Missouri University of Science and Technology Scholars' Mine Chemistry Faculty Research & Creative Works Chemistry 1-1-1985 Self-Diffusion of Water in Polycrystalline Smectic Liquid Crystals Frank D. Blum Missouri University of Science and Technology Alapat S. Padmanabhan Rana Mohebbi Follow this and additional works at: http://scholarsmine.mst.edu/chem_facwork Part of the Chemistry Commons Recommended Citation F. D. Blum et al., "Self-Diffusion of Water in Polycrystalline Smectic Liquid Crystals," Langmuir, American Chemical Society (ACS), Jan 1985. The definitive version is available at http://dx.doi.org/10.1021/la00061a021 This Article - Journal is brought to you for free and open access by Scholars' Mine. It has been accepted for inclusion in Chemistry Faculty Research & Creative Works by an authorized administrator of Scholars' Mine. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. Blum, Padmanabhan, and Mohebbi 128 Langmuir, Vol. 1, No. 1, 1985 liquid crystals can also lead to uncertainties in the interpretation of the PFGSE results. In this study, we report the results of self-diffusion measurements on polycrystalline smectic liquid crystals of sodium 4 41'-heptylnony1)benzenesulfonate (SHBS) and water. This system was chosen for study because of the simplicity of the primary structure of the surfactant as compared to other double-tailed naturally occurring surfactants such as phospholipids. The SHBS-water system also exhibits structure, thermal behavior, and molecular dynamics that are quite similar to those found in phospholipid-water systems.17J8 Unlike phospholipids, the SHBS head group is simple and contains only one hydrophilic moiety. This results in a proton resonance for water that is narrow enough to use in self-diffusion measurements. In addition, it is possible to prepare the sample so that the effects of either small domain size or defects in the liquid crystals are insignificant. It is therefore possible to estimate the diffusion coefficient of the water parallel to the surface of the bilayer. For comparison, the temperature dependence of the self-diffusion coefficients of water in bulk and an ionic solution is also studied. Sodium nitrate is the salt chosen for this purpose because it is similar to the SHBS molecule in that it has the same cation and a singly charged anion with three oxygens. Experimental Section Sodium 441'-heptylnony1)benzenesulfonate was obtained from the University of Texas and recrystallized from n-butyl alcohol before use. Samples were prepared for self-diffusion measurements by weighing the dry surfactant in a 5-mm NMR tube and then adding a known amount of distilled water. The samples were then annealed at 80-90" C for 2 h to overnight in tightly capped tubes. This procedure converts almost all of the surfactant into planar smectic liquid crystal~.~~*'~ The compositionof the liquid crystals is ca.75 wt % SHBS and 25 w t % water." The solubility of the surfactant in water at room temperature is only 0.06 wt %, The sodium nitrate and cyclohexane used were reagent grade and used without further purification. The pulsed-field gradient spin-echo (PFGSE) NMR method was used to measure the self-diffusion coefficients. The measurements were made by proton NMR at 90 MHz on a JEOL FX-9OQ. The PFGSE pulse sequence used is as previously described21 and is similar to the Stilbs modificationzz of the Stejskal-Tannerz3method. The advantage of this modification is that the time between the 90' pulse and echo, 2A, is kept constant while the field gradient pulse time, 6, is varied. This also keeps the J-modulation and transverse relaxation effects constant, so that the effects of diffusion are probed separately. The resulting equation for the NMR intensity, A , is 21,zz A = A, exp[-y2G2D,&2(A- 6/31] (1) where A. is the intensity with 6 = 0, y is the gyromagnetic ratio of the nucleus under study, G is the field gradient strength, and Dlabis the self-diffusion coefficient in the laboratory frame. For an isotropicdy diffusing species a plot of In A vs. @,where /3 = P ( A - 6/3), should yield a straight line with a slope of -yzGzD. Simple