.f‘r-‘A\g 3 ‘ 2‘; .\ «yr. .v -,-.;::._l;g.‘ « 4&3,“ ‘ Q <34. 97:5, 5- 1 9 sh- ,. § 4'. 44k» 2"» . A. ‘9.~c.,-;.,._. ‘ .4 ‘-;A’0 - b' v \. gullgr #2 w .. ..v~- ,; amighucwji‘xur- q . a sh .’-A:.‘ . 1-?" 'u YI'- ‘ . .t. czu‘v,:.:‘- '¢.. . : 32-3-, ,3“. . ._. ‘. .'.v... M4??? {r /' ‘a- ”My '1 ‘ _. 3,4 . C. ‘ A my.» I:.}fI-¢-,v{ é! >,v ‘ #34 W24: V,‘ I‘- A" . C" 1 l‘)‘ . ‘ v../ . 4 3‘ ‘1 ’43-" , w 4’ {mfg/z), A'JIEVLB’RJ: ”1§u’.1; ‘ “fife”: "x, i‘ Z‘"::J":.;.}':'. ” ‘ “'91"x~.~ by I’ ‘ ‘(u 4%)": 43' '2'); v I ‘4! of); (A, ‘ $7? ('4') n f .7 2% ”WWW“ ‘- ‘ n9: :2 z. m,» ‘ {33315.},43' a :72"? \u . -l “6‘13 " '1' ,: 4 \ Emu» ’.‘ ~O . 2IW3”"”‘ HGI AN STATE UNIVERSITY LIBRAR RIES __IIIIIIIIIIII|I III II III IIIIIIIII 3 1293 00550 3432 LIBRARY Michigcn Stat. UniversitL This is to certify that the dissertation entitled Modeling the sorption of water, and the effect of sorbed water on the solubility and diffusivity of oxygen in an amorphous polyamide. presented by Ruben J. Hernandez-Macias has been accepted towards fulfillment of the requirements for Ph. D. Chemical Engineering degree in Major professor Date February 23, 1989 MSU is an Affirmative Action/Equal Opportunity lrutitun'on 0-12771 IV1£3I_J RETURNING MATERIALS: Place in book drop to LiaaAhias remove this checkout from —c—. your record. FINES will be charged if book is returned after the date stamped below. "@3413 ‘ FE? I 3 i; . , 4 _ - it mm (+3 , III“ 4 0 o ; “(N u 4 , ' I; at: H ' rd: v.1 .3 .II‘ ‘ AUG 2 a coon 8 WI" 3 a - 1 2000 Wt ‘ 3» i??? “ " :9 2 a 1m MODELING THE SORPTION OF WATER, AND THE EFFECT OF SORBED WATER ON THE SOLUBILITY AND DIFFUSIVITY OF OXYGEN IN AN AMORPHOUS POLYAMIDE. by Ruben J. Hernandez A DISSERTATION Submitted to Michigan State University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Department of Chemical Engineering 1989 5457fi2I ABSTRACT MODELING THE SORPTION OF WATER, AND THE EFFECT OF SORBED WATER ON THE SOLUBILITY AND DIFFUSIVITY OF OXYGEN IN AN AMORPHOUS POLYAMIDE. by Ruben J. Hernandez Glassy amorphous polyamides are part of a new kind of polymeric material that have excellent physical and mechanical properties. These materials are non-crystalline and show interesting mass transfer behavior with vapors and gases. In the case of Nylon 61/6T, a totally amorphous polyamide recently developed, its interaction with water vapor affected the transport of oxygen. Sorption, permeation, FTIR spectroscopy, density and thermal relaxation studies have been applied to describe the behavior of the system amorphous polyamide/water and amorphous polyamide/water/oxygen. The dual-mode sorption model presented in this study was found to describe accurately the sorption of water by the amorphous polyamide, over a broad range of water activity and predicted clustering of the sorbant. The Langmuir equation was used to describe the chemisorbed solute and the Flory-Huggins equation was used to describe the volume fraction of water that is not chemisorbed. The sorbed molecules of water in the glassy amorphous polyamide, showed a depression in the oxygen permeability values as a function of polymer moisture content. The oxygen permeability behavior was analysed in terms of the multiplicative effect of a mobility and solubility term. The analysis of the oxygen solubility values within the polymer/water system, provided a complementary framework for the dual-mode sorption model. Copyrigth by Ruben J. Hernandez Macias 1989 To Natalia and Daniel Federico. Let us hold the torch of Science even if it is only for a 'second. ACKNOWLEDGMENTS I wish to thank the Department of Chemical Engineering, the Division of Engineering Research and the School of Packaging for offering me the support and facilities to carry out these studies. I also want to acknowledge the grant received from E. I. DuPont de Nemours and Company Inc. I want to thank Drs.E. A. Grulke and J. R. Giacin for continuous advise and support. I am grateful to my Guidance Committee members Drs. K. Jayaraman, L. T. Drzal, from the Department of Chemical Engineering, and Dr. C. Talkowski from E. I. DuPont Co. I also want to thank V. Kalankyar, Dr. P. Blatz from E. I. DuPont Co. and Dr. J. DeLong, from The Division of Engineering Research for helping to run some tests. At last, but not least, my deepest appreciation to my parents Vicente Hernandez and Dolores Macias, and to my wife Alicia Gardiol. I could not have done it without them. LIST OF CONTENTS PAGE LIST OF TABLES. . . . . . . . . . . . . . . . . . . . . ix LIST OF FIGURES . . . . . . . . . . . . . . . . . . . . xi INTRODUCTION. . . . . . . . . . . . . . . . . . . . . . 1 References. . . . . . . . . . . . . . . . .. . . . 7 CHAPTER I. THE EVALUATION OF THE AROMA BARRIER PROPER- TIES OF POLYMER FILMS. . . . . . . . . . . . . . . 11 INTRODUCTION. . . . . . . . . . . . . . . . . . . . 11 Modeling Considerations. . . . . . . . . . . . . . .17 Permeability Measurements. . . . . . . . . . . . . .20 Isostatic Method. . . . . . . . . . . . . . . .20 Quasi-isostatic Method. . . . . . . . . . . . .25 Sorption Measurements. . . . . . . .. . . . . . L . 27 Polymer Films. . . . . . . . . . . . . . . . . 27 Polymer Spheres. . . . . . . . . . . . . . . . 28 Desorption Measurements. . . . . . . . . . . . . . 3O Solubility Coefficient. . . . . . . . . . . . . . . 32 Diffusion Coefficient. . . .'. . . . . . . . . . . .32 METHODS. . . . . . . . . . . . . . . . . . . . . . .34 Determination of Permeation Methods. . . . . . . . .34 Isostatic procedure. . . . . . . . . . . . . . 34 Quasi-isostatic Procedure. . . . . . . . . . . 37 Sorption Measurements. . . . . . . . . . . . . . . .39 APPLICATIONS. . . . . . . . . . . . . . . . . . . . 42 Quasi-isostatic Procedure. . . . . . . . . . . 42 Isostatic Procedure. . . . . . . . . . . . . . 46 vi Sorption Procedure. SUMMARY. REFERENCES. CHAPTER II. THE SORPTION OF WATER VAPOR BY AN AMORPHOUS POLYAMIDE. ABSTRACT. INTRODUCTION. DUAL MODE SORPTION MODELS. Model for Gas Sorption in Glassy Polymers. Models for Polar Systems at High Solute Activities. CLUSTERING OF SOLUTE MOLECULES. Modified Dual Mode Sorption Model. EXPERIMENTAL METHODS. Polymer Films. Equilibrium Sorption Data. Density Experiments. Fourier Transform Infrared Spectroscopy. DSC and Dielectric Experiments. RESULTS AND DISCUSSION Equilibrium Sorption Isotherm. Parameter Estimation for Equation 8. Sensitivity Coefficients. Clustering Analysis. Physical Evidence for Solute Binding. Relaxation Temperatures. Density Data. vii .47 .49 50 56 56 57 .58 58 .59 62 .64 65 65 66 66 66 67 .67 67 7O .74 77 .78 83 .84 Proposed Mechanism for Effects of Water Sorption on Physical Properties of Amorphous Polyamide. . . . . . . . . . . . . . . . . . . 87 LITERATURE CITED. . . . . . . . . . . . . . . . . . 88 CHAPTER III. EFFECT OF WATER CONTENT ON THE SOLUBI- LITY, DIFFUSION AND PERMEABILITY IN NYLON 6I/6T. . . . . . . . . . . . . . . . . . . . . 93 INTRODUCTION. . . . . . . . . . . . . . . . . . . . 93 Oxygen Permeability as Function of Polymer Water Activity. . . . . . . . . . . . . . . . .95 Oxygen Solubility and Diffusion coefficient. . 96 EXPERIMENTAL METHODS. . . . . . . . . . . . . . . . 99 Polymer Films. . . . . . . . . . . . . . . . . 99 Equilibrium Sorption Data. . . . . . . . . . . 99 Oxygen Permeability Studies. . . . . . . . . .100 RESULTS AND DISCUSSION. . . . . . . . . . . . . . .102 Equilibrium Sorption isotherms. . . . . . . . 102 Calculation of Oxygen Solubility. . . . . . . 108 Conditions for Applying Eqn. 10 . . . . . . . 110 Permeability Data . . . . . . . . . . . . . . 113 Oxygen Solubility. . . . . . . . . . . . . . .123 Oxygen Diffusion Coefficient. . . . . . . . . 132 CONCLUSIONS . . . . . . . . . . . . . . . . . . . 135 SUMMARY. . . . . . . . . . . . . . . . . . . . . . 136 REFERENCES. . . . . . . . . . . . . . . . . . . . .138 APPENDIX A. . . . . . . . . . . . . . . . . . . . .140 APPENDIX B. . . . . . . . . . . . . . . . ... . . .149 viii CHAPTER TABLE 1 1 10 LIST OF TABLES Permeability constants and lag time diffusion coefficients for toluene in selected polypropylene based structures. Values for eqn.(23) obtained for the system Oxygen/Nylon 6I/6T, at 22.00C and water activity = 0.441. Models for polar system at high solute activities. Experimental data at 23 OC. Langmuir and Flory-Huggins volume frac- tion contributions. Amide I, Amide II and CH absorption frequencies. Intensity ratios of Amide I and Amide II with respect to CH bands. Water polymer isotherm at 5 0C Water polymer isotherm at 23 oC Water polymer isotherm at 42 OC Values of X_, K and B as a function of temperature. Water activity values at the onset of cluster formation. Solubility of oxygen in Nylon 6I/6T as a function of pressure at 24 oC. Diffusion, solubility and permeability values of oxygen at 11.9 0C. Diffusion, solubility andopermeability values of oxygen at 22.0 C. Diffusion, solubility andopermeability values of oxygen at 40.3 C. Values of the constants for eqn. 6 ix PAGE 43 48 60 68 73 80 80 103 104 105 109 109 111 114 115 116 123 11 12 13 APPENDIX B Experimental of oxygen at Experimental of oxygen at Experimental of oxygen at and calculated solubility 11.9 C. and calculated solubility 22.0 00. and cglculated solubility 40.3 C. Activation energy as a function of Aw_ 126 127 128 173 CHAPTER FIGURE 1 1 LIST OF FIGURES Transmission rate profile curve for toluene vapor Bhrough oriented PET at 90 ppm and 23 C. Generalized transmission rate profile curve by quasi-isostatic method test. A plot of M /M¢,vs. t 1/2 for d-limone- ne by high density polyethylens/sealant structure at 1.5 ppm and 20.5 C. Schematic diagram of the isostatic test apparatus. Schematic diagram of the quasi-isostatic tets apparatus. Schematic diagram of the electrobalance test apparatus. Effect of penetrant concentration onothe transmission of toluene vapor at 23 C through coextruded OPP. Effect of penetrant concentration 8n the transmission of the toluene at 23 C through biaxially oriented polypropylene. Experimental sorption values and Flory- Huggins fitting. Experimental sorption values and Flory- Huggins fitting at low activity values. Best fit for the Langmuir-Flory-Higgins model. Sensitivity coefficients as a function of activity. Clustering function as a function of water act1v1ty. Typical FTIR spectrum of the amorphous polyamide recorded at room temperature. Spectrum region of Amide II as a function of activity. xi PAGE 21 26 29 35 38 41 44 45 69 71 72 75 76 79 81 APPENDIX B 10 11 12 l3 14 Glass transition temperatures as a func- t1on of act1v1ty. Density as a function of activity. Oxygen permeability apparatus. Water sorption isotherms at 5 C, 23 OC and 42 C. Values of K and B of the Langmuir equation. Solubility of oxygen as a function of partial pressure at 240C. Oxygen permeabiligy values at 11.9 0C, 22. 0 OC and 40. 3 C. Diffusion coefficient values at 11.9 0C, 22.0 C and 40.3 C. Oxygeg solubilityO values at 11.9 0C, 22. 0 C and 40. 3 OC. Solubility and diffusion coefficient of oxygen at 11. 