Marcel Kröger*,
Kaarlo Nieminen,
Han Tao and
Eero Kontturi
*
Department of Bioproducts and Biosystems, Aalto University, FI-00076 Aalto, Finland. E-mail: marcel.kroger@aalto.fi; eero.kontturi@aalto.fi; Tel: +358 453227721 Tel: +358 503442978
First published on 14th July 2025
The surface charge of nanoparticles is usually quantified under the assumption that strong electrolytes fully dissociate in aqueous systems. Here, we demonstrate the effect of counterion condensation on charge through meticulous corrections to the individual dissociation constants. By considering the electrostatic potential energy of charged moieties on the particle surface and by applying Poisson–Boltzmann statistics to assess the electrostatic double layer surrounding the particles, we were able to simulate experimental potentiometric and conductometric titration curves for both solutions and colloidal systems with decent correlation. As such, we can predict that due to counterion condensation, our chosen rod-like particles (phosphorylated cellulose nanocrystals) never carry more than 0.5 mmol g−1 charge, amounting to a mere fraction of the theoretical maximum of 2 mmol g−1. In addition, we gained insight into the role of carbonate impurities in the system, which reliably indicate the first equivalence point of the highly charged nanorods by causing the brief rise in conductivity before a plateau is reached. We therefore discourage the interpretation of conductometry curves for nanoparticles by traditional linearization. Instead, we propose a more reliable method for nanoparticle charge determination from the conductometric data based on calculating the fraction of counterions entering the bulk solution instead of merely observing conductivity or pH.
For polymeric polyelectrolytes, which can be envisioned as charged lines, this phenomenon of suppressed dissociation has been mathematically described by Manning and termed counterion condensation.9 Independent of the actual dissociating species, Manning highlighted the distance between two distinct charges along the linear polyelectrolyte as crucial, with sufficient overlap of the individual potentials giving rise to counterion condensation.9–11
This general concept applies to all dissociation equilibria contributing to the net surface charge, whether the charges are lined up on a polyelectrolyte in a single dimension or spread over a two-dimensional surface.12–14 However, Manning's theory, by virtue of relying exclusively on the comparison to the thermal energy level and a critical charge density, fails under conditions of elevated ionic strength or charge densities below the theorized onset of counterion condensation.15,16 Several intricate accounts have detailed the influence of the size of a spherical particle and its curvature on the extent of the dissociation,17–19 while concurrent studies focus on the reduced bulk ionic strength to renormalize the expected, bare surface charge to take counterion condensation into account.20–22 The latter studies managed to provide methodologies to accurately describe the results of Monte-Carlo simulations of (theoretical) dissociating polyelectrolytes and nanoparticles and provide credible values for the decrease in surface charge in response to ionic strength independent of Manning's deliberations.
Yet the dissociation of individual, tightly packed charged moieties on a nanoparticle surface has never been scrutinized with regard to the chemical equilibrium of the individual dissociation reactions. The key consequence of the surface charge affecting a shift of the dissociation constants is that the acidity of the surface groups decreases significantly, which is reflected in potentiometric titrations.22–24 Additionally, as the counterion condensation effect is not limited to protolysis reactions, other cations will condense onto the particle surface just as well.4,5,13 This shift in the dissociation equilibria results in reduced ionic strength in the dispersion medium, which can be quantified by conductometry.7,25
As such, both titrimetric analyses, despite being among the most common techniques to quantify surface charge, are tainted by fluctuating surface potentials, which, if not taken into account, may lead to misguided interpretations which are quantitatively significant.26–30 Here, we suggest an alternative approach to determining the equivalence points in conductometric titration by quantifying the fraction of counterions entering the bulk solution to complement observations from conductivity or pH. The approach is based on monitoring immobilized, chargeable functional groups on a nanorod surface that can be quantitatively addressed by counterion condensation and Poisson–Boltzmann theories, leading to an updated dissociation equilibrium.
