Björn
Braunschweig
*abcd,
Felix
Schulze-Zachau
acd,
Eva
Nagel
a,
Kathrin
Engelhardt‡
a,
Stefan
Stoyanov
e,
Georgi
Gochev
ef,
Khr.
Khristov
e,
Elena
Mileva
e,
Dotchi
Exerowa
e,
Reinhard
Miller
f and
Wolfgang
Peukert
abcd
aInstitute of Particle Technology (LFG), Friedrich-Alexander-Universität Erlangen-Nürnberg (FAU), Cauerstraße 4, 91058 Erlangen, Germany. E-mail: bjoern.braunschweig@fau.de
bCluster of Excellence Engineering of Advanced Materials (EAM), Nägelsbachstr. 49b, 91052 Erlangen, Germany
cErlangen Graduate School in Advanced Optical Technologies (SAOT), Paul-Gordan-Straße 6, 91052 Erlangen, Germany
dInterdisciplinary Center of Functional Particle Systems, Haberstraße 9a, 91058 Erlangen, Germany
eInstitute of Physical Chemistry, Bulgarian Academy of Sciences, 1113 Sofia, Bulgaria
fMax-Planck-Institute of Colloids and Interfaces, 14476 Golm/Potsdam, Germany
First published on 13th June 2016
β-Lactoglobulin (BLG) adsorption layers at air–water interfaces were studied in situ with vibrational sum-frequency generation (SFG), tensiometry, surface dilatational rheology and ellipsometry as a function of bulk Ca2+ concentration. The relation between the interfacial molecular structure of adsorbed BLG and the interactions with the supporting electrolyte is additionally addressed on higher length scales along the foam hierarchy – from the ubiquitous air–water interface through thin foam films to macroscopic foam. For concentrations <1 mM, a strong decrease in SFG intensity from O–H stretching bands and a slight increase in layer thickness and surface pressure are observed. A further increase in Ca2+ concentrations above 1 mM causes an apparent change in the polarity of aromatic C–H stretching vibrations from interfacial BLG which we associate to a charge reversal at the interface. Foam film measurements show formation of common black films at Ca2+ concentrations above 1 mM due to considerable decrease of the stabilizing electrostatic disjoining pressure. These observations also correlate with a minimum in macroscopic foam stability. For concentrations >30 mM Ca2+, micrographs of foam films show clear signatures of aggregates which tend to increase the stability of foam films. Here, the interfacial layers have a higher surface dilatational elasticity. In fact, macroscopic foams formed from BLG dilutions with high Ca2+ concentrations where aggregates and interfacial layers with higher elasticity are found, showed the highest stability with much smaller bubble sizes.
Particularly for foams in dairy products the interactions of BLG, a major whey protein, and Ca2+ ions is important due to the high concentration of Ca (∼33 mM)10 in bovine milk which is naturally rich of calcium. While calcium binding to whey proteins is important, the latter does also play a major role in the cell metabolism11 where Ca2+ can have many functions such as co-factors for enzymes or as promoter for signal transduction. However, little molecular-level information is available on the effects of Ca2+ ions for charge regulation of protein surfaces at gas–water interfaces or the importance of Ca2+ for protein–protein interactions. For proteins in bulk solutions, previous studies indicate that a charge reversal can be caused by interaction with Ca2+ ions: Molina-Bolívar et al.12 determined the ζ-potential of protein-covered latex particles and showed that it could be tuned from negative to positive values at a concentration of ∼50 mM CaCl2. The authors attribute the polarity change of the ζ-potential to a specific ion effect of Ca2+ that is not seen in NaCl solutions. Evidence that Ca2+ can interact with BLG's carboxylates comes from a study by Simons et al.13 where the authors show that the concentration of Ca2+ needed to increase thermal aggregation scaled with the number of available carboxylate groups which were systematically varied using modified BLG proteins. In addition, improved thermal aggregation was not found for monovalent salts indicating that Ca2+ effects are ion specific.13 In particular for BLG in the bulk solution, Zittle et al.14 report that in the pH range of 6 to 8 binding of Ca2+ ions is equivalent to the net charge. Consequently, it is possible to use the interaction of Ca2+ with BLG to efficiently screen the protein's net charge at mildly basic pH values or even cause a charge reversal. Furthermore, Beierlein et al.15 applied molecular dynamics (MD) simulations of bulk BLG proteins and reported that Li+, Na+, and K+ cations can form contact-ion pairs (CIPs) with Asp and Glu carboxylates at the BLG surface. In the case of Li+ metal-cations, MD simulations show a charge reversal within the first solvation shell at 100 mM LiCl.
