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Processes 2018, 6(6), 70; doi:10.3390/pr6060070
The Influence of Cation Treatments on the Pervaporation Dehydration of NaA Zeolite Membranes Prepared on Hollow Fibers
State Key Laboratory of Materials-Oriented Chemical Engineering, College of Chemical Engineering, Nanjing Tech University, 5 Xinmofan Road, Nanjing 210009, China
The authors contribute equally to this work.
Received: 21 April 2018 / Accepted: 23 May 2018 / Published: 1 June 2018
NaA zeolite membrane is an ideal hydrophilic candidate for organic dehydrations; however, its instability in salt solutions limits its application in industries as the membrane intactness was greatly affected due to the replacement of cation ions. In order to explore the relationship between the structural variation and the cation types, the obtained NaA zeolite membranes were treated by various monovalent and divalent cations like Ag+, K+, Li+, NH4+, Zn2+, Mg2+, Ba2+ and Ca2+. The obtained membranes were subsequently characterized by contact angle, scanning electron microscopy (SEM), pervaporation (PV), and vapor permeation (VP). The results showed that all of the hydrophilicities of the exchanged membrane were reduced, and the membrane performance varied with cation charges and sizes. For the monovalent cations, the membrane performance was largely determined by the cation sizes, where the membrane remained intact. On the contrary, for the divalent cation treatments, the membrane separation was generally reduced due to the presence of cation vacancies, resulting in some unbalanced stresses between the dispersive interaction and electrostatic forces, thereby damaging the membrane intactness. In the end, a set of gas permeation experiments were conducted for the two selected cation-treated membranes (K+ and Ag+) using H2, CO2, N2 and CH4, and a much higher decreasing percentage (90% for K+) occurred in comparison with the permeation drop (10%) in the PV dehydration, suggesting that the vaporization resistance of phase changing for the PV process was more influential than the water vapor transport in the pore channel.
Keywords:NaA zeolite membrane; pervaporation; cation treatments; membrane separation; hollow fibers
Fuel ethanol is considered as a promising alternative to the conventionally used fossils due to its significant advantages in terms of environment protection, energy intensity, and resource abundancy [1,2,3]. At present, microbial fermentations are the mainstream route that is used in the industry to produce fuel ethanol; however, by-products and water generated during the fermenting activities  should be removed simultaneously in order to maintain the production efficiency. Among the diverse separation strategies, the membrane-based pervaporation (PV) process, as a newly emerging technique, has attracted considerable attention due to its significant advantages of less energy consumption and operational convenience over the traditional separation methods, such as extraction and distillation.
In general, the membranes that are used for organic dehydrations can be classified into two categories, which include (i) polymeric and (ii) inorganic membranes. Although the polymer is easy to fabricate due to its high flexibility, it suffers from weak mechanical strengths and swelling problems, thereby limiting its application [5,6,7]. Not only has the inorganic membrane demonstrated good mechanical strengths, but also strong chemical resistance and high thermostability were also derived, so it is more promising to be used in harsh solutions containing additives, like dimethylformamide (DMF), tetrahydrofuan (THF) and salts. Among the various types of inorganic membranes, zeolite membrane, making use of its unique pore structure and surface properties, are widely deployed for organic dehydrations . In the past two decades, many types of zeolites have been fabricated as the supported zeolite membranes [7,9], including LTA [10,11], FAU , T , MOR  and MFI [15,16,17]. Among these candidates, The tubular NaA zeolite membrane has been widely applied in pharmaceutical and food industries for solvent recoveries . NaA zeolite contains sodium cations, and the chemical formula is Na12[(AlO2)12(SiO2)12]∙27H2O , where the sodalite cages are connected through double four-membered rings (4MR) in order to form a large cavity. For the NaA zeolite membrane with a Si/Al ratio of 1.0, high permselectivities can be achieved due to its strong hydrophilicity. Since the first commercial application of tubular NaA membranes in practical factories by Mitsui Engineering and Shipping in the 1990s, over 200 sets of the membrane plants have been established in the world for various purposes [20,21,22]. However, the tubular NaA membrane often contains large diameters and thick walls, so the packing density and flux in a certain membrane module are limited, thereby increasing the membrane facility investment.