9 OC. Solubility and diffusion coefficient of oxygen at 22.0 C. Solubility and diffusion coefficient of oxygen at 40.3 C. Oxygen solubility at 11.9 0C as function of a w Oxygen solubility at 22.0 0C as function of a w Oxygen solubility at 40.3 0C as function of aw. Activation energy as a function of water activ1ty. Activation energy versus pre-exponential term for the diffusion of oxygen in the amorphous nylon, xii 85 86 101 106 107 112 117 118 119 120 121 122 129 130 131 134 174 INTRODUCTION The presence of sorbed or diffusing low molecular weight penetrants in polymer solids often has a marked effect on material properties. The way in which the penetrant is sorbed and distributed within the polymeric matrix can be expected to affect the penetrant mobility, the local polymer chain segmental mobility, and related parameters such as free volume distribution and eventually, efficiency of free volume utilization [1]. Two major classes of polymer properties that are controlled by the segmental mobility of the polymer chain are the transport and mechanical properties. The mobility of polymer chains is determined by the polymer structure and its morphology, and is affected by sorbed molecules and the mode of sorption. For a given polymer structure, the transport and mechanical properties will therefore depend on the precise interaction and the sorbed penetrant. Penetrant molecules are sorbed within the polymer in different modes [2]. The nature of interactions between penetrant and polymer is an important factor in the manner in which the molecules of penetrant are distributed within the polymeric matrix. Particular sorption modes of interest are the localization of penetrant molecules at specific polymer sites that may be more or less active, randomly 1 dispersed (free) penetrant molecules and sorbed-sorbed molecules resulting in clustering formation. The total penetrant sorption process will probably be the result of the combination of these three different mechanisms or sorption modes. The specific sorption process may be described as a function of penetrant concentration or activity, temperature, and time to reach equilibrium, as well as the composition of the penetrant-polymer system. Therefore, polymer structure, availability of specific active sites of interaction in the polymer, chain stiffness or segmental mobility, plus the physico-chemical characteristics of the penetrant (gas, water or organic compounds) determine the mode and mechanisms of sorption and transport of the penetrant within the polymer. A very common model that describes sorption of penetrants in glassy polymers was introduced by Matthes in 1944, using the concept of the dual-mode sorption mechanism [3]. He combined a Langmuir and a Henry's law type expression to describe the sorption of water by a cellulosic material. A large number of other investigators have extended the use of this model to describe the sorption of fixed gases (most of them above the critical temperature) such as C02, CH4, C2H6’ etc., by different polymers, [4]-[12]. This model has also been used to correlate the sorption of mixed gases in glassy polymers [13]. Although this model based, on Langmuir and Henry equations, may well describe the sorption of gases by polymers, it actually overpredicts the sorption of vapors by polymers, and is not able to predict the cluster formation of the absorbed molecules. Another important characteristic of this model is that Henry's law of dissolution does not distinguish solutions containing only molecules of ordinary size from those solutions of very large molecules. Flory [14-15] and Huggins [l6],derived an equation for the activity coefficient of a solute in a polymer, as a function of volume fraction of the solute. At low activity values, this equation underpredicts the sorption of vapor by polymers and predicts clustering of the solute within the polymer in the whole range of solute activity. The formation of clusters can be predicted by applying the clustering function to a specific model describing the sorption behavior of a penetrant-polymer system. The clustering function ([17], [18]) is a monotone, increasing function of the probability of finding molecules of the same kind close to one another. Orofino et al., [19], applied the clustering function to several polymer-water systems obeying Flory-Huggins thermodynamics. However, when the clustering function is applied to the Flory-Huggins model, clustering is predicted in the whole range of vapor activity. Polyamides, as most polymeric materials, sorb both water and organic vapors. In the past years polyamide-water systems have been the subject of a number of studies, [19]-[23]. The amide function of the polymer participates in hydrogen bonding, where the hydrogen on a nitrogen atom associates with the carbonyl oxygen atom of an adjacent molecule. Such non-covalent bonds are relatively strong (8 kcal/mol), and serve to provide a cross-link network between polymer molecules. They exist in the amorphous as well as in the crystalline regions of polyamides [20]. Disruption of hydrogen bonding in the noncrystalline region is necessary for a solvent to attack polyamides and is a major factor in the mechanism of absorption of molecules that surround the polymer [24]. Puffr and Sabenda [23] suggested a mechanism of water sorption into Nylon 6 at room temperature, which involved two neighboring amide groups in water-accessible regions forming a sorption center. This sorption center could accommodate up to 3 water molecules, involving hydrogen bonding between adjacent amide groups. Additional sorbed water molecules may be accommodated via a clustering mechanism. Papir et al. [25], working also on the nature of the absorption of water in Nylon 6 confirmed the hypothesis of Puffr and Sabenda, in that two "types" of water, tightly bound and loosely bound, can exist within the polymer matrix. Fourier transform infrared (FTIR) spectrosc0py is considered a powerful tool for polymer characterization, [27]-[28]. In the present study FTIR spectroscopy has been employed to glean information related to the nature, strength, and number of intermolecular forces occurring between sorbed water and an amorphous polyamide. The FTIR spectroscopy studies focused specifically on the detection of possible changes in hydrogen bonding between N-H and carbonyl groups. This was done by observing the vibrational modes of the amide group, consisting of the Amide I and Amide II bands, as a function of polymer water content. In recent years, a totally amorphous polyamide has been developed, the 6I/6T (70/30) amorphous nylon [29]. Preliminary studies on the effect of water sorption on the barrier properties of this polymer showed atypical behavior, as compared to semicrystalline nylons under the same conditions. For example, oxygen permeability in Nylon 66 increases as a function of moisture content of the polymer, while it showed a decrease in the amorphous nylon 6I/6T. Further, the tensile modulus for Nylon 66 decreases as a function of moisture content, while the tensile modulus for the amorphous nylon increases with increase in moisture content. The intriguing behavior of the water-nylon systems has made evident the need of a model that would provide a more quantitative description of the mechanism of the sorption process of water by polar polymers. The thrust is also to look for a model that may be used to explain the sorption and diffusion behavior of organic vapor penetrants in polar polymer. This is important not only for theoretical but also for practical reasons. Most polymer materials are normally exposed to vapors (water or organic) and the interaction that takes place affects the performance of such polymer as is the case for example, in polymer composites or product-package interactions. The present research work has addressed, therefore, two major objectives: I. To complete an experimental description of the equilibrium sorption process of the binary system water- amorphous polyamide, and to describe the experimental behavior of the diffusion and solubility of oxygen within the system water-amorphous polyamide. II. To develop a theoretical framework for interpreting the mechanism of sorption equilibrium of the binary system water-polymer, and of the three components system oxygen- water-polymer. It is expected that the conclusions of this work will be valid to describe the equilibrium soption of organic compounds-polymer systems. REFERENCES Sfirakis, A. and C. E. Rogers, Effects of Sorption Modes on the Transport and Physical Properties of Nylon 6, Polym. Eng. Sc., 20, 4, 294-299 (1980). Rogers, C. E., Physics and Chemistry of the Organic Solid State, Vol II, Chapter 6, Interscience, N. Y. (1965). Matthes, A., Zur Theorie des Quellungsvorganges an Gelen, Kolloid-Z. Z., 108, 79-94 (1944). Michaels, A. S., W. R. Veith and J. A. Barrie, Diffusion of Cases in Polyethylene Terephthalate, J. Appl. Phys., 35, (1), 13-65 (1963). Veith, W. R. and J. A. Eilenberg, Gas Transport in Glassy Polymers, J. Appl. Polym. Sc., 16, 945-954 (1972). Veith, W. R., J. M. Howell and J. H. Hsieh, Dual Sorption Theory, J. Membr. Sc., 1 (1976) 177-220. Koros, W. J., and D. R. Paul, Transient and Steady State Permeation in Polyethylene Terephthalate, J. Polym. Sc. Phys. Ed., 21, 441-465 (1983). 10. 11. 12. 13. Kulkarni, S. S. and S. A. Stern, The Diffusion of C02, CH4, C2H4 and C3H8 in Polyethylene at Elevated Pressures, J. Polym. Sc. Phys. Ed., 21, 441-465 (1983). Barrie, J. A. and P.S. Sagoo, The Sorption and Diffusion of Water in Epoxi Resins, J. Membr. Sc., 18 (1984) 197- 210. Barrer, R. M., Diffusivities in Glassy Polymers for the Dual Mode Sorption Model, J. Membr. Sc., 18 (1984) 25- 35. Koros, W. J., R. T. Chern, V. Stannett and H. B. Hopfenberg, A Model for Permeation of Mixed Cases and Vapors in Glassy Polymers, J. Polym. Sc. Phys. Ed., 19, 1513-1530 (1981). Uragami, T., H. B. Hopfenberg, W. J. Koros, D. K. Yang, V. Stannett and R. T. Chern, Dual-Mode Analysis of Subatmospheric-Pressure CO2 Sorption and Tramsport in Kapton H Polyimide Film, J. Polym. Sc. Phys. Ed., 24, 779-792 (1986). Koros, W. J., Model for Sorption of Mixed Cases in Polymers, J. Polym. Sc. Phys. Ed., 18, 981-992 (1980). 14. 15. 16. 17. 18. 19. 20. 21. Flory, P. J., Thermodynamics of High Polymers Solutions, J. Chem. Phys., 10, 51 (1942). Flory, P. J., Principles of Polymer Chemistry, Cornell University Press, Ithaca, NY, (1953). Huggins, M. L., Thermodynamic Properties of Solutions of Long-Chain Compounds, Ann. NY Acad. Sci., 42, 1 (1942). Zimm, B. H. and J. L. Lundberg, Sorption of Vapors by High Polymers, J. Phys. Chem., 60, 425-428 (1956). Lundberg, J. L., Clustering Theory and Vapor Sorption by High Polymers, J. Macrom. Sci. Phys., B3 (4), 693-711 (1969). Orofino, T. A., H. B. Hopfenberg and V. Stannett, Characterization of Penetrant Clustering in Polymers, J. Macrom. Sci. Phys., B3 (4), 777-788 (1969). Cannon, C. G., Spectrochim. Acta, 16, 302 (1960). Starkweather, H. W., The Effect of Water on Some Properties of Oriented Nylon, J. Macrom. Sci. Phys., B3 (4), 727-736 (1969). 