In this article we address the question if interfacial properties of BLG and adsorbate induced charging of air–water interfaces can be changed in a way that affects also macroscopic foam stability via structure–property relations from the interface to the macroscopic foam. In addition, addressing the solvation of proteins at interfaces is not only important for foam formulation but does have also larger implications as it is equally important in colloid science and protein purification.
Using a combination of experimental techniques on several length scales from asymmetric air–water interfaces, foam films (symmetric air/liquid/air interfaces) and macroscopic foam we provide a coherent understanding on BLG stabilized aqueous foam and the effects of Ca2+.
(1) |
PC = 2γ/R | (2) |
h = 2h1 + h2 | (3) |
(4) |
Fig. 1 (a) Schematic representation of the structure of a BLG foam film (not to scale). Note that this scheme is only relevant for very low Ca2+ concentrations before significant charge screening and a possible charge reversal occurs at the interface; see also the discussion of Fig. 2. (b) Photograph of the modified porous plate cell with horizontal part of the capillary for experiments at low capillary pressures; the liquid from the porous plate is transferred into the horizontal part of the capillary and stays at the level of the film thus avoiding the action of a hydrostatic pressure. |
An Exerowa–Scheludko porous plate cell was used to measure the critical pressure of rupture Pcr of foam films.25,26 Foam films are formed in a small hole (radius of 0.5 mm) that is located in the center of a porous glass plate after the meniscus of a solution drop penetrates into the porous material. We used a modified version of this cell type with an elongated horizontal portion of the glass capillary (see Fig. 1b). This modification allows a higher precision for measurements at low capillary pressures of <100 Pa. This is particularly important for investigations during foam-film formation. The pressure in the glass chamber of the cell is controlled by a membrane pump and measured by a digital manometer with a sensitivity of ±1 Pa. The pressure applied onto the film surfaces is equal to the disjoining pressure ΠD in an equilibrium film with constant thickness. This allows for measuring ΠDvs. a thickness isotherm for the foam films under investigation. By this technique, it was possible to form films at pressures around 50–60 Pa and then to gradually increase the pressure until the film ruptures. For every studied solution, five films were formed sequentially and the pressure of rupture was measured. After film rupture, the solution drop was recovered in the hole of the porous plate and equilibrated again for another 30 min until the interfaces were saturated. Then the next foam film was formed. In this paper we present experimental data on foam film thickness h at constant pressure and the critical pressure of film rupture Pcr.
All measurements were reproduced at least three times and the results were averaged. The structure of foam and the bubble size distributions were determined with the foam structure module of the DFA100.
Fig. 3 Effects of Ca2+ concentration on (a) the bulk ζ-potential and (b) layer thickness h1 (black circles) of β-lactoglobulin (BLG) modified at air–water interfaces as measured by ellipsometry and surface pressure Π (red triangles). (c) Intensity of O–H stretching band at 3200 cm−1 from SFG spectra in Fig. 2b. (d) Surface dilatational elasticity E′ (black squares) and viscosity E′′ (red circles). (e) Foam film thickness h at a capillary pressure PC of (100 ± 4) Pa. (f) Critical pressure of film rupture Pcr and (g) stability of macroscopic foams from aqueous 15 μM solutions of BLG as a function of Ca2+ concentration and foam age. Lines are a guide to the eye. |
A close inspection of Fig. 2 and 3c reveals a dramatic effect of Ca2+ concentrations on the SFG intensity of O–H stretching vibrations. At low concentrations (<2 mM) a substantial decrease in the intensity with increasing CCa2+ is observed, while in the concentration range between 2 and 10 mM, the O–H intensity remains at a local plateau. Further increase in CCa2+ above 10 mM leads first to a decrease in O–H intensity that is followed by a weak but noticeable recovery beyond 100 mM Ca2+. While O–H vibrational bands are strongly dependent of CCa2+, contributions from C–H vibrational bands are for all concentrations very similar (Fig. 2a). Small changes in relative intensities of the contributing CH3 bands are actually caused by interferences with the O–H bands and their variations with CCa2+. Obviously the net orientation of the contributing CH3 groups is not impaired by the Ca2+ induced increase in surface pressure and layer thickness (both Fig. 3b). This can only be explained when the inclusion of additional BLG proteins to the adsorbate layer occurs in a highly disordered state. In this state, the orientational average and thus the contribution of BLG molecules to the SFG spectra is negligible (see eqn (1) and discussion of Aq). In previous studies where the O–H intensity and the charging state of the interfaces were controlled by the bulk pH, aggregate formation at the interface was found while little changes in intensity of the C–H bands were seen.24,28 As aggregates can be one possibility for the above observations, we will address this aspect in more detail below.