In order to prove the point in our case study, we have selected a challenging substrate to work with. Cellulose nanocrystals (CNCs) are essentially rigid, highly crystalline nanorods, but their top-down isolation from bio-based plant fibers means that slightly heterogenous morphologies with undefined cross-sections are encountered.31,32 Nevertheless, they may be regarded as one-dimensional, roughly cylindrical particles with defined aspect ratios.33,34 Our CNCs are stabilized in dispersion by phosphate moieties introduced by surface esterification, each of which carry one strongly acidic and one weakly acidic proton.35 As such, their deprotonation may result in a potentially divalent charge, immobilized exclusively on the particle surface. The size distributions notwithstanding, we show how diligent application of existing physico-chemical theories2,12,36–38 is sufficient to describe the dissociation phenomena accurately enough to simulate conductometric and potentiometric titration curves with good correlation and extract accurate values for surface charges and de facto dissociation constants.
Sodium hydroxide solution (1 M) was diluted to a concentration of 0.1 M with degassed Milli-Q water and used for conductometric titrations. Sodium chloride and for use as background electrolyte in conductometric titrations was dissolved in degassed Milli-Q water at 0.5 M.
We found that the subsequent washing procedure defines the obtained titration curves through the remaining counterions. Therefore, we include the treatment for our relevant batch of pCNC here. After HCl gas hydrolysis, wetting and neutralization (pH 7), the obtained modified and hydrolyzed pulp was washed exhaustively by centrifugation and redispersion in deionized water, until a pH of 8.9 and a conductivity of <20 μS cm−1 of the supernatant were reached. The obtained pulp was then protonated by adjusting the pH to 1 using 37 wt% HCl solution. This solution at pH 1 was again treated to centrifugation and redispersion cycles until a final pH of 4.5 and a conductivity of <20 μS cm−1 of the supernatant were reached. At this point, the individual nanocrystals were dispersed by microfluidization using a Microfluidics M-110P microfluidizer. The washed pulp was suspended in water at a concentration of 1 wt% and passed three times at 1500 bar through a pair of Z-type collision chambers with dimensions of 400 and 200 μm, respectively.
Unexpectedly, we found that this dispersion step has no noticeable consequence on the titration curves of 300 mg cellulose analyte in 500 mL water, although the surface area of the analyte was undoubtedly increased upon dispersion. Pulp, pCNC dispersed at pH 4.5 and pCNC dispersed at pH 7 yielded nearly identical datasets after normalization.
The electrode was calibrated using YSI conductivity standard solution.
Titration curves of pulp (before) and dispersed pCNC (after microfluidization) were found to be identical. The dispersion state did not noticeably affect the neutralization process as observed by conductometry.
![]() | (1) |
![]() | (2) |
The physical meaning of the conversion from conductance to conductivity in eqn (1) is to scale the measured raw conductance by the measurement geometry. Our normalization according to eqn (2) extends this frame of the raw measurement to the entirety of the analyte volume. The normalized values are in between conductivity and conductance and can be converted back to conductivities if divided by a reference volume of the analyte or give conductances if divided by the (constant) square of the electrode distance. Nevertheless, in the following, we will refer to this normalized quantity as conductance.
Secondly, in order to compare the individual datasets containing slightly varying amounts of analyte and excess HCl, the x-axis was normalized to the amount of phosphate surface groups as determined by elemental analysis for the cellulosic analytes; correspondingly the sodium phosphate salt titration curve was normalized to the amount of phosphate in the analyte. This step allows us to account for the slight contamination through the carbonation reaction as well. The volumes of added NaOH were converted into equivalents according to eqn (3) for phosphorylated nanocellulose and eqn (4) for sodium phosphate standards.
![]() | (3) |
![]() | (4) |
We emphasize that manalyte and cP,analyte refer to the dry mass of cellulose in the aliquot of cellulose dispersion added to the analyte solution and the concentration of phosphate groups in the (dry) cellulosic material. We also consider the stoichiometric amounts of carbonate rather than its valency as the neutralization of bicarbonate occurs at elevated pH and does not influence the first two equivalence points of the phosphate neutralization that we are interested in. The surface area of the electrolyte was assumed to be constant throughout the measurements.