exponential behavior was found for cyclohexane,used for gradient calibration, bulk distilled water, and aqueous sodium nitrate solutions. The water diffusion in bulk water and 5.3 M NaNO, solutions was studied for comparison with SHBS dispersions. The 5.3 M NaN03 solution has the same salt/water (17) Blum, F. D.; Miller, W. G. J . Phys. Chem. 1982,86, 1729. (18)Blum, F. D. Ph.D. Thesis, University of Minnesota, Minneapolis, MN, 1981. (19) Blum, F. D.; Russo, P. E., Neitering, K.; Miller, W. G., unpublished results. (20) Frames, E. I.; Puig, J. E.; Talmon, Y.; Miller, W. G.; Scriven, L. E.; Davis, H. T. J. Phys. Chem. 1980,84, 1547. (21) Cheever, E.; Blum, F. D.; Foster, K. R.; Mackay, R. A. J. Colloid Interface Sci., in press. (22) Stilbs, P. J . Colloid Interface Sci. 1982, 87, 385. (23) Stejskal, E. 0.; Tanner, J. E. J. Chem. Phys. 1965, 42, 288. W I/'I Figure 1. Normal proton NMR spectrum of a 75 wt % SHBS-25 wt % ,+', water dispersion. The sharp component is the water peak. I' <- Figure 2. Typical PFGSE spectra for a 50 w t % SHBS-50 wt % water sample at 25 "C. Only the water peak has significant echo intensity. mole ratio ( l / l O . l ) as the liquid-crystalline domains. Diffusion coefficients for the solutions were calculated from the raw data using log linear least-squares fits. The nonexponentialdecay seen in the liquid-crystallinedispersions was fitted to the theory by using the IMSL ZXSSQ routineF4 The criteria for the best fits were minima in the sums of the squares of the residuals. (In many cases multiple local minima were found in the fitting process and the values reported believed to represent the global minima.) The field gradient used had a value of ca. 0.05 T/m and was generated using the homospoil accessory. Typical spectra were taken with a 1000-Hzwindow, 2048 points, and a pulse delay of 4 s. The value of A used was 0.07 s, but the same results were obtained with A = 0.14 s. The sample temperature was maintained to f 1"C with a JEOL temperature controller. Samples were dowed to equilibrate for 15 min at each temperature before the spectra were run. Since most of the samples were biphasic, the position of the sample tube was kept constant so that the contribution of water in the isotropic phase was similar for each temperature studied. Results and Discussion A normal proton NMR spectrum of a 75 w t % SHBS-25 wt % water is shown in Figure 1. The sharp resonance is due to the water. The much broader resonances on either side of the water peak are due to the aromatic protons on the phenyl ring and the aliphatic protons on the tails. The broadness of the surfactant resonances is due to the anisotropic motion of the surfactant in the smectic phase and is similar to that observed in the 13C NMR.17 As can be seen, the water resonance is not completely resolved near the baseline. The spectrum for this sample is similar to that found for samples with lower water contents except for the contribution from water in the isotropic phase. The results of a PFGSE experiment on a 50 wt % SHBS-50 wt % water sample at 27 "C are shown in Figure (24) IMSL Fortran Subroutines Library IMSL, Houston, TX. Langmuir, Vol. I, No. I , 1985 129 Self-Diffusion of Water in Liquid Crystals I - - 1 L '9 Figure 4. Bilayer fixed axis system showing the orientation of the director at an angle B with respect to the laboratory (field gradient) axis. Table I. Best Fit D and A Values for Water Self-Diffusion from Ea 4 as a Function of the First B Value Used p > 3.7 x 10493 p > 2.0 x 10-5 s3 T,"C D, W 0m2/s D, mz/s 10 27 51 68 85 p~io~(~3) Figure 3. PFGSE data for a 50 wt % SHBS-50 wt % water sample aa a function of temperature: (e) 10,(M) 27, (A)51,(0) 68,( 0 )85 O C . The curves drawn are the best fits to the model and the vertical scales are shifted for display purposes. In the insert is shown the behavior at low p values for the (U) 27 "C SHBS sample, (---)bulk water, and (---) water in 5.3 M NaN03solution. 