1. Introduction
The motions of solid particles in viscous fluids at small Reynolds numbers continue to receive plentiful attention from investigators in the fields of chemical, biomedical, civil, mechanical, and environmental engineering. This creeping motion is fundamental in nature, but permits us to develop rational thoughts of various practical systems and industrial processes such as sedimentation, filtration, agglomeration, electrophoresis, microfluidics, aerosol technology, rheology of suspensions, and motions of cells in blood vessels. The theoretical investigation of this topic grew out of the classic work of Stokes [
1] on the motion of a hard (impermeable) sphere in an unbounded Newtonian fluid, and was extended to the creeping motion of a composite sphere [
2].
A soft sphere of radius
is a composite particle with a hard sphere core of radius
covered by a porous (permeable) layer of uniform thickness
. In the limiting cases of
and
, the soft sphere degenerates to a hard sphere and a porous sphere, respectively, of radius
. A biological cell with protein surface attachments [
3] and a polystyrene latex with a macromolecular surface layer [
4] are examples of a soft particle. To achieve the steric stabilization of colloid suspensions, polymers are deliberately adsorbed onto hard particles to form permeable layers [
5].
In practical cases of creeping motion, the particles are not isolated, and the ambient fluid is bounded by solid walls. Therefore, it is important to determine if the existence of adjacent boundaries affects the motion of the particles significantly. The low-Reynolds-number motions of a hard sphere confined by boundaries, such as those within a concentric or nonconcentric spherical cavity [
6,
7,
8,
9], near one or two large planes [
10,
11,
12,
13,
14,
15], and in a circular cylinder [
16,
17,
18], were analyzed extensively. Some fluid streamline plots showing the recirculation flow for the case of a spherical particle within the concentric spherical cavity were presented [
6]. Similarly, the creeping motions of a soft sphere inside a concentric spherical cavity [
19,
20,
21,
22], near one or two large planes [
4,
23] and in a circular cylinder [
24], were theoretically investigated. Although the motions of an entirely porous sphere [
25,
26,
27] within an eccentric spherical cavity were examined, the translation of a general soft particle inside a non-concentric cavity has not been studied yet.
The system of a soft sphere translating within a spherical cavity can be viewed as an idealized model for the capture of composite particles in a filter composed of connecting spherical pores. The hydrodynamic interaction between the soft particle and the cavity wall determines the deposition behavior of particles toward confining walls and the capture efficiency of filters. The objective of this article is to obtain a theoretical solution for the quasi-steady slow translation of a soft spherical particle in a non-concentric spherical cavity along their common diameter. A boundary collocation method [
7] will be used to solve the creeping flow equations applicable to this system, and the wall-corrected hydrodynamic drag exerted on the particle will be obtained in many cases. The drag results reveal some interesting features of the influence of the cavity wall on soft particle motion. Although the drag force generally increases with increasing the particle-to-cavity radius ratio, a weak minimum (even less than that for an unconfined soft particle) may occur at low ratios of core-to-particle radii and of the particle radius to permeation length. This drag force generally increases with increasing eccentricity of the particle position, but for low values of these ratios, the drag force may decrease slightly with increasing eccentricity.
2. Analysis
As shown in
Figure 1, we consider the quasi-steady flow caused by a soft spherical particle of radius
translating with a velocity
in an incompressible Newtonian fluid inside an eccentric spherical cavity of radius
along their common diameter (
axis). Here,
and
represent the circular cylindrical and spherical coordinate systems, respectively, with their origins attached to the cavity center. The soft particle has a hard core of radius
and a porous layer of thickness
. The center of the particle is situated at a distance
from the cavity center instantaneously. The purpose of this is to determine the correction for the hydrodynamic drag experienced by the particle because of the existence of the cavity.
Owing to the low Reynolds number (
), the fluid motion is governed by the Brinkman (inside the porous surface layer) and Stokes (outside the soft sphere) equations for the axisymmetric creeping flow,
where
is the spherical coordinate system based on the center of the soft particle,
is the permeation length or square root of the fluid permeability in the porous layer,
and
are stream functions of the flow in the porous layer and external flow, respectively, related to their nontrivial velocity components
and
in spherical coordinates by
the Stokes operator
and
or 2.
The boundary conditions for the fluid flow are
Here,
and
are the nontrivial stress components in the spherical coordinates
for the flow in the porous surface layer and external flow, respectively,
and
are the matching pressure profiles, and Equations (5)–(7) take a reference frame translating with the soft particle. For axisymmetric motions with the effective viscosity of the fluid in the porous layer equal to the bulk fluid viscosity [
2,
28] and satisfying Equation (6a) simultaneously, the boundary condition (6b) is equivalent to [
29]
The various boundary conditions to describe flow characteristics at the boundary between a porous medium and a free fluid have received considerable attention in the literature [
28,
30]. Although a jump in shear stress was suggested to be accounted for in Equation (6b) [
31], the present case of zero jump can be physically realistic and mathematically consistent [
2].