22. 23. 24. 25. 26. 27. 28. 29. 10 Skirrow, G. and Young K. R., Sorption, Diffusion and Conduction in Polyamide-Penetrant systems: I. Sorption Phenomena, Polymer, 15, 771-776 (1974). Puffr, R. and J. Sabenda, On the Structure and Properties of Polyamides: XXVII. The Sorption of Water in Polyamides. J. Polym. Sc. Part C, 16, 79-93 (1967). Kohan, M. I., Nylon Plastics, J. Wiley, N.Y. (1973). Papir, Y. S., Kapur, S., C. E. Rogers and E. Baer, Effect of Orientation, Anisotropy, and Water Vapor on the Relaxation Behavior of Nylon 6 From 4.2 to 300 0K, J. Polym. Sc. A-2, 10, 1305 (1972). Koening, J. L., Fourier Transform Infrared Spectroscopy of Polymers, Advances in Polymer Science, 54, 87 (1984). Painter, P. C., M. M. Coleman and J. L. Koening, Theory of Vibrational Spectroscopy with Application in Polymers, J. Wiley, N. Y. (1981). Siesler, H. W. and K. Holland-Moritz, Infrared and Raman Spectroscopy of Polymers, M. Dekker Inc. N. Y. (1980). Blatz, P. and C. Talkowski, Personal Communication (1987). CHAPTER I THE EVALUATION OF THE AROMA BARRIER PROPERTIES OF POLYMER FILMS** Key Words: Aroma barrier, organic penetrants, diffusion, sorption, permeability, barrier polymer films, polypropylene, high density polyethylene. INTRODUCTION The shift from absolute barrier type packages, such as cans and bottles, to semi-permeables polymeric packaging systems has created a need to develop a better understanding of the transport of gases, vapors, and other low molecular weight moieties through polymer films. The transport of permeants such as oxygen, carbon dioxide and water vapor through polymer structures has been the subject of numerous investigations, and standard test methods are availables for determining transmission rates for these permeants (ASTM E96-66, ASTM D3985-81). ** This review paper was published in the Journal of Plastic Film and Sheeting. Volume 2, 187-211 (1986). 11 12 In contrast, while the transport of organic penetrants through packaging materials have been the subject of several recents investigations, there is a paucity of data available in this area. This paper will, therefore, focus on the various procedures developed for quantifying the rate of diffusion of organic penetrants through barrier membranes and describe in detail the specific procedure employed in the studies reported. Pye et al. (1976) described a continuous or isostatic procedure for measuring the diffusivity properties of polymer membranes that employed two gas chromatographs connected to a cell. One chromatograph was equipped with flame ionization detection and the second was based on a thermal conductivity cell. This was achieved by incorporating gas sampling valves in the carrier gas stream. With multiples detectors, the authors were able to study the diffusion of gases as well as organic vapors through polymer films. The system described by Pye et al. also included a gas and organic vapor mixture generating apparatus. Niebergall et al. (1978) also described a method for determining the difusivity values of the various organic penetrant/barrier film systems based on the isostatic procedure of test. The apparatus developed by these authors was designed to allow measurement of transmission rates for mixtures of organic vapors through barrier structures as 13 function of penetrant concentration, temperature and relative humidity. Zobel (1982) has also reported an isostatic method for measuring the permeability rate of films to organic vapors at low penetrant concentrations and, in recent articles, described a modification of the previous procedure which incorporated an absorption/desorption cycle, Zobel (1984, 1985). An isostatic procedure was described by DeLassus (1986), who studied the transport of d-limonene vapor through a series of polymer films typically used for food packaging. The author employed techniques on photoionization and atmospheric pressure ionization, Caldecourt and Tou (1985), for quantifying the permeation rate of d-limonene through the respective test films. Hernandez (1984) and Bauer et a1. (1986) also employed an isostatic procedure for determining the diffusion coefficient from permeability data of organic penetrants through polymer membranes. Analysis of permeated vapor was based on a gas chromatographic technique with flame ionization detection. Smith and Adams (1981) and Pasternak (1970) also reported permeability studies using a continous flow or isostatic method. Hilton and Nee (1978) developed an accumulation or quasi- isostatic test method for determining the permeability of organic vapors through barrier films, where the polymer film was mounted in a permeability cell above a reservoir of liquid permeant. The permeant vapor which has diffused 14 through a barrier film accumulates in the low concentration chamber of the test cell and was quantified by a gas chromatographic technique. A similar procedure for determining the permeability of organic vapors through barrier films was reported by Murray and Dorschner (1983). In a more recent publication, Murray (1985) expanded on this procedure and reported a number of examples for which the test apparatus was employed to determine the relative permeation rates of organic vapors through barrier structures. These methods are limited, however, to determining the transmission rates and permeability constant values at only one concentration given by the saturation equilibrium vapor pressure of the liquid penetrant at a given temperature. Gilbert et a1. (1983) also evaluated the barrier properties of polymeric films to various organic penetrants by a quasi- isostatic test procedure. To provide a constant concentration or partial presure gradient, wherein the net movement for the penetrant is from high partial pressure to low partial pressure, these author continually flowed a penetrant vapor stream through the high concentration chamber of the permeability cell. Baner et al.(1984) described a test apparatus based on the quasi-isostatic procedure for determining the diffusion of organic penetrant through polymer films, and also employed the continous flow of organic vapor through the high concentration cell chamber 15 to assure a constant vapor gradient. A chromatographic method was developed for the permeation rate measurements. Peterlin (1975) has studied the concentration dependence of the diffusion and permeability coefficient in a homogeneous membrane. In addition to the permeation methods described above, the transport of small molecules in polymers can also be evaluated by absorption-desorption methods. Fujita (1961) has decribed the general behavior of sorption and permeability of organic vapors. Bischoff et a1. (1984) have studied the effect of the polymer molecular orientation on the sorption of toluene by high density polyethylene (HDPE). Applying a succesive sorption method, Choy et al. (1984) studied the sorption and diffusion of toluene vapor in oriented polypropylene (OPP) film of varying draw ratios. By this method the authors obtained values of the difussion coefficient (D), solubility (S) and permeability (P) of the polymer, as well as information on the structure and molecular dynamics of OPP as a function of draw ratio. Berens (1978) described vapor sorption studies on polyvinyl chloride (PVC) powders as a mean of studying the transport of low molecular weight organic molecules in glassy polymers. For a detailed rewiew of the sorption method for measuring the sorption and diffusion coefficients of small molecules in polymers, the reader is referred to Berens (1978) and references cited therein. 16 Bauer (1986) applied the sorption equilibrium method by using a electrobalance to studiy the sorption and diffusion of toluene vapor in OPP and Saran (trademark of the Dow Chemical Company for its polyvinylidene chloride and copolymers) film samples as a function of penetrant concentration. Knowledge of the diffusion, solubility and permeability of organic penetrants through polymer structures has both theoretical and practical importance. In terms of theoretical importance, such studies can aid developing a better understanding of the mechanism of diffusion of organic penetrants through polymer membranes and particularly for the case of permeant molecules that have strong interaction with the polymer. The diffusion and solubility of organic penetrants will be of practical importance for example in the case of packaged goods, when product quality is related to the transfer of organic vapors when polymers materials are used. For example, the aroma barrier properties of a package system are important, since the retention of product aroma constituents and the exclusion of sensorially objectionable organic molecules from the package external environment contribute to the keeping quality and, thus, the shelf life of the product. Further, knowledge of the aroma barrier propeties of polymeric packaging materials can provide a mean of designing and/or selecting a barrier structure for a specific end use application. 17 Knowing solubility data for essential flavor ingredients in certain polymers is of paramount importance in avoiding the effect of "flavor scalping". For example, d-limonene, a common flavor component present in foods has a relative high solubility in HDPE, Mohney et al., (1986). Since the flavor compounds are normally present in low concentration in the foodstuffs, there is a potential risk to "lose" aroma constituent due to absorption by the package polymeric material. MODELING CONSIDERATIONS Diffusion (D) and solubility (S) coefficients are usually determined by observing the change in weight (increase or decrease) of a polymer sample during a sorption process. Such a process can involve the absorption or the desorption of low molecular weight moieties by the polymer sample. Diffusion and permeability (P) values can be obtained from permeability experiments where the transport of a permeant through a polymer membrane is continually monitored (isostatic procedure) or by quantifying the amount of the penetrant that has passed through the film and accumulated as a function of time (quasi-isostatic procedure). The basic equations for decribing the diffusion process are Fick‘s first and second law of diffusion (Crank, 1975). 