Despite containing the same amounts of phosphate units, the conductivity of the CNC-containing analyte is significantly reduced. In part, this is due to the discrepancies in molar conductivities of the ionic and immobilized phosphates. The major cause for the discrepancy, however, is the impact of counterion condensation,7 which significantly reduces the ionic strength of the bulk phase around the colloidal analyte. Simultaneously, the comparison of the pH curves reveals the perceived increase in basicity of the bound phosphate moieties in accordance with previously reported studies.18,24 Also, the individual shapes of the conductometric titration curves of immobilized27,28,39 and ionic25 phosphates have been reported previously, but the peculiar shape of the former ones went without more detailed discussion. It is evident in Fig. 3 and demonstrated in Fig. S3 (ESI†), however, that the analysis of the immobilized phosphate content by linearization leads to a significant overestimation of the actual result. In order to eventually address this issue, it is necessary to understand the nature and extent of the individual ionic dissociation processes that are the foundation of the analytic method.
The dissociation reactions connecting the different phosphate surface group species are shown in Fig. 4. We are neglecting the formation of disodium and trisodium orthophosphate here, given that, for one, no equilibrium constants to describe these processes accurately were available and, for another, their concentrations can be considered negligible in high dilution and below pH 12. Besides the phosphate analyte, pH-active carbonate species are present in the system. These arise from the limited exposure of the analyte solution to ambient air, allowing for carbonation reactions to take place. The species we deem necessary to be considered and their dissociation processes are shown in Fig. 5. Again, while it is theoretically possible that disodium carbonate is formed in solution, under the highly diluted conditions we deem its concentrations negligible.
![]() | ||
Fig. 5 Carbonation reaction responsible for the formation of bicarbonate and carbonate, which consume titrant and contribute to the conductivity of the analyte. |
All individual reactions are described by their own individual equilibrium constants, which are summarized in Table 1. The equilibrium constant for the interconversion of sodium phosphate and disodium phosphate was estimated as shown in the ESI.†
j | Dissociation constant | Association constant | Ref. | ||
---|---|---|---|---|---|
Kdis | pKdis | Kas | pKas | ||
a1 | 1.10 × 10−2 | 1.96 | 91.2 | −1.96 | 40 |
a2 | 6.17 × 10−8 | 7.21 | 1.62 × 10−7 | −7.21 | 40 |
a3, eff | 6.31 × 10−13 | 12.2 | 1.28 × 10−12 | −12.2 | 40 |
d1 | 0.56 | 0.25 | 1.78 | −0.25 | 41 |
d2 | 2.09 × 10−12 | 1.68 | 47.9 | −1.68 | 41 |
d3 | 0.22 | 0.65 | 4.47 | −0.65 | 42 Estimate (see ESI) |
a4, eff | 4.47 × 10−7 | 6.36 | 2.24 × 10−6 | −6.36 | 43 |
a5 | 4.68 × 10−11 | 10.35 | 2.14 × 10−10 | −10.35 | 43 |
d4 | 1.51 | −0.18 | 0.66 | 0.18 | 43 |
d5 | 9.77 × 10−2 | 1.01 | 10.2 | −1.01 | 43 |
Kw | 1.0 × 10−14 | 14 | 1.0 × 10−14 | −14 |
With the knowledge of the accurate volume of the considered analyte and the total amounts of all components in the analyte, the concentrations of all individual species in the interconnected dissociation equilibria can be calculated. The details will be outlined in the following.
