solution for
g
0
. In fact the problems for
g
0
and
d
are identical in the limit
Pe
→
0.
In the linear-response regime, whether the forcing is by external means,
g
0
,orby
thermal fluctuation,
d
, the resulting mobility reduction or diffusivity –
kT
times the
mobility – is the same.
At the next order in
Pe
, we resolve the vector
d
into scalar components parallel
and transverse to the direction of the probe’s velocity,
d
=
d
z
u
,
d
⊥
,x
=
d
x
e
x
and
d
⊥
,y
=
d
y
e
y
.The
O
(
φ
b
Pe
) fluctuation makes no contribution to the microdiffusivity –
in keeping with scaling predictions, since
nd
(1)
∼
u
·
nnn
and the displacement of a
sphere has no coupling to odd tensors.
Proceeding to the next order in
Pe
, the singular nature of the problem becomes
evident, as the solution by regular perturbation expansion fails to decay to zero
far from the probe. An asymptotic expansion in the inner region is matched to
the solution in the outer region, giving the proper far-field condition for the inner
solution. The first correction to the fluctuation that gives rise to microdiffusive
198
R. N. Zia and J. F. Brady
behaviour is then
d
(2)
=
β
[
−
13
48
−
(
67
360
r
r
3
−
11
480
[
3
r
r
5
−
5
uu
:
rrr
r
7
]
)
·
u
]
−
β
[
13
144
(
[
r
r
3
−
3
uu
:
rrr
r
5
]
−
1
96
(
41
r
r
−
15
uu
:
rrr
r
3
))
·
u
]
,
(4.4)
d
(2)
⊥
=
β
{
−
7
80
r
2
+
13
48
uu
:
rr
r
4
+
11
480
[
1
r
4
−
5
uu
:
rr
r
6
]
+
5
32
[1
−
uu
:
rr
]
r
·
e
y
}
,
(4.5)
which yields for the microdiffusivity in the limit of
Pe
1 (plotted in figure 6):
D
micro
=
79
180
(
1+
a
b
)
2
D
a
Pe
2
φ
b
,
(4.6)
D
micro
⊥
=
11
60
(
1+
a
b
)
2
D
a
Pe
2
φ
b
.
(4.7)
When forced very weakly through a dilute suspension, a probe particle diffuses with
its bare diffusivity
D
a
minus an entropic hindrance due to the presence of the bath
particles that scales as
φ
b
D
a
plus an enhancement due to hard-sphere collisions with
the bath particles – characteristic of the Taylor dispersion for particles in a bulk
flow. As predicted by scaling arguments in
§
1, in the low-
Pe
limit, the force-induced
enhancement to the diffusion is quadratic in the forcing; it is also linear in the
volume fraction of bath particles,
φ
b
, and anisotropic, preferentially diffusing along
the direction of forcing (as compared to the transverse direction) by a factor of 2
.
39.
4.2.
High-Pe limit
For very large P
́
eclet number, the shape of the microstructure in front of the probe
is deformed into two distinct regions: an outer region in which advection dominates
diffusion and the microstructure is undisturbed, and an inner region – a 1
/
Pe
-thin
boundary layer that forms on the upstream face of the probe – where diffusion
balances advection. A
Pe
-long wake of particle deficit forms behind the probe, where
probability for a probe/bath particle collision is small. The particles that reside
inside the boundary layer provide the most probability for a strong hard-sphere
deflection of the probe (cf. figure 3). Inside the boundary layer, a coordinate rescaling
R
=(
r
−
1)
Pe
∼
O
(1) preserves the diffusive term, properly reflecting the physics of the
inner region and allowing satisfaction of the no-flux condition at contact. A singular
perturbation expansion in powers of
Pe
−
1
then obtains the deflection field in the
boundary layer on the upstream face of the probe,
π
/
2
θ
π
:
d
=
−
β
12
u
·
n
(
u
·
e
θ
)
2
(
1+(
u
·
n
)
3
)
e
Pe
(
r
−
1)
u
·
n
Pe
+
O
(1)
,
(4.8)
d
⊥
=
−
β
12
(
u
·
n
)(
u
·
e
θ
)(
n
·
e
y
)e
Pe
(
r
−
1)
u
·
n
Pe
+
O
(1)
,
(4.9)
where
u
·
n
0,
θ
is the angle between
u
and the normal
n
and
e
θ
is a unit vector in
the direction of
θ
. As expected from earlier scaling arguments, the microdiffusivity is
linear in the forcing when
Pe
1:
D
micro
=
1
4
(
1+
a
b
)
2
(
ln 2
−
1
4
)
D
a
Pe
φ
b
+
O
(1)
,
(4.10)
D
micro
⊥
=
1
32
(
1+
a
b
)
2
D
a
Pe
φ
b
+
O
(1)
.