To further reduce the membrane cost, the packing density of the membrane module should be significantly increased. Therefore, there is an on-going effort to prepare the NaA membrane on hollow fibers with a much smaller diameter and thinner walls. However, at present, the NaA membranes prepared on the hollow fiber are still unsatisfactory due to their low selectivity. This could be caused by the high curvature of the substrate surface, which induces stresses between the membrane and substrate surface, thereby leading to the presence of the inter-crystalline defects [23,24]. Therefore, it is necessary to use chemical approaches to improve the membrane performance in order to increase the adhesive forces between the membrane layer and substrate. To fix the membrane defects derived during the preparation, cations exchanges could be employed to cover interstitial gaps by changing the crystal cell parameters, which resulted in the contraction and expansion of the zeolite particles. Further, inorganic salts are generally presented in organic solvents used in the fields of organic chemicals, fine chemicals, and pharmaceutical chemicals. The salts inevitably interacted with the NaA zeolite and thus affected the separation performance of the NaA zeolite membrane by changing the zeolite structure and surface hydrophilicity. According to the work by Breck and co-workers , the pore size of LTA zeolite could be tailored using various cation treatments. For the zeolite that was treated by potassium, the effective pore size was reduced to 0.28 nm; on the contrary, the calcium salt produced a larger pore size of 0.51 nm. Francisco et al.  investigated several ion-exchanged NaA/carbon membranes for hydrogen purification, and it had found that the Rb-LTA and Cs-LTA/carbon membranes provided better separation performance. Shirazian et al. . Prepared the K-exchanged LTA zeolite membranes for the dehydration of natural gas; however, the separation factors were still close to the prediction of Knudsen diffusion. Yang et al. studied the influence of several inorganic salts on the PV performance for the ethanol/H2O/salt mixtures, and a significant flux drop was found, which was assumed to be caused by the pore blocking and surface precipitation of salts [28,29,30,31]. However, the above research only involved a limit number of cations, and the membrane structural changes caused by the cation exchanges were not explicitly correlated with the ionic size and charge, but were lumped with the driving force variations and transport resistance increments during the PV characterization.
Based on above discussion, it is necessary to scientifically and systematically explore the relationship of separation variations with cation sizes and charges using both PV dehydration and gas permeation techniques, so as to provide guidance in order to broaden the industrial application of hollow fibered supported NaA zeolite membranes. In this paper, we prepared hollow fiber supported NaA zeolite membranes in a batch mode with acceptable separation performances, which was later treated by different cations solutions (monovalent and divalent cations) to derive ion-exchanged NaA zeolite membranes. Then, the ion-exchanged membranes were characterized by PV for 90 wt % ethanol/water solution. The variations of permeation fluxes and selectivities were studied and were used to correlate the coordinated effect between the cation size and charge. In the end, the PV decrement for several cation treatments was compared with that for the gas permeation and vapor permeation (VP) tests to evaluate the importance of the surface hydrophilicity and the vaporization resistance of the NaA zeolite membranes for water molecules.
The monovalent and divalent salts (monovalent: NaCl, LiCl, NH4Cl, KCl and AgNO3; divalent: ZnCl2 MgCl2 6H2O, CaCl2 and BaCl2) were purchased from commercial companies, and they were used as received without any purification. The silica sol, water glass and NaAlO2 were used as Si and Al sources with industrial purity. The original NaA zeolite seeds (cubic crystals, with a size of 2–4 μm) and deionized water were produced in the laboratory. The alumina four channel hollow fibers (4CHF) were used as the support (homemade, out diameter: 3.4–3.8 mm, length: 70 mm, porosity: 45–55%).
2.2. Synthesis of NaA Zeolite Membranes and Ion-Exchange Processes
The preparation process of NaA crystal suspension: 0.2 g silica sol was added to a certain amount of ball-milled NaA zeolite crystal solution so as to improve the viscosity and to prevent the agglomeration of seeds; after that, the solution was mixed by an ultrasonic cell grinder (power 200 W) for 30 min, in order to obtain a uniformly dispersed seed suspension. Seeding the hollow fiber: the hollow fibers, soaked with 0.1 mol·L−1 sodium hydroxide solution for 12 h, were placed in a 60 °C oven and were dried overnight; after that, the hollow fibers were pre-coated by the dip-coating method for 5–15 s.
The preparation process of the NaA zeolite membrane was provided in Figure 1. At the beginning, the sodium hydroxide that was dissolved in deionized water to provide basic conditions, was later mixed with sodium aluminate to derive a clear solution, and then a certain amount of water glass was added into the mixture under vigorously stirring for 1.5 h, where the molar ratio of the synthesis solution is Al2O3:SiO2:NaOH:H2O = 1:2:2:120. Subsequently, the treated supports that were vertically placed in a Teflon-stainless steel autoclave containing the synthesis sol, were transferred into the oven for 4 h at 100 °C. The as-synthesis membrane was washed with deionized water several times, before drying at 70 °C overnight.