Firstly, the total amounts of chloride as well as sodium, carbonates, and phosphates are defined by the mass balance of all relevant species. Trivially, the concentration of chloride ions is equal to the total concentration of chloride in the system (eqn (5)). Analogously, however, the total amount of all species containing sodium (eqn (6)), phosphate (eqn (7)) and carbonate (eqn (8)) is known and can be expressed as follows:
[Σ(chloride)] = [Cl−] | (5) |
[Σ(sodium)] = [Na+] + [NaRPO4−] + [HNaRPO4] + 2[Na2RPO4] + [NaHCO3] + [NaCO3−] | (6) |
[Σ(phosphate)] = [H2RPO4] + [HRPO4−] + [RPO42−] + [NaHRPO4] + [NaRPO4−] + [Na2RPO4] | (7) |
[Σ(carbonate)] = [CO2,aq] + [HCO3−] + [NaHCO3] + [NaCO3−] + [CO32−] | (8) |
The exact concentrations of all individual species contained in eqn (6)–(8) can be assessed when all dissociation processes are at their equilibrium states. At equilibrium, the ratios of dissociated and associated species are defined by the individual dissociation constants, provided in Table 1. However, as discussed in the introduction, in the presence of surface potentials, the equilibrium constants for the dissociation of the phosphate surface groups require additional correction. If and when this phenomenon becomes relevant can be assessed by considering the electrostatic potential energy between two charges as expressed in eqn (9)
![]() | (9) |
![]() | (10) |
with
![]() | (11) |
In eqn (9), (10) and (11), U is the electrostatic potential energy, ε0 and εr are the vacuum permittivity and the relative permittivity of water, q1 and q2 are the amounts of charge interacting, and r1 and r2 are the locations of two interacting charges, with dcharge being their Euclidian distance, kB is the Boltzmann constant, T is the absolute temperature and λB is the Bjerrum length. If the distance between the two charges is large, their electrostatic interaction is negligible. In close proximity, however, the electrostatic potential energy quickly increases as the individual electric fields overlap. According to Manning, the threshold for counterion condensation is reached, when the electrostatic potential between two neighboring charges non longer decreases below the thermal energy level according to eqn (10). In this context, it is sensible to express the distance between two charges in terms of the Bjerrum length λB (see, eqn (11)), which defines the distance, in which the potential of a single elementary charge decreases to thermal level. Following Manning's theory, if the charges are separated by less than a Bjerrum length, the superposition of their individual potentials leads to significantly enhanced electrostatic interactions that induce counterion condensation. This is an absolute criterion in Manning's original theory, which does not allow for degrees of surface interactions. Either the threshold is exceeded or not, which makes this theory unsuited for low surface charges. Similarly, by taking into account chemical potentials of the dissociating ions, Manning was able to describe selectivities for mixtures of counterions,44 but his model fails, for instance, for nearly quantitative protonation of polyacids.16 Nevertheless, the concept of separately considering the effects of the dissociation free energies and the electrostatic contributions on the overall dissociation reactions, as outlined in Manning's later work,12 can be applied more universally, to overcome the aforementioned limitations. This is illustrated in Fig. 1d and can be expressed according to eqn (12) and (13).
ΔG0total = ΔGdissociation0 + Usite | (12) |
![]() | (13) |
By treating the electrostatic interactions of the site with the surrounding surface as an additive component to the free energy ΔG of the main dissociation reaction, it follows that this contribution can be applied to the equilibrium constant as a correctional factor Kcondensation according to eqn (13). This simplification means that we neglect entropic differences between the colloidal and ionic phosphates that originate from the presence of an electrostatic double layer around the colloidal particles, as well as potential changes in the hydration of immobilized and dissociated phosphate moieties. However, there is precedent for the separate contemplation of the ionic interactions between the two dissociating charges and a background potential,2,5,45 and treating entropic changes as negligible seems reasonable when considering that for both ionic and immobilized phosphate, dissociation events increase the total number of particles by the same increment: 1. this means that the absolute entropies of ionic and immobilized phosphate systems must be differing due to the anionic and cationic charge concentrations around the particles, but the entropy changes due to individual dissociation events can be considered nearly identical.
