Xin
Peng
ab,
Xing-Zhong
Yuan
b,
P.
Somasundaran
c and
Partha
Patra
*c
aNational and Local United Engineering Laboratory for New Petrochemical Materials and Fine Utilization of Resources, Key Laboratory of Resource Fine-Processing and Advanced Materials of Hunan Province and Key Laboratory of Chemical Biology and Traditional Chinese Medicine Research (Ministry of Education of China), College of Chemistry and Chemical Engineering, Hunan Normal University, Changsha, 410081, P. R. China
bCollege of Environmental Science and Engineering, Hunan University, Changsha 410082, P. R. China
cLangmuir Center for Colloid and Interface Science, Columbia University, New York, 10027, USA. E-mail: pp2295@columbia.edu
First published on 30th September 2015
The micro-polarity anisotropy behaviour across the aqueous phase of a SDS (sodium dodecyl sulphonate)–hexane reverse micelle (RM) relies on the SDS packing in the oil–water interfacial self-assembled surfactant structure of the RM.
:
surfactant (ω0) ratio.3 A reliable estimate of MPA is critical to predict and regulate the enzyme activity in RMs.4,5 The common approaches assess MPA(
) (
– the radial distance, Fig. 1) in terms of the microstructural characteristics of water in RMs6 and the electrostatic potential distribution (ψ(
)) across the aqueous phase (Fig. 1b).7,8 Spectroscopy studies and molecular dynamic simulations reveal that, in terms of the micro-polarity attributes, the RM aqueous phase comprises at least two spatially separable regions (Fig. 1a and b), the interfacial region (ordered water) and the core region (bulk water).6,9 The ψ(
) profile that exemplifies the MPA results from the oil–water interfacial charge density levels (per volume of water in a RM) of the surfactant head groups, and the distributional aspects of the counter ions in the aqueous phase. The ψ(
) profiles exhibit an exponential form (Fig. 1b).6–9 For the aqueous phases in the vicinity of the surfactant-stabilized oil–water interfaces, the ψ profile is attributed to the surfactant chemistries. The ψ profile for these interfacial systems is developed as per the electrical double layer (EDL) models.10–13 Conversely, as the volume of the confined (nano-sized) aqueous phase of a RM is much lower, the EDL characteristics are governed by the interfacial charge density levels (per RM water content), which decrease as the ω0 values become higher. The charge density level, even at a particular ω0 value, could vary depending on the degree of surfactant packing (inter-surfactant distances) in the self-assembled surfactant structure (SASS) of a RM.14 Thus, the EDL characteristics that determine the MPA are attributed to the surfactant-types and -density/packing in a SASS.7,8 We assessed the MPA(
) as a function of surfactant density/packing in the SASSs for the SDS (sodium dodecyl sulphonate)–hexane RMs.15
The RMs were devised by adding desired amounts of water to SDS–hexane solutions (ESI,† 1). Cryo-SEM (ESI,† 2) images indicated that the RM sizes were <50 nm (ω0 ≈ 24; Fig. 1c). Analytical ultra-centrifuge (AUC) studies (ESI,† 2) reveal the RMs as spherical in shape (Fig. 1d). The RMs with ω0 in the range of 5 to 25 were spherical and of sizes in the range of 10 to 50 nm. For ESR studies (ESI,† 1), a 16-DSA (16-DOXYL-stearic acid) probe containing the NO˙ radical was added to the RM samples in desired amounts. The hyperfine splitting constant (aN) – MPA(
), and the rotational correlation time (τc) – surfactant packing in the SASS, were estimated for these RM systems. The application of the ESR technique is a reliable option as the energy absorbance value of a probe with free radicals, which can locate in the aqueous and SASS regions, allows concurrent estimation of the MPA and SASS packing aspects. The microstructural aspects of RM water were studied using IR (attenuated total reflection-infrared) spectroscopy (ESI,† 1).
We compartmentalize a RM's environment into three spatially segregated and sequentially placed regions (Fig. 1a and b), and the MPA(
) of these regions was assessed in terms of their contribution to the RM's ψ(
) profile. The non-linear Poisson–Boltzmann description of the ψ(
) profile that associates these three regions is:
![]() | (1) |
) for a RM can be written as:![]() | (2) |
![]() | (3) |
.