18 dc F = - D (1) dx and dc d dc —-=-—-[D—] (2) dt dx dx Where F is the flux or the rate of transfer of penetrant per unit area, expressed as a mass of diffusant per unit area per time; c is the concentration of the penetrant in the film, expressed in the same unit of mass of diffusant per unit of volume or mass of the polymer; D is the mutual diffusion coefficient, in unit of (length)2/time; t is time and x is the length in the direction in which the transport of the penetrant molecules occurs. To obtain the flux F, or the diffusion coefficient D, equation (1) or (2) must be solved together with the initial and boundary conditions associated with the experiment to give the desired values. Solution to eqn. (2), and respective initial and boundary conditions, can be performed analytically or numerically to calculate D. In the first case a power-series of solutions usually arises when solving for the unsteady state case. 19 In this paper, simplified equations related to the first approximation of the power-series are presented (Crank, 1975). It should benoted that when the diffusion coefficient is calculated using these equations, only approximated values will be obtained. More accurate estimation of this parameter D, can be carried out by using, for example, a non linear maximum likelihood sequential method based on the Gauss linearization method (Beck and Arnold, 1977). To relate the concentration of the penetrant in the polymer, (solubility), to the penetrant concentration in the gas or vapor phase in equilibrium with the polymer, Henry's law is assumed S.p (3) 0 ll Where p is the partial pressure of the penetrant in the gas phase and S is the solubility coefficient of the penetrant into the polymer. The partial pressure of the penetrant is further related to the penetrant concentration in the gas phase through, for example, the ideal gas law. Application of the ideal gas law is justified when the concentration of the diffusant in the gas phase is lower than one atmosphere. 20 The diffusion coeffient D, can be independent or, a function of the penetrant concentration c in the polymer. In the latter case, the diffusion coefficient would not be constant but would be concentration dependent. In either case, it is assumed that the diffusion process is fickian. If the diffusion coefficient is time dependent, the diffusion process is said to be non-fickian (Meares, 1965). Permeability Measurements Isostatic Method A representative transmission rate profile curve for describing the transport of a permeant through a polymer membrane by an isostatic method is shown in figure 1. From such an experiment, diffusion and permeability coefficient values are obtained, and while the specific experimental configuration may vary among investigators, the basic equations describing the permeation phenomenom are similar. Solution of eqn. (1) depend on the boundary conditions of the experiment, in this case given by: ( ( Ahd At A1 :31 Aha ). 21 L0? 0.8- 0.6»- 0.4 U 0.2!- 130 150 170 190 Time (hours) G L 90 110 Figure 1. Transmission rate profile curve for toluene vapor through oriented polyethylene terephthalate (PET) at 90 ppm and 23 C (thickness of the film was 3.49 x 10"5 m, crystali- nity 27%). 22 c = CO at x = 0 t = 0 c = 0 at x = L t > O L-x C=c2 at O -1 (6) V1 1 - 2 x V l for a constant value of x. eqn 6 always predicts clustering in the range, 0 < V1 < l/2x. The equation is not defined at the upper limit of the range (Vl - l/2x), which is the spinodal point indicating phase separation. Neither the conventional dual mode sorption model or the Flory-Huggins model with a constant value for x correctly describe the apparent clustering in the systems mentioned above (Table 1). M d d u In this study, eqn 1 has been modified by using the Flory-Huggins equation to describe non-specific solution rather than Henry's law. This modification should allow the model to fit over the activity range, 0 < a1 < 1. Other choices for the solution model are possible, but the Flory-Huggins equation is relatively simple to apply. Because the non-specific sorption term is nonlinear, the complete model can have an inflection point and should predict clustering somewhere over the range of activity values. For convenience, the modified dual mode sorption model is expressed in terms of volume fractions and solute activity: 1 + V1 (7) 65 where V1FH refers to the Flory-Huggins contribution to the solute volume fraction. Since eqn 2 is nonlinear, it is convenient to determine the value for V1FH by numerical methods, such as the Newton-Raphson technique and eqn 7 becomes: K a V1 - FH (a1, X) +- ______1__ (8) l + B a1 The clustering function based on eqn. 8 is: G V K a V PH 1 _11 - _.Z __l._ + 1 - __ (9) 2 2 FR FH V1 V1 (1+3 a1) l-V1 (1+2sz ) V1 Equation 9 predicts clustering for some values of the constants but is undefined when: 1-v1m(1+2xv2m)-0 (10) This occurs when V1 is 1.0 (pure solvent) or l/2x (phase separation). W Pol er ms The amorphous polyamide used in this study was provided by E. I. du Pont De Nemours and Company. The polymer was synthesized from hexamethylene diamine and a mixture of 70/30 isophthalic and terephthalic acids. The random placement of the acid isomers in the polymer chain prevents 66 crystallization. No evidence of a crystalline melting point was found for this polymer. Equilibrium Sorptign Data Equilibrium sorption data was taken on polymer films using a Cahn Electrobalance Model RG. A stream of nitrogen adjusted to specific values of water activity provided the source of water vapor in equilibrium with the polymer films. The apparatus and operation are described elsewhere [27]. Closed containers with salt solution to provide selected values of water activity were also used. The experiments were conducted at room 5 termperature. The film samples, of 2.93 x 10- m thickness (1 mil), were dried under vacuum at 1000 C before each run. De it Film densities were determined in a density gradient column with the gradient made of toluene and carbon tetrachloride. Fourier T s o d The sample for infrared analysis was prepared by casting a thin film onto a zinc sulfide (ZnS) crystal from a 2% solution with l,l,l,3,3,3- hexafluoro-Z-propanol (Kerr Company, Novi, Michigan). After evaporation of the solvent at room temperature, the sample was dried in a vacuum oven at 1000 C to remove residual solvent and water. The sample was then equilibrated with water vapor at selected water activity values. After 67 attaining equilibrium, the sample was immediately covered with another crystal of ZnS and transferred to the instrument. Diffe ential ca n a e e 5 Film samples were prepared for these analyses by vacuum drying at 1000 C and equilibrating with the vapor over salt solutions to give selected water activities. W191! Equilibrium Sogptiog Isgthgzm Sorption equilibrium values of water weight fraction and volume fraction in the amorphous polyamide at 230 C are presented in Table 2. Experimentally determined and calculated densities for the water-polymer solution also are presented. Isotherm data was obtained over a wide activity range (0.046 < a1 < 0.96) in order to provide a good test of the modified dual mode sorption model. Figure 1 shows the sorption isotherm for water in the amorphous polyamide. - ~ The solid curve through the data is the Flory-Huggins equation (eqn 2) with a x value of 1.632. The value of the interaction parameter was calculated by using a Box-Kanamazu modification of the Gauss method of minimization of sum of squares for nonlinear models [28]. This model represents the data at high activities very well. 68 Table 2. Experimental Data Temperature: 23C Water Uptake Uptake Experim. Calcul. weight Volume Activity Weight Percent Density Density Fraction Fraction 0.0000 0.00000 0.0000 1.1938 1.1938 0.00000 0.00000 0.0460 0.00470 0.4700 --- 1.1939 0.00468 0.00560 0.0560 0.00657 0.6572 --- 1.1940 0.00653 0.00781 0.0720 0.00752 0.7520 --- 1.1941 0.00746 0.00893 0.0800 0.00787 0.7870 1.1938 1.1942 0.00781 0.00935 0.0900 0.00836 0.8360 --- 1.1943 0.00829 0.00992 0.1100 0.00938 0.9380 --- 1.1944 0.00929 0.01113 0.1550 0.01211 1.2110 --- 1.1950 0.01197 0.01433 0.1890 0.01290 1.2900 --- 1.1955 0.01274 0.01526 0.2520 0.01670 1.6700 --- 1.1964 0.01643 0.01970 0.2690 0.01596 1.5960 --- 1.1967 0.01571 0.01884 0.3080 0.02200 2.2000 1.1975 1.1973 0.02153 0.02583 0.4100 0.03040 3.0400 1.1986 1.1989 0.02950 0.03545 0.4400 0.03568 3.5680 --- 1.1993 0.03445 0.04142 0.5650 0.04180 4.1800 --- 1.2008 0.04012 0.04829 0.5800 0.04580 4.5800 --- 1.2009 0.04379 0.05272 0.5850 0.04340 4.3400 --- 1.2010 0.04159 0.05007 0.6350 0.05050 5.0500 1.2012 1.2014 0.04807 0.05789 0.7350 0.06190 6.1900 1.2017 1.2019 0.05829 0.07022 0.7900 0.07110 7.1100 --- 1.2020 0.06638 0.07998 0.8600 0.07870 7.8700 --- 1.2021 0.07296 0.08791 0.8800 0.08200 _ 8.2000 1.2022 1.2022 0.07579 0.09132 0.9630 0.09000 9.0000 1.2022 1.2024 0.08257 0.09951 Volume Fraction x (E + 03] B} CD 69 100 - —Florv-lluuins a Experimental . 80 - 60 - 40 r- : l 1 L I 1 0 .2 .4 .5 .8 Water Act! Figure 1. Experimental sorption values and Flory-Huggins fitting. 1.0 70 Parameter stimatio o E us 7 Parameter values estimated for eqn 7 were sensitive to the method used to determine them. A nonlinear regression method was used to determine the values of the three parameters simultaneously. This resulted in Langmuir coefficients with a high amount of error and a fit using eqn 7 which was no better than the fit using eqn 2. The least squares technique was not sensitive to deviations between the data and the model at low activities. However, the deviation of eqn 2 from the data is systematic. Figure 2 shows an expanded view of the low water activity data and the underprediction of eqn 2. An alternative parameter estimation method gave coefficients with lower error. The data for a1 > 0.4 were used to determine a range of x values which could represent this portion of the curve. x should be between 1.6 and 1.85 to minimize the least square error for this data set. The data for a1 < 0.4 were used to determine the Langmuir coefficients. The nonlinear regression method gave the coefficients and the R2 parameter for a set of X values in this range. The R2 value was plotted as a function of x to find the best estimates of the parameters. Figure 3 shows eqn 8 as the solid curve (x - 1.7, K - 0.395 and B - 95.2) and the complete data set. Table 3 shows the contribution of the Langmuir and Flory-Huggins factors to the solute volume fractions over the activity range. At low activities, the Langmuir contribution is high compared to the Flory-Huggins contribution and at a1 - 0.4, it is just over 10% of the total volume fraction of solute. The Langmuir contribution is nearly constant (> 90% of its maximum value) at activities greater than 0.11 and the curve at high water activities should be insensitive to the values of the Langmuir coefficients. Therefore, the estimation method is consistent with the parameter values. Volume Freotlon x (E + 03) 71 —FIorv-Ilogoins a a Experimental hi :3 d C: 0J— ' I I 0 .l .2 .3 .4 Water Activity Figure 2. Experimental sorption values and Flory-Huggins fitting at low activity values. 72 100 — tang. + Fii a Experimental CD CD CD :3 I I Volume Fraction x (E + 03) a l l l l l J I .4 .o .8 1.0 Water Activity Figure 3. Best fit for the Langmuir-Flory-Huggins model. Values of the parameters are7-= 1.70, K = .385 and B -= 95.15. 