We have detailed our assessment of the electrostatic potential energy and its impact on the dissociation equilibria in Appendix A (ESI†). These deliberations are equivalent to previously published charge renormalization methodologies.20,21,46,47 We, too, consider the promotion of ion association to the surface, which reduces the degree of dissociation of the potentially charged sites, but from the perspective of the individual dissociation events. This means that our terminology varies from that of established charge renormalization considerations. Charge normalization is founded in the solution of the nonlinear Poisson–Boltzmann equation describing the charge distribution and potential decrease within the confines of a Wigner–Seitz cell around a colloidal particle with a defined bare charge. With the knowledge of the electrostatic potential at the cell boundary and the bulk ionic strength, it is possible to linearize the Poisson–Boltzmann equation and calculate effective surface charges, by considering the integrated charge density and balancing it against the net charge of the Wigner–Seitz cell.20,46 In this context, the bare surface charge is considered partially neutralized by unspecific ion association, which neglects ionic affinities. Nevertheless, accurate results are obtained when the association constants of competing counterions are several magnitudes apart.22,48 Here, instead, we consider the surface dissociation processes as directly impacted by the surface potential, meaning phosphate functionalities carrying bound protons or forming ion pairs with sodium ions are considered as uncharged. Therefore, in our consideration, we follow the affinities of individual counterions for individual surface functionalities through their corresponding equilibrium constants, and emerging surface charges are directly comparable to the otherwise renormalized values.22 This methodology allows us to track both strong and weak acidic functionalities, as well as associates of both protons and sodium ions, simultaneously.
Following eqn (13), the influence of the surface energy can be expressed as an additional constant Kcondensation. As such, eqn (14) and (15) describe the deprotonation of phosphate surface groups, while eqn (16)–(18) describe the analogous dissociation of sodium phosphate entities and sodium hydrogen phosphate.
![]() | (14) |
![]() | (15) |
![]() | (16) |
![]() | (17) |
![]() | (18) |
Analogous expressions describe the protonation (eqn (19) and (20)) and the sodium dissociation equilibria (eqn (21) and (22)) for bicarbonate and carbonate, respectively. As these are dissolved, ionic species, counterion condensation plays no role here.
![]() | (19) |
![]() | (20) |
![]() | (21) |
![]() | (22) |
These equilibrium conditions yield the ratios of the considered species if the concentration of free protons is known. This concentration, in turn, follows from the charge balance of all species in the system (eqn (23)) and the ion product of water (eqn (24)).
0 = ([OH−] + [Cl−] + [HRPO4−] + 2[RPO42−] + [NaRPO4−] + [HCO3−] + 2[CO32−] + [NaCO3−]) − ([H−] + [Na+]) | (23) |
![]() | (24) |
By rearranging eqn (5)–(24) into matrix form as shown in Appendix B (ESI†), we obtain a system of equations described by eqn (25), that defines the equilibrium concentrations of all dissociation equilibria considered here. In this context, it is convenient to convert the expressions involving dissociation constants into logarithmic form. This means that the concentration quotients are converted into sums, which are easier to handle, and which prevent the consideration of negative values for the real concentrations. The logarithmic values of the concentrations can be obtained by numerically solving eqn (25).