In this work, we have chosen a pH where the BLG molecules in the bulk solution carry a high negative net charge which leads to a ζ-potential of bulk BLG molecules close to −20 mV in the absence of Ca2+ (Fig. 3a). Obviously, the adsorption of BLG causes a macroscopic electric field at the air–water interface which can lead to polarized and ordered interfacial water molecules at high electric field strengths.6,15,21,24,29 As we have previously shown, SFG spectroscopy of BLG interfacial layers can be applied to determine relative changes in the interfacial electric field.5,24 In fact, the oscillator strengths Aq of O–H stretching bands and their phases can be used as highly sensitive markers for the charging state of electrified air–water interfaces.30 As can be clearly identified from Fig. 3a, increasing CCa2+ leads to a dramatic decrease in the ζ-potential of BLG in the bulk to nearly zero values at ∼100 mM Ca2+. Small positive ζ-potentials are observed for concentrations >100 mM Ca2+. Obviously, additions of Ca2+ ions to the protein solution effectively influence the surface electric potential of the BLG entities in the solution at their shear plane and cause charge screening as well as overcharging at high concentrations. Taking these bulk processes into account, it is not surprising that the O–H intensity decreases because of the very efficient screening effect of Ca2+ counterions on the interfacial electric field that is induced by the presence of charged BLG molecules.
In addition to the latter observation, an apparent change in polarity of aromatic C–H stretching vibrations at ∼3060 cm−1 for concentrations between 0.1 and 2 mM can be inferred from a close inspection of Fig. 2b. This is likely due to a change in the phase of O–H vibrational bands caused by a charge reversal at the interface. In fact, previous studies on the effect of pH4,5,28 and oppositely charged surfactants6,24 on the properties of BLG layers have shown that similar but much more pronounced changes in the shape of the aromatic C–H band can be observed when the net charge within the interfacial plane is reversed.
In that case, a local minimum in SFG intensity at ∼3060 cm−1 is transformed into a local maximum. The phase reversal of the O–H bands at the air–water interface, that can be associated with a reversal of the interfacial net charge, occurs at much lower Ca2+ concentrations (∼1 mM) compared to the concentration where the ζ-potential of BLG proteins in the bulk solution is negligible (∼100 mM). Since ion specific effects of Ca2+ with BLG were already suggested by previous work,13 our results indicate that effects of Ca2+ at the interface are much more pronounced than in the bulk and lead, consequently, to an interfacial charge reversal at lower Ca2+ concentrations (∼1 mM). Further support for the strong interaction of calcium with BLG comes from an early study by Zittle et al.14 who have applied analytic ultracentrifugation to determine the binding of calcium to native and denatured β-lactoglobulin. In fact, the study by Zittle et al. and also other studies31 show that within the pH range 6–7.2, a BLG molecule is capable to bind several Ca2+ ions.
Additional measurements of the thickness of the adsorption layers h1, the surface pressure and the surface dilatational rheology characteristics provide together with the SFG results a more complete picture of the molecular structure and interfacial properties which serves as a base to analyse the stability of foams and foam films as their building blocks. The layer thickness is presented in Fig. 3b. At concentrations <1 mM, a layer thickness h1 = 5.5 ± 0.6 nm is established. Such a value is compared to the thickness of BLG layers in the absence of Ca2+ already by a factor of two thicker than what was reported previously by ellipsometry4,24 and neutron reflectivity.18 This suggests that already at low Ca2+ concentrations BLG adsorption and possibly also aggregation at the air–water interface is promoted. However, the relative constant layer thickness h1 at low concentrations is accompanied by a gradual increase of both the surface pressure (Fig. 3b) and the surface dilatational elasticity E′ (Fig. 3d) which accounts for a compression of the surface layer and more intense intermolecular interactions that are responsible for the visco-elastic behaviour of the layer. A further increase in Ca2+ concentrations beyond ∼1.5 mM causes a jump to a second plateau of the layer thickness to h1 = 8.8 ± 1.3 nm. At concentrations >0.1 M where the bulk ζ-potential changes from negative to positive values (Fig. 3a), the most prominent changes in E′ and E′′ (Fig. 3d) occur. At 0.1 M the surface dilatational viscosity reaches a pronounced local minimum while the elasticity runs into a local maximum. At Ca2+ concentrations >0.3 M substantial increase in layer thickness h1 is observed from ∼9 to ∼23 nm at 1 M concentration. Comparing these changes with the O–H intensity which has decreased to nearly zero values at 0.1 M and which is dominated by electrostatic and orientation effects (see Section 2.4), it is reasonable to assume that the above changes must be caused by a change in intermolecular interactions within the surface layer which are dominated for concentrations <0.1 M by electrostatic interactions while for concentrations above 0.1 M the interfacial electric field is fully screened and van der Waals as well as hydrophobic forces can become dominant and consequently change the surface rheology of the layer. As we will show below, the molecular structure and changes in the magnitude and the type of the interactions have important consequences for the stability and thickness of foam films and the stability and structure of macroscopic foam.