73 Table 3. Langmuir and Flory-Huggins volume fraction contributions. x - 1.7 k - .384707 B - 95.14954 Activity Lang. F-H Total 0 0 0 0 .01 1.9713458-03 6.7405093-04 2.6453968-03 .02 2.6504188-03 1.3521268-03 4.0025458-03 .03 2.9942288-03 2.0342783-03 5.0285078-03 .04 3.2019022-03 2.720568-03 5.9224628-03 .046 3.2912265-03 3.1343323-03 6.4255588-03 .056 3.4042853-03 3.827329E-03 7.2316153-03 .072 3.5281782-03 4.9450292-03 8.4732085-03 .08 3.5736998-03 5.5080513-03 9.0817498-03 9.000001E-02 3.620418-03 6.215795E-03 9.8362048-03 .11 3.6905748-03 7.6447413-03 1.1335312-02 .155 3.7864432-03 1.09277eE-02 1.471418E-02 .189 3.8301963-03 1.347346E-02 1.7303662-02 .252 3.8813112-03 1.8349342-02 2.2230658-02 .269 3.8911573-03 1.9702435-02 2.3593598-02 .308 3.9097718-03 2.2870325-02 2.6780093-02 .41 3.9421328-03 3.1612522-02 3.5554655-02 .44 3.94886E-03 .0343221 3.8270963-02 .565 3.9693493-03 4.6401532-02 5.0370882-02 .58 3.9712233-03 4.7946433-02 5.1917665-02 .585 3.9718263-03 4.8466413-02 5.243823E-02 .635 3.9773555-03 5.381052E-02 5.778788E-02 .735 3.9861875-03 6.538535E-02 6.9371543-02 .79 3.9900998-03 7.2345758-02 7.633585E-02 .86 3.9943688-03 8.194831E-02 8.5942688-02 .88 3.9954632-03 8.4867963-02 8.8863423-02 .963 3.9995312-03 9.7993338-02 .1019929 74 Sensitivit Coef ent Sensitivity coefficients indicate the magnitude of the change of a function due to perturbation in the values of its parameters [28]. Sensitivity coefficients for eqn 8 are given by the first derivative of the volume fraction with respect to x, B and K. XK_5V1-_31 (11) 6 K 1 + B al 6 V -K a 2 XB-__1-_1_ <12) 6 B (l + B a1)2 m m xx-L‘ii-‘h—YL (13) 5x 2v1FH-1 Where XK’ XB’ and XX are the sensitivity coefficients of K, B and x. These coefficients were evaluated as a function of activity, al. at the optimum values of K, B, and x and the results are plotted in Figure 4. For a1 > 0.1, XX changes with activity while XR and XB are essentially constant. For high activity values, it will be difficult to distinguish between K and B parameters. At low activity values, they are non-linear dependent and better estimates for them can be obtained. The results shown in Figure 4 suggest that a simultaneous search for the three parameters will be difficult over the entire activity range, that high activity data will be insensitive to K and B, and that the best estimates for K and B will be obtained at low activity values. Eqs. 11-13 give a protocol for evaluating the method of determining the constants and are an improvement over the 75 -1 5 1 1 1 1 1 1 1 1 1 0 .2 .4 .6 .8 I . 0 WI!" Activity Figure 4. Sensitivity coefficients as a function of activiy. 76 1.0 Langmuir-FIory-liuppins (eqn. 01— 4 3th. Order Polynomial --- 4th. 0rder Polynomial ---° 0.8 - 3' 0.0 h E ‘5 a: 0.4 - 0.2 - 0.0 ' 1 1 1 1 1 1 -3l -21 -II -I 4 Cluster Function Figure 5. Clustering function as a function ofactivity. 77 suggestion that the constant(s) for the solution phenomenon should be determined when the solute partial pressure is much larger than the Langmuir affinity constant, b [10]. Clustering Analysis Equation 9 and polynomial expressions were used to compute the clustering function for the water sorption data. The polynomial expressions fit the data with similar least square errors. Both expressions approached but did not pass throught the zero activity-zero volume fraction point, and neither expression replicated the S-shaped curve of the data. Figure 5 shows the clustering function estimated from two polynomial fits (third and fourth order) and the modified dual mode sorption model. All three equations predict clustering (Gll/V1 > -1) but differ in the solute activity at which this should occur. The fourth order polynomial predicts clustering in the activity range, 0.34 < a < 0.96. The third order polynomial 1 predicts clustering for a1 > 0.27 but the clustering function does go through a maximum at a1 - 0.60. There is no obvious physical explanation for why clustering should decrease, or disappear, at high water activities. 78 Equation 9 predicts clustering at a1 - 0.38 and the function is increasing monotonically over the whole activity range. Ph sica vi e e fo 0 u e The Langmuir isotherm was derived based on chemisorption of a chemical species to a specific binding site characterized by a single activation energy. Solute sorption described by this isotherm for the water-polyamide solution might result in observable changes in physical properties of the polymer, particularly if the water is associated with a specific group on the polymer backbone. One obvious possibility is water interaction with the amide group. FTIR spectroscopy studies were done to detect possible changes in hydrogen bonding between N-H and carbonyl groups by observing the vibrational modes of the amide group (Amide I and Amide 11 bands). The Amide I mode includes contributions from C-O stretching, C-N stretching and C-C-N deformation vibrations. The Amide II band includes N-H plane bending, C-N stretching and C-C stretching vibrations. Figure 6 shows a typical FTIR spectrum taken at room temperature over the range, 800-4000 cm'1 for a cast polyamide sample. The Amide I and Amide II modes occur at 1640 and 1541 cm'l, respectively, for the dry sample and are the most intense bands. The frequency scale and the relative intensity of the Amide I and Amide II modes were internally calibrated with reference to the CH2 stretching band at 2858 cm-1. Table 4 lists the absorption frequencies, and Table 5 lists the intensity ratios for the Amide I and Amide II bands of the sample recorded as a function of water volume fraction and activity. The frequency of the CH2 stretching band, which served as the interal calibration band, is presented for reference. Figure 7 shows the absorption 79 too 80 '- 5 la; all"- .2 g 1 a .— ,: 40 i? :5 U u _ Z 9 20 - :3 ES - SE ‘3 ‘I l l . l l, 4000 3000 2000 1000 1200 cm"1 Figure 6. Typical FTIR spectrum of the amorphous polyamide recorded at room temperature. 80 Table 4. Amide I, Amide II and CH absorption frequencies. Activity CH Peak Amide I Amide II 0 2858 1640 1541 0.08 2858 1640 1545 0.308 2858 1641 1545 0.56 2858 1641 1545 0.88 2858 1641 1546 Unite: cm Table 5. Intensity ratios of Amide I and Amide II with respect to CH bands. ACTIVITY AHIDE I / C-H AHIDE II / C-H 0 1.77 5.47 0.08 1.78 5.44 0.308 1.87 5.11 0.56 1.80 5.43 0.88 1.84 5.14 81 1.8 8.8 ' n 8.8 - = 1 g , 3 ' / ‘ 88 a C 8.4 F “W 8.2 - - o.o' - . . . 1888 1588 1528 cm"1 Figure 7. Spectrum region of Amide II as a function of activity. 82 region from 1500 to 1600 cm.1 (Amide II mode) as a function of al. The spectrum are displayed on an absolute absorbance scale. The Amide I band remained essentially constant at 1640 cm.1 as did its intensity. The peak maxima of the Amide II band shifted to higher frequency, 1541 to 1546 cm'l, over the range, 0% to 9.1%, water volume fraction. The intensity ratio of the Amide II band remained essentially constant. The shift of the Amide II band to higher frequency with increasing water content is consistent with an increase in the average hydrogen bond strength [29]. These data suggest that the water does not change the hydrogen-bonding strength of the carbonyl group but does change the hydrogen bonding strength of the N-H group. The shift in the Amide II band is completed at the water activity at which 90% of the Langmuir sites would be filled (Table 3). In linear, aliphatic homopolyamides there is essentially 100% hydrogen bonding, as evidenced by the absence of bands in the infrared spectra above 3300 cm"1 [30]. In structurally irregular copolymers, such as amorphous polyamide, both the N-H stretching region and the Amide11.region can be resolved into "free” and hydrogen bonded stretching modes. Skranovek et a1 [29] resolved the N-H stretching region into three components: a "free" N-H mode, a hydrogen-bonded N-H stretching mode and an Amide II mode. The Amide I band was resolved into a ”free" and hydrogen-bonded carbonyl mode. Most of the first water molecules sorbed form hydrogen bonds with the "free" N-H groups of the amorphous polyamide. This would be an exothermic process and should have a single activation energy associated with it. The formation of these new hydrogen bonds should have a negligible enthalpic effect [21],[31]. The extent of disruption of the self-association of polyamide neighboring groups by water molecules is not known. Both the 83 model and the FTIR data suggests that chemisorption has been completed at activities well below those at which clustering occur. At a water activity of 0.08 (where the Langmuir sites are 89% saturated), the total amount of chemisorbed water is only 4% of the total water volume fraction. This amount corresponds to 3.34 x 10"3 g of water per gram of polymer, or one molecule of water per 22 repeating units of the polymer. Each repeat unit contains 2 amide groups so only 2.3% of the amide groups available form hydrogen bonds with water. Relaxation Temperatures Several relaxation temperatures have been described for semicrystalline polyamides. Papir et a1 [31] related the gamma relaxation peak (1400K) of Nylon 6 to the movement of methylene and polar groups. Sfirkis and Rogers [12] reported that the gamma peak for the Nylon 6-water system was affected by water concentration. The change in intensity of the gamma peak with changing water concentration leveled off at a concentration corresponding to the apparent onset of water clustering. The gamma relaxation temperature was measured via the dielectric constant at 1 kH. The gamma peak of the amorphous polyamide was 1730 K in the dry state. The peak was not observed for samples equilibrated at a1 > 0.08. The difference could be due to the interaction of water with the amide group decreasing the units available to participate in the relaxation process. 84 Data for the alpha relaxation temperature (glass transition temperature) were obtained by DSC measurements. The effect of sorbed water on T8 is shown in Figure 8, where Tg values are plotted with water volume fraction. There is an apparent change in slope of T8 with activity near a1 - 0.40. A similar trend was observed on T8 versus water volume fraction obtained from the dielectric experiments. The slope change occurs near the activity at which clustering is predicted. A similar trend was observed by Sfirakis and Roger [12] for the change in the 1 peak intensity for the system water-nylon 6. Density Data Figure 9 shows the change in total density with water activity. The amorphous nylon solution becomes more dense as water is added. This is the opposite effect expected from a mixing rule depending on additive molar volume fractions. A similar result has been reported for an epoxy system [32]. Notice that there is little change in density below water activities of 0.1, where the Langmuir coefficients suggest that chemisorption (or "hole filling") is essentially completed. It is interesting to point out that the permeability of this amorphous nylon to oxygen decreases by a factor of 2 for films at water activities greater than 0.10 compared to a sample from which water has been removed. An inflection point occurs in the density curve near the water activity range (0.30 - a1 at the maximum of d0/da1 for these data) over which clustering is predicted to begin. The water activity at this inflection point is similar to that near the apparent change in Tg vs a1 curve (Fig. 8). 