The preparation of ion-exchanged NaA-type zeolite membrane: the 90% ethanol/water solution was mixed with a certain amount of NaCl, LiCl, NH4Cl, KCl, AgNO3, ZnCl2, MgCl2, CaCl2, or BaCl2, respectively, to derive a mixture with a salt concentration of 0.05 mol/L–0.10 mol/L by sonicating for 30 min; the ion-exchange solution was pumped into the liner that was equipped with the prepared NaA zeolite membrane to exchange for 24 h at 50 °C. After the exchanging, the membrane was immersed in deionized water for 2 h, and was then was dried for characterizations.
The preparation of ion-exchanged NaA zeolite powder: the salt solutions were prepared according to the above method, and then 40 g of the salt solution and 0.6 g NaA crystal were stirringly mixed in a conical flask immersed in a water bath of 50 °C for 4 h. After the exchanging, the suspension was centrifuged for several times and dried.
2.3. Characterization of NaA Zeolite Particles and Membranes
The morphologies of the as-synthesis NaA zeolite powders and membranes were characterized by field emission scanning electron microscopy (FESEM) and installed with a cold field emission gun that was operating at 5 kV and 10 µA (S-4800, Hitachi, Tokyo, Japan). The crystal structure of the sample was analyzed by X-ray diffraction (XRD) at a tube voltage of 40 kV and a tube current of 15 mA (MiniFlex 600, Rigaku, Tokyo, Japan), where the Cu target and the Ni filter were used to generate Kα rays and to remove Kβ rays, respectively. The tests were performed at room temperature with a diffraction range of 5°–50°, and a scan rate of 12°/min. After exchanging, the elemental content of the sample was measured by inductively coupled plasma optical emission spectrometry (ICP-OES, optima 7000DV, PerkinElmer, Waltham, MA, US), where the samples were dissolved in an acidic mixture before testing.
2.4. PV Test and Single Gas Permeation
The separation performances of NaA zeolite membranes were evaluated by dehydrating 90 wt % ethanol-water solution at 75 °C by a PV apparatus, as reported in our previous work . The compositions of the feed and permeate were analyzed by gas chromatography (GC-6890, Ruihong, Tengzhou, China). The PV performance of each membrane was determined by the separation factor (α) and flux (J), which were, respectively, defined as follows:where yw and ye are the mass fractions of water and ethanol in the permeate, respectively; xw and xe correspond to the fraction values in the feed, respectively; m is the mass (kg) permeated over a time period of Δt (h); and, A is the effective membrane area (m2).
By excluding the influence of the membrane hydrophilicities, gas permeation at room temperature was used to characterize the importance of the vaporization effect in the NaA zeolite membranes that were treated by different cations. For the permeation experiment, the membrane was sealed by silicone O-rings and the volumetric flow rates of single gases (H2, CO2, CH4 and N2) were measured using a bubble flow meter. The tested gas on the feed side provided a driving force for gas permeation from the outside of the membrane to the lumen inside, where the gas permeation flux (Pmi) can be expressed as:where Pmi represents the molar quantity of the gas flowing through the membrane per unit time and per unit area under per unit pressure difference( mol∙m−2∙h−1∙Pa−1); n corresponds to the moles of the gas; and, ΔP is the pressure difference (Pa).
3. Results and Discussion
3.1. PV Performances of the Exchanged NaA Zeolite Membrane
Figure 2 depicted the ion exchange model for the NaA zeolite with high aluminum content to show how different cation affects the open pore passages. As suggested, cation charges affect the exchange number of ions during the exchange in order to maintain the valence balance of the zeolite. According to the law of conservation of charge, each divalent cation consumes two replacements of monovalent sodium ion, and vice versa. In the cation treatment, in order to ensure the full exchange of ions with the membrane, an exchanging time of 24 h and a cation concentration of 0.1 mol/L were firstly selected. To initially examine the effect of ion exchanges of different cations on the membrane performance, both the feed and permeate were analyzed by a gas chromatograph, where the PV solution was a 90 wt % ethanol/water mixture.
Table 1 summarized the PV results for different salts, where the corresponding cation sizes were provided in Table 2. As suggested, the kinetic radii of the monovalent cations, like K+ and Ag+ (1.49 Å and 1.26 Å), are greater than that of Na+ (1.17 Å), and the PV separation factor of the membrane was increased and the permeate flux was decreased. This is probably because K+ or Ag+ entered into zeolite cage and replaced the original Na+, which resulted in the decrease in accessible pore size. Smaller pores yielded lower permeation fluxes, but higher separation factor. For the smallest monovalent cation (Li+), when the original Na+ was replaced by Li+, the pore was significantly opened, which led to a much higher permeate flux, but without any selectivity during the PV test. For the treatment by the acidic cation solution of NH4Cl, both the permeation flux and the separation factor were considerably reduced, suggesting that the membrane structure was significantly changed. The decrease in the permeation flux could be explained by the ionic size effect (1.48 Å versus 1.17 Å), where the water passage in the membrane was blocked by the larger cation. The decrease in the separation factor was caused by the chemical attack to the zeolite skeleton due to the presence of H proton that was released from the cation for the NH4Cl solution being acidic. On the other hand, the surface precipitation of salts on the membrane surface could also cause the decrease of permeation flux. To evaluate such an effect, the NaCl solution was used as a reference. As given in the Table 1, before and after the treatment with NaCl solution, the permeation flux and the separation factor of the membrane only change slightly, so the surface precipitation effect could be neglected in the experiment.