Cln(VB) = M−1 × K(VB) | (25) |
The concentrations obtained by eqn (25) describe the dissociation of the surface groups accurately if the estimate account for the counterion condensation is accurate. However, the bulk concentrations of the mobile ions, which account for the measured conductances, remain veiled by the diffuse layer of counterions around the surface charge. As illustrated in Fig. 6 and 7, the electric surface potential attracts counterions around the particle, compensating the charge.37,49 Fig. 6 also emphasizes the fact that the zeta potential – as the potential along the slipping plane – depends on several external factors and is not directly proportional to the surface charge density. For reference, we have reported the zeta potential values of pCNCs in our earlier publication.35
![]() | ||
Fig. 6 Schematic representation of the electrostatic potential decrease throughout the diffuse layer, situated between bulk phase (r > rB) and Stern layer (rP < r < rP + rion). The measured zeta potentials (yellow) tend to be slightly larger than thermal potential,35 placing the slipping plane closer to the particle surface than our assumed boundary plane. |
The loosely bound ions close to the surface are kinetically tied to the particles, which reduces their bulk activities and their ability to conduct electricity. Using the known surface charge, it is possible to evaluate the concentrations of cations and anions in the diffuse layer by applying Poisson–Boltzmann statistics,36,50,51 as has been demonstrated by studies predicting the osmotic pressure of colloidal dispersions.20,21
By integrating the ion densities predicted by the Poisson Boltzmann approach over the volume of the electrostatic double layer, it is possible to “count” the ions that are immobilized close to the particle surface.20,36 Thus, following the methodology outlined in Appendix C (ESI†), we can obtain activity values for the dissociated ions calculated in eqn (25) by balancing the number of ions immobilized in the diffuse layer against the total number of ions in the system. These activity values can then be applied to obtain the bulk concentrations of the individual species according to eqn (26) and (27).
cbulk(VB) = γ(VB)·c(VB) | (26) |
Cbulkln(VB) = Cln(VB) + γln(VB) | (27) |
The real (non-logarithmic) bulk concentrations, in turn, can be converted into conductivities according to eqn (28) using the individual limiting equivalent conductivities Λ0i listed in Table 2.
![]() | (28) |
Λ0i | Literature values at 25 °C | Values at 20 °C | Ref. |
---|---|---|---|
a In literature, the conductivities of tribasic monosodium phosphate and monosodium carbonate ions have been estimated to be equal to hydrogen phosphate and bicarbonate ions, respectively.41,54 | |||
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349.85 (mS cm−1) (L mol−1) | 325.52 (mS cm−1) (L mol−1) | 52 |
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198.3 (mS cm−1) (L mol−1) | 179.2 (mS cm−1) (L mol−1) | 52 |
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50.1 (mS cm−1) (L mol−1) | 44.8 (mS cm−1) (L mol−1) | 52 |
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76.4 (mS cm−1) (L mol−1) | 69.7 (mS cm−1) (L mol−1) | 52 |
![]() |
32 (mS cm−1) (L mol−1) | 28.43 (mS cm−1) (L mol−1) | 52 |
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57.2 (mS cm−1) (L mol−1) | 50.82 (mS cm−1) (L mol−1) | 52 |
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![]() ![]() |
![]() ![]() |
41 |
![]() |
46 (mS cm−1) (L mol−1) | 41.4 (mS cm−1) (L mol−1) | 53 |
![]() |
![]() ![]() |
![]() ![]() |
54 |
![]() |
69.3 (mS cm−1) (L mol−1) | 62.4 (mS cm−1) (L mol−1) | 55 |
Λ0CNC | Eqn (D8) (ESI) |
The conductivity of the CNC depends on their charge as well as the mobility of the counterions in the double layer and can be estimated as described in Appendix D (ESI†).
The conductivity data that can be obtained with these calculations are compared to the experimental data in Fig. 8a, while the measured data for the pH during the titration are compared to the calculated values in Fig. 8b.
It is clear from Fig. 8a and b that for dissolved sodium dihydrogen phosphate, the calculated data for both pH and conductivity are in excellent agreement with the measured data. Evidently, our model for the dissociation equilibria of the phosphate species describes the observed phenomena accurately. By contrast, both calculated datasets for the immobilized phosphate surface groups accurately describe the trends in the inhibition of the dissociation of the surface groups which leads to higher observed pKa values as well as lower overall conductance and widened curve shapes in conductometry, but the clear discrepancies in theoretical and practical values expose flaws in our model. As such, the conductance curve in Fig. 8 is generally underestimating the conductance until sodium hydroxide is added in excess, raising the bulk anion concentration in particular and ionic strenght in general. This suggests that the corrections we employed for the counterion condensation effect are too strong. Specifically, this means that either the surface potential or the amount of ions trapped in the electrostatic double layer are overestimated. Additional experiments in environments with different background ionic strenghts, which are shown in Fig. 9, indicate, that it is in fact the overestimation of the surface potential that is to blame.