The ξ term is dependent on the association coefficient of the counter ions, given as β.10,19 The parameters that allow differentiation of the ψ(
) profile for the regions R2 and R3 are:
For RRM ≤ lB, ψ decreases in an exponential manner from the interface to the core, and a plateau region of the ψ(
) profile is absent. For RRM ≫ lB, the plateau part of the ψ(
) profile represents the
≈ 0 − (RRM − lB) region (R3). And, this plateau region changes minimally with increase in RM sizes, as the micro-polarity contributions are due to the bulk-type water therein. In order to gain insights into how the ψ(
) profiles differentiate for the RMs of different sizes, the responses of the NO˙ of 16-DSA in RMs of different sizes were determined. These responses were in terms of the energy absorbance values of the NO˙ in the aqueous phases of the RMs. We define the NO˙ radical (in a RM) system as a π-electron system; m π electrons and n core atoms; m + n = N. The charge and position vectors of the jth particle in this system are ej and rj, ρπr is the π-electron density, and QHCH is the σ–π parameter. The hyperfine splitting value, aHr, for a hydrogen-bonded carbon atom (rth carbon atom) of 16-DSA is:
| aHr = QHCHρπr and ρπr = ckr2 | (4) |
![]() | (5) |
, where R is the electric field of the RM aqueous phase, and as per the counter ion density levels in the R2 and R3 regions, and the charge density (surfactant head groups) levels in the R2 region. If NO˙ radicals reside in a spherical RM having an isotropic solvent (relative permittivity εr) with a point dipole at the core as pr, the Block Walker reaction field RR16 for NO˙ is:RR = (pr/RRM3)(ε ) | (6) |
) acting on the NO˙ radicals. We determined the aN values for RMs of different sizes. The changes in the micro-polarity of the
= 0 − (RRM − lB) region (bulk water) are negligible as a function of the RRM values (ω0 levels).8,16 Thus, the aN values vary as per the micro-polarity aspects of the R2 region. Therefore, the aN values, as a function of RRM, provide a measure of how aN would be as a function of
for a RM. We developed the ‘aNvs. ω0’ correlation, which is representative of the aNvs.
for the SDS RMs.
Due to the non-polarity attribute of the R1 region, the aN values for this region are negligible in comparison to those for the R2 and R3 regions. The rotational coefficient τc is particularly pronounced for the non-polar R1 region. Thus, the changes in aN for the R1 region, and τc for the R2 and R3 regions, as a function of ω0, are negligible. The aN and τc values can be accounted as:
| 〈Δτc〉 = p1〈Δτc〉 + p2+3〈Δτc〉 ≈ p1〈Δτc〉 | (7) |
| 〈ΔaN〉 = p1〈ΔaN〉 + p2+3〈ΔaN〉 ≈ p2+3〈ΔaN〉 | (8) |
The 〈aN〉 vs. ω0(
) profile was considered to assess the MPA(
) of a RM of a particular size.17Fig. 2 (inset) shows that this profile exhibits a maxima. The lower 〈aN〉 values are observed as
→ RRM (interface) and
→ 0 (core). The lower 〈aN〉 value at the ω0 ≈ 5 level justifies highly ordered forms of water in the R2 region, and presumably due to the relative population of the head groups and the counter ions across the interfacial region being significantly higher. Across the 5 < ω0 < 10 range, the 〈aN〉 values are higher with ω0, which is due to the increase in the volume of the R2 region having less ordered forms of water (in comparison to the highly ordered region at ω0 ≈ 5). The drop in the 〈aN〉 vs.
profile beyond the maxima, at the ω0 > 10 levels, is due to the increase in the bulk-type water content of the R3 region. At ω0 ≫ 10 levels, the bulk water content is higher, and the plateau region of the aNvs.
profile mostly accounts for the micro-polarity of the bulk-type water in the R3 region. Though these inferences that are made from the aNvs.
(ω0) profile provide an assessment of the MPA(
), these inferences are based on the assumption that: the surfactant charge density levels in the SASSs, as per ω0 levels, exhibit a linear relationship. The surfactant density level, according to the Debye–Stokes–Einstein equation is:
![]() | (9) |
). We considered a normalized value of 〈aN〉 as 〈aN〉/〈τc〉, which accounts for the variability associated with the degree of surfactant-packing in the SASSs for different ω0 levels.