For the divalent cations of Mg2+ and Zn2+ with smaller ion sizes (0.72 Å and 0.74 Å), both the permeation flux and the separation factor of the NaA zeolite membranes dramatically decreased after cation exchanging. This was because of the displacement of Na+ cations around the six-membered ring-like structures. When the Na+ ions were deprived from zeolite pores by the smaller divalent cations of Mg2+ and Zn2+, the open pore size became larger than the molecular size of ethanol, so the separation factor was reduced. In addition, since the molar ratio of ion exchanging between Na+ and Mg2+/Zn2+ was 2, the remaining cation sites in the zeolite were vacancies, so some unbalanced stresses were induced, where the membrane porosity was reduced due to some collapse. When the effect of porosity decrement outweighed the effect that was caused by the pore enlargement, the overall permeation flux still decreased. For the other two divalent cations (Ca2+ and Ba2+) with larger ion sizes (1.0 Å and 1.35 Å), the coordinated effect between open pore size and unbalanced stresses due to cation vacancies were similar except the pore size that was caused by Ba2+ treatment became smaller. The decrease in open pore size should cause the increase in the separation factor; however, the unbalanced stresses generated some defects between crystals in the membrane, so the membrane intactness was reduced, which caused the decrease in the separation factor. Another evidence for the presence of defects in the Ba2+ treatment was the increase in flux.
3.2. Surface Morphology of the Exchanged NaA Zeolite Membrane
To further testify the above structural alternations, which gave rise to the changes in permeation fluxes and separation factors, the surface morphologies of NaA zeolite membranes after various cation treatments were examined by the scanning electron microscopy (SEM) technique. The obtained images for the monovalent cation treatment were depicted in Figure 3. As suggested, no large cracks of crystal particles and interstitial defects were found on the surface of the zeolite membrane after being treated with 0.1 M AgNO3, NaCl, KCl and NH4Cl solutions, so the membranes intactness was maintained in the cation treatments. When compared to the feature of the original NaA zeolite crystals in Figure 3a, no significant changes occurred to the samples that were treated with KCl and NaCl solutions in Figure 3b,f. Further, for AgNO3 treatment in Figure 3c, a large amount of amorphous substances were found on the membrane surface, which may be caused by the partial destruction of particle due to the crystal cell expansion by the replacement of Ag+, i.e., the interstitial defects between the particles were largely fixed, which increased the separation factor but decreased the permeation flux. However, for the NH4Cl treatment in Figure 3d, the zeolite crystals on the membrane surface started to dissolute as the sharp edges of the crystal particles were absent. This was largely due to the dealumination in the zeolite framework under acidic conditions (NH4Cl solution is acidic), thereby resulting in collapses of the skeleton and the partial dissolution of the membrane. For the smallest monovalent cation treatment of LiCl in Figure 3e, no amorphous substances were found on the membrane surface, and the crystal shapes remained unchanged except with larger interstitial spaces due the crystal cell contraction, which may be responsible for the membrane leaking in the PV tests in Table 1.
The SEM images for divalent cation treatments were provided in Figure 4, where the crystal shapes were unaffected, with larger interstitial spaces. However, for the treatment by BaCl2 solution in Figure 4b, some amorphous substances were found on the membrane surface. Similar to the explanation for AgNO3, the amorphous substances were generated by the cell expansion due to the replacement of larger ionic sizes of Ba2+. Since the interstitial gaps were covered, the separation factor was slightly increased. As the PV results given in Table 1, the coordinated effect between the pore blocking effect and the minimization of intercrystals gaps by the amorphous substance led to the slight variation of PV performances of NaA zeolite membrane treated by Ba2+. However, for other small divalent cations, due to the unbalanced exchange number between Na+ and M2+, some cation sites in the zeolite structure were left vacant, so some porosities of crystals were lost due to the structural collapse, which resulted in a complex behavior of fluxes and separation factors.