We can express the stream functions as [
7,
23]
where
and
are the modified Bessel functions of the first and second kinds of order
, respectively, and
is the Gegenbauer polynomial of the first kind of order
and degree
. The unknown coefficients
,
,
, and
(
or 2) will be determined using Equations (5)–(7). When constructing the solution (10), the general solutions of Equation (2) in the two spherical coordinate systems can be superimposed due to the linearity of this equation.
Application of Equation (3) to Equations (9) and (10) leads to the components of fluid velocities,
and
for the flow inside the porous layer and external flow, respectively, in circular cylindrical coordinates as
where
,
,
,
,
,
,
,
,
,
,
, and
are functions of spherical coordinates
defined by Equations (A1)–(A12) in
Appendix A. Applying boundary conditions (5)–(7) to Equations (11) and (12), we obtain
where
,
,
,
,
,
,
,
,
,
,
,
,
,
,
,
,
,
,
,
,
, and
are functions of
defined by Equations (A13)–(A34).
Equations (10), (12), (14), and (15) can be expressed in a single spherical coordinate system by using the following transformation formulas between
and
:
The subscripts 1 and 2 of the coordinates
and
in the previous equations can be interchanged through the sign conversion of
.
To exactly satisfy the conditions in Equations (13)–(15), solutions of the whole infinite unknown constants
,
,
, and
are required. But, the collocation technique [
7] enforces boundary conditions at a limited number of discrete points on the longitudinal semicircle of each of the spherical surfaces (from
to
at
,
, and
) and truncates the infinite series in Equations (9)–(12) to finite series. If the longitudinal semicircle is approximated by
discrete points satisfying the conditions in Equations (5)–(7), then the infinite series in Equations (9)–(12) are truncated after
terms, resulting in
linear algebraic equations in the truncated form of Equations (13)–(15). These equations can be solved numerically to produce the
unknowns
,
,
, and
required for the truncated Equations (9)–(12). Once these unknowns are solved for a sufficiently large number of
, the fluid velocity can be fully obtained. Details of the boundary collocation scheme are given in a previous paper on the translational motion of a hard spherical particle in a cavity [
7].
The drag force exerted by the external fluid on the soft particle (in the opposite direction of
) can be determined from [
7]
where
is the viscosity of the fluid. The previous equation indicates that only the lowest-order constant
contributes to the hydrodynamic force acting on the particle. If the soft sphere is located at the center of the spherical cavity (
),
can be obtained analytically as Equation (A35).
When the porous layer of the soft particle vanishes, it reduces to a hard particle of radius , Equations (1), (5), (6b), (8), (9), (11), (13), and (14c,d) are trivial, , , and Equations (14a,b) and (15) only are needed to be solved for the unknown constants , , , and . When the hard core disappears (), the soft sphere reduces to a porous particle of radius , Equations (5) and (13) are trivial, , and Equations (14) and (15) only are needed for the unknowns , , , , , and .
In the limiting case of
, the soft sphere is unconfined, and Equation (17) can be expressed analytically as [
2,
19]
where
For the cases of
and
, Equation (18) becomes Stokes’ law (
) for a hard sphere and the corresponding result for a porous sphere, respectively. In the limits
(impermeable in the porous surface layer of the particle) and
(completely permeable in the porous surface layer), Equation (18) again simplifies to Stokes’ law for hard spheres of radii
and
, respectively.
3. Results and Discussion
Results of the hydrodynamic drag force acting on a soft sphere translating inside an eccentric spherical cavity, obtained with good convergence by using the boundary collocation technique described in the previous section for various values of the ratios of the core-to-particle radii
, particle-to-cavity radii
, distance between the centers to radius difference of the cavity and particle
, and particle radius to porous layer permeation length
, are presented for cases of porous sphere (
) and general soft sphere in
Table 1 and
Table 2, respectively. The drag force
acting on an identical particle in the unbounded fluid given by Equation (18) is used to normalize the cavity-corrected value
. These results converge to at least the significant digits as given in the tables, and agree with the available analytical solution in the concentric limit
given in
Appendix B. Also, our results in the limit
(vanishing cavity wall curvature compared with the particle) but finite in
are in agreement with the results for a soft spherical particle translating perpendicular to a large plane wall obtained by Chen and Ye [
23]. In the limit
(or
), our results agree with those [
7] obtained for a hard sphere translating in a corresponding cavity.
as
(the cavity wall is far away from the particle) as expected, irrespective of the other parameters.