19,0 85 To Versus Volume traction 130 f ” a l 10 - A 90 - £3 70 - (3 so . ° ; 1 1 1 l 1 11. 1 1 1 3"0 . .3 .5 .7 .9 t .01 Volume traction [x 10] Figure 8. Glass transition temperature as a function of activity. 1.2 Density p/cc 86 t A 1.9.. 1.2 - l 1.19 1 1 1 1 1 1 1 1 0 .l .3 .5 .7 .9 Water Activity Figure 9. Density as a function of activity. 87 Pro osed Mech i £0 E ec s W e o s Pro erties of Amor hous 0 am de At water activities less than 0.10, water preferentially chemisorbs to amide bonds, although a low mole fraction of the total hydrogen bonding sites on the polymer are occupied. The chemisorption process can be detected by observing the wave shift in the amide group absorbance. The filling of these "open" positions reduces the permeability of the polymer system to other, nonchemisorbing, species, such as oxygen. Chemisorption is essentially completed at a1 - 0.1 (about 1 vol % water). There is no measurable change in system density at this water activity. As with other dual mode sorption systems, polymer history and relaxations probably affect the Langmuir sorption capacity, C'H, although such data have not been taken in this study. At higher water activities, the permeability of oxgyen and water change little, even though water clustering is predicted. System density increases nonlinearly as water activity increases. A change in the T3 of the system with respect to water activity coincides with the clustering predictions as does the inflection point in the density-activity curve. Clustering may be associated with the increase in density (and decrease in system volume). The effects of water sorption on transport properties will be treated in another paper. The dual mode sorption model with a Flory-Huggins term to represent non-specific sorption predicts clustering at activities similar to those determined by numerical analysis of the data. 88 LTTERNTURE CITED 1)P. Blatz and C. Talkowsky, Personnel Commicuation, (1987). 2)A.S. 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Young, Polmer, Sorption Diffusion and Conduction in Polyamide-Penetrant Systems: I Sorption Phenomena, 15, (1974), 771. 23M.T. Aronhime, X. Peng and J.K. Gillhan, J. Appl. Polym. Scig, Effect of Time-Temperature Path'of Cure on the Water Absorption of High T. Epoxy Resins, 32, (1986), 3589. 203.11. Zimm and J.L. Lundberg, J. Phys. Chem., Sorption of Vapors by High Polymers, 60, (1956), 425. 25)J.L. Lundberg, J. Macromol. Sci. Phsy., Clustering Theory and Vapor Sorption by High Polymers, 4, (1969), 693. 267r.A. Orofino, H.B. Hopfenberg and V.T. Stannett, J. Macromol. Sci. Phys. Ed. , Characterization of Penetrant Clustering in Polymers, 4, (1969), 777. 27)R.J. Hernandez, I..A. Baner and J.R. Giacin, J. Plast. Films 8. Sheeting, The Evaluation of the Aroma Barrier Properties of Polymer Films, 2, (1986), 187. 28)J.V. Beck and K.J. Arnold, Parameter Estimation in Engineering and Science, J. Wiley and Sons, NY, (1977). 92 29)D.J. Skronovek, S.E. Howe, P.C. Painter and M.M. Coleman, Macromolecules, Hydrogen Bonding in Polymers: Infrared Temperature Studies of an Amorphous Polyamide, 18, (1985), 2218. 30)D.S. Trifan and J.R. Terenzi, J. Polm. Sci., Extends of Hydrogen Bonding in Polyamides and Polyurethanes, 28, (1958) , 443. 31)Y.S. Papir, S. Kapur and C.E. Rogers, J. Polym Sci., Effect of Orientation, Anisotropy, and Water on the Relaxation Behavior of Nylon 6, from 4.2 to 300°K, A-2, 10, (1972), 1305. 32)E.L. McKague, J.D. Reynolds and J.E. Halkias, J. Appl. Polym. Sci. , Swelling and Glass Transition Relations for Epoxy Matrix Material in Humid Environments, 22,(1978\, 1643. CHAPTER III EFFECT OF WATER CONTENT ON THE PERMEABILITY, SOLUBILITY, AND DIFFUSION OF OXYGEN IN NYLON 6I/6T. INTRODUCTION In general, physical properties of hydrophylic polymers such as polyamides are affected by the presence of water within the polymer matrix. Nylon 6I/6T, a totally amorphous polyamide which was recently developed, is synthesized from hexamethylenediamide and a 70/30 (weight percent) mixture of isophthalic and terephthalic acids. Preliminary studies on the effect of water sorption on the barrier properties of this polymer showed atypical behavior, as compared to semicrystalline Nylons under the same conditions. For example, oxygen permeability in Nylon 66 increases as a function of moisture content of the polymer, while the permeability of oxygen in Nylon 6I/6T shows a decrease in value, with increasing water content of the polymer. Further, the tensile modulus for Nylon 66 decreases as a function of moisture content, while the tensile modulus for Nylon 6I/6T increases with increasing moisture content. 9'! 94 The behavior of this amorphous polyamide has lead Hernandez et al. [1] to study the mechanism of water sorption into this polymer. The authors proposed a dual-mode sorption model, based on a Langmuir and Flory-Huggins mechanism. At water activities below 0.1, water preferentially chemiabsorbs to amide bonds, although, only a low mole fraction of the total hydrogen bonding sites on the polymer are occupied (2.3%). Chemisorp- tion is essentially completed at water activity a1 =0.1, and represented about 4% of the total water absorbed. At the same time, randomly non-chemisorbed water molecules dissolve within the polymer matrix are described by Flory-Huggins equation. At higher water activities, a1< 0.3-0.4 the model predicts that water molecules start clustering among themselves. This mechanism results in an increased capacity of the polymer to accommodate water molecules. The model is given by: + V PH (1) where V1 is the total volume fraction of water within the polymer, and the superscripts L and FH refer to Langmuir and Flory-Huggins water sorption contributions, respectively. These contributions are expressed as: vL= (2) 95 and FH FR 2] a1 = exp [1n vl + (1-v1FH) +1: (1-v1 ) (3) where 31 is water activity,)(is the Flory-Huggins interaction parameter, and K and B are parameters of the Langmuir equation. Equation (3) can be written in implicit form as: V1FH = FH(al,X) (4) Applying cluster function to equation (1), the following expression is obtained [1]: (1+3 a1) 1—v1FH(1+2 xv1 ) v1 Where Gll/Vl is the cluster function. Oxygengpermeability as a function of polymer water activity When oxygen permeability experiments were carried out on films of Nylon 6I/6T as a function of water content, it was found that permeability values decreased with an increase in 96 water content, with the largest relative percent decrease being observed at low water activity values, al<0.2. Similar results were reported by Chern et al., [2], for CO2 permeability through Kapton Polyimide at 60°C, for upstream pressure levels up to 240 psia (16.33 atm), with and without water vapor in the feed stream. The authors found that CO2 permeability was depressed by the presence of water molecules (experiments were carried out at 0, 5.5 and 9.3% relative humidity). These results suggested that competition between the two species for Langmuir sorption sites takes place [2]. The effect of a low partial pressure of water and pentane on the permeability of H2 and CH4 through several polyimide films has been measured by Pye et al., [3]. These investigators reported a decrease in the flux or permea- bility for H2 and CH4, when the experiments were performed at values of 50% of water vapor. Oxygen solubility and diffusion coefficient In the present study, a series of experiments was carried out to characterize the effect of water content of Nylon 6I/6T on the permeability of oxygen, as well as on the solubility and diffusion coefficient of oxygen. The experimental conditions covered water activity values from 0 to 1 and temperatures of 11.9, 22.0 and 40.30C. Upstream oxygen pressure was maintained at 1 atm, while the 97 downstream oxygen partial pressure value was approximately zero, as a nitrogen carrier gas was flowed continually through the downstream cell chamber. From permeability experiments, values of the solubility and diffusion coefficient of oxygen were calculated [4]. Solubility data showed that oxygen competes with water molecules for Langmuir active sites. A semiempirical model is presented, based on the depression of oxygen solubility, and is described in terms of the Langmuir component of eqn. (1): V = V - F (6) Where V is the solubility of oxygen in the polymer, expressed as cc 02 (of critical volume)/ cc polymer-water system, V* is the solubility of oxygen in the polymer at dry conditions and F is a empirical constant that relates sorption values of oxygen and water associated with Langmuir sorption mode, and is defined by: F = (7) 98 J— Where V“ is the solubility of oxygen, expressed as volume fraction of liquid oxygen (at critical conditions) in the dry polymer, Veq is the solubility of oxygen, expressed as volume fraction of oxygen liquid (at critical conditions) at water activity 31 = 1, and VlLeq is the volume fraction of liquid water given by the Langmuir mode at a1=l, according to eqn. 2. Values of the diffusion coefficient of oxygen increased initially and then showed a plateau as a function of water activity, suggesting that its numerical values depend both on the effect of plasticization of the polyamide by the water molecules and by the clusters of water. 99 EXPERIMENTAL METHODS Polymer films An amorphous polyamide, known as Nylon 6I/6T, was provided by the E.I. Du Pont De Nemours and Co. The polymer was synthesized from hexamethylenediamine and a mixture of isophthalic (70%) and terephthalic (30%) acids. Since the acid isomers were randomly placed into the polymer backbone, resulting in structural irregularity, no crystallization of the polymer matrix was observed. No evidence of crystalline melting point was found, by performing differential scanning calorimeter (DSC) analysis. Equilibrium Sorption Data Equilibrium sorption data was taken on polymer films using a Cahn Electrobalance Model RG, (Cahn Instuments Inc., Cerrito, California). A stream of nitrogen gas adjusted to specific values of water activities provided the source of water vapor in equilibrium with the polymer films. The apparatus and its operation were described in Chapter I. Closed containers with salt solutions were also used to obtain equilibrium sorption values. 