(4.11)
Single-particle motion in colloids: force-induced diffusion
199
Pe
= 20
Pe
= 5
Pe
= 1
Pe
= 0.01
Figure 4.
(Colour online) The fluctuation field longitudinal to probe forcing. Blue areas
indicate regions of weak or no deflection; red areas indicate probability of strong deflection.
Pe
= 20
Pe
= 5
Pe
= 1
Pe
= 0.01
Figure 5.
(Colour online) The fluctuation field transverse to probe forcing. Blue areas
indicate regions of weak or no deflection; red areas indicate probability of strong deflection.
As in the low-
Pe
limit, the large
Pe
microdiffusivity is also transversely anisotropic,
with a longitudinal-to-transverse preference of approximately 7
/
2. The effect of the
hard-sphere collisions is a
Pe
-large diffusive scattering of the probe’s trajectory.
The high-
Pe
analytical results are shown in figure 6 alongside those for small
Pe
.
When scaled with the volume fraction of bath particles and the probe’s bare diffusivity
D
a
, the asymptotic limits of
Pe
1and
Pe
1 form a framework to guide the analysis
for intermediate values of the P
́
eclet number, which is developed in the next section.
4.3.
Numerical solution for arbitrary Pe
To obtain the fluctuating microstructure over the full range of
Pe
, a numerical solution
of the full Smoluchowski equations (3.6)–(3.8) and (3.9)–(3.11) is required. The radial
coordinate is rescaled with
Pe
−
1
to obtain the stretched coordinate
R
=
Pe
(
r
−
1).
Because the flow is axisymmetric about the line of external forcing, derivatives of
g
0
and
d
in the azimuthal angle are zero.
A central difference scheme is used to discretize gradients over the two-dimensional
domain. Once a boundary layer forms, i.e. beyond
Pe
O
(1), the radial gradients in
the microstructure are almost entirely confined to the boundary layer. As
Pe
continues
to grow and the boundary layer thins, a grid point concentration function that varies
with
Pe
increases the density of grid points close to contact, yet retains sufficient
resolution far from the probe to capture the physics throughout the upstream domain.
The difference coefficients and operators for both radial and angular directions are
compactly arranged into first- and second-order sparse matrices (Swaroop 2004). The
solutions for the steady and fluctuating pair-distribution function are then obtained
in
Matlab
using a
LaPack
iterative banded solver.
The steady microstructure is solved first (figure 3), and the gradients
∇
g
0
used
to drive the fluctuation field
d
. Contour plots for the deflection field are shown in
figures 4 and 5; the anisotropy is evident. The longitudinal fluctuations show that at
200
R. N. Zia and J. F. Brady
10
–2
10
–1
10
0
10
1
10
2
(
D
micro
/
D
a
)/
φ
b
10
–2
10
–1
10
0
10
1
10
2
Pe
=
F
ext
b
/
kT
(ln 2 – )
Pe
2
φ
b
79
45
Pe
2
φ
b
11
15
Pe
φ
b
1
8
Pe
φ
b
1
4
Figure 6.