The normalized drag force
of a porous sphere (
) translating axisymmetrically within a non-concentric spherical cavity is plotted against the parameters
,
, and
in
Figure 2,
Figure 3 and
Figure 4, respectively. For fixed values of
and
, the normalized force
increases monotonically with a decrease in permeability or an increase in
from unity (with
) at
to a finite value (or infinity at the limit
where the particle seals the cavity and
) as
, as illustrated in
Table 1 and
Figure 2a,
Figure 3b, and
Figure 4a,b.
changes weakly with
and
(less than 27% for all cases with
) as
. When
and
are not close to unity, the normalized force
on a porous particle with
approaches that when
(a porous sphere of little permeability performs as a hard sphere), but when the porous sphere is near the wall, the difference in
can become significant.
For given values of
and
, as illustrated in
Table 1 and
Figure 2a,b,
Figure 3a, and
Figure 4b, the normalized force
acting on a porous sphere generally is an increasing function of the ratio of the particle-to-cavity radii
from unity at
to a finite value (or infinity if
) at
. This is because the closer the cavity wall is to the particle surface, the stronger the hydrodynamic hindrance effect of the cavity wall. Unexpectedly, when
is not near zero (the particle eccentricity within the cavity is not negligible) and
is smaller than about two (the porous sphere is relatively permeable),
may not be a monotonic function of
, and will reach a minimum either greater or less than unity at medium values of
. That is, the existence of a confinement wall can decrease the hydrodynamic force on a porous sphere, and this counter-intuitive behavior seems to be caused by the approximations in the porous particle where the volume-averaged superficial velocity of the local fluid is used, and its effective viscosity is equal to the bulk fluid viscosity [
28]. The dependence of
on
disappears at the limit
, but is strong when
is large.
For specified values of
and
, the normalized force
generally increases with the increasing eccentricity parameter
from one finite value in the concentric situation
to another value at the contact limit of the particle and cavity surfaces
, as shown in
Table 1 and
Figure 2b,
Figure 3a,b, and
Figure 4a. These results indicate that the hydrodynamic hindrance of particle motion due to the proximity of the cavity wall is enhanced on the proximal side and reduced on the distal side of the particle, with an enhanced net effect. But, when the value of
is small (say, less than about 3) or
is large (say, greater than about 0.8, as indicated in
Figure 3a),
may decrease slightly (even to less than unity) as
increases. This behavior seems to be also caused by the approximations in the porous particle where the volume-averaged superficial velocity of the local fluid is used. The variation of
with
vanishes at the limits
and
, but is obvious when the value of
is large.
Having realized the hydrodynamic effects of the non-concentric cavity on a translating porous particle, we can examine the general case of a translating soft particle. In
Figure 5,
Figure 6,
Figure 7 and
Figure 8 and
Table 2, the normalized force
on a soft spherical particle within the cavity is shown as functions of the particle-to-cavity radius ratio
, core-to-particle radius ratio
, shielding parameter
, and eccentricity parameter
, respectively. Likewise,
is a monotonically increasing function of
from a constant at
to a finite value (or infinity at the limit
) as
, generally increases with
from unity at
to a finite value (or infinity in the limit
) at
, and generally rises with increasing
from one finite value in the concentric situation
to another at the contact limit
, keeping the other parameters unchanged. When the value of
is small,
is not near zero, and
is smaller than about two,
may first decrease as
increases from unity at
, reach a minimum with
, and then rise with the further increase in
up to a value larger than unity at
, as shown in
Figure 6 and
Table 2. In addition, when the values of
and
are small (such as less than 3 and 0.5, respectively),
may decrease slightly (even to less than unity) as
increases, as illustrated in
Table 2 and
Figure 5,
Figure 7, and
Figure 8.
For fixed values of
,
and
,
Figure 5,
Figure 6,
Figure 7 and
Figure 8 and
Table 2 show that the normalized force
on a translating soft sphere within a spherical cavity monotonically increases with a rise in the ratio of core-to-particle radii
, in which the cases of
and
denote the porous particle (the hard core disappears) and solid particle (the porous surface layer vanishes), respectively. That is, for given values of the particle radius, permeability of the porous layer, and separation from the wall (
,
, and
), the force acting on the particle becomes less if the porous surface layer is thicker (
is smaller). All force results of the soft particle fall between the upper and lower bounds of
and
, respectively. When the porous layer of the soft particle has small to moderate permeability (say.
),
on the soft particle with
being less than about 0.8 within a spherical cavity can be well approximated by the normalized force on a porous particle having identical permeability, radius, and eccentricity inside an identical cavity, as illustrated in
Figure 5b and
Figure 8. Here, the hard core of the soft sphere barely feels the relative motion of the fluid and exerts only negligible hindrance. But, this approximation does not apply to surface layers with high permeability.