3.3. The Structural Analysis of the Exchanged NaA Zeolite Powders
Due to the replacements of new cations, not only were the cell parameters of NaA zeolite crystals changed to some extent, but also new substances were obtained, which in turn led to the variation of permeation flux and separation factors, and such a variation could be confirmed by the XRD characterization. Figure 5 illustrated the XRD results for the cation treated zeolite particles. As suggested in Figure 5a, the XRD peak intensities of the sample that was treated by AgNO3 were dramatically reduced, suggesting the presence of amorphous substances. In Figure 5b, a similar trend also occurred in the sample that was treated by Ba2+, so the interpretation for the membrane surface morphologies was validated. In general, the PV performances of divalent cation treated NaA zeolite membrane were unsatisfactory. For Mg2+, Ca2+ and Zn2+ ion treatments, both the permeation flux and the separation factor of the membrane decreased, which had little change in Ba2+ treatment. For the monovalent cation treatments, the permeation fluxes of the membrane after the exchange of Ag+ and K+ slightly decreased, but the separation factor has been greatly improved. Therefore, the variation trends of the membrane performance after M2+ exchange depended on the coordinated effect between porosity losses and ionic sizes, where a smaller ionic size generally reduced the membrane porosity due to structural collapse, and such an effect could be inhibited in the case for larger size cations due to a stronger dispersive interaction. For monovalent cations, in addition to the acidic/basic condition, the ionic size played a dominating role in the predication of membrane performance variations as no cation site was left vacant after exchanging treatments.
By observing the variations of crystal morphologies and the cation contents for the powder sample, a deeper understanding of ion exchanging could be achieved for the membranes. Table 3 illustrated that the ICP characterization results for the treated and original NaA zeolite crystals. It could be found that the content of Na+ only increased slightly after NaCl solution treatment. However, according to the conservation of charge, the content of Na+ should be unchanged in theory. The possible reasons were due to the presence of a small amount of residual ions in the crystals. For other cations, the content of Na+ steadily decreased. For the monovalent salts, about 90%, 16% and 59% of Na+ was replaced by Ag+, Li+ and K+, respectively. In comparison, for the divalent salts, about 78%, 49%, 66% and 81% of Na+ were replaced by Zn2+, Mg2+, Ca2+ and Ba2+, respectively. In addition, the relative molar content of the positive charge was very close to 1 for all of the samples, matching well with the NaA zeolite structure.
Since the cations were successfully incorporated in the NaA zeolites, the SEM technique was used to examine the morphology changes of the crystals, with the results being summarized in Figure 6. As suggested in Figure 6b,e,f, the salts of KCl, NaCl and LiCl had no destructive effects on the crystals; on the contrary, the crystals after the AgNO3 treatment were rounded in some way (Figure 6c), as the distinct edges became blurred due to swelling. For the NH4Cl treatment in Figure 6d, the crystals became less distinctive and smaller, indicating that acidic fluid dissolved the crystalline structures. Based on above discoveries, it was evident that the influence of Ag+ on the NaA zeolite structure was relatively significant, which was consistent with the discoveries that were based on the SEM image for AgNO3 solution in Figure 4b. Further, after the divalent salt treatments by CaCl2, BaCl2, ZnCl2 and MgCl2 solution in Figure 6g–j, not only did some damages occur to the particles during the replacements of cations, but also a small amount of amorphous substances were found on the crystal surface, which may be related to the flux decrement in the treated membranes, i.e., pore blocking effect due to the porosity loss.
3.4. The Concentration Effect on the Exchanged Membrane
Since the PV performance of the NaA zeolite membrane that was treated by divalent cations was not improved, only the concentration effect of monovalent cations on the PV performance was explored for the exchanged membrane. Table 4 summarized that the PV performances of different NaA zeolite membranes that were treated by various monovalent cations with several concentrations. For a high concentration of 0.10 M, it was evident that the separation factor of the NaA zeolite membrane was greatly improved after conducting KCl, AgNO3 exchanging, where the decrease in the flux was caused due to the pore blocking effect of K+ and Ag+ cations. For the lower concentrations of K+ and Ag+ with a value of 0.05 M, the membrane separation factors were still very high (>10,000), and the corresponding fluxes became 4.45 and 5.87 kg∙m−2∙h−1, respectively, which were slightly lower than that for the original NaA zeolite membrane (4.96 kg∙m−2∙h−1 and 6.51 kg∙m−2∙h−1, respectively). This was due to the faster exchanging rate with Na+ ions that was caused by the higher concentration. As the highest separation factor occurred to the mild concentration, it was reasonable to conclude that higher exchanging rate may also induce some unbalanced structural variations in the membrane. Similarly, the exchange effect of NH4Cl at a concentration of 0.05 M is better than that of 0.1 M by PV characterization. This was caused by the stronger acidity of the 0.1 M NH4Cl solution, which dissolved the membrane layer to some extent. For LiCl, no differences were obtained for the two conditions as the leakages occurred due to the smaller kinetic diameter of Li+, which permitted both water and ethanol molecules passing through the membranes. Based on the PV results for the treated NaA-type zeolite membranes, it was evident that the concentration of 0.05 M was more suitable for Ag+ and K+ to fix the membrane defects.