The double layer potential is screened by increasing the ionic strength of the supporting electrolyte.25 This is also valid for the case of BLG foam films at a pH that is different from the isoelectric point pI, where an increase in ionic strength leads to a decrease in foam film thickness.32
Let us now consider the thickness of BLG foam films as a function of Ca2+ concentrations in the tube cell. As discussed in the previous section, the interfacial BLG layers are negatively charged at the pH (>6) of the solutions that were used in our study, at least for CCa2+ < 1 mM. Fig. 3e shows that initially the film thickness gradually decreases due to the screening effect of the increasing concentration of Ca2+ counterions. In the range of CCa2+ between 0.05 and 0.2 mM, common thin films (CTF) are obtained as their equilibrium thickness is homogeneous (see Fig. 4) and comparatively large from 60 to 90 nm (Fig. 3e). This range of film thicknesses is attributable to weak electrostatic screening by these electrolyte concentrations. CTFs consist of two adsorption layers each with thickness h1 = 5.5 ± 0.6 nm (see the left-hand-side plateau in Fig. 3b) and a large solution core. The real film thicknesses h (Fig. 1a), presented in Fig. 3e, were calculated according to eqn (3) and (4) from the measured equivalent thicknesses hw of the foam films. Here we have assumed a refractive index of the film core that is identical to the refractive index of neat water (n2 = 1.33) and a thickness of the adsorption layer h1 that is equal to 5.5 nm. Note that this value was previously determined from our ellipsometric measurements at the air–water interface for these concentrations (Fig. 3b).
For 1 mM bulk solutions, common black films (CBF)25 were obtained with thicknesses h of 35 ± 5 nm. Apparently, at this concentration the electrostatic disjoining pressure dominates the film thickness with a thickness of the electrolyte core h2 (Fig. 1a) of 24 ± 5 nm. The microscope image of this CBF is shown in Fig. 4. However, inhomogeneities in the film thickness are observed, which are indicative for the presence of protein aggregates confined between the two foam film surfaces. Obviously, these aggregates have sizes comparable to or larger than the liquid film core. In addition, at 1 mM we observe slower film drainage (not shown) than for the CTFs at CCa2+ < 1 mM.
At CCa2+ = 10 mM, the foam films drain slowly and exhibit island-like patterns due to the presence of larger aggregates that are confined within the film interior. Similar behaviour was reported in a study by Rullier et al.3 where BLG aggregates have been produced and intentionally introduced into the bulk solutions. However, in our study, formation of black portions in the film is observed after a few minutes. These black areas have highly irregular shapes which are caused by the retarded film drainage and a comparatively high viscoelasticity of the film surfaces (Fig. 3d). Such portions of black film at 10 mM CaCl2 (Fig. 4) are identified as CBF with a thickness of about h = 20 ± 12 nm, which was calculated using eqn (3) and (4) from the measured equivalent film thickness hw = 24 ± 10 nm and h1 = 8.8 ± 1.4 nm from ellipsometry (see the right-hand-side plateau in Fig. 3b). Note that the given value for h is an average over several measurements at different spots within the black portions of the foam film. The relatively large error is then related to inhomogeneities in the black film thickness. Foam films produced from BLG solutions with 30 and 900 mM CaCl2 were analysed in the same manner as for 10 mM and showed thicknesses in the black portions of h = 23 ± 4 nm and h = 26 ± 5 nm, respectively. We point out that the slight increase in h of the CBFs for CCa2+ > 10 mM is comparable to the measurement error and is thus not necessarily associated with a real trend of a thickness increase.
