Multiple phoretic mechanisms in the self-propulsion of a Pt-insulator Janus swimmer
Yahaya Ibrahim, Ramin Golestanian, Tanniemola B. Liverpool

TL;DR
This paper provides a comprehensive theoretical analysis of how multiple electrokinetic mechanisms, including diffusiophoresis and electrophoresis, influence the self-propulsion of Pt-insulator Janus particles, highlighting the impact of coating thickness and fluid properties.
Contribution
It introduces a detailed model accounting for variable Pt coating thickness and ionic effects, revealing the combined influence of neutral and ionic phoretic mechanisms on swimmer motion.
Findings
Motion results from neutral and ionic diffusiophoretic and electrophoretic effects.
Varying ionic properties alters the interplay of propulsion mechanisms.
Coating thickness dependence significantly affects propulsion behavior.
Abstract
We present a detailed theoretical study which demonstrates that electrokinetic effects can also play a role in the motion of metallic-insulator spherical Janus particles. Essential to our analysis is the identification of the fact that the reaction rates depend on Pt- coating thickness and that the thickness of coating varies from pole to equator of the coated hemisphere. We find that their motion is due to a combination of neutral and ionic diffusiophoretic as well as electrophoretic effects whose interplay can be changed by varying the ionic properties of the fluid. This has great potential significance for optimising performance of designed synthetic swimmers.
| Description | Symbol | Value | Units (SI) |
|---|---|---|---|
| Boltzmann energy scale (at K) | J | ||
| Permittivity (water) | |||
| Electronic charge | C | ||
| Average surface charge density (at zero salt conc.) | Cm-2 | ||
| Viscosity of water (at 300K) | Nm-2s-1 | ||
| Diffusiophoretic characteristic mobility | m5 s-1 | ||
| Peroxide diffusion coefficient | |||
| Oxygen diffusion coefficient | |||
| Protons diffusion coefficient | |||
| Swimmer radius | m | ||
| H2O2 decomposition reaction rate | |||
| (Ebbens et al., 2014; Brown & Poon, 2014) | |||
| % w/v H2O2 number concentration | m-3 | ||
| Effective proton absorption/release rate () | |||
| Proton pole-to-equator rate ‘difference’ () |
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Multiple phoretic mechanisms in the self-propulsion of a Pt-insulator Janus swimmer
Yahaya Ibrahim\aff1
Ramin Golestanian\aff2
Tanniemola B. Liverpool\aff1,3
\aff1School of Mathematics, University of Bristol , University Walk, Bristol BS8 1TW, UK \aff2Rudolf Peierls Centre for Theoretical Physics, 1 Keble Road, Oxford, OX1 3NP, UK \aff3 BrisSynBio, Tyndall Avenue, Bristol, BS8 1TQ, UK
Abstract
We present a detailed theoretical study which demonstrates that electrokinetic effects can also play a role in the motion of metallic-insulator spherical Janus particles. Essential to our analysis is the identification of the fact that the reaction rates depend on Pt-coating thickness and that the thickness of coating varies from pole to equator of the coated hemisphere. We find that their motion is due to a combination of neutral and ionic diffusiophoretic as well as electrophoretic effects whose interplay can be changed by varying the ionic properties of the fluid. This has great potential significance for optimising performance of designed synthetic swimmers.
Key ideas: (1.) non-uniform reaction rates due to Pt-coating thickness variation, (2.) charged intermediates in the catalysis by the Platinum.
keywords:
propulsion, micro-/nano-fluid dynamics.
1 Introduction
In recent years there has been a flurry of activity in developing micro- and nanoscale self-propelling devices that are engineered to produce enhanced motion within a fluid environment (Kapral, 2013). They are of interest for a number of reasons, including the potential to perform transport tasks (Patra et al., 2013), and exhibit new emergent phenomena (Marchetti et al., 2013; Volpe et al., 2011; Theurkauff et al., 2012; Palacci et al., 2013; Kümmel et al., 2013; Bricard et al., 2013). A variety of subtly different methods, all based on the catalytic decomposition of dissolved fuel molecules, have been shown to produce autonomous motion, or swimming. Commonly studied systems are catalytic bimetallic rod shaped devices (Kline et al., 2005b) and metallic-insulator spherical Janus particles that are half-coated with catalyst (e.g. Platinum) for a non-equlibrium reaction (e.g. the decomposition of Hydrogen Peroxide) (Howse et al., 2007) [see Figure 1 (a)]. The propulsion mechanism is thought to be phoretic in nature (Anderson, 1989; Golestanian et al., 2007), but many specific details, such as which type of phoretic mechanism drive propulsion, remain the subject of debate (Golestanian et al., 2007; Gibbs & Zhao, 2009; Brady, 2011; Moran & Posner, 2011). A fundamental understanding of the mechanisms is key for developing the knowledge of how to use and control them in applications, and how to build up a picture of the collective behaviour through implementation of realistic interactions between catalytic colloids.