The SEM images of the NaA membranes that were treated by different concentrations were shown in Figure 7. It was observed that the ion exchanging rate difference due to the cation concentration clearly occurred to Ag+ and NH4+ in Figure 7a,b and Figure 7c,d due to the larger cation sizes, which yielded a limited exchanging rate. For the size identical cation of K+ in Figure 7e,f, and the difference between the two conditions was negligible due to the close similarity of crystals in two conditions.
3.5. PV Stability Test of NaA Zeolite Membrane
Since improved performances were found for the monovalent salts of KCl and AgNO3, respectively, the PV stability tests were conducted for the treated NaA zeolite membranes that were derived under a salt concentration of 0.05 M for 24 h at 60 °C. The results were shown in Figure 8. As given in Figure 8a for KCl, the flux increased after the first immersing. This was due to the initial dissolution of some amorphous substance on the membrane surface, where the membrane intactness and the crystal structure were affected. Since a lower transport resistance occurred, the flux was increased without affecting the separation factor. After the secondary immersing, the membrane flux increased from 4.96 kg∙m−2∙h−1 to 7.6 kg∙m−2∙h−1. This could be explained that the amorphous substances dissolved in the solution exposed the interstitial defects, thereby increasing the flux but reducing the selectivity. After the third immersing, the PV performance tended to be stable, where the flux remained at 6.5 kg∙m−2∙h−1, with the water content as high as 99.7%. In total, within 220 h, the KCl-exchanged NaA membrane maintained adequate fluxes with enough water purity in the permeate (above 99.6 wt %), and no significant damages occurred to the membrane. For the durability test of Ag+ exchanged zeolite membrane in Figure 8b, the flux tended to decrease significantly with the extension of operation time. This was caused by the preferential adsorption of water molecules on the membrane surface, leading to the blockage of the pore channel, thereby, resulting in a decrease in flux. However, after immersing in the raw material fluid for a long time, the flux increased due to a partial dissolution and destruction of the amorphous material on the membrane surface. Since the membrane intactness was still neat, the permeate purity was hardly affected. In total, the NaA zeolite membrane that was treated with Ag+, could keep a high performance in the PV test in 230 h. Since the amorphous substances were crucial to the performance evolution for the ion-exchanged membranes, the Energy-dispersive X-ray spectrometry (EDX) analysis was used to detect its chemical compositions, and the corresponding results were provided in Figure 9. As suggested, besides the elements (K or Ag) from the salts, the elements of Al, Si and O were also found, so the amorphous substances on the membrane surface were regarded as aluminosilicate.
3.6. Gas Permeation of NaA Zeolite Membranes
NaA zeolite membranes have exhibited high performance in liquid separation, but it has to admit that the membrane performance for gas separation is still far below the expectation, as the non-zeolitic pores and defects permit gas molecules passing through the membrane layer via Knudsen diffusion rather than by molecular sieving . However, the gas permeation characterization provides effective insights for the structural changes in the membrane layer by excluding the hydrophilicity variation of the membrane surface due to the cation exchanges. In order to further elucidate the relative importance of the pore channel variation on NaA zeolite membrane due to the cation replacement, the contact angle was first used to inspect the variation of membrane hydrophilicity, and such a result was provided in Table 5. As suggested, all the hydrophilicities of the exchanged NaA zeolite membranes were considerably reduced in comparison with that of the original membrane, suggesting interplay between the pore variation and hydrophilicities in the complex behaviour of the exchanged membrane that was treated by different cations.