The force-induced diffusivity
D
micro
, scaled with the probe bare diffusivity
D
a
and
the volume fraction of bath particles
φ
b
. Analytical solutions for asymptotically small and large
forcing are shown by solid lines (longitudinal) and dotted lines (transverse). Curved asymptotes
exclude the entropic contribution (dashed for longitudinal; dash-dotted for transverse). Open
symbols represent the numerical solution of the full Smoluchowski equation (circles for the
longitudinal microdiffusivity, squares for the transverse microdiffusivity).
very small
Pe
(similar to
Pe
=0
.
01 in the figure), the fluctuations form a dipole about
the probe, with highest probability of a strong kick at the upstream face of the probe,
and decaying as
∼
1
/r
2
.AstheP
́
eclet number is increased, the boundary layer thins
(similar to
Pe
= 20 in figure 4), and strong kicks to the probe result from particles
swept into the boundary layer on the front of the probe. Particles diffuse and weakly
advect around the probe, the boundary layer detaches and a wake forms behind it –
resulting in strong fore–aft asymmetry of probe fluctuations.
The transverse probe fluctuation field is shown in figure 5; for very weak forcing
(similar to
Pe
=0
.
01 in the figure), the region of highest probability for a strong
deflection is at
θ
=
π
/
2, with the distribution mirrored across the axis of symmetry.
The resulting probe deflection is perpendicular to its mean motion. As
Pe
is increased,
the probability of a lateral deflection is confined to the boundary layer.
The first moment of the fluctuation is numerically integrated over the surface of
contact between the probe and the bath to obtain the microdiffusivity for a range of
0
.
01
<
Pe
<
1000, as shown in figure 6. For very weak and very strong forcing, the
numerical solution matches the analytical asymptotes.
Note that two sets of asymptotes are shown for
Pe
1 in figure 6. The straight
asymptotes correspond to the high-
Pe
microdiffusivity as given by (4.10) and (4.11).
Recall that for the large-
Pe
analytical solution we found
d
, the total fluctuation
field, rather than that due to force-induced collisions only,
d
(cf. (2.13)). This is
asymptotically correct for
D
micro
as
Pe
→∞
.But
D
micro
is defined in terms of
d
and,
therefore, to be consistent, we should use
d
rather than
d
– which gives the curved
asymptote. For large values of the P
́
eclet number the two coincide.
Single-particle motion in colloids: force-induced diffusion
201
5. Solution via Brownian dynamics simulation
The dynamics of probe and bath particle motion are governed by the Langevin
equation, a force balance which includes Brownian, external, hydrodynamic and other
interparticle forces. In the present case this equation reads
0
=
F
ext
+
F
B
+
F
P
,
(5.1)
where the left-hand side is zero because inertia is not important in colloidal
dispersions, and
F
ext
=
0
for all particles except the probe. A probe of size
a
is
placed among a randomly distributed bath of particles of size
b
. The external force
is prescribed, and the other forces in (5.1) are given by
F
B
=0
F
B
(0)
F
B
(
t
)=2
kT
(6
π
ηa
i
)
I
δ
(
t
)
,
(5.2)
F
P
=
F
HS
.
(5.3)
Here, the overbar denotes a time average and
δ
(
t
) is the Dirac delta function;
a
i
≡
a
for the probe and
a
i
≡
b
for a bath particle. At each time step in the simulation the
particle positions are updated with a Brownian step and in the case of the probe, an
externally forced step. The hard-sphere displacement due to a collision between probe
and bath particle is added next; since the hard-sphere force is singular – non-zero at
contact only – special treatment is needed. To this end we use a modified ‘potential-
free’ algorithm (Heyes & Melrose 1993; Carpen & Brady 2005), in which overlaps
resulting from the external and Brownian steps are corrected along the line of centres
of the two particles, for a hard-sphere step
x
HS
. For a complete description of
Brownian dynamics of active microrheology, see Carpen & Brady (2005).