100 5 m thickness (2 mils) dried under Film samples of 5.1 x 10- vacuum at 100 0C for two hours before each run, were used in each experiment. Oxygen Permeability Studies Oxygen permeability studies were performed using a continuous gas flow system similar to the one described in Chapter I. These studies were carried out on an Ox-Tran 100 Permeability Tester (Modern Controls, Inc., Elk River, Minnesota). This apparatus was modified to allow the two streams, oxygen and carrier gas, to be adjusted to specific water vapor activities. An schematic of the modified apparatus is shown in Figure (1). As shown, each stream is formed by mixing a wet and a dry gas component to obtain the required activity value. Water activities were measured using hygrometer sensors (Hygrodynamic Co., Silver, Spring, Maryland). Samples of 2.93 x 10.5 m thickness (1.15 mils), were dried under vacuum at 100 0C before each run. The equilibration process between the polymer film and the gas phase, at the selected values of water activities, was done with the sample film mounted into the permeation cell. The required time to reach equilibrium was previously determined by gravimetric method, using the Cahn electrobalance. Although time consuming, this procedure avoided sample handling and assured correct conditions of tests. 101 PACKAGE LOOP \/ ._ DIFFUSION CELL 31311 CATALYST 3?: SPECIMEN T OXYGEN CARRIER PURSE q PURSE INSERT -“~ SENSOR BYPASS v ., SENSOR 2 v1 ‘ A ll SENSOR :: I i i l i LOAO RESISTOR Figure 1. Oxygen permeability apparatus. 102 RESULTS AND DISCUSSION_ Equilibrium Sorption lsotherms Values of the equilibrium sorption of water in Nylon 6I/6T at 5, 23 and 420C, expressed as fraction volume, are presented as a function of water activity in Tables 1, 2 and 3, respectively. Density data were only available at 230C and these were used to calculate the volume fraction values. Figure 2 presents a plot of the three isotherms and, as Shown, the solubility of water in the polymer decreases when temperature increases. The apparent Shape of the three isotherms indicates that they follow the Lamgmuir-Flory- Huggins model, given by eqn. (1). As outlined in Chapter II, equilibrium sorption data was treated to obtain the parameters of the model. Table 4 shows the values forJK , K and B at 5, 23 and 42°C. An Arrhenius plot of K and B is presented in Figure 3, and the following expressions correlate the constants B and K with the temperature: U5 II 15.7 x exp(-0.232/T) (8) 751 ll 2.05E-03 x exp(0.9135/T) (9) 103 TABLE 1. Water/polymer isotherm at 5°C. Experimental Calculated Calculated Water Volume Flory-Huggins Langmuir Activity Fraction Component Component Aw leloo VlFHx100 Vle100 0 0 0 0 0.096 1.21 0.692 0.51 0.185 1.90 1.38 0.52 0.36 3.37 2.84 0.53 0.402 3.76 2.84 0.53 0.60 5.78 5.24 0.53 0.685 6.80 6.23 0.57 0.83 8.72 8.17 0.55 0.91 9.98 9.42 0.56 0.975 11.15 10.57 0.58 104 TABLE 2. Water/polymer isotherm at 23°C Experimental Calculated Calculated Water Volume Flory-Huggins Langmuir Activity Fraction Component Component Aw lelOO VlFHxIOO vle100 0.046 0.56 0.313 0.329 0.560 0.781 0.383 0.340 0.072 0.893 0.494 0.353 0.080 0.935 0.551 0.357 0.090 0.992 0.622 0.362 0.110 1.113 0.764 0.369 0.155 1.433 1.093 0.378 0.189 1.526 1.347 0.383 0.252 1.970 1.835 0.388 0.269 1.884 1.970 0.389 0.308 2.583 2.287 0.391 0.041 3.545 3.161 0.394 0.440 4.142 3.430 0.395 0.565 4.839 4.640 0.396 0.580 5.272 4.795 0.397 0.585 5.007 4.847 0.397 0.635 5.789 5.381 0.398 0.735 7.022 6.538 0.399 0.790 7.998 7.235 0.399 0.860 8.791 8.195 0.399 0.880 9.132 8.487 0.400 0.963 9.995 9.800 0.400 105 TABLE 3. Water/polymer isotherm at 42°C. Experimental Calculated Calculated Water Volume Flory-Huggins Langmuir Activity Fraction Component Component Aw V1x100 VlFHx100 VleIOO 0 0 0 .078 0.67 0.505 0.165 .265 2.00 1.820 0.18 .395 3.01 2.838 0.172 .48 3.74 3.561 0.179 .57 4.56 4.383 0.177 .777 6.75 6.567 0.183 .82 7.27 7.086 0.189 .91 8.46 8.27 0.19 000000000 Volume Fraction .09 .08 .07 .06 .05 .03 .02 .01 106 U I 23°C 5°C 42°C p J l J .2 .3 .4 .5 .8 .7 .8 .9 aw(Water Activity) Figure 2. Water sorption isotherms at 5 °C, 23 °C and l+2"C. 107 2x52 1x52 . *k a 1x E1 1 fl, 3.15 3.3 3.45 1ITXE03 Figure 3. Values of K and B of the langnuir equation. 3.6 108 The clustering function values were calculated from the equilibrium sorption values. The onset of the cluster formation was taken to be when the value of Gll/Vl = -l, [5]. Table 5 shows the corresponding values of water activity for the onset of clustering at 5, 23 and 420C. The computer program used to calculate the cluster function values, as well as the output are included in Appendix A. Calculation of Oxygen Solubility Oxygen permeability experiments were conducted at 11.9, 22 and 40.3OC. Diffusion coefficient and solubility values were obtained from these experiments according to the procedure outlined in Chapter I. Permeability experimental data obtained for this study are tabulated in Appendix B. The diffusion coefficient was calculated from a least-squares linear analysis of values from the unsteady state region for each permeability run. Values of 4Dt/L2 were used as the dependent variable versus time. The corresponding values of the correlation coefficient were also calculated, to I indicate the goodness of fit. Solubility values were calculatated from the expression, S = P/D (10) Where P, S and D stand for permeability, solubility and diffusion coefficient, respectively. The solubility of oxygen is expressed as S in cc 02 (STP)/cc polymer-water system or V in cc (liquid 02 at its critical Specific volume)/cc polymer-water system. 109 TABLE 4. Value of X., K and B as a function of temperature. Parameter SOC 220C 420C X. 1.66 1.70 1.76 K 0.46 0.385 0.19 B 81.36 95.15 102.0 TABLE 5. Water activity values at the onset of cluster formation. Temperature Water Activity 00 5 0.42 22 0.37 42 0.28 110 Conditions for ApplyinggEqn. 10 AS previously discussed in Chapter I, when eqn. 10 is applied to calculate solubility values from permeability and diffusion coefficients, it is assumed that the permeant/polymer system follows the Henry's law of solubility, [6]. For this work, which was intended to Study the effect of water activity on the diffusion of oxygen, it is necessary to show that the oxygen diffusion coefficient is independent of the oxygen pressure in the range up to 1 atmosphere. To show that the solubility of oxygen in Nylon 6I/6T follows a Henry's law behavior and that the oxygen diffusion coefficient was independent of the pressure (in the range of the experimental conditions of this work), permeability experiments were conducted in the range of 0 to 1 atmosphere oxygen. Summarized in Table 6 are the values of the oxygen solubility and diffusion coefficient in Nylon 6I/6T at 0.2, 0.366, 0.50, 0.745 and 1.0 atm of pressure and a temperature of 24°C. AS shown, D remains constant through the experimental range of pressure. For better illustration, Figure 4 presents a plot of the oxygen solubility values. The solubility of oxygen in Nylon 61/6T as a function of oxygen partial pressure is given by: s = 0.144 x p (11) 1.11 TABLE 6. Solubility of Oxygen in Nylon 6I/6T as a function of pressure at 240C. Pressure D x E9 S x 10 V x E4 atm (a) (b) (C) 0.2 1.08 0.277 0.91 0.366 1.11 0.530 1.73 0.50 1.04 0.750 2.53 0.745 1.18 1.073 3.52 1.0 1.13 1.44 4.71 (a)- in (cm2/sec) (b)- in (cc 02/cc polymer) (c)- in (cc O2 liq./cc polymer) D = 1.11 x 10E09 Standard error = 5% s, ccoz (STPilcc polymer 112 8.2 0.15 - / O 0.1 - 0.05 > 0 a 1 .1 1 0 e4 .8 1.2 Pressure, atm Figure 4 . Solubility of oxygen as a function of partial pressm'e at 24 ’C. 113 where S is the solubility in cc 02 (STP)/cc polymer and p is the pressure in atm. Permeability Data Tables 7, 8 and 9 present the values of permeability, diffusion coefficient and solubility of oxygen in Nylon 61/6T at 11.9, 22 and 40.3OC, respectively. Figures 5, 6 and 7 illustrate the effect of temperature on the permeability coefficient, the diffusion coefficient and the solubility of oxygen in Nylon 6I/6T, as a function of water activity. Figures 8, 9 and 10 Show the Simultaneous change of the diffusion coefficient and the solubility of oxygen aS a function of water activity at 11.9, 22 and 40.30C. AS shown in these figures, oxygen permeability values decreased as a function of water activity. The values of oxygen permeability were factored into a solubility and a mobility term according to eqn. 11. The solubility term decreased 5 times and the D values increased by 2 as a fun- ction of water activity (average values for all temperatu- res). From these findings it became apparent that the in- crease in the diffusion coefficient was not enough to com- pensate for the depression of the oxygen solubility values, and the result was a depression in the permeability values. An attempt is made here to interpret these results in the framework of the dual-mode sorption model presented in Chapter II. 114 TABLE 7. Diffusion, solubility and permeability values of oxygen at 11.9OC. Water D x E10 S x 10 P V x E4 Activity (a) (b) (c) (d) 0 3.06 3.46 31.3 11.33 0.06 3.65 1.67 18.1 5.47 0.175 3.65 1.34 ' 14.3 4.39 0.32 3.70 1.13 12.4 3.70 0.452 4.03 0.85 11.4 2.78 0.594 4.84 0.72 10.4 2.36 0.74 4.9 0.73 10.6 2.39 0.753 4.91 0.71 10.3 2.32 0.881 4.90 0.69 10.0 2.26 (3)“ in (cmzlsec) (b)- in (cc O2/cc polymer) (c)- in (cc 02/m2.day) (d)- in (cc 02 1iq./cc polymer) 115 TABLE 8. Diffusion, solubility and permeability values of oxygen at 22.00C. Water D x E10 3 x 10 P V x E4 Activity (a) (b) (c) (d) 0 5.54 2.97 48.8 9.71 0.048 7.19 1.58 33.7 5.13 0.153 7.36 1.21 26.3 3.96 0.275 7.90 1.04 24.4 3.40 0.445 9.34 0.774 21.4 2.53 0.545 9.54 0.71 20.2 2.32 0.75 9.89 0.67 19.52 2.19 (a)- in (cmz/sec) (b)- in (cc 02/cc polymer) (c)- in (cc 02/m2.day) (d)- in (cc O2 1iq./cc polymer) 116 TABLE 9. Diffusion, solubility and permeability values of oxygen at 40.300. Water D x E10 8 x 10 P V x E4 Activity (a) (b) (c) (d) 0 11.5 2.56 87.6 8.37 0.040 13.6 1.50 60.7 4.91 0.096 12.5 1.3 50 4.25 0.15 14.38 1.10 48.5 3.6 0.253 17.54 0.87 45.1 2.84 0.392 22.25 0.65 42.6 2.13 0.535 24.41 0.52 37.3 1 7 0.67 27.42 0.46 37.6 1.5 0.81 27.67 0.45 36.5 0.1.47 (a)- in (cm2/sec) (b)- in (cc 02/cc polymer) (c)- in (cc 02/m2.day) (d)- in (cc 02 liq./cc polymer) 117 N E. 5 A > 0. fi \ ~ A 9- \ 1- A 9 \A o A A 9 A n.’ \A o \A 22 C \A N A 119°C A o 4 - 1 . 0 .1 .2 .3 .4 .5 .6 .7 .8 .9 aw( Water Activity) Figure 5. Oxygen permeability values at ll.9°C, 22.0°C and 40.31:. Dx Eta, cmzleec 118 30 A—————A 403°C / /A A 20 /A A’ A’A f 22°C 10 ' A—— A—— A A/ A-—— 4/ 119°C A A AA 0 1. . 1 1 0 .1 .2 .3 .4 .5 .8 .7 .8 .9 “(Water Activity) Figure .6. Diffusion coefficient values at ll.9°C, 22.0'C and L10.3”C. Sxto, cc02 (STPllcc polymer 4.0 119 E" 0 1° 0 10 K °\\e° ' . \OSOi'Q‘? 0 °\' "22°c° °-o o-40.3°C 0 4 4 1 1 o 1 .2 .3 .4 .5 .e .7 .s .9 1 ”Water Activity) Figure 7. Oxygen solubility values at ll.9°C, 22.0'C and l+0.3"C. 011 E10, cmzlsec 120 5.0 4.0 O/& o A Solubility o Diffusion Coefficient 4,5 1- 1 3.0 4.0- ° «2-0 A \ <0 o—m 3.5 - \ 1 o ‘ ‘~—Ae-——A 3L0 - .1 1 o 0.1 .2 .3 .4 .5 .o .7 .a .9 1 “(Water Activity) Figure 8. Solubility and diffusion coefficient of oxygen at ll.9°C. 8x10, cc02 (STPilcc polymer Dx E10, cm2/eec 121 3.0 1" o '3 3x10, cc02 (S‘i’Pllcc polymer 10 0...... ASoiublllty O/ olefuslon Coefficient o / 9. 