The gas permeation test was carried out on NaA ion-exchanged membrane with good PV dehydration performances, and the blocking effect of Ag+ and K+ was determined by the changes of permeance. Figure 10 illustrated the variation of permeance through the membrane as a function of the kinetic diameter of gases, using a driving pressure of 2.0 bar at 25 °C, where flow rates of single gases (H2, CO2, N2 and CH4) were measured by bubble flow meter. As suggested, for the original NaA zeolite membrane, the experimental permeance order followed a Knudsen pattern of H2 > CH4 > N2 > CO2. For the smallest gas of H2, the permeance reached up to 7.66 × 10−7 mol∙m−2∙s−1∙Pa−1, much higher than that for the rest gases of CO2, N2 and CH4. For the most strongly adsorbed component of CO2, the molecules were anchored in the zeolitic cavities due to dispersive interactions, and the transport was controlled by the molecular movements, thereby leading to a lower CO2 permeance than that of N2 and CH4, which have higher thermal velocities. After the membrane was treated by AgNO3 solution, despite the same permeance pattern of gases, all of the permeances were decreased by a factor of 35%. This was because the larger size of Ag+ (1.26 Å) reduced the accessible pore passage. In comparison, for the membrane that was treated with KCl solution with even larger cation size (K+ = 1.49 Å), the gas permeance decreased more sharply, and a factor of 90% was found for all of the gases. Since the effect of the hydrophilicity was excluded in gas permeation, the pore narrowing effect was further confirmed. On the other hand, it has been noted that the percentage of permeance drop for gases was more significant than that for the PV dehydration in Table 1. For instance, the drop of permeation flux for the KCl exchanges was only 10% in Table 1, which is far below the value of 90% in gas permeation. Clearly, the smaller decreasing was irrelevant of the variation of the membrane surface hydrophilicities, and it could be mainly attributed to the extra vaporing resistance in the PV operation, where the water molecules escape from the liquid feed to the water vapor phase. Since the permeance difference for PV dehydration is much smaller than that for the gas permeation, so it was reasonable to conclude that the vaporization process of phase change is much more influential than the vapor transport in the zeolite pores. A similar result was also found in the vapor permeation (VP) characterization using different feed mixtures of ethanol/water for Ag+ and K+, where the variation of the permeance and separation factor was provided in Figure 11. As suggested, a greater decreasing percentage of 60% for the permeance was obtained for the vapor mixture with 10 wt % water content, thus confirming that the importance of vaporization resistance in PV dehydration outweighed that of vapor phase transport in the pore channel under current conditions.
Different cation-exchanged NaA zeolite membranes were successfully derived on hollow fibers, using monovalent and divalent salts. For the monovalent cations, the membrane showed very stable membrane structure and dehydration performances, except for the very acidic salts of NH4+, as the dealumination effect occurred in the zeolite frameworks. For the rest monovalent cations of (Li+, K+ and Ag+), it had been found that the permeation flux variations in dehydration largely related to the cations size. For the smaller sizes, like Li+, a much higher permeation flux was obtained, but the separation factor was completely lost due to the over enlargement of accessible passages that was caused by the replacement of Na+ by Li+. For the larger cations, like K+ and Ag+, a mild decrement of permeation flux occurred to the treated membrane, but the separation factors became higher for both cations, which was because the accessible passage became narrower. For the divalent cation-treated membrane, the membrane permeance variation was complex, where the permeation flux was generally reduced due to the interplay between the cation size and charges. For larger cation (Ba2+), the PV dehydration performances were slightly reduced for both permeation flux and separation factor, indicating that the membrane intactness was largely maintained and the unbalanced stresses was minimized. For other cations with smaller sizes, both the permeation flux and separation factor were reduced. This was because the number of Na+ was unevenly exchanged with M2+ to balance the charge, so some cation vacancies were left in the treated membrane and thus induced unbalanced stresses in the membrane, thereby damaging the membrane intactness. To further verify the structure variation of the treated membrane by excluding the hydrophilicity factor occurring in the liquid separation, gas permeation using H2, CO2, N2 and CH4 was conducted for the treated NaA zeolite membrane by Ag+ and K+, and all of the permeance of gases was found to be decreased, which was consistent with the result that was obtained in the PV dehydration. Thus, the narrowing of the accessible pore channel due to the larger cation replacement in the membrane was firmly validated. However, it has been found that the decrement percentage (90% for K+) in the gas permeation was far above that for the PV dehydration (10% for K+), and this could be explained by the higher importance of vaporization resistance of water molecules from liquid to vapor phases, which outweighs the vapor transport resistance in the pore channels in the membrane.
X. Gao and B. Gao conceived and designed the experiments; B. Gao and R. Shi and X. Wang performed the experiments; B. Gao and R. Ur Reshman analyzed the data; X. Gao and X. Gu supervised the project and provided research ideas. X. Gao and B. Gao contributed to the drafting of this paper.
This work is supported by National Natural Science Foundation of China (51502311), and the Doctorial Programs for Innovation and Entrepreneurship of Jiangsu Province.
Conflicts of Interest
The authors declare no conflict of interest.
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Figure 1. Cation treatment diagram of NaA zeolite membranes.
Figure 2. Different cation exchange model of the NaA-Type zeolite. (a) Monovalent cation and (b) Divalent cation.
Figure 3. Scanning electron microscopy (SEM) images of NaA zeolite membrane (a) and its cation treated surface morphologies by (b) KCl, (c) AgNO3, (d) NH4Cl, (e) LiCl and (f) NaCl solutions.
Figure 4. SEM images of NaA zeolite membrane surface morphologies treated by (a) CaCl2, (b) BaCl2, (c) ZnCl2 and (d) MgCl2 solutions.
Figure 5. X-ray diffraction (XRD) patterns of NaA zeolite seeds and after treatment seeds with (a) monovalent cations and (b) divalent cations.