For CCa2+ between 40 and 100 mM, foam films with highly irregular film thicknesses were observed. For this reason a direct thickness measurement was not possible. The drainage of these films is blocked, which is consistent with rigid film surfaces and corresponds to the increase in surface dilatational elasticity E′ (Fig. 3d) and the nearly negligible ζ-potentials at ∼100 mM Ca2+. Surprisingly, this film behaviour changes with a further increase in Ca2+ concentrations, where again the formation of films with CBF portions is observed (see above).
The other parameter that we have used to characterise BLG foam films is the critical pressure of film rupture Pcr (Fig. 3f) which was studied in a modified porous plate cell. The highest stability of the foam films at concentrations <10 mM are attributable to the stabilizing effect of the electrostatic disjoining pressure ΠEL25,32 and along with the decrease in film thickness, a reduction of the ΠEL-magnitude leads to a decrease in foam film stability. However, a slight increase in Pcr was observed for 900 mM Ca2+ (Fig. 3f).
The increase in macroscopic foam stability is accompanied by a change in foam structure as shown in Fig. 5 for three representative concentrations. Additional foam structures for concentrations of 10, 100 and 300 mM CaCl2 can be found in the ESI.† The initial structures at 1 and 30 mM are very similar, while for higher concentration, where much more stable foams are formed (Fig. 3e), the structure is drastically different. In fact, increasing the Ca2+ concentration leads to a substantial change in bubble size distribution: for CCa2+ < 100 mM bubbles with a mean equivalent diameter of ∼80 μm and a large size fraction of bubbles between 250 and 500 μm is found directly after foaming (30 s in Fig. 5), while for CCa2+ > 100 mM directly after foaming significantly smaller bubbles with a mean diameter of 9 μm are found with a much lower frequency of bubbles in the 250 to 500 μm size fraction (ESI†). Analysis of the changes in foam structure as function of foam age indicates that bubble coalescence and drainage are major destabilization pathways.
Fig. 5 Structure and aging of macroscopic foam from 15 μM β-lactoglobulin solutions with 1 M, 30 mM and 1 mM CaCl2 concentrations. Foam age was as indicated, 30 s indicate that time after the gas flow was stopped. The lateral resolution was for images identical and is as indicated in the top left image. Bubbles are false colour coded for certain size fractions. Additional concentrations can be found in the ESI.† |
By comparing the changes in the SFG spectra of BLG modified air–water interfaces and in the layer thickness h1 (Fig. 3b), we find that the first increase in layer thickness at 0.5 to 2 mM Ca2+ coincides with a steep decrease in O–H intensity that is accompanied by a change in polarity of the aromatic C–H band at 3060 cm−1 from a dip-like structure to a weakly pronounced maximum (Fig. 2b). As noted above similar changes were previously attributed to a change in the orientation of the mean electric field at the interface that is caused by the adsorbed BLG including their solvation shells.4–6,15,24
We now propose that the rapid decline in O–H intensity is caused by specific interaction of BLG with calcium ions. The strong interaction of Ca2+ with BLG molecules first rapidly screens the interfacial net charge (CCa2+ < 1 mM) leading to conditions of a partial charge reversal and overcharging at high concentrations (CCa2+ > 1 mM).
At this point, the question on possible binding sites and motives of Ca2+ at the BLG protein surface arises. Previous studies have shown that in many cases specific ion effects can be rationalized with a simple electrostatic model of ions and their affinity to bind water molecules – the so-called Law of Matching Water Affinities.34 Using this model, contact ion pair formation between Ca2+ and R–COO− from amino acid side chains is likely because their water affinities are nearly matched. Allen and co-workers35 report in their SFG study of palmitic acid surfactants at air–water interfaces that complexes of Ca2+ ions with the carboxylate group can be formed. The authors concluded that at equilibrium conditions a mixture of bridging (2 Ca2+:1 R–COO−) and chelating (1 Ca2+:1 R–COO−) configurations is established for low concentrations of Ca2+ (0.1 M) while at 0.3 M concentrations only the bridging configuration is favoured. This means that at pH ∼ 6, binding of three Ca2+ ions to a BLG monomer are needed in order to neutralize the net charge of approximately −6e.36,37 For a further analysis we assume that at low concentrations Ca2+ binding occurs predominantly on carboxylate groups in bridging configurations. In addition, Tanford and co-workers36 report that 50 side chains with R–COO− groups are accessible to Ca2+ ions. Because each of these groups can bind Ca2+via contact ion pair formation, a calcium coverage of θ = 3/50 exists at conditions with a neutralized net charge (1–2 mM Ca2+). If we now apply a simple Langmuir adsorption model for the binding of Ca2+