The curves shown in Fig. 9 show similar discrepancies between modeled and measured datasets. The varying ionic strengths have a significant impact on the Debye length, which describes the screening of the surface charges as well as the thickness of the electrostatic double layer. Despite the increased screening at high ionic strengths, however, the observed discrepancies remain similar.
Consulting the pH curves in Fig. 8b further supports these deliberations. It is evident, that the calculated pH values are consistently larger than the observed values in the acidic regime, illustrating the overly reduced acidity in the theoretical dataset. In the basic regime, in turn, the pH is underestimated, which can be attributed to the growing concentration of sodium ions in the system. Our model assumes that too many sodium ions are associated to the surface groups, facilitating the dissociation of protons. It must be considered, however, that past the first equivalence point, the discrepancies between measured and calculated pH describe discrepancies in hydroxide concentration that are lower than 0.01% and well below the uncertainties of the concentrations of the standard solutions used in the titrations.
Possible causes for the overestimation of the surface potentials lie in the total amounts of surface area and charge, respectively, as well as in their arrangement on the surface and the strength of their interaction. While we can regard the overall charge content as reliable, having confirmed it via elemental analysis and found corresponding results from the ash contents in thermogravimetric analyses, the size of the crystallites is less clear. The CNC have been isolated in a top-down approach from natural fibers and therefore display distributions around median values for length and, crucially, height,33,35,56 which translates to the surface area of the individual particles. Furthermore, while it is clear from their dimensions, that the particles are aggregates of several crystallites, the actual arrangement of these elemental fibril fragments57,58 and that of cellulose chains along their cross-sections59 remains unclear. Therefore, while we cannot specify where exactly the surface groups are located on the particle surface, the most prudent assumption is that of cylindrical particles of average diameter with a homogenous charge distribution on the mantle area as described in Appendix A (ESI†).
Despite this simplification, it is evident that our model is still a good approximation of the observed data. It correctly describes the significant decrease in conductivity compared to the dissolved phosphate, as well as the emergence of a local minimum close to the first equivalence point ahead of the plateau phase leading up to the second equivalence point. Around the second equivalence point, our model predicts an idealized linear behavior that is not reflected in the measured data, but the final increase in conductance due to excess sodium hydroxide is reflected very accurately. Therefore, while reviewing them critically, the calculated data can still give insight into the processes that need to be considered in the analysis. First and foremost, the counterion condensation parameter, which is displayed in logarithmic form in Fig. 8b, illustrates that the acidic strength of the phosphate surface groups is decreased significantly, raising the observed pKa-value for the first acidic dissociation reaction from 3.5 to 4.5 depending on the surface charge. Consequently, during the initial deprotonation, the surface groups are strongly acidic as are dissolved phosphate ions, but then the acidic strength of the surface groups decreases significantly. That is the cause for both the significant broadening of the titration curve and the decreased initial conductivity. Simultaneously, the model estimate of effective pKa values in the order of 3.5 to 4.5 for the stronger acidic proton illustrates that the analysis of the conductometric titration curve merely by linearization does not apply here. The surface groups are transitioning from strongly acidic to weakly acidic as a surface potential is generated, which precludes accurate quantification.
Instead, the minimum in the curves preceding the plateau phase is a more reliable feature for identifying the equivalence point. This claim is supported by the change in the bulk sodium concentration according to our model, which is shown in Fig. 10.