2 as a function of p. It is noted that, even though the surfactant resonances overlapped with the water resonance in the normal spectrum, the PFGSE experiment yields a well-resolved peak. This is because the T2'sof the surfactant are short enough that no observable echo is obtained in 2A from the surfactant peaks. The T2value for the water is long enough so that a strong echo is obtained. In Figure 3, the data for the PFGSE results for the 50 wt % SHBS-50 wt % water sample as a function of temperature are shown. The plot of In A vs. /3 does not yield a straight line. This is indicative of anisotropic diffusion. The dashed and center lines shown in the insert represent the behavior of water in bulk and sodium nitrate solution at room temperature, respectively. As can be seen, the contribution from the bulk water should be negligible at values of /3 of about 10 X lo4 s3 or possibly less depending on the amount of bulklike water present. At short gradient times the contributions from bulklike water in the isotropic phase varied. For longer gradient times the intensities were independent of composition for samples from 60 to 25 wt % water, provided that proper annealing conditions were met. In the annealed samples, most of the liquidcrystalhe material is found in large planar domains.18 The lack of dependence of the intensities on the amount of isotropic phase suggests that the liquid-crystalline domains are planar and static over the PFGSE time scale. Thus the diffusion behavior of water in the liquid-crystalline domains is constant over this range. It appears that the composition of the equilibrium liquid crystal is ca. 75 wt % SHBS-25 wt % water and the domain size is large enough that domain boundaries and/or imperfections are negligible or at least constant. A t higher water contents, the large fraction of isotropic water, plus the reduced domain size and increased curvature of the crystals, results in faster reorientation of the domains and the water in them, making interpretation of the results difficult. In the analysis of the data, we model the water layers in the smectic liquid crystals as infinite parallel plates. On a bilayer fixed coordinate system the diffusion tensor is diagonal with elements D,, = D, D, = D, and D,, = AD, where we define D as the diffusion coefficient parallel to 0.46 0.83 1.4 2.1 4.6 0.40 0.74 1.1 1.8 2.6 the bilayer surface. The geometry is shown in Figure 4. Since the water layer is only about 10 8, thick,lg we can neglect the restricted diffusion within the water layer perpendicular to the bilayer surface. However, if the water can penetrate the bilayer, leave the domain, or pass into another layer through a crystalline defect, an apparent perpendicular component will result and is represented by AD, where A is a constant representing the fraction of the parallel component seen perpendicular to the bilayer surface. In the NMR experiment, spins are labeled along the direction of the field gradient, which in this case is the laboratory 2 axis. The relationship between the bilayer coordinate system and the laboratory system is given by the Euler angles.2s This results in a laboratory diffusion coefficient given by DIab = ZTPDbiPTZ (2) where 2 is a unit vector in the 2 direction and extracts the laboratory 2 component, P is the transformation matrix containing the Euler angles, and Dbi is the bilayer fixed diffusion tensor. Insertion of Dlab result into eq 1yields, for a given domain, A = A, exp[-y2G2D((sin2e) - A(cos2e))] (3) where 6 is the angle between the static field (laboratory 2 axis) and the bilayer director. This is essentially the same formula derived by Callaghan et a1.26except they define their parallel and perpendicular diffusion components with respect to the director and ours me with respect to the bilayer surface. This is also the correct expression for use in oriented b i l a y e r ~ . ~ J A ~ Jsomewhat ~ - ~ ~ different approach to the same problem has also been taken by StejskaL2'3 In our polycrystalline samples the directors of the bilayers are randomly oriented and the appropriate average of eq 3 is A = A ( J r exp[-y2G2D((sin2e) + A(cos2@)]sin6 dB (4) where A,' also contains the appropriate normalization factors. Since the contribution from isotropic water is (25) Arfkin, G. 