The 〈aN〉/〈τc〉 vs.
(ω0) profile was examined to study the MPA(
). The slopes of this profile, (Δ(〈aN〉/〈τc〉)/Δ
), provide a direct estimate of how the MPA(
) varies as per the differences in the packing attributes of the SASSs. The slope value was higher at the ω0 > 15 levels, than that at the ω0 < 10 levels (Fig. 2, dotted lines). At the ω0 < 10 levels, the lower slope value is due to the ordered form of water in the R2 region, which could be interpreted from the aNvs.
(ω0) profile as well Fig. 2 (inset). At ω0 > 15 levels, RRM ≫ lB, the higher slope value is due to the plateau region of the ψ(
) profile that represents the bulk water in the region |
| ≤ 0 − (R − lB). Instead of the plateau region, as seen in the 〈aN〉 vs.
(ω0) profile, a higher slope value is seen for the 〈aN〉/〈τc〉 vs.
(ω0) profile as τc decreases with increase in ω0 – decrease in the SASS volume. A non-linearity in the 〈aN〉/〈τc〉 vs.
(ω0) profile – the deviation shown in a circle in Fig. 2 – demonstrates that the aqueous phase constitutes two spatially segregated regions, having markedly different micro-polarity behaviour. This non-linearity in the 〈aN〉/〈τc〉 vs.
(ω0) profile is pronounced at a critical distance,
c, and demarcates the two regions of a RM. Such a demarcation is the maxima (Fig. 2 (inset)) in the 〈aN〉 vs.
(ω0) profile; the degree of surfactant packing in SASSs is not considered in making this demarcation. Thus, the 〈aN〉/〈τc〉 vs.
(ω0) profile allows to reliably demarcate the two spatially separable R2 and R3 regions for SDS–hexane RMs,
ω0 ≈ 12. Though here, the slope values were similar across the ω0 < 10 and ω0 > 15 ranges, it could well be possible that the slope values could vary significantly due to marked differences in the SASS packing aspects.10
The 〈aN〉/〈τc〉 vs.
profiles were developed for the RMs (ω0 levels) having HRP enzymes at different concentration levels. In comparison to the 〈aN〉/〈τc〉 values for the RMs alone, the 〈aN〉/〈τc〉 values were significantly lower for RMs having HRP enzymes (Fig. 2). The lower values of 〈aN〉/〈τc〉 are due to the HRP-concentration dependent micro-polarity attributes. The differences in the slope values were almost an order of magnitude less with HRP in the RMs (Fig. 2), which strongly suggested that the RM water exhibits an ordered form not only in the R2 region but in the R3 region as well. Wherein, the bulk-type water is in negligible amounts in RMs having HRP enzymes. In order to examine the microstructural aspects of the ordered form of water, we studied the O–H/O–D stretching vibration spectroscopic (ATR-IR) absorbance line shapes. In terms of the HRP structural dynamics, there were significant conformational changes of the HRP enzymes in the RMs (ESI,† 4). The amide I peak of HRP in RMs shifted to lower frequencies, and suggested the transformation of the α-helix structures of HRP to β-sheet types. Based on the negligible changes in the amide III peak positions and shapes, the possibilities of HRP denaturation in the RMs were eliminated. In terms of the microstructural features of water, for the RM of the ω0 ≈ 20 level, the blue shifts of the OD- and OH-bands positions (Fig. 3a and b) were prominent for RMs with HRP. These shifts confirmed the ordered forms of water in the R2 and R3 regions. This ordered forms of water could be ascribed to the 〈aN〉/〈τc〉 values. In the cases where other shapes of RM are possible and, depending whether the RMs coalesce, the slope values are likely to be different. It would be interesting to see how the 〈aN〉/〈τc〉 vs.
(ω0) profile could be applicable for RM–enzyme systems to study the dependency of the MPA(
) on the surfactant-packing in a SASS with surfactants of different chemistries.
Footnote |
| † Electronic supplementary information (ESI) available. See DOI: 10.1039/c5sm01950h |
| This journal is © The Royal Society of Chemistry 2016 |