For bimetallic swimmers, a plausible proposal is that the two metallic segments, usually platinum and gold, electrochemically reduce the dissolved fuel, in a process that results in electron transfer across the rod (Paxton et al., 2005; Kagan et al., 2009). This together with proton movement in the solution (Farniya et al., 2013) and the interaction between the resulting self-generated electric field and the charge density on the rod produces (self-electrophoretic) motion (Moran & Posner, 2011). The direction of travel and swimming speed for arbitrary pairs of metals are well understood in the context of this mechanism (Wang et al., 2006), as well as the link between fuel concentration and velocity (Sabass & Seifert, 2012). For Pt-insulator Janus particles, the absence of conduction between the two hemispheres suggests a mechanism independent of electrokinetics. Hence, a natural first proposal is that a self-generated gradient of product and reactants can lead to motion via self-diffusiophoresis (Golestanian et al., 2005), provided the colloid is sufficiently small (Gibbs & Zhao, 2009). A number of predictions have been made based on this mechanism (Golestanian et al., 2005; Rückner & Kapral, 2007; Sabass & Seifert, 2010; Valadares et al., 2010; Popescu et al., 2009; Brady, 2011; Sharifi-Mood et al., 2013) which have to date shown good agreement with the experimental dependency of swimming velocity on the size of the colloid (Ebbens et al., 2012), and fuel concentration (Howse et al., 2007). It would thus appear that a key difference between the bimetallic and metallic-insulator Janus particles is that the motility in the latter system does not require conduction or electrostatic effects. However recent experiments have raised the possibility that this assumption might not be completely correct (Ebbens et al., 2014; Brown & Poon, 2014; Das et al., 2015).
Here we present a detailed theoretical study which demonstrates however that electrokinetic effects (Pagonabarraga et al., 2010) can also play a role in the motion of metallic-insulator spherical Janus particles expanding on our previous analyses briefly presented in (Ebbens et al., 2014). We find that their motion is due to a combination of neutral and ionic diffusiophoretic as well as electrophoretic effects whose interplay can be changed by varying the ionic properties of the fluid (see Fig. 8). This has great potential significance as the effect on the swimming behaviour, of solution properties such as temperature (Balasubramanian et al., 2009), contaminants (Zhao et al., 2013), pH, and salt concentration are of critical importance to potential applications (Patra et al., 2013).
We consider a Janus polystyrene (insulating) spherical colloid of radius , half coated by a Platinum (conducting) shell. It is known that such colloids are active i.e. self-propel in hydrogen peroxide solution. This is due to gradients generated by the asymmetric decomposition of on the Pt-coating and the interaction of the reactants and products with the sphere surface. In the rest of the paper we will call this process self-phoresis.
Generically the catalytic decomposition of the hydrogen peroxide by the Platinum catalyst is given by
[TABLE]
however there is still some debate about the nature of the intermediate complexes Hall et al. (1998, 1999b, 1999a); Katsounaros et al. (2012).
In this article, we outline a detailed calculation of the self-phoresis problem. Our approach is guided by the well studied problem of a phoretic motion of a colloid in an externally applied concentration gradient or electric field. To model the effect of the non-equlibrium chemical reaction sketched above on the motion of the Janus particle, we study the concentration fields of all the species involved in the reaction. The half coating of the colloid by catalyst is reflected by inhomogeneous reactive boundary conditions on its surface. The reaction involves the production of charged intermediates which can also lead to changes in the electric potential on the swimmer surface and hence the possibility of local electric fields. Our flexible calculation framework allows us to study a variety of different schemes for the reaction kinetics of the intermediate complexes. Using this we analyse in detail a scheme with both charged and uncharged pathways (see Appendix A) whose results are consistent with all the behaviour observed in the recent experiments.
2 The model
A Janus sphere of radius has the catalytic reaction of hydrogen peroxide decomposition occurring on its Pt coated half. We choose without loss of generality that the normal to the plane splitting the hemispheres is aligned with the -axis [see Figure 2]. We propose a theoretical framework based on generally accepted properties of the reaction scheme for Pt catalysis of H2O2 degradation to water and O2 (Hall et al., 1998, 1999a, 1999b). A key feature of our analysis of self-propulsion is that it takes account of the existence of charged intermediates within the catalytic reaction scheme, namely protons and that the reaction rates varies with the Pt coating thickness (see Figure 1).
The state of the system is therefore described by the local state of the Pt on the coated hemisphere, the electric potential, , the fluid velocity, , the local concentrations, of H2O2, O2 and H+ respectively, i.e. the various reactive species, and the local concentrations, , of hydroxide and salt ions, respectively. The background concentrations (far from the Janus sphere) of the salt, H2O2, H+, and OH- are respectively. Positions outside the Janus sphere (in the bulk) are represented by the vectors (in Cartesian coordinates) while positions on the surface are parametrised by the unit vectors . We note that the vector and in spherical polar coordinates. Each of the neutral species interacts non-electrostatically with the surface of the swimmer via a fixed short ranged potential energy , that depends on the distance from the Janus sphere surface. The interaction range, is taken to be the same for all neutral species.
2.1 Equations of motion
The relevant equations are Nernst-Planck equations (Probstein, 2003) for the concentration of charged species, ,
[TABLE]
drift-diffusion equations (Chandrasekhar, 1943) for the neutral species, ,
[TABLE]
Poisson’s equation (Jackson, 1975) for the electric potential
[TABLE]
and the incompressible Navier-Stokes equations (Lamb, 1932) for the fluid velocity
[TABLE]
where , is the hydrostatic pressure at , is the viscosity, Boltzmann constant and temperature, is the diffusion coefficient of ’th solute and its valency if charged. These equations together with the inhomogeneous boundary conditions (BC) on the surface of the Janus sphere and as (see next section) define a boundary value problem whose approximate solution is the subject of this paper.
We consider the system in the steady-state (time derivatives equal to zero), the dynamics of the fluid around the swimmer in the zero Reynolds number (Re) limit of the Navier-Stokes equations for incompressible fluid flow. In this paper we restrict ourselves to zero Peclét number, equivalent to assuming that diffusion of the solutes occurs much faster than their convection by the flows generated by the Janus particle - very reasonable for the experimental systems we attempt to describe. Thus, the fluid velocity given by obeys the Stokes equation, while the solute concentration fields are governed by the steady-state drift-diffusion equations.
[TABLE]
where we have defined , the local hydrodynamic stress tensor.
2.2 Boundary conditions
The hydroxide and the salt ions are not involved directly in the catalytic decomposition of the fuel (1) so we impose zero flux boundary conditions for their concentrations on the surface of the Janus particle,
[TABLE]
where the unit vector, in spherical polar coordinates. We define a catalyst coverage function, which is on the Platinum hemisphere and zero on the polystyrene hemisphere,
[TABLE]
The presence of protons as intermediates of the fuel decomposition reaction (1) and the the variation of the reaction rates across the Pt-coated hemisphere leads to non-zero flux boundary conditions for the proton concentration on the surface of the Janus sphere
[TABLE]
where the proton current, , varies with (position along the Pt-coated hemisphere). The specific form of the proton current will depend on the details of the reaction kinetics (see section 2.4 and Appendix A). However, we note that implies a chemical reaction producing protons while implies a proton sink.
The fuel decomposition reaction involves the neutral species, H2O2 and O2 giving rise to non-zero flux boundary conditions for their concentrations on the Janus-particle surface,
[TABLE]
where indicates H2O2 decomposition while indicates production of the O2. Because of the variations in thickness of the Pt-coating, both , defined in Appendix A, are functions of position along the Pt-coated hemisphere.
All the concentrations, decay to their background values, as .
We have Dirichlet boundary conditions for the electric potential on the particle surface
[TABLE]
where is a possibly varying function over the swimmer surface. The potential, will in general be pH-dependent and will also depend on the particular reaction scheme of catalytic fuel decomposition. For our analysis, it is sufficient to know the average value and in the following we take . The potential can be related to the swimmer surface charge by double-layer models (Russel et al., 1992).
The boundary conditions for the fluid velocity field are
[TABLE]
where are respectively the total linear and angular propulsion velocities of the swimmer. These are unknown and their calculation is the goal of this paper
2.3 Constraints
(Quasi-steady state condition) As we study the system in a quasi-steady state, this requires that the average proton current on the swimmer surface vanishes,
[TABLE]
and note that this also guarantees conservation of the surface charge (Moran & Posner, 2011).
(Swimming conditions) We consider a freely swimming Janus particle with no external load on the colloid which requires that there is zero total force and torque on the swimmer:
[TABLE]
where () is the differential surface (volume) element. These two conditions uniquely determine both propulsion velocities (Anderson, 1989).
The linearity of the Stokes equation and the limit of vanishing Peclét number, mean that we can divide the linear and angular velocities into non-electric, i.e. neutral diffusiophoretic, (due to the terms on the rhs of equation (7) depending on the ), and electric, i.e. ionic diffusiophoretic and electrophoretic, contributions (due to the terms on the rhs of equation (7) depending on ), which can each be calculated separately,
[TABLE]
where () are electric and () are non-electric. We expect (and indeed find) that the neutral diffusiophoretic contribution to the propulsion is much smaller than the electrophoretic contribution. While we will later briefly outline the calculation of the neutral diffusiophoretic contribution to the propulsion velocity in section 3.2, in this article we will focus on the electrophoretic and ionic diffusiophoretic contributions. Detailed calculations of the neutral diffusiophoretic contribution can be found in the literature (Anderson et al., 1982; Golestanian et al., 2005, 2007; Michelin & Lauga, 2014).
Due to the axisymmetry of the swimmer and the constraint of zero torque (19), the angular velocity vanishes identically . Therefore in the following we will only consider the swimmer velocity .
2.4 Dependence of reaction rate constants on Pt-coating thickness
The cornerstone of our analysis in this paper is the identification of the fact that the reaction rate of H2O2 decomposition depends on the Pt-coating thickness (Ebbens et al., 2014). A further observation is the well known presence of additional chemical pathways in the decomposition which involve charged intermediates, in particular protons, (Hall et al., 1998, 1999a, 1999b). These charged intermediates, in conjunction with the variation of Pt-coating thickness, allow an electric current to be established in the Pt shell due to varying decomposition rates of the hydrogen peroxide on different parts of the shell. We approximate for simplicity that this thickness variation is linear in , with a peak at the pole and the minimum at the equator,
[TABLE]
where is the reaction rate ‘costant’ for ’th reaction step in reaction (1) above and is the Legendre polynomial of order . The Legendre moments . We assume weak variation () allowing us to work perturbatively in the variation. As long as there is a competition between a neutral pathway and a pathway involving charged intermediates, conservation of charge in the steady-state requires that the varying reaction rates across the Pt-coating lead to establishment of electric currents in the Pt shell. This is described in detail for a particular reaction scheme involving protons in Appendix A, however the qualitative features of our results do not depend on the details of the scheme.
3 Analysis
Guided by current experiments, we analyse the coupled problem of the concentrations, electrostatic potential and fluid flow by considering situations in which the length-scale of the interactions (Debye screening length, for charged species and effective interaction range for the neutral species) is small compared to the size (radius ) of the swimmer. We verify a posteriori that this is indeed the case. The effective diffusiophoretic interaction range for all the neutral solutes is defined , where is the characteristic diffusiophoretic mobility of the Janus particle. Hence the problem can naturally be viewed as one with two very separate length-scales with small parameters \lambda=1/(\kappa a),{\color[rgb]{0,0,0}\definecolor[named]{pgfstrokecolor}{rgb}{0,0,0}\pgfsys@color@gray@stroke{0}\pgfsys@color@gray@fill{0}\chi=L_{\text{eff}}/a} for charged and neutral species respectively. A robust bound for comparison with experiment would be . A useful approach to multi-scale problems with a small parameter multiplying the differential operator of highest order, is the decomposition of the domain of the solution into a boundary layer, where the fields vary on the small length-scale ( for the diffusiophoretic contribution) and an outer domain where the characteristic length-scale is the size of the swimmer ’’. To do this most efficiently, we group the dimensionful quantities into useful dimensionless groups whose variation determines the behaviour of the system.
3.1 Self-electrophoresis and ionic self-diffusiophoresis
In this section, we describe detailed calculations of the electrophoretic and ionic-diffusiophoretic contributions to the swimming velocity which is the main focus of the paper.
3.1.1 Dimensionless equations
We non-dimensionalize the equations as follows. The position vector is measured in units of the swimmer size ’’, concentrations in units of the steady-state background values , electric potential in terms of the thermal voltage (with , Boltzmann constant and temperature), ionic solute fluxes, in terms of , with the diffusion coefficient of ’th solute and its valency. The fluid flow velocity is rescaled by , while the pressure is rescaled by . Hence we express dimensionless quantities (without overbar) in terms of the dimensionful (with overbar): .
It is useful for us to define the dimensionless deviations of the solute concentrations, from their bulk values. Hence we obtain the following dimensionless equations of motion:
- (1)
The steady-state equations for concentration differences of the charged species; protons , hydroxide ions , and the salt ,
[TABLE]
where . We consider only monovalent salts . 2. (2)
The dimensionless Poisson’s equation for the electric potential ,
[TABLE] 3. (3)
The dimensionless Stokes equations for the fluid velocity ,
[TABLE]
where the dimensionless parameters and are defined as
[TABLE]
the permittivity of the solvent, and is the electronic charge. is the Debye screening length and is the Bjerrum length (Russel et al., 1992). We note that the stress is the sum of the hydrodynamic stress tensor and the Maxwell stress tensor due to the interactions of the charged species with each other and the colloid surface.
The zero total force condition which determines the propulsion velocity becomes
[TABLE]
3.1.2 Dimensionless boundary conditions
For the electric potential on the swimmer surface,
[TABLE]
and decays to zero in the bulk far from the swimmer, .
For the flow field on the swimmer surface,
[TABLE]
and far in the bulk, where is the electric contribution to the propulsion velocity.
For the hydroxide and the salt concentrations, the zero flux boundary conditions due to the impermeability of the Janus particle surface,
[TABLE]
For the proton concentration, the non-zero flux boundary condition,
[TABLE]
The essential mechanism which drives this process depends on the presence of a (1) varying proton flux (as a result of variation of Pt thickness) which (2) averages to zero over the metallic hemisphere (due to charge conservation in the steady-state). In the limit of small linear variation in the thickness, this leads to a proton flux of the general form
[TABLE]
where both . We note that for a uniform thickness coating, and is the deviation of the local electric field and proton concentration from their surface average. is a measure of the scale of typical production and consumption of protons across the metallic hemisphere. Since both terms on the rhs of eqn. (33) integrated over the surface give zero, the flux, automatically satisfies the steady state requirement (17) and hence the conservation of total charge on the swimmer surface.
Systems which possess both properties above, with both , will show all the qualitative behaviours described in this article, however their values will depend on the specific details of the chemical reaction scheme. A specific reaction scheme described in detail in Appendix A gives :
[TABLE]
is the typical scale of the average proton consumption and production while is the scale of the difference between the rates at the pole and equator (see Appendix A for their derivation from reaction kinetics) .
We note that the conservation of protons also requires a relationship between the pH of the solution and the potential on the surface of the Janus particle, which depends on the reaction kinetics (see Appendix A);
[TABLE]
leading to an estimate of the average swimmer surface charge using the Gouy-Chapman model (Russel et al., 1992) of the interfacial double layer
[TABLE]
where is the Bjerrum length, with the solution permitivity.
In this electrostatic problem, the inner boundary-layer (double layer) fields, are expanded as
[TABLE]
while the outer fields, are expanded as
[TABLE]
where is the bulk-scale coordinate. Similar expansions will apply for the self-diffusiophoretic problem, with replaced by .
The essence of the matched asymptotic method involves obtaining asymptotic expansions of the solutions of the equations in the limit for both the inner and outer fields and matching the results in the intermediate region:
[TABLE]
In the next section, we will proceed to solve the outer problem in the limit of , i.e thin double-layer limit where the swimmer radius is much larger than the Debye-layer thickness . The details of the inner (Debye-layer) calculations (Prieve et al., 1984; Yariv, 2011) can be found in the Appendix B (see Figure 3).
3.1.3 Outer concentration and electric fields
In the bulk, the fields vary over length-scales comparable to the the swimmer size, with leading order fields and are expanded as
[TABLE]
We drop the (0) superscript in the following as we will consider only the leading order terms in the expansions for the fields
The leading order solute concentrations and electric potential outside the Debye-layer obey the equations
[TABLE]
where is defined in equation (27). It is useful for the rest of our analysis to treat all the ionic solutes together. Combining the two equations (41,42), we obtain,
[TABLE]
where we have defined the sum of the deviations of concentration of all of the ionic solutes and its value at .
[TABLE]
The boundary conditions for and are obtained by matching to the inner solutions (see Appendix B), giving
[TABLE]
The fluid velocity field in the outer region obeys the equation
[TABLE]
with the slip boundary condition (Prieve et al., 1984)
[TABLE]
and quiescent fluid far away from the swimmer, as . The slip boundary condition for is obtained by matching to the inner solution (see Appendix B).
3.1.4 Linear response and propulsion velocity
We note that with uniform coating, , which implies , the deviations of the electric potential and the ionic concentrations vanish (). The zeta potential for this trivial solution is
[TABLE]
In addition, this implies the fluid velocity field vanishes , and hence the contribution of self-electrophoresis to the propulsion velocity vanishes . However, a varying thickness coating and the consequent non-zero , lead to a qualitatively different scenario. To explore this we perform an expansion to linear order in of the fields for the concentrations, fluid velocity, pressure and electric potential: for , where are defined in equation (34).
We first expand the deviations of the concentrations and the electric field as
[TABLE]
with and keeping only linear terms. Substituting these perturbative fields into eqns. (43,44), we find that at leading order, {C^{*}}^{(\gamma)}\ decouples from the electric potential field {\Phi}^{(\gamma)}\ - with both obeying Laplace equations
[TABLE]
and the boundary conditions, from the matching with the inner solution, at this order are
[TABLE]
where , .
Now, the Laplace equations above for {C^{*}}^{(\gamma)}\ ,{\Phi}^{(\gamma)}\ in conjunction with the electroneutrality condition (41) imply (see Figure 4)
[TABLE]
where ’s are the Legendre polynomials. The unknown coefficients ’s are determined by the boundary conditions in equation (55) above.
Finally, the coefficients are obtained as a self-consistent system of equations,
[TABLE]
where .
Using the orthogonality of the Legendre polynomials, we obtain a linear system of equations for the coefficients ’s,
[TABLE]
or more compactly
[TABLE]
where , and the matrix and vector entries are given by
[TABLE]
The infinite linear system of equations (58) above can be solved approximately by truncating the infinite system after a finite number of components, reducing the description to the first Legendre coefficients ’s. The approximate (numerical) solution requires inversion of an matrix (see Figure 5). However, we can extract asymptotic regimes of this solution for and . Note that in both limits.
In this regime, and
[TABLE]
In this regime,
[TABLE]
where is a positive constant whose value can be determined numerically. The asymptotes show that the perturbations of and decay to zero for large (proportional to swimmer size) - when the diffusion time becomes large compared to the reaction time.
In Fig.5(a), the deviations of the proton concentration and electric potential on the surface from their bulk values are plotted showing the an excess at the equator and depletion at the pole. Increasing the number of Legendre polynomial modes () improves the accuracy of the fields on the polystyrene hemisphere. The proton depletion (excess) at the pole (equator) is stronger for larger swimmer sizes (see Fig. 5(b)).
The calculated coefficients ’s above determine the slip velocity and we can now solve the Stokes flow problem. Hence, as above, we expand the velocity and pressure fields about the trivial solution ,
[TABLE]
and the propulsion velocity about the stationary colloid,
[TABLE]
Then, the Stokes equations become
[TABLE]
with the slip boundary condition from matching to the inner solution,
[TABLE]
where . Recall that is the zeta potential for the trivial solution with .
Solving the homogeneous Stokes equations (67) with these boundary conditions gives the following structure for the flow generated by the electrophoretic and ionic diffusiophoretic contributions:
[TABLE]
expressed in terms of the leading order fundamental singularities of the Stokes equation:
[TABLE]
with the strengths given by
[TABLE]
where the are obtained from solving equations (58). Imposing the constraint of zero total force, equation (28), leads to an expression for the electrophoretic and ionic-diffusiophoretic contributions to the propulsion velocity,
[TABLE]
Written in dimensional form (see Figure 6),
[TABLE]
where is the average zeta swimmer average zeta potential. A plot of this electrophoretic contribution against the solution salt concentration (ionic strength) is shown in Fig. 6(a). As expected, this contribution is strongly sensitive to salt concentration. Interestingly, the swimmer speed is only weakly dependent on pH (see Fig. 6(c)) under weakly acidic conditions (high ). This is due to the competition between the dependence on of (decreases with ), (increases with ) and the denominator of the expression for (increases with ). This is consistent with recent experiments (Brown & Poon, 2014) which showed a minor reduction of swimming speed on addition of sodium hydroxide (NaOH). Furthermore, the propulsion speed is inversely dependent on swimmer size, for large swimmer sizes as shown in Fig. 6(b). This is consistent with the experimental observation of propulsion velocity decay for large swimmer sizes (Howse et al., 2007).
3.2 Self-diffusiophoresis
In this section, we outline a solution of the equations of motion for the neutral solutes in the outer region to calculate the neutral diffusiophoretic contribution to the propulsion velocity, . Detailed calculations for the inner interaction layer where the fields varies at the lengthscale can be found in the literature (Anderson et al., 1982; Golestanian et al., 2005, 2007; Howse et al., 2007; Michelin & Lauga, 2014).
Here since there is a finite propulsion velocity, , for the uniformly coated system, , then a weak variation of rates due to a varying thickness leads to a small correction which we can ignore. Hence we set for the rest of this section.
3.2.1 Dimensionless equations
The position vector is measured in units of the swimmer size ’’, concentrations in units of the steady-state background values (note that is measured in units of ), the short-ranged interaction potential of solutes with the Janus sphere, in terms of the thermal energy scale , neutral solute fluxes, in units of , with the diffusion coefficient of ’th solute. The fluid flow velocity is rescaled by , where is the characteristic diffusiophoretic mobility, the pressure is rescaled by . Hence, the dimensionless quantities (no overbar) are expressed in terms of dimensional ones (with overbar) as follows . As before we define the dimensionless difference of the concentrations from their bulk values as .
The dimensionless equations for in the outer region are thus Laplace equations for the concentration deviations
[TABLE]
and the Stokes equations for the fluid velocity ,
[TABLE]
where is the hydrostatic pressure at (Anderson, 1989; Golestanian et al., 2005, 2007; Howse et al., 2007; Michelin & Lauga, 2014) .
3.2.2 Dimensionless boundary conditions
Matching with the inner layer (Anderson, 1989; Golestanian et al., 2005, 2007; Howse et al., 2007; Michelin & Lauga, 2014), gives rise to non-zero flux boundary conditions for hydrogen peroxide and oxygen
[TABLE]
and vanishing concentration deviations far from the swimmer as . , the catalyst coverage function, is on the Platinum hemisphere and zero on the polystyrene hemisphere. From the reaction kinetics in Appendix A, we obtain non-zero fluxes for hydrogen peroxide and oxygen
[TABLE]
We have defined dimensionless , where is the effective rate of consumption of the hydrogen peroxide (see Appendix A for details of the derivation).
The boundary conditions for the fluid velocity are
[TABLE]
where is the neutral self-diffusiophoretic contribution to the propulsion velocity. is the self-diffusiophoretic slip velocity obtained by matching with the inner solution (Anderson et al., 1982; Anderson, 1989) and is a unit matrix. The dimensionless self-diffusiophoretic mobility is given by (Anderson, 1989).
Finally, the zero total force condition on the swimmer
[TABLE]
determines the diffusiophoretic propulsion velocity .
3.2.3 Outer concentration fields
The general solution of the Laplace equations (74,75) for the neutral solutes is of the form
[TABLE]
where are the Legendre polynomials and note that we have used the fact that . The amplitudes ’s, are determined from either of the boundary conditions;
[TABLE]
This gives rise to a system of equations :
[TABLE]
From this, using the orthogonality condition of the Legendre polynomials, we obtain the linear system of equations for the amplitudes, :
[TABLE]
where , and more explicitly
[TABLE]
where the matrix and vector entries are given by
[TABLE]
Here as in the ionic section, we solve a truncated approximation of the linear equations above, including all modes up to the ’th Legendre mode. As above, we can obtain analytic asymptotic solutions for and :
In this regime, and
[TABLE]
In this regime,
[TABLE]
where is some constant to be determined numerically. Since (swimmer size), this implies the limit corresponds to large swimmer size. For m sized swimmer in % w/v H2O2 solution, and the measured reaction rates in table (1), the estimate of the dimensionless reaction rate coefficient is . Hence, this puts the current experimental measurements (Ebbens et al., 2014; Brown & Poon, 2014) in the first regime . We note that in this regime .
The coefficients , determine the solute concentration, and hence the slip velocity which act as boundary conditions for the Stokes flow problem. Hence the velocity fields generated, expressed in terms of the fundamental singularities (see equation (70)) of Stokes flow are
[TABLE]
where the coefficients () are
[TABLE]
Imposing the condition of net zero total force, we obtain the the neutral diffusiophoretic contribution to the propulsion velocity as
[TABLE]
where since we have taken the interaction potential, identical for all species, we have identical neutral diffusiophoretic mobilities for all the neutral solute species, . From the modes calculated above, we thus obtain
[TABLE]
where is the combined effective diffusiophoretic mobility.
3.3 Comparison of ionic and neutral velocities
Finally, we can now compare the two contributions to the swimmer propulsion from ionic and neutral solutes using dimensional quantities. From equations (72,97), the relative speed
[TABLE]
where is the electrophoretic mobility and is the diffusiophoretic mobility both in dimensional form. For a fixed swimmer size, and in the limit , the above ratio takes the simple analytic expression
[TABLE]
where is the effective rate of the hydrogen peroxide consumption and is the scale of the difference between the rates at the pole and equator due to the Pt thickness variation (defined in Appendix A for a particular example of reaction model). These rates are linear functions of the concentration for low fuel concentration. In Fig. (7), it can be seen that the electrophoretic contribution vanishes at large ionic strengths, and the swimmer speed asymptotically approaches the diffusiophoretic contribution value . The self-diffusiophoretic speed (see table 1) for the chosen system parameter values in the plot (Fig. 7).
4 Summary and discussion
Therefore, the total propulsion velocity of the metallic-insulator sphere from both electrophoresis and diffusiophoresis, from equations (72 and 97), in dimensional form is
[TABLE]
where and are the electrophoretic and diffusiophoretic mobilities. The scale of the difference between the rates at the poles and equator due to the Pt thickness variation is defined in Appendix A for a particular reaction kinetic model. We point out that these results are qualitatively independent of the details of the reaction kinetics, provided the reaction involves both charged and neutral pathways for the reduction of the hydrogen peroxide and the reaction rate varies along the catalytic cap.
The ionic contribution to the expression above has a number of important simple features that are in agreement with recent experimental results on this system Howse et al. (2007); Ebbens et al. (2012); Brown & Poon (2014); Ebbens et al. (2014); Das et al. (2015): (1) it depends linearly on the fuel, at low concentrations and the dependence weakens at high concentrations, (2) it is independent of at small and behaves as for large due to fuel depletion as shown in Ref. Ebbens et al. (2012), and (3) it is a monotonically decreasing function of salt concentration, starting from a finite value when and tending to zero as becomes large. Hence at high salt concentration the swimming speed saturates to the neutral diffusiophoretic value (see Fig. 7). The electrophoretic contribution, which can be much larger than the diffusiophoretic part, vanishes if there is no variation in the rates on the surface.
Adding salt to the solution containing the swimmer would influence the propulsion in three possible ways (1) pH neutral salts that do not specifically adsorb to the surface would enhance the solution conductivity thereby reducing the effective screening length (2) while alkali or acidic salts would in general alter the total surface charge in addition to the increased solution conductivity (3) Pt catalytic decomposition of is known to strongly depend on the solution pH (Liu et al., 2014; McKee, 1969). Hence, non-pH neutral salts would also affect the Pt catalytic activity.
We note also that due to the existence of the two separate reaction loops, the overall catalytic reaction rate (measured from the current above) can be significantly reduced with only small reductions to the swimming speed; say by a significant decrease in . This type of behaviour would be expected from any reaction scheme which has this topological structure.
In conclusion, we have shown that in a system with catalytic reaction with charged intermediates, the existence of thickness-dependence in the reaction rates up to a certain limit (a few nanometres), allows us to create—by tapering the catalyst layer—spatially separated nonequilibrium cycles that could lead to large scale (many microns) ionic currents in the form of closed loops in the bulk. This remarkable effect, combining long range electrostatic interactions with nonequilibrium chemical reactions to substantially enhance surface generated flows has potential for application in many different areas of nanoscience.
5 Acknowledgments
This work was supported by EPSRC grant EP/G026440/1 (TBL, YI), and HFSP grant RGP0061/2013 (RG). YI acknowledges the support of University of Bristol. TBL acknowledges support of BrisSynBio, a BBSRC/EPSRC Advanced Synthetic Biology Research Centre (grant number BB/L01386X/1).
Appendix A Reaction kinetics
In this section, our goal is to obtain the fluxes on the surface of the swimmer, of all the chemical species involved in the H2O2 decomposition
[TABLE]
Though a complete picture of the intermediate complexes in reaction (101) remains elusive, it is known that there are neutral pathways as well as ionic electrochemical pathways (Hall et al., 2000; Katsounaros et al., 2012). However, we find that our results are qualitatively independent of many details of the reaction scheme considered as long as they involve both neutral and charged pathways. So our lack of knowledge of the microscopic chemical kinetics is not such a hindrance. To illustrate this, we consider two different reaction schemes involving a neutral as well a charged pathway. We emphasize that both schemes are provided simply as examples as the precise details of the chemical kinetics are not known.
A.1 Reaction scheme 1
First, we consider a reaction scheme for the reaction (101) made up of two pathways, one neutral
[TABLE]
and the other ionic involving charged intermediates,
[TABLE]
The reaction scheme above and the intermediate states denoted by are enumerated in Fig. (9).
The kinetics of the Pt catalyst complexation in stationary state reads
[TABLE]
where ’s are the complexation probabilities. Solving for these probabilities , we obtain
[TABLE]
where the normalization condition was used and we have defined
[TABLE]
This leads to expressions for the fluxes of
[TABLE]
and for the fluxes of hydroxide and the salt, . Measurements of the reaction rates (Ebbens et al., 2014) imply that and vary with the Pt coating thickness (of nm scale). Hence we may assume that the rate ‘constants’ ’s vary in a similar manner.
Since the thickness of the coating varies across the Pt cap, the reaction rates ’s vary over the coated hemisphere, and can be expanded in Legendre polynomials. We consider a simple linear approximation
[TABLE]
in and we assume weak variation of the rates.
The solute fluxes above in eqns. (111 - 113) require the inner (Debye-layer) proton concentration profile
[TABLE]
from eqn. (164) in Appendix B, where and are the deviations from the uniform background of proton concentration and electric fields. is the electric potential on the swimmer surface. Hence, the proton flux at the outer edge of the double-layer reads
[TABLE]
Furthermore, Taylor-expanding the flux up to linear order in , and the deviations ;
[TABLE]
where . We define
[TABLE]
Now, imposing net charge conservation, equation (17) on the swimmer surface, equation (117) for the proton flux leads to
[TABLE]
Then, substituting for ’s (from eqns. 118-120) and simplifying ;
[TABLE]
For a uniform coating (i.e for all ’s), which has the trivial solution , the zero total current condition gives rise to
[TABLE]
which is all that is required for a linear expansion about a uniform coating. Hence solving for the swimmer potential , we obtain the equation
[TABLE]
where (with measured in molar units) and
[TABLE]
Therefore, eliminating the swimmer potential and proton background concentration () by substituting eqn. (125) into eqn. (117) and keeping only linear perturbations, the proton flux assumes a simple form
[TABLE]
where we have defined
[TABLE]
is the typical scale of the average proton consumption and production and the scale of the difference between the rates at the pole and equator due to variation of coating thickness over the surface. is the deviation of the perturbative fields from their surface average; which promotes/penalise the oxidation/reduction reactions. The proton flux is linear in for low fuel concentration and the dependence weakens for high fuel concentration. It is noteworthy that with uniform coating, and the deviation fields vanish ().
The fluxes of neutral solutes from eqns. (111,112) give
[TABLE]
where the effective rate of hydrogen peroxide consumption is defined
[TABLE]
and the effective rate of proton consumption/desorption is defined in equation (129). Note that and are linear in for low fuel () concentration, and show the saturation typical of Michaelis-Menten kinetics at high fuel concentration.
A.2 Reaction scheme 2
Alternatively, we may consider a different reaction scheme, with the same neutral pathway
[TABLE]
but with a different electrochemical pathway
[TABLE]
This is the reaction scheme commonly used in modeling the electrophoretic motion of the bimetallic nanorods (Paxton et al., 2005; Dhar et al., 2006; Kline et al., 2005b, a; Sabass & Seifert, 2012). As for the reaction scheme considered in the previous section, we can write down the equations of motion for the kinetics for this scheme (see Fig. 10).
Hence, we can, as in the previous section, obtain the fluxes ’s,
[TABLE]
where here
Now, imposing the steady state constraint , and following the same procedure as in the previous section (with ), we obtain the same expression for the proton flux as equation (128)
[TABLE]
where here we have
[TABLE]
The deviation retains its previous definition as given in equation (131). Finally, we obtain the same relation and the kinetically defined potential for this scheme is .
It is noteworthy that both reaction schemes possess many similar qualitative features: the solute fluxes ’s retain the same functional dependence on the fuel concentraton and the variation in reaction rates.
Appendix B Derivation of the slip velocity
In the Debye-layer, where the fields varies on the Debye-lengthscale , we re-scale the radial coordinate by the ,
[TABLE]
and expand the deviation fields in the form
[TABLE]
where . It is noteworthy that the expansion for the pressure field begins with to balance radial electric stresses that could not be accounted by the viscous stresses at the interface (Anderson, 1989; Yariv, 2011).
B.1 Ionic solute concentrations
Exploiting the axisymmetry of the problem, we write the steady state Nernst-Planck equations (23) in spherical polar coordinates, with only radial and polar angle dependence.
[TABLE]
where
[TABLE]
We therefore expand the fluxes in the inner coordinates , noting that
[TABLE]
where we define radial and polar components of the currents (see eqns. 144 and 145)
[TABLE]
Hence, equation (148) can be written
[TABLE]
from which performing an expansion in and equating terms order by order gives the following equations at order
[TABLE]
where are arbitrary functions of . Matching the currents in the inner and outer regions,
[TABLE]
which implies for all the species. Furthermore, the next order matching
[TABLE]
providing the solution ; where are defined in Appendix A and is defined in equation (11). Therefore, the outer flux boundary conditions at leading order are,
[TABLE]
In the following we drop the (0) subscript for the outer fluxes as we are interested only in the leading order contributions (i.e we have set for ).
Next, we obtain the concentration profiles by first matching the inner fields with the outer fields ;
[TABLE]
Integrating equation (153) and using equations (157,160) and (163), we obtain the leading order concentration profile
[TABLE]
This method can be iterated to obtain the higher order concentration fields such as from equation (159) above.
B.2 Electric field
Writing out Poisson’s equation, in spherical polar coordinates,
[TABLE]
which at the leading order in the inner expansion, reduces to
[TABLE]
Substituting the concentration profiles from eqns. (164) into to the foregoing eqn. (166), we have
[TABLE]
In addition, applying electroneutrality in the outer region (see eqn. 41 in the main text) at leading order,
[TABLE]
leads to the simpler expression
[TABLE]
where we have defined
[TABLE]
Introducing a convenient factor
[TABLE]
and integrating once gives
[TABLE]
where the matching condition (since the outer electric field expansion begins at ) was applied. Thus, we obtain the electric field in the Debye-layer using the identity ,
[TABLE]
Integrating once again, we obtain
[TABLE]
Now, using the hyperbolic identities , we obtain (Anderson, 1989; Yariv, 2011)
[TABLE]
where .
B.3 Momentum conservation
Writing the Stokes equations in spherical polar coordinates,
[TABLE]
[TABLE]
To the leading order in the inner expansion (see eqns. 144-146), the static pressure balances the electrostatic stresses normal to the surface (Anderson, 1989; Yariv, 2011)
[TABLE]
Note that the expansion for the pressure field begins at to balance radial electric stresses that cannot be accounted by the viscous stresses (Anderson, 1989; Yariv, 2011). The viscous stresses balances the static pressure gradient and tangential electric stresses along the surface
[TABLE]
with the leading order incompressibility constraint
[TABLE]
Therefore, to leading in eqn. (179), the static pressure balances the radial electrostatic stresses
[TABLE]
which gives the static pressure field
[TABLE]
where matching with the outer solution implies (since the outer field expansion begins at ). The next order in eqn. (179) momentum balance is
[TABLE]
where the continuity equation (181), (i.e is independent), implies
[TABLE]
At in eqn. (180), viscous stresses balance the tangential pressure gradient and the tangential electrical stress;
[TABLE]
Using equations (183) and (169), we obtain
[TABLE]
where . Using the identity ,
[TABLE]
It is helpful to write the coefficients of the RHS first and second terms as
[TABLE]
Using eqn. (175) and integrating once, we obtain
[TABLE]
where and such that matching with the outer solution imposes . In obtaining the above expression, we have used the following integral identities
[TABLE]
Finally, integrating again,
[TABLE]
Therefore, in the thin-layer limit and ,
[TABLE]
Finally, matching with the leading order outer flow field
[TABLE]
we obtain the slip velocity boundary condition for the outer flow (Anderson et al., 1982; Yariv, 2011)
[TABLE]
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