1 8 _ o A / o 7b A \‘ q \‘ 6 \7 “ 5_ 1, . . , O .1 .2 .3 .4 .5 .8 .7 .8 .9 1 ”Water Activity) Figure 9. Solubility and diffusion coefficient of oxygen at 22:0 C. 011 E10, cmzlsec 122 30- :: Solubility A Diffusion Coefficient o —————°-— 25 o / t 2.0 o 20 - A\ A \‘ O 15 . ’o’o \A\ o 3.0 . 1.0 10 - _. - 1 o 1 O .1 .2 .3 .4 .5 .6 .7 .8 .9 ”Water Activity) Figure 10. Solubility and diffusion coefficient of oxygen at 40.3 C. 51110, cc02 (STPilcc polymer 123 Oxygen solubility Equation (6) was applied to model the solubility of oxygen in Nylon 6I/6T, as a function of water activity at 11.9, 22.0 and 40.300. The values of the constants necessary for eqn. (6) are presented in Table 10. TABLE 10. Values of the constants for Eqn 6. Temperature F K B cc 02(Liq) cc water 0 -1 C a1 cc water cc polymer 11.9 .187 .42 86.7 22.0 .188 .385 95.15 40.3 .373 .19 102 Numerical values of F indicate that at the same temperature the volume fraction of liquid oxygen associated with active Sites within the polymer is only 0.19-0.37 of the volume fraction of the chemiabsorbed water. The value of the constant F at 40.30C appears to be somewhat higher than the 124 other two values. This lack of trend may be due to the numerical error associated with the values of the constants of the Langmuir equation that describe the chemisorbed molecules of water into the polymer. As Shown in Chapter II, the sensibility coefficients of the parameters K and B indicated the importance of the values at low water activity when calculating these constants. In order to get better values for the constants, K and B, more data at low water activity values may be required. ' Tables 11-13 present experimental and calculated (using eqn. 6) values of oxygen solubility at 11.9, 22.0 and 40.30C respectively. For better illustration, the tabulated data is presented graphicaly in Figures 11-13 where oxygen solubility is plotted as a function of water activity of the polyamide. The experimentally determined solubility values are also included to Show the validity of the model. AS Shown, good agreement between calculated and experimental data is observed, except in the range of 0.1 to 0.3 of water activity, where the model predicted a lower solubility than that found experimentally. These findings indicate that the solubility of oxygen in Nylon 6I/6T is comprised of two components: one, simple dissolution of O2 molecules within the polymer matrix and not affected by the presence of water molecules, and second, 02 molecules related to active Sites of the polymer and able to be easily displaced by water molecules. The simple dissolved molecules contribution is about 20% of the 125 total oxygen solubility (20% at 11.900, 21% at 22.000 and 18% at 40.300). The fact that 80% of the total dissolved oxygen was displaced by molecules of water associated with active sites of the polymer matrix, indicates the importance of these active Sites in the mechanism of the solubility of oxygen within the Nylon 6I/6T. Polarity and molecular size may be important factors in determining the final equilibrium sorption values of water and oxygen molecules within the polymer matrix. 126 TABLE 11. Experimental and calculated solubility of oxygen at 11.9OC. Aw Experimental Calculated (cc 02(Liq) per cc of polymer-water) x E4 0 11.32 11.32 0.06 5.41 3.73 0.175 4.39 2.81 0.32 3.70 2.59 0.452 2.59 2.49 0.594 2.42 2.42 0.74 2.39 2.39 0.753 2.26 2.31 0.881 2.26 2.31 v* - v (11.36-3.26)XE-4 eq. F = = = 0.187 v L 0.00484 127 TABLE 12. Experimental and calculated solubility of oxygen at 22.000. Aw Experimental Calculated (cc 02(Liq) per cc of polymer) X E4 0 9.72 9.72 0.048 5.15 3.43 0.153 3.96 2.53 0.275 3.41 2.31 0.445 2.53 2.21 0.545 2.32 2.18 0.75 2.19 2.15 V - Veq. (9.72-2.19)xE-4 F = = = 0.188 L V1 eq. 0.004 128 TABLE 13. Experimental and calculated solubility of oxygen at 40.3OC. Aw Experimental Calculated (cc 02(Liq) per cc of polymer) x E4 0 8.34 8.34 0.04 4.91 2.78 0.096 3.92 2.06 0.15 3.60 1.86 0.253 2.80 1.70 0,392 2.12 1.60 0.535 1.70 1.57 0.67 1.50 1.54 0.81 1.47 1.50 v* — veq_ (8.34-l.47)xE-4 F = = = 0.373 v L 0.00185 S, cc02 (STPi/cc polymer oe‘ ‘ P or 9 no 0.1 129 A Experimental — Calculated A AA A ‘ J .3 .4 .5 .6 .7 .8 .9 aw(WSter Activity) Figure 11. Oxygen solubility at ll.9'C as function of aw. S, cc02 (STPllcc polymer 130 0.4 A Experimental - Calculated 0.3 0.2 A 0.1 ’ \A A A A 0 1 - 1 o .1 .2 .3 .4 .5 .9 .7 .a .9 a“,( Water Activity) Figure 12. Oxygen solubility at 22.0°C as function of aw. s, cc02 lSTPl/cc polymer 131 0.3 A Experimental - Calculated 002‘ h A A 0.1 i A A A A A 0 c A 4 A —‘V O .1 .2 .3 .4 .5 .6 .7 .8 .9 aw(Water Activity) Figure 13. Oxygen solubility at HO.3°C as function of aw. 132 Oxygen diffusion coefficient Values of the oxygen diffusion coefficient D in the amorphous polyamide/water system were presented in Figures 8-10 as a function of water activity al, for three temperatures. As shown, the general trend in the change of D values as function of a1 was similar in the three cases. In general, the diffusion coefficient increased with increasing water activity up to a value of 0.5-0.6 activity, after that, D values showed a plateau. The value of water activity at which the diffusion coefficient approached a constant value (0.5-0.6), was immediatelly above the value of a1 at which the clustering of water within the polyamide was predicted (0.3-0.4). This behavior was observed for all temperatures except at 11.9 0C where D showed constant values for O.05O.4. The change of ED values took place for the range O.150.4 may be a indication that clusters of water molecules opposes the passage of oxygen molecules, creating a more tortuose path to the diffusing molecule [8]. If this is true, the oxygen diffusion coefficient studies as a function of water activity may be considered as a experimental proof of the clustering of water molecules within the polymer. CONCLUSIONS Results from the study of oxygen solubility and diffusivity complemented the Fourier Transform Infrared spectroscopy, temperature relaxation and density studies that were performed on the polyamide water system. Further, these results provided additional supportive evidence for the dual-mode sorption model proposed in Chapter II. Water is rapidly chemisorbed to dry Nylon 6I/6T, bounded to amide groups through hydrogen bonds. Saturation of the amide actives sites is completed before water activity reaches a 136 value of 0.1. There is also a simultaneous process of dissolution of water non-chemisorbed and randomly distributed within the polymer. This water is easily removed from the polymer and does not present hystersis during the desorption process. When water activity reaches a value between 0.3 and 0.4 molecules of water tend to self associate forming clusters of molecules. The degree to which molecules of water preferentially self associate rather than exist as loosely dissolved within the polymer is not known. However, it appears to be large enough to result in a increase in the activation energy for the diffusion process of oxygen molecules. Techniques such Nuclear Magnetic Resonance spectroscopy and isotopes tracers studies may help to elucidate this important question. SUMMARY The sorption of water molecules by a glassy amorphous polyamide, Nylon 6I/6T, showed a depression in the oxygen permeability values as a function of polymer moisture content. The oxygen permeability behavior was analysed in terms of the multiplicative effect of a mobility and a solubility term. The analysis of the solubility values of the oxygen within the polymer-water system, provided a complementary framework for the dual sorption model presented in Chapter II. The model provided a theoretical 137 basis for interpreting transport behavior in polymer-vapor- gas systems. This may prove important in relation with the new generation of materials that are characterized by high glass transition temperature, molecular backbone rigidity and eventually made of polar groups such as Nylon 6I/6T. 138 REFERENCES . Hernandez, R. J., J. R. Giacin and E. A. Grulke, The sorption of Water by an Amorphous Polyamide, submmitted to the Journal Membrane Science. Chern, R. T., w. J. Koros, E. S. Sanders and R. Yui, ”Second Component" Effect in Sorption and Permeation in Glassy Polymers, J. Membrane Sc., 15 (1983) 157-169. Pye, D. G., M. M. Moehr and M. Panar, Measurement of gas Permeability of Polymer, II. Apparatus for Determination of the Permeability of Mixed gases, J. Applied Sc., 20 (1976) 287-301. . Hernandez, R. J., J. R. Giacin and A. L. Baner, The Evaluation of the Aroma Barrier Properties of Polymer Films, J. Plastic Film Sheeting, 2 (1986) 187-211. Lundberg, J. L.,Clustering Theory and Vapor Sorption by High Polymers, 4 B3 (1969) 263-711. Crank, J. and G. S. Park, Diffusion in Polymers, Academic Press, London, (1968). 139 DiBenedetto, A. T. and D. R. Paul, An Interpretation of Gaseous Diffusion Through Polymers Using Fluctuation Theory, J. Polym. Sc.: Part A, 2 (1964) 1001-1015. Paul D. R. and A. T. DiBenedetto, Diffusion in Amorphous Polymers, J. Polym. Sc.: Part C, 10 (1965) 17-44. Kumins, C. A.,Transport Through Polymer Films, J. Polym. Sc.: Part C, 10 (1965) 1-9. APPENDIX A 100 110 120 130 140 150 160 165 170 175 180 190 191 195 200 205 210 140 REM BOX KANAMAZU METHOD FOR FLORY HUGGINS MODEL CLS: DIM A1(20),v1(20),ETA(20),X(20) INPUT "HOW MANY POINTS?", N INPUT "HOW MANY ITERATIONS?", ITE INPUT "ENTER THE FIRST ESTIMATE OF CHI", B PRINT "ENTER FIRST Al'S AND THEN Vl'S" A1(1)=.056:A1(2)=.08:A1(3)=.11 : A1(4)=.189 :A1(5)=.252 A1(6)=.308 A1(7)=.41 : A1(8)=.44 :A1(9)=.565 : Al(10)=.585 A1(11)=.63S : A1(12)=.735 Al(l3)=.79 :A1(l4)=.86 :Al(15)=.88 : Al(16)=.963 : A1(l7)=.58 V1(l)=.0076 : Vl(2)=8.000001E-03 : V1(3)=.0109 :Vl(4)=.0139 Vl(5)=.0912 REM V1(6)=.02515 : V1(7)=.03442 : V1(8)=.04016 :Vl(9)=.05097 V1(10)=.04843 Vl(11)=.05591 : Vl(12)=.06768 :Vl(l3)=.07696:Vl(14)=.0845: V1(15)=.0877 :Vl(16)=.0955:V1(17)=.0109 215 220 225 230 240 250 255 260 270 280 290 295 300‘ 310 315 320 330 PRINT " H", " Sl", " CHI" RL =0! RL=RL+1 XTX=O£ : XTY=0£ :SO=0! :Sl=0! REM EQUATION FOR THE MODEL FOR K=l TO N V2=1 -V1(K) ETA(K)=V1(K)*EXP(V2+B*V2*V2) NEXT K REM EQUATION FOR THE SENSITIVITY COEFF FOR K=l TO N V2=1!-V1(K) X(K)=Vl(K)*V2*V2*EXP(V2+B*V2*V2) NEXT K REM CALCULATE SO, XTX, XTY FOR K=l TO N SO=SO+ (Al (K) -ETA (K) ) * (Al (K) -E TA (K) ) 340 350 360 370 380 390 400 410 420 430 440 445 450 460 560 570 580 590 600 610 615 620 630 640 650 660 670 680 141 XTX=XTX+X(K)*X(K) XTY=XTY+X(K)*(A1(K)-ETA(K)) NEXT K DELTAB=XTY/XTX REM CALCULATE G G=DELTAB*DELTAB*XTX IF (G<0!) OR (G=0!) GOTO 670 H=11 B=B+DELTAB*H REM CALCULATE ETA'S WITH B'S FOR K=l TO N V2=ll-V1(K) ETA(K)=Vl(K)*EXP(V2+B*V2*V2) NEXT K REM CALCULATE $1 FOR K=l TO N 51 =Sl+ (A1 (K) -E TA (K) ) * (Al (K) 'E TA (K) ) NEXT K JJ=SO-(2-(1/l.l))*G IF (Sl