Figure 6. SEM images of NaA zeolite particles (a) and ion-exchanged zeolite with (b) KCl, (c) AgNO3, (d) NH4Cl, (e) LiCl, (f) NaCl, (g) CaCl2, (h) BaCl2, (i) ZnCl2 and (j) MgCl2 solution treatment.
Figure 7. SEM images of NaA zeolite membrane treated by different concentration cations of AgNO3 (a) 0.05 M, (b) 0.1 M, NH4Cl (c) 0.05 M, (d) 0.1 M, KCl (e) 0.05 M and (f) 0.1 M.
Figure 8. PV dehydration of 90 wt % ethanol/water mixture with different cation-treated NaA zeolite membranes (a) KCl solution treatment, (b) AgNO3 solution treatment.
Figure 9. Energy-dispersive X-ray spectrometry (EDX) analysis for different cation-treated NaA zeolite membranes (a) AgNO3 solution treatment, (b) KCl solution treatment.
Figure 10. Gas permeance through (a) the original, (b) the AgNO3 treated and (c) the KCl solution treated NaA zeolite membrane as a function of the gas kinetic diameter at 25 °C and 2.0 bar.
Figure 11. Vapor permeation (VP) dehydration of different ethanol/water mixtures using salt treated NaA zeolite membrane. (a) AgNO3 solution and (b) KCl solution, where the vapor pressure was 1.4 bar under a temperature of 100 °C.
Table 1. Pervaporation of 90 wt % ethanol/water mixture through NaA-type zeolite membrane and its cation-exchanged membrane (exchange condition: 12 h at 60 °C and cation concentration of 0.1 M).
|Ion Valence State||Material||Processing Conditions||Fluxes/kg·m−2·h−1||Separation Factor|
|1||KCl||Un-exchange||4.05 ± 0.019||449 ± 2.4|
|Exchange||3.58 ± 0.023||1062 ± 12.8|
|NH4Cl||Un-exchange||7.42 ± 0.023||306 ± 1.1|
|Exchange||1.44 ± 0.005||38 ± 0.1|
|LiCl||Un-exchange||4.58 ± 0.019||208 ± 0.5|
|Exchange||leaking||1 ± 0.01|
|NaCl||Un-exchange||4.75 ± 0.023||449 ± 2.4|
|Exchange||4.83 ± 0.018||519 ± 3.1|
|AgNO3||Un-exchange||6.51 ± 0.027||548 ± 3.6|
|Exchange||5.98 ± 0.025||2136 ± 50.7|
|2||MgCl2||Un-exchange||5.05 ± 0.025||2167 ± 52.5|
|Exchange||1.99 ± 0.014||47 ± 0.1|
|BaCl2||Un-exchange||4.80 ± 0.024||208 ± 0.6|
|Exchange||5.19 ± 0.025||162 ± 0.4|
|CaCl2||Un-exchange||6.45 ± 0.025||306 ± 1.2|
|Exchange||6.07 ± 0.024||52 ± 0.1|
|ZnCl2||Un-exchange||5.06 ± 0.019||2156 ± 53.4|
|Exchange||2.90 ± 0.015||5 ± 0.04|
Table 2. The cation radius of the used salts.
|Cations||Hydrated Radius, Å ||Bare Radius, Å |
Table 3. Inductively coupled plasma (ICP) tests of NaA zeolites treated by different cations.
|Type||Relative Content of Na||Relative Content of Positive Charge a|
a [(Na+ + M+)/Al or (Na+ + 2M2+)/Al]. Each element represents its molar content.
Table 4. Pervaporation (PV) performances of the NaA zeolite membranes treated by various concentrations of monovalent cation solutions, by dehydrating 90 wt % ethanol/water mixture.
|M1||-||-||4.96 ± 0.03||449 ± 2.4|
|M1′||K+||0.05||4.45 ± 0.02||>10,000 ± 198.2|
|M1″||K+||0.1||3.58 ± 0.02||1062 ± 12.8|
|M2||-||-||6.51 ± 0.03||548 ± 3.6|
|M2′||Ag+||0.05||5.87 ± 0.03||>10,000 ± 198.2|
|M2″||Ag+||0.1||5.98 ± 0.03||2136 ± 50.9|
|M3||-||-||7.42 ± 0.03||306 ± 1.2|
|M3′||NH4+||0.05||4.95 ± 0.02||107 ± 0.2|
|M3″||NH4+||0.1||1.44 ± 0.01||38 ± 0.1|
Table 5. The contact angles of the NaA zeolite membrane treated by different cations.
|Cation Type||Exchanged NaA Zeolite Membranes||Contact Angle/θ|
|Original||NaA zeolