Surface Pressure of Charged Colloids at the Air/Water Interface
Charged colloidal monolayers at the interface between water and air (or oil) are used in a large number of chemical, physical and biological applications. Although a considerable experimental and theoretical effort has been devoted in the past few decades to investigate such monolayers, some of their fundamental properties are not yet fully understood. In this paper, we model charged colloidal monolayers as a continuum layer of finite thickness, with separate charge distribution on the water and air sides. The electrostatic surface free-energy and surface pressure are calculated via the charging method and within the Debye-Hückel approximation. We obtain the dependence of surface pressure on several system parameters: the monolayer thickness, its distinct dielectric permittivity, and the ionic strength of the aqueous subphase. The surface pressure scaling with the area, , is found to be between in the close-packing limit, and in the loose-packing limit. In general, it is found that the surface-pressure is strongly influenced by charges on the air-side of the colloids. However, when the larger charge resides on the water-side, a more subtle dependence on salt concentration emerges. This corrects a common assumption that the charges on the water-side can always be neglected due to screening. Finally, using a single fit parameter, our theory is found to fit well the experimental data for strong to intermediate strength electrolytes.
Molecular monolayers at the water/air or water/oil interfaces have been investigated intensively for more than a century, starting with the pioneering works of Langmuir and Blodgett Langmuir1918 (); Blodgett1935 (); Vogel2012 (); Gaines (); Adamson (); Fundamentals (); Binks2006 (). Not only do they provide an important manifestation of thermodynamics of two-dimensional (2D) systems, but they equally offer several interesting applications in nano-lithography, micro-patterning and optical coatings Vogel2012 (); Szekeres2002 (); Krogman2005 ().
Related systems are monolayers of colloidal particles deposited at fluid/fluid interfaces. Much interest of the latter systems followed the seminal work of Pieranski Pieranski1980 (), who found that sub-micron polystyrene spheres are trapped at the air/water interface and self-assemble into a 2D triangular lattice due to electrostatic repulsive interactions. More recently, a wide range of studies, including crystallization and aggregation of colloidal particles, have been performed on such colloidal monolayers Onoda1985 (); Hurd1985A (); Garcia1997 ().
Another key property of colloidal monolayers is their surface pressure/area isotherm. Such quantitative knowledge allows a direct control of particle spreading and self-assembling at the interface. The surface pressure can be used to fine tune the inter-particle spacing when the monolayer is deposited from an aqueous solution Mbamala2003 (). Furthermore, from measurements of inter-particle forces and the monolayer surface pressure, one can infer the magnitude of the effective colloidal charge Aveyard2000 (); Petkov2014 (); Petkov2016 (); Bossa2016 (), as this quantity is otherwise hard to measure.
Several approaches have been suggested for calculating the surface pressure Levental2008 (); Andelman1970 (); Hachisu1970 (). Levental et al. Levental2008 () modeled a charged monolayer as a surface with continuous and uniform charge density, and calculated the electrostatic contribution to the surface pressure, denoted hereafter as . Using the nonlinear Poisson-Boltzmann (PB) theory yields a nonlinear expression for , expressed in terms of hyperbolic functions. This result, when treated within the linearized PB theory (the Debye-Hückel theory – DH, valid for strong electrolytes) yields a surface pressure that scales with , the monolayer area, as . In the opposite limit of weak electrolytes, however, the scaling is found to be Levental2008 (). Since the model is only valid for a uniform surface charge density, it is restricted to the close-packing limit of the colloids, where the monolayer surface charge can be considered as approximately uniform.
In the other limit of large inter-particle separation, Aveyard et al. Aveyard2000 () studied the surface pressure of a charged monolayer at the water/oil interface, and calculated using a superposition of inter-particle forces. These forces can be explained as a consequence of trapped charges residing at the particle/oil surface (in contact with the oil phase), away from the oil/water interface. The charges induce opposite image charges inside the aqueous phase, as a way to satisfy the dielectric discontinuous jump at the water/oil interface. The monolayer in the dilute limit can be treated as a dipolar layer and yields a surface pressure that scales as . We note that the same scaling law was found to be in agreement with their own experimental results Aveyard2000 ().
The model by Aveyard et al. Aveyard2000 () mentioned above does not take into account the bulk concentration of ions in the aqueous sub-phase, and is a reasonable approximation only in the high-ionic strength (hence screened) limit. Moreover, as the model does not consider explicitly the distinct value of the dielectric constant of the colloidal monolayer, the dependence of on the Debye screening length and monolayer dielectric constant have not been calculated.
Recently, Petkov et al. Petkov2014 (); Petkov2016 () measured the monolayer surface pressure, , for charged silica particles deposited at the air/water interface. They calculated derived from the Maxwell stress tensor, employing the so-called Bakker formula Bakker (). The electrostatic field is assumed to vanish in the aqueous phase and was calculated in the air phase by postulating some specific ionic profiles at the surface. The surface charge density of each colloid and its accompanying screening was evaluated within a cell model, which is superimposed on a 2D square lattice. In the large inter-particle separation limit, it was found that the surface pressure scales as .
This scaling was shown to be in good agreement with experimental data Petkov2014 (); Petkov2016 (); Vermant2006 () measured either in the absence of salt or for weak electrolytes, but contradicts the scaling law found earlier in Ref. Aveyard2000 (). Albeit the agreement between the model and experiment, the model was not derived in a self-consistent fashion. In particular, the use of the Bakker formula cannot be justified, because it relies on the homogeneity of the surface charge distribution, and the ionic profiles were postulated a priori to have a preset form. Furthermore, the ansatz used to express the screening resembles the form of a typical solution in the DH (strong electrolytes) theory, although the considered experimental regime (weak electrolytes) is clearly beyond the scope of this approximation.
Motivated by these different models, which yield distinct scaling forms (, where Levental2008 (), Aveyard2000 () or Petkov2014 ()), we present in this paper a different, more fundamental and self-consistent approach. The thermodynamic definition of the surface pressure is employed without the need to have any further assumptions other than using the linearized DH theory. Our calculation shows that for small inter-particle separation, the collective monolayer surface charge behaves as a continuum density, and the surface pressure scales as , in agreement with Ref. Levental2008 (). For large separation, the colloids show a dipole-like behavior, and the scaling becomes , recovering the results of Ref. Aveyard2000 (). Our model, therefore, agrees with the two limiting scenarios of colloidal packing of previous works Aveyard2000 (); Levental2008 (), and a smooth crossover between them. The theory derived herein also agrees well with available experimental data Aveyard2000 (); Vermant2006 () within the DH regime.
The present study addresses a generalized setup, where the colloidal monolayer has a finite thickness and an arbitrary value of the effective dielectric constant. We allow the colloidal charge distribution to be different on the water-side versus the air-side of the monolayer. The surface pressure is found to depend differently on the monolayer permittivity in the two limits of inter-particle separation. Furthermore, the dependence on the salt concentration can become non-monotonic for specific values of the charge density at the water-side. This finding is in contrast with the commonly employed assumption that the pressure depends solely on the charge located on the air-side of the colloids, for which the dielectric constant is much smaller, and when there is no screening.
The paper is organized as follows. In Section II, we derive a general formalism for calculating the surface pressure of arbitrarily charged surfaces within the DH theory. In Section III, we present the setup for the colloidal monolayer with a finite thickness and different charge distributions. The surface pressure is computed in Section IV, for a specific colloid charge distribution, and in Section V, we compare our findings to available experimental results. In Section VI, we discuss the surface pressure in the dilute and close-packing inter-particle separation limits, as well as its dependency on the ionic strength and monolayer dielectric constant. Finally, our conclusions are presented in Section VII.
Ii Monolayer Surface Pressure
We present a general framework for calculating the surface pressure of an arbitrarily charged interface coupled to a bulk ionic solution. The definition of the surface tension, , is
where is the free energy of the system (comprising of an interface coupled with a bulk), and is the overall surface area.
The surface pressure is related to the change in surface tension. For a charged monolayer, we can compare the surface tension with and without the charges
where and denote the surface tension in the absence and presence of surface charges, respectively. The electrostatic contribution to the surface pressure, , is expressed in terms of , the change in electrostatic surface free-energy,
The surface free-energy, , is defined as the amount of work (per unit area) needed to construct the surface. We introduce now the spatially averaged surface free-energy
and write the surface pressure as
It is important to consider how the surface area is controlled in experiments. For monolayers comprising of a uniform surface density, two fundamentally different situations can occur, and they are known as the Gibbs monolayer and the Langmuir monolayer Fundamentals (). For Gibbs monolayers, the particles are soluble in the aqueous sub-phase. The monolayer is an open system exchanging particles with the bulk, such that the chemical potential remains fixed. For a charged monolayer, it means that when the monolayer expands or contracts, its surface charge density remains constant, because the underlying physical properties that determine the surface coverage, such as the adsorption energy per unit area, approximately remain fixed Markovich2014 (); Markovich2015 (). As a result, is independent of the surface area and, , by virtue of Eq. (5).
On the other hand, for Langmuir monolayers, the particles at the surface are completely insoluble in the water sub-phase, and the monolayer is a closed system with a fixed number of particles. The total charge, , remains fixed, meaning that even when the monolayer undergoes expansion or compression. For a uniformly charged surface and within the linear DH theory, the surface free-energy satisfies , and from Eq. (5), .
Although these two simple cases may seem similar at first glance, the Gibbs and Langmuir monolayers yield an opposite relation between and , as shown above. Clearly, these two extreme cases of uniform surface charge density are an over-simplification, and for non-uniform surface charge densities, the relation between and becomes more intricate.
In the present study, we only consider the case of insoluble Langmuir monolayers, where the total charge (and particle number) of the monolayer is constant but the charge density (per unit area) can vary. Our approach is general and enables us to calculate for any configuration of surface charges. The charged surface is coupled to an electrolyte solution, and is calculated using the Poisson-Boltzmann (PB) theory Andelman1995 (); Markovich2017 (). The water and air phases are treated as two continuum media with dielectric constants, and , respectively. The mobile ions in the aqueous solution are taken to be point-like, yielding the well-known PB equation for a monovalent 1:1 electrolyte
where is the electrostatic potential, the elementary charge, the vacuum permittivity, the relative permittivity of water, the bulk concentration of the electrolyte and the thermal energy.
For a surface with surface charge separating an aqueous solution from the air (or oil), the electrostatic boundary condition is
where denotes the unit vector normal to the surface. The superscripts denote the external () and internal () regions with respect to the surface, and the direction of is chosen to point from inside toward the outside.
Equations (4) through (8) are sufficient to obtain the surface pressure in the most general case
for cases when . In the above equation, the inverse Debye screening length is , and the Bjeruum length is about nm in water () at room temperature.
This formula can be generalized for two charged surfaces, , each with surface potential, , and surface charge, ,
Eq. (11) is obtained by the linearization of the expression presented in Ref. BenYaakov2013 (), in the context of two interacting charged surfaces. In the following section, the above equation will be used to calculate the free energy for Langmuir monolayers that are modeled as two charged interfaces separated by a dielectric layer.
Iii Modeling of the Colloidal Monolayer
The charged colloidal monolayer is schematically depicted in Fig. 1. It is located at the interface between a dielectric medium of dielectric constant (non-aqueous medium such as air or oil) on its top side, and a monovalent 1:1 electrolyte solution, of dielectric constant , on its bottom side. The monolayer itself is treated as a continuum medium with finite thickness, , and a dielectric constant, . Each colloidal charge is modeled as a patch of surface charge, located at the air-side and water-side of the particle, with different values assigned to each side.
In order to calculate the surface pressure, we need to evaluate first the electrostatic potential. The potential in the air phase, , as well as inside the colloidal monolayer region, , satisfies the Laplace equation,
while the potential in the aqueous phase, , satisfies the DH equation, Eq. (9)
and depends on the solution ionic strength via the Debye screening length, .
As mentioned above, the charges on the colloidal monolayer are modelled by two parallel and charged layers. The first located on the air-side (), and the second on the water-side (). The monolayer itself is constructed by repeating the surface charge patches (each representing an individual colloid) on a 2D periodic square lattice with lattice parameter , as is seen in Fig. 1. Note that the patches can have an arbitrary shape and charge distribution with typical length scale, . For an arrangement on a square lattice, the surface charge densities on the monolayer air-side and water-side, and , are periodic functions in and .
The boundary conditions at the and planes are obtained from Eq. (7),
and at infinity we demand that the electrostatic field vanishes, i.e., . The two periodic charge densities, and , can be expressed by their 2D Fourier series
where is the 2D in-plane vector. For a square lattice, the integer numbers parameterize the discrete -vector of the reciprocal space with , and , , is the -component of the Fourier transform of a single colloid charge distribution (i.e., within the unit cell).
The surface potentials evaluated at the top and bottom surfaces, and , can also be written in terms of their Fourier components:
with , while denotes the Fourier coefficients of .
A linear relation between the surface potential and surface charge density will emerge from the boundary conditions as our model is linear. Similar to the notation used in Eq. (11) and in Appendix A, the generalized linear response is written in Fourier space as,
where in a compact notation, and are vectors, and is a matrix. The diagonal components of the matrix are the differential capacities (per unit area) of the ‘a’ and ‘w’ surfaces, while the off-diagonal ones represent cross-capacitive terms between the two surfaces.
Next, as the colloid arrangement is periodic, the spatial average over the surface free energy [Eq. (4)] can be taken over a single lattice cell of area . Hereafter, we shall omit the bracket notation from for the sake of simplicity, but the free energy is always averaged over one unit cell. Using the Parseval theorem, this quantity is equal to a summation over the reciprocal lattice vector , given by
Adopting the notation of Refs. Petkov2014 (); Petkov2016 (), we introduce a dimensionless parameter, , which is the ratio between the particle diameter, , and the inter-particle separation, . The limit denotes the dilute monolayer density (), while corresponds to the close-packing limit (). Using and the dimensionless , the above summation is written as
where the function is defined as
depends on the Kronecker delta function, , where we made use of the square lattice symmetry of our setup.
Equation (21) is the general expression for the surface pressure for our model. Furthermore, the framework provided above can be generalized for any model within the DH approximation. In the following section, we will use this result for a specific choice of the charge distribution.
In order to calculate of Eq. (21), one has to evaluate the derivative of from Eq. (20). The function depends on the details of the surface charge distribution of a single colloid, , as well as on the boundary conditions. We proceed by assuming that is a radial symmetric function and has a separate Gaussian form on the ‘a’ and ‘w’ sides of the monolayer
where , and or is the charge on the ‘a’ or ‘w’ sides, respectively. This, in turn, leads to a Fourier transform of , which also has a Gaussian form,
The explicit solution for the electrostatic potential profile in the three spatial regions (‘a’, ‘c’ and ‘w’) and the capacitance matrix are given in Appendix A. Based on these solutions, the function is written as
We will use and in order to evaluate the surface pressure analytically in the close-packing () and dilute () limits.
iv.1 Close-packing colloid limit,
In the close-packing limit, can be derived analytically by investigating and its derivative in the limit. The dominant contribution to Eq. (24) originates from the first term, since a simple substitution of in Eq. (24) implies that the contributions from the two remaining series are exponentially small, approximately of order , and can be safely neglected. Then, from Eqs. (24) and (25) one can derive
where we substituted in Eq. (28). Therefore, in the close-packing limit, the surface pressure scales as , and is consistent with the continuum limit of the monolayer surface charge. As the colloids approach each other, their double-layers overlap and resemble the response to a uniform surface charge density at the air/water interface.
iv.2 Dilute colloid limit, : an effective dipolar monolayer
For the dilute limit, , we remark that has the form of a Riemann sum Abramowitz (). Using the Euler-Maclaurin formula (see Appendix B), we expand to leading orders
The surface pressure in Eq. (30) scales as for . This dilute-limit result and stems from effective dipole-dipole interactions between the colloids, primarily mediated by the air phase. Indeed, by substituting and after some rearrangements, we find
where the effective dipole moment is written as the sum of two terms,
In Appendix C, we calculate in the dilute limit directly from the dipole-dipole interaction energy. This calculation suggests that the dilute limit, as in Eqs. (31)-(32), is independent of the specific functional form of the surface charge density. One might indeed expect this behavior as the inter-particle distance satisfies , and the details of the colloidal charge distribution are washed out.
where is the surface pressure for a vanishing screening length. From Eq. (33), we deduce that for , is a monotonic function of the Debye screening length, and converges to , for very high electrolyte concentrations.
However, if the ratio becomes negative, might even vanish for certain values of , as can be seen in Fig. 2 for a specific choice of . Moreover, is non-monotonic with respect to the salt concentration. This presents a compelling evidence that surface charges on both sides of the colloid particle can play a role in determining the magnitude of . We shall further discuss this observation below.
We conclude this subsection by noting that there are two separate cases for the effective dipole moment, Eq. (32): (i) for strong electrolytes, where , is approximated as,
Here mainly depends on , since the air-exposed charge induces an image charge in the aqueous phase, with a charge separation distance of . (ii) For weak electrolytes, namely, , is well approximated by the second term, ,
The relevant charge determining the dipole moment is the net charge on both sides of the particle, as a result of the electro-neutrality due to screening. The charge separation is then proportional to the screening length.
iv.3 The general case
The surface pressure, , of Eq. (21), can be calculated numerically for any intermediate value of . We limit ourselves to the more common case of strong electrolytes, , with , and . We have chosen on the water side, without loss of generality, because it merely sets the strong electrolyte regime to .
The function is calculated by summing one hundred terms of the two series in Eq. (20), where their explicit form is given in Appendix A. Choosing a Gaussian form for , the colloid charge distribution of Eq. (22) yields a better convergence of the series for small values of , as compared with for a uniform charge distribution on each colloid. The space-averaged surface free-energy, , can be calculated via Eq. (19), and the function is evaluated via Eq. (21), by taking numerically the first derivative of .
The quantities and , rescaled by their maximal values at ( and , respectively), are shown in Fig. 3 on a log-log plot. Clearly, both coincide in the close-packing limit (), where the continuum limit holds, i.e., . However, in the dilute regime (), the surface free-energy and surface pressure differ considerably as and .
A plot of , rescaled by its maximal value, is given in Fig. 4 for different values of the monolayer dielectric constant, and . The variation of the rescaled surface pressure with is quite substantial only in the dilute-packing limit, where it varies as , as is implied by Eq. (30). We note that (the rescaling prefactor) is the close-packing value of , , and is by itself proportional to , [see Eq. (28)].
V Comparison to experiments
It would be of value to compare our theoretical predictions to previous experiments. In Refs. Aveyard2000 () and Vermant2006 (), the surface pressure of charged polystyrene latex particles is measured at octane/water and decane/water interfaces, respectively. The fit to these experimental data shown in Fig. 5 employs the full expression as prescribed in Eqs. (21), (24) and (40)-(41), and uses a single fit parameter, which is the air-exposed surface charge of a single colloid, .
In general, there are two fit parameters, and . However, we observe that the experiments considered here Aveyard2000 (); Vermant2006 () used intermediate to high salt concentrations. Thus, nm is much smaller than the colloid particle size , and for the two bounding media. It is then justified to neglect in this case, since the contribution from the water charges becomes much smaller (see Section VI for more details). We also find that employing as a second fit parameter makes no substantial difference in this case. Nevertheless, there might exist physical scenarios where the assumption is inaccurate (as is discussed below).
Figure 5 presents the fit with the data of Ref. Aveyard2000 (). The data corresponds to an experimental setup with a mM NaCl solution, and particles of diameter m. The resulting air-exposed surface charge is obtained as a fit parameter, , which is a reasonable surface charge density. We set the layer thickness to be equal to the particle diameter , thus, ignoring effects of colloid immersion in the aqueous phase due to wetting. The dielectric permittivities were taken to be , and for the water, polystyrene latex beads and oil (decane or octane) phases, respectively. This represents a good fit in the intermediate ionic strength regime.
In a similar fashion, Fig. 5 shows multiple fits to the data of Ref. Vermant2006 (). The surface pressure was measured for different aging times, by varying the exposure time of the monolayer in contact with mM NaCl solution, between 2, 19 and 115 hours. As was mentioned in Ref. Vermant2006 (), the number of dissociated groups on the colloid surface, corresponding to the surface charge, diminishes with time. Hence, Fig. 5 shows a decrease of the surface pressure with aging time.
Figure 6 shows measurements done in the strong electrolyte case and mainly in the close packing regime Vermant2006 (). The prediction of the close-packing power law, , follows quite well the data points. On the contrary, Fig. 6 shows that in the absence of salt, the measurements done in Ref. Vermant2006 () and by Petkov et al Petkov2014 () exhibit a different scaling, . This result is beyond the scope of the present theory that employs the DH approximation.
Scaling laws derived from the analytical results for the surface free-energy and surface pressure are obtained in two limits (see Fig. 3): (i) the dilute limit (), Eq. (31); and, (ii) the close-packing limit (), Eq. (28).
In the dilute limit, we have found that the surface pressure can be described in terms of dipole-dipole interactions, where the effective dipole moment , Eqs. (34)-(35), arises from ionic screening in the aqueous phase. The charge separation corresponding to this dipole moment, , is given in terms of the colloid thickness , for [Eq. (34)] in the strong electrolyte limit, or in terms of the Debye screening length for [Eq. (35)], in the weak limit. The sum of these two contributions, , constitutes the effective dipole moment of each colloid. This description is valid for intermediate cases, and demonstrates an explicit dependence on the monolayer dielectric permittivity and the subphase ionic strength. We note that previous works Aveyard2000 (); Oettel2008 (); Hurd1985 () derived less general results for the dilute limit, with either Aveyard2000 () or (and only for ) Oettel2008 ().
The colloidal monolayer permittivity strongly affects the surface pressure through the magnitude of , Eq. (34). The rescaled surface pressure of Fig. 4 scales as in the dilute-packing limit, implying that [see Eq. (28)]. However, in the close-packing limit, the rescaled surface pressure is independent of ; hence, . The latter observation stems from the difference between the two regimes: dipole-dipole interactions vs. a uniform electric double layer.
Several comments can be made on the salt effects. First, for strong electrolytes, the surface pressure is nearly independent of ionic strength. This result is consistent with experimental findings of a weak dependence of the inter-particle force and surface pressure on salt concentration Aveyard2000 (); Aveyard2002 (). An exception occurs when and have opposite signs. For example, in Fig. 2, we plot the dependence of on and show that it is non-monotonic and even vanishes for a specific salt concentration.
The dependence on salt is quite different for weak electrolytes. A clear divergence of the surface pressure is observed for very weak ionic strength. We remark that Eq. (33) might become inaccurate in this limit, since the validity of the DH approximation breaks down for high surface charges and weak electrolytes. In this case, it may be more appropriate to consider methods other than the DH approximation Oettel2008 (); Frydel2007 (); Park2008 ().
We would like to pay special attention to the charge on the water-side, . Although it was conveniently set to zero in Fig. 5, nevertheless we find that can, in certain cases, affect the surface pressure. Since the energetic cost of charging a surface in contact with a low dielectric material is high, it is commonly believed Petkov2014 (); Bossa2016 (); Oettel2008 () that ions from the water phase prefer to diffuse to the air-side of the layer. These ions neutralize some of the air-side charges reducing their net charge. As a result, the water-facing charge can become much higher than .
In contrast to previous theoretical derivations Aveyard2000 (); Aveyard2002 (); Petkov2014 (); Bossa2016 (); Uppapalli2014 (), which a priori neglected , we can compare the contributions to the surface pressure from charges located at the top and bottom sides of the monolayer. For example, in the dilute limit (), we calculate separately the surface pressure that results from charges residing only on the colloid/air interface ( for ), and for the opposite case, when they reside only on the colloid/water interface ( for ). The ratio between the two is given by,
Clearly, the contribution of the water-side charges cannot be neglected when the surface charge residing on the air-side is much smaller than the one on the water-side. The corresponding ratio is estimated to be quite large. For example, this ratio can be for a mM ionic aqueous solution at room temperature and for silica particles of diameter m. This scenario might be achieved in some setups. Using the same logic, a similar conclusion may also be drawn for the close-packing limit.
In this work we study the surface pressure of a monolayer composed of charged colloids at the air/water interface, within the linear PB theory (DH theory). The colloidal monolayer is treated as a continuum dielectric, with dielectric constant and finite thickness , separating two phases: an electrolyte solution and air (or oil), with . Charges of the colloidal particles facing the water-side and air-side are modeled as surface charge patches superimposed on a 2D square lattice. As was previously suggested for similar setups Hachisu1970 (); Andelman1970 (), the presence of charged particles at the air/water interface results in an excess of surface free-energy, and the surface pressure can be calculated directly from the latter [see Eq. (11)].
Although the exact solution of the surface pressure requires a numerical summation of many terms in Eq. (24) (see Fig. 3), the scaling forms are obtained analytically, yielding for the close-packing limit (), and for the dilute limit (), . The former is consistent with the uniform surface charge density Levental2008 (); Hachisu1970 (); Davies1951 (), while the latter can be viewed as originating from dipolar interactions between discrete dipoles Aveyard2000 (); Oettel2008 () (see also Appendix C).
The effective dipole moment, , of the charged colloids is calculated analytically, and is found to depend on the ionic strength (Fig. 2), the dielectric properties of the colloidal particles (Fig. 4), and the amount of charges residing on the water-side () and air-side () of the colloid. We detail physical conditions for which the contribution of the water-side charges to the surface pressure is not small, in contrast to the common belief. In addition, the dependence on salt concentration is explored. For close-packing and dilute colloid limits, the monolayer permittivity () is shown to affect the surface pressure in different ways.
Our model agrees well with available experimental data (Fig. 5), and explains the physical behavior for strong electrolytes ( in the close-packing limit). However, some experimental results Petkov2014 (); Petkov2016 (); Vermant2006 () exhibiting longer-ranged interactions () for weak electrolytes are yet poorly understood. In addition, a previous work Levental2008 () hints that the proper scaling in the no-salt regime for uniform surface charge can become as weak as . We hope that our study, restricted to the DH regime, will stimulate even further theoretical and experimental investigations, which will hopefully shed light on the abnormal surface pressure scaling of charged colloidal monolayers in the no-salt regime.
Acknowledgements. This work is supported in part by the ISF-NSFC joint research program under Grant No. 885/15. TM acknowledges support from the Blavatnik postdoctoral fellowship programme, and DA is grateful for a Humboldt award.
Appendix A Derivation of the Electrostatic Potential
We present the explicit calculation of the electrostatic potential in the various spatial regions for our model as depicted in Fig. 1. Using the same notations introduced earlier, is the spatial mode of , with the wavevector where . For clarity sake, we omit the subscripts from the and refer to the Fourier mode simply as . Denoting the potential in the top air phase, middle colloidal monolayer and bottom water phase as , and , respectively, the potential in the three spatial regions is obtained from Eqs. (12)-(16):
with . It is easy to see that the potential given in Eq. (A) is continuous at the and boundaries, where it is equal to and , respectively.
Appendix B Calculation of for
The function can be evaluated in the limit of small , given that it is expressed as
Here, is a general well-behaved function of two variables. If , both the single and double sums have the form of a Riemann sum. To zero-th order in , they are equal to the one- and two- dimensional improper integrals over and , respectively.
However, in order to evaluate the derivative, , the zero-th order in of these sums is not sufficient, and we use of the Euler-Maclaurin formula Abramowitz (),
where are the Bernoulli numbers, with the first five given by
If for all , Eq. (43) implies that the expansion of in powers of is
For the double sum, the generalization of the Euler-Maclaurin formula is given by
If has a radial symmetry, it can be written as where , coinciding with the expression of in Eq. (40), where . We can then calculate the double integral in polar coordinates (), while recalling that and all of its -derivatives should vanish at infinity. These assumptions lead to the following expansion for the double sum,
Appendix C Surface pressure and dipole interactions for
We present another way to obtain Eqs. (31)-(32). We start by considering the interaction energy between two parallel point-like dipoles of magnitude at a large separation that is perpendicular to the dipole direction. The dipoles are placed in the upper half-space having permittivity . Assuming that there is no contribution from the lower half-space (with permittivity ), the dipole-dipole interaction energy is Oettel2008 ()
and is equal to one half of the familiar expression for interacting parallel dipoles. Summing over all pairs of parallel dipoles placed on a 2D lattice embedded in 3D space, the lattice cohesive energy, , is given by
where is an in-plane lattice vector, the number of particles (and lattice sites), and the total surface area. Similar to the derivation of Eq. (8), we neglect the entropy of the large colloidal particles. Moreover, the entropy of the mobile electrolyte ions approaches the bulk-solution value, which is independent of the area, yielding
In Eq. (49), we performed a summation over all lattice sites,
The surface pressure is then recovered by taking ,
Comparing Eq. (50) with Eq. (31), we find the value as calculated above is of the in Eq. (31). Hence, in the dilute limit, Eq. (32) can be regarded as the effective dipole moment of the colloidal particle.
- Although the above charging method takes into account the entropy of the mobile ions in the solution, it does not include the entropy of the surface charges. In our model, those charges originate from the charge distribution on large colloidal particles, forming a monolayer at the air/water interface. However, since the colloids are considered as macro-particles, this entropy contribution can be ignored.
- Given that the three isotherms approach the same nonzero constant, it seems that there may be a systematic offset in the measurements. We compensate for this offset by introducing in our fit an additive constant to the surface pressure. We first fit the two-hour aging time isotherm and obtain a value of for the additive offset. Then, we use this value for the two remaining isotherms.
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