A dilute bath can be achieved in two ways: first, a single bath particle and a
single probe can be placed in the simulation cell and many, many simulations run in
order to obtain a statistically large number of interparticle collisions. Alternatively,
many ‘ideal-gas’ bath particles can be placed in the cell with one probe – i.e. only
probe–bath particle collisions occur, and the bath particles simply pass through each
other. Thus, an individual time step contains only one deterministic and one Brownian
step – for each particle in the cell – but it could contain zero, one or several hard-
sphere displacements, depending on the number of bath particles within one step of
contacting the probe. Since the bath particles do not directly see each other, they have
no size except when they encounter the probe. It is their number concentration
n
b
,
the contact length scale (
a
+
b
) and the Brownian diffusivities
D
a
and
D
b
that govern
the system dynamics. Varying the value of
φ
b
thus provides a means to compress the
time required to obtain a sufficient number of collisions for statistical analysis, and
should have no effect on probe diffusivity (although this turns out not to be precisely
the case, as we show below). To this end, volume fractions of bath particles from
0
.
1
φ
b
0
.
9 were tested.
Simulations were conducted with values of the P
́
eclet number ranging from 0.1
to 100, volume fractions
φ
b
=0
.
1
,
0
.
3
,
0
.
5
,
0
.
7and0
.
9, and
a/b
= 1. On average, a
hard-sphere collision occurs during approximately 2 % of the total number of time
steps. Hence, to obtain sufficient resolution of the data, a set of 480 simulations of
10
6
time steps each was run for each
Pe
and for each
φ
b
. The overall displacement of
the probe,
x
(
t
), was recorded at each time step.
The effective diffusivity of the probe,
D
eff
, is obtained from the time rate of change
of the mean-square displacement of the probe according to
D
eff
(
t
)=
1
2
d
d
t
x
(
t
)
x
(
t
)
,
(5.4)
202
R. N. Zia and J. F. Brady
200
180
160
140
120
100
80
60
40
20
0
〈
x
′
x
′
〉
48
44
40
36
32
28
24
20
16
12
8
4
t
Pe
= 20
Pe
= 5
Pe
= 1
Pe
= 0
Figure 7.
Longitudinal mean-square displacement of the probe as a function of time
via Brownian dynamics simulation. Volume fraction of bath particles shown is
φ
b
=0
.
1.
Displacements are made dimensionless as (
a
+
b
); time is scaled with the correlation time
τ
,
where
τ
∼
a
2
/D
a
for
Pe
1and
τ
∼
a/U
for
Pe
>
1. Each curve is an ensemble average over
480 simulations.
where
x
≡
x
(
t
)
−
x
(
t
)
and the angle brackets
denote an ensemble average over
time and over all simulations. A plot of the probe’s average mean-square displacement
versus time is shown in figure 7, where it can be seen that at long times
x
x
grows
linearly in time – confirming that the force-induced dispersion of the probe is indeed
diffusive, with a constant diffusivity.
To determine the effect of external forcing on the probe’s diffusivity, the effective
diffusivity in the absence of flow, i.e. at
Pe
≡
0, is subtracted from
D
eff
to yield the
force-induced diffusion
D
micro
:
D
micro
=
D
eff
−
D
eff
(
Pe
=0)
,
(5.5)
which corresponds to (2.14) defined in text. Results are plotted in figure 8, where
D
micro
is made dimensionless with probe self-diffusivity
D
a
and scaled with the volume
fraction of bath particles
φ
b
.
For
φ
b
=0
.
1, the Brownian dynamics data match the theoretical solution over the
full range of
Pe
, but the data for other values of
φ
b
do not collapse together as
expected. The data follow the same qualitative trend, but for
φ
b
>
0
.
1 lie beneath
the numerical solution, indicating a dependence on volume fraction – even though
the bath is modelled as an ideal gas. This surprising result can be understood by
noting that the bath particles’ motion is correlated via their interactions with the
probe. Although the bath particles do not interact directly, a probe–bath particle
collision changes the position of the probe relative to the other nearby particles,
giving rise to a correlation between the bath particles. That this correlation must
exist can be seen from the dilute pairwise expression for the equilibrium long-time
self-diffusivity of a probe equal in size to the bath particles,
D
s
∞
=(1
−
2
φ
b
)
D
a
.This
result predicts a negative diffusion coefficient for
φ
b
>
0
.
5 if only pairwise interaction