'Mathematical Methods for Physicists"; Academic Press: New York, 1970. (26) Callaghan, P. T.; Jolley, K. W.; Lelievre, J. Biophys.J. 1979,28, 133. (27) Stejskal, E. 0. J. Chem. Phys. 1965, 43,3597. (28) Stejskal, E. 0. Ado. Mol. Relaxation Process 1972, 3, 27. 130 Langmuir, Vol. 1, No. 1, 1985 Blum, Padmanabhan, and Mohebbi _a 10 o - ~ - * m E Y a -io 10 -n 10 1.6 d.0 d.2 d.4 3.6 1000/T Figure 5. Temperature dependence of water self-diffusion Coefficients for 50 wt % SHBS-50 wt % HzO, ( 0 )p > 20 X lo+ and (A)p > 3.7 X lo4 mz/s. For comparison those for (A)pure water and (0) 5.3 M NaN03 solutions are shown. difficult to quantify, the data were fitted first by using fl values greater than 3.7 X lo4 s3 and then greater than 2.0 X s3. Intensities from values of p less than 3 X lo4 s3 were believed to contain contributions from bulklike water. The results are shown in Table I. The best fits are also drawn in Figure 3 for the fl > 3.7 X lo6 s3 data. Except for the 10 "C data with = 2.0 X s3,all of the data showed "best fits" with A 0. This suggests that the diffusion perpendicular to the bilayer is negligible. It is therefore likely that domain boundaries or crystal imperfections are unimportant in these annealed systems. Water in smaller or imperfect liquid-crystalline domains will probably escape into the isotropic phase, diffuse rapidly, and only contribute to the intensities for the first few 0 values. As a result the experiment at longer values is only sensitive to water trapped in a single liquid-crystalline domain. The temperature dependence of both sets of data for the different values is shown in Figure 5 along with the results for water diffusion in bulk and in 5.3 M NaN03. The large value of D for the 85 "C data at the shorter value is probably due to a larger contribution of water which escapes the bilayers and biases the data. If one excluded this datum point, an energy of activation of 20.2 f 1.2 (SD) kJ/mol is obtained for both data sets. For comparison the diffusion coefficients for water in bulk and a 5.3 M NaN03 solutions are shown to be over an order of magnitude faster. The temperature dependence for pure water was found to be non-Arrhenius. Between 25 and 65 "C an apparent energy of activation of 20.3 f 1.1 kJ/mol was found. This compares with Mills previous results for pure water from which an energy of activation for diffusion of 19.6 (1-15 OC) and 17.6 (kJ/mol (15-45 "C) was determined.29 For the salt solution the temperature dependence was more or less Arrhenius with an activation energy of 17.0 f 1.0 kJ/mol. The fact that the diffusion of water in an aqueous salt solution is much faster than seen in the dispersions suggests that the geometry plays a major role in the reduce diffusion coefficients observed and not binding to the rather mobile counterions. Comparison with Other Systems. To the authors' knowledge, this is the first systematic study of the tem(29) Mills, R. J . Phys. Chem. 1973, 77, 685. perature dependence of water diffusion in smectic liquid crystals. This is partially due to the fact that many systems only form smectic liquid crystals over a very limited temperature range. In addition, it is often difficult to prepare the system so that the domain size is large. Rigaud et al.30used labeled water to measure the HTO self-diffusion coefficient in lecithin-water systems. Their results at 30% water suggest D = 0.9 X m2/s at 22 "C, which is just slightly higher than our results. The consistency of their results and ours suggests that the transport in the lamellar phase must be the dominant mechanism for water transport in their radiolabeling experiment. Results from Tiddy et al.13J4on perfluorooctanoates at 23 "C show the effects of sample preparation but suggest very rapid diffusion of water. Both D,, and D , in their studies on oriented samples are of the same order of magnitude as bulk water. Callaghan et al.15 have obtained D = 8.5 X 10-lo m2/s for D20 in a 70/30 potassium palmitate/D20 dispersion at 65 "C. Finally, Ukleja and DoanelGhave also measured a 70/30 potassium palmitate/H20 sample and estimated D to be 2.5 X and 1.6 X m2/s at 100 and 75 "C, respectively. These