It is clear from Fig. 10, that in the case of dissolved phosphate ions, the association of sodium ions is negligible before the first equivalence point is reached. Subsequently, the formation of divalent hydrogen phosphate ions leads to the simultaneous formation of sodium hydrogen phosphate associates, which extends past the second equivalence point, when the sodium ion concentration in the system keeps increasing. Therefore, the amount of sodium ions in the bulk phase increases, but a fraction of the added ions associates to phosphate moieties. This effect is substantially more significant for the immobilized phosphate surface groups. In fact, the amount of sodium ions entering the bulk phase of the solution between the first and second equivalence points is near zero, illustrating that a maximal surface charge is reached. At this point, further deprotonation is accompanied with immediate association of a sodium ion. However, at the first equivalence point, the rate of sodium entering the bulk phase of the system spikes. This is an indirect consequence of the decreased acidity of the surface groups, shifting the jump in pH at the first equivalence point from 3–5 to 4–6 (see, Fig. 8b). This means that in the case of the immobilized phosphate units, any carbonic acid impurities in the system are being neutralized inbetween the first and second protons of the phosphate units, immediately after the first equivalence point is reached. During the deprotonation of the carbonic acid, the surface charge of the cellulose fibers increases to a lower degree, meaning that more free sodium ions enter the bulk phase. This increase in carbonate and sodium ions in the bulk phase is visible in the titration curves in Fig. 8a and Fig. 9 as the slight increase in conductivity after the first equivalence point. By contrast, in the case of dissolved phosphate, where the deprotonation of the dihydrogen phosphate ions starts already at a pH level of 5, both dihydrogen phosphate (pKa 7.21) and carbonic acid (apparent pKa 6.35, see, Table 1) deprotonate simultaneously when the pH increases.
Lastly, our modeled data give access to surface charge values, which take into account the incomplete dissociation and the screening of the surface charges by the surrounding diffuse layer. We should point out here, that these surface charge values correspond to the renormalized values discussed in other studies.20–22,46,47 The net charges at the boundary layer are not related to those studies, as they do not consider this boundary between diffuse layer and bulk phase. Our data are shown in Fig. 11.
As shown in Fig. 8 and 9, the calculated values are in reasonable agreement with the measured data and accurately describe the decrease in conductivity for the particles caused by incomplete dissociation. This means that the calculated surface charge densities of less than 0.5 mmol g−1, which translates to less than 0.35 mmol g−1 at the boundary plane need to be taken seriously, even if this suggests that less than 25% of potentially chargeable sites on the surface are actually dissociated at any given time. It must be noted that our model describes a decrease in surface charge leading up to the second equivalence point. This is where calculated and measured data have their largest discrepancy (see, Fig. 8). Therefore, this reduction in surface charge is most likely an artifact caused by the overestimation of the counterion condensation effect. Furthermore, our model predicts an increase in surface charge with increasing ionic strength. While this seems counterintuitive, given more efficient screening of the surface charge in conditions with reduced Debye lengths, the cause for this effect can be seen in eqn (A4) (ESI†). The surface potential also depends on the Debye length, meaning that an increased charge density in the diffuse layer also causes screening of the surface charges’ interactions among each other. This means that the effective surface potential is reduced with increasing ionic strength, shifting the surface equilibrium reactions back towards dissociation. The dependance of the surface charge on the ionic strength is further illustrated in Fig. 12.
During the neutralization processes, the bulk ionic strength remains nearly constant, the net reaction being the replacement of protons in the system with sodium ions. Only after the second equivalence point is reached, the ionic strength increases due to excess sodium and hydroxide ions accumulating in the system. In this context, Fig. 12 illustrates that our model calculates very similar surface charges for comparable ionic strengths for all experiments, regardless of the actual particle concentrations.
Footnote |
† Electronic supplementary information (ESI) available: Particle dimensions, demonstration of the reproducibility of titration experiments, comparison of titration curves of dispersed CNC and modified pulp, illustration of linearization analyses of dissolved and immobilized phosphates, estimation of the dissociation constant of disodium hydrogen phosphate, quantification of carbonate contaminants, ionic composition of the simulated experiments, Appendix A, Appendix B, Appendix C, Appendix D, symbols index, MATLAB scripts for the simulated conductometric titration curves. See DOI: https://doi.org/10.1039/d5cp01616a |
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