Having established a picture for the molecular structure and electrostatic interactions of BLG interfacial layers as a function of CCa2+, we now address the effects of Ca2+ on the structure and stability of foam films and macroscopic foam. As discussed in Section 3.2, the thickness of foam film strongly decreases with Ca2+ concentration until common black films with apparent aggregates are formed at 1 mM. Taking into account the results for the foam film thickness h in Fig. 3e, it becomes clear that electrostatic forces have been significantly screened between 1 and 10 mM Ca2+. This is fully consistent with our attribution of the spectral changes in vibrational SFG that point to a charge reversal at ∼1.5 mM. Furthermore, images of foam films in Fig. 4 indicate that for higher Ca2+ concentrations aggregates are formed and have in addition to the higher surface dilatational elasticity E′ (Fig. 3d) a stabilization effect on the foam films at >100 mM Ca2+. The presence of aggregates at the interface is consistent with the negligible change of C–H bands in our SFG spectra (Fig. 2) when the Ca2+ is increased while the surface pressure and layer thickness both increase simultaneously. As explained above, this is only possible if the additional molecules at higher Ca2+ concentrations have no net orientation which is the case when averaging over a larger number of aggregates at the interface. This stabilization due to aggregate formation in foam films and possibly also in the lamella of macroscopic foam, and the increase in E′ are obviously directly related to higher stabilities of macroscopic foam and partly to the origin of the smaller mean bubble sizes as compared to BLG foams from solution with CCa2+ ≪ 100 mM. At this point we need to stress also the adsorption kinetics. At a bulk protein concentration of 15 μM, the adsorption of BLG to the interface is already fast (ESI†). Considering the kinetic data from surface pressure measurements (Fig. S5 in ESI†), we observed that increasing CaCl2 concentration remarkably enhances the rate of the adsorption kinetics (the slope dΠ/dt increases) within the first few seconds (<5 s) of the adsorption process. Such time scale is comparable to that of the foam formation process and therefore, adsorption kinetics can be responsible for the observed smaller bubble sizes in the final foam at very high CaCl2 concentrations. For solutions aged more than ca. 1 min, comparison of the rate of the surface pressure change with time for solutions with 15 μM BLG and CaCl2 concentrations between 0 and 1 M reveals only slight acceleration of the rate of adsorption with an increase in CaCl2 concentration.
As we have shown above in Fig. 3a, also the bulk ζ-potential is fully screened at 100 mM and it is thus likely that also in the bulk solution BLG aggregates are formed to some extent. Their concentration is, however, relatively low as we could not find evidence for aggregates from dynamic light scattering (DLS). At this point it is interesting to discuss the study by Rullier et al.3,39 on foams and foam films stabilized by BLG aggregates that were obtained by a thermal treatment of BLG solutions. These authors find that even for a very low quantity of aggregates (1%), the stability of macroscopic foam was substantially improved, while optical microscopy of foam films indicated the presence of aggregates as well. Rullier et al.40 propose three different stabilization mechanisms that depend on the relative concentration of protein aggregates. It is proposed that at high concentrations of aggregated proteins, a gel-like network with non-aggregated proteins is formed while at intermediate concentrations aggregates can crosslink the two foam film surfaces and contribute to their stabilization in the process. The origin of the stabilization of foams with aggregate concentrations as low as 1% (at 1 g l−1 total concentration) is less clear from the latter study and is attributed to aggregates that are trapped inside the plateau borders in macroscopic foam where they can slow down drainage. Similar behaviour was recently reported for particle stabilized aqueous foams by Carl et al.41
Obviously, the study by Rullier et al.40 brings strong support to our conclusion that the increase in foam as well as foam film stability is driven by a combination of aggregated BLG molecules, that either form in the bulk solution at CCa2+ ≫ 100 mM or predominantly at the interface at low concentrations <100 mM. In addition, Lexis and Willenbacher8 have proposed by comparing interfacial rheological properties with the rheology of macroscopic foam that BLG aggregates across foam lamellae can determine foam properties. The exact role of BLG aggregates at the air–water interface in the stabilization of the foam is, however, at this point unclear. Either the changes in molecular structure and lateral interactions at the air–water interface as discussed above are the only reasons, or these changes are additionally accompanied by a blocking effect where BLG agglomerates accumulate within the plateau borders and prevent or slow down foam drainage in the process.
Footnotes |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/c6sm00636a |
‡ K. E. is now at Bayer AG, Leverkusen Germany. |
This journal is © The Royal Society of Chemistry 2016 |