values, even though taken at similar water contents, show significantly faster diffusion than observed in this study. We suggest that this disagreement could be due to one of two possibilities. First, it is possible that the single-tailed surfactants used in the other studies are much more mobile than SHBS and consequently the aqueous region is also. This is possible considering that SHBS is a much larger molecule than single-chain surfactants. This effect may be seen in the lateral diffusion coefficients of surfactants at 24 "Ce9 The double-tailed surfactants in systems with 30-40% water are all about an order of magnitude slower than the single-tailed ones. Second, it is also possible that defects in the structure allow the water molecule to change domains over the course of the NMR experiment. This results in an apparent diffusion coefficient that is faster than that actually occurring in between the bilayers. Finally, we note that for our system we found that the diffusion perpendicular to the bilayer was negligible compared to that parallel to the bilayer. Results for oriented potassium palmitate/water (70/30) suggest a very similar result in that respect. Values of Dli/Dl are on the order of 25-35.15J6 This would certainly be consistent with our measurements although it is impossible to put more than a lower limit of about a factor of 10 on this ratio using unoriented samples. We believe our A = 0 results suggest that the water molecules responsible for the intensities at high fl values do not leave their domains and the domains do not reorient during the NMR experiment. Results such as those obtained in the perfluorooctanoate systems13J4are probably dominated by crystalline defects or small domains because the ratios from these systems are on the order of 2 or less. Conclusions Using the NMR PFGSE technique it is possible to measure the translational diffusion coefficients of water in polycrystalline smectic liquid crystals. For the SHBS system it is found that the self-diffusion coefficients are much slower than those found in other systems. It is found that the diffusion perpendicular to the bilayers is negligible compared to that parallel to the bilayers. The energies of activation for this diffusion is 20.2 f 1.2 kJ/mol and is slightly larger than bulk water or sodium nitrate solution. (30)Rigaud, J.-L.; Gary-Bobo, C. M.; Lange, Y. Biochem. Biophys. Acta 1972, 266, 12. Langmuir 1985,1, 131-135 We believe that these results are truly representative of the two-dimensional diffusion in the planar layers between the bilayers. Acknowledgment. We acknowledge the financial support of the donors of the Petroleum Research Fund, 131 administered by the American Chemical Society, Research Corporation, National Science Foundation, the Drexel University Graduate School, and Computer Center. We also thank Prof. C. Rorris for helpful discussions. Registry No. SHBS,67267-95-2;water, 7732-18-5. Kinetics of Displacement and Charge-Transfer Reactions Probed by SERS: Evidence for Distinct Donor and Acceptor Sites on Colloidal Gold Surfaces C. J. SandrofPt and D. R. Herschbach*t Exxon Research and Engineering Co., Annandale, New Jersey 08801 Received August 17, 1984. In Final Form: October 19, 1984 Both the electron donor W F and the electron acceptor TCNQ give large SERS signals upon adsorption onto colloidal gold particles, but only TTF displaces previously adsorbed pyridine, indicating that molecular donors and acceptors ockupy different surface sites. The acceptor (Lewis acid) site probably involves a reducible metal complex of Au+ while the donor (Lewis base) site may be associated with AuO. The kinetics for the charge-transfer reaction involving two distinct TTF oxidation states, TTF0.3+ TTF'.O+, can be explained by migration of the adsorbate from the donor to the acceptor site. - Introduction The degree of charge transfer between certain molecular adsorbates and metal surfaces can be determined from vibrational frequency shifts observed by surface-enhanced Raman scattering.l We have found that electron donors and acceptors based on tetrathiafulvalene (TTF) and tetracyanoquinodimethane (TCNQ) form with the noble metals particularly harmonious adsorbate/metal systems. These molecules absorb very strongly on silver and gold surfaces, transfer considerable amounts of charge, and give rise to large surface-enhanced Raman (SERS)signals. In experiments with these charge-transfer systems, we observed chemical transformations on gold colloidal surfaces involving two distinct oxidation states of adsorbed TTF a partially oxidized TTF species, TTF0.3+, disappeared in favor of the radical cation, TTF'.O+. Here we report a kinetic study of this surface oxidation and competitive adsorption experiments with pyridine, TTF and TCNQ. Our results can be rationalized by assuming that molecular donors and acceptors occupy different sites on the gold colloidal surface. The surface sites which act as acceptors or Lewis acids seem to involve a gold complex with the metal in a high oxidation state. These sites are readily reduced by proficient electron donors like 'ITF which have exceptionally low ionization potentials. The surface sites that serve as donors or Lewis bases behave like the neutral metal and readily give up charge to acceptors like TCNQ with sizable electron affmities. The donor sites, in contrast to acceptor sites, seem to possess substantial amphoteric character; they can behave as Lewis acids or bases depending on the difference between the work function of gold and the electron affinity or ionization potential of the adsorbate molecule. Thus TTF, when adsorbed as the partially oxidized TTF0.3+,binds to the Auo site, while TTF'.O+ attaches strongly to the Au+ site. The relative populations of and T"F1.'H do not remain constant in time after the initial adsorption onto the gold colloids. Rather, TTF0.3+converts to the radical cation with a fmliorder rate constant of 1 X lo4 s-l. The two-site model suggests that this interfacial charge transfer involves migration from a donor to an acceptor site. Experimental Section Aqueous colloidal suspensions consisting of 150-&diametergold particles at a concentration of 2 X lo1' cm-3 were prepared by the sodium citrate method of Turkevich et al.2 Adsorbates were introduced to 20 cm3 of the sol by adding 2 drops of a 5 X M solution. (Solventswere water for pyridine and acetone for the charge-transfer compounds.) The colloid turned from red to blue 30 min after the addition of pyridine, indicating partial aggregation of the sol particle^."^ Addition of TTF turned the sol to blue instantly, showing that TTF is much more effective at reducing the net (negative)charge on the colloidal surface than is pyridine. The very fast aggregation caused by "Fis consistent with the flocculation time predicted by Smoluchowski's6theory of diffusion-limited aggregation. For our dilute colloidal suspension, aggregation should occur in about 1s once the repulsive interactions between the charged particles are significantly reduced.' As in previous work? only after aggregation had occurred could strong SERS signals be seen. In contrast to electron donon like pyridine and TIT, the electron acceptor TCNQ did not cause any significant aggregation, and SERS spectra of TCNQ were obtained only after the colloid was aggregated by pyridine or TTF. (1) Sandroff, C. J.; Weitz, D. A.; Chung, J. C.; Herschbach, D. R. J. Phvs. Chem. 1983 87. 2127. 12) Turkevich, J.; Stevenson, P. C.; Hillier, J. Discuss. Faraday SOC. 1947. 11. 58. ( 3 ) Creighton, J. A.; Blatchford, C. G.; Albrecht, M. G. J. Chem. SOC., Faraday Trans. 2, 1979, 75, 790. (4) See: Creighton, J. A. In 'Surface Enhanced Raman Scattering"; Chang, R. K., Furtak, T. E., Eds.; Plenum Press: New York, 1982; "Metal Colloids". (5) Turkevich, J.; Garton, G.; Stevenson, P. C. J. Colloid Sci., Suppl. 1954, 1, 26. (6) Von Smoluchowski, M. Physic 2. 1916, 17, 557, 858; Z. Phys. Chem. 1917,92, 129. ~~ 'Present address: Bell Communications Research, Murray Hill, NJ 07974. Exxon Faculty Fellow from Harvard University. * 0743-7463/85/2401-0131$01.50/0 (7) 'Colloid Science"; Kruyt, H. R., Ed.; Elsevier: Amsterdam, 1952; p 278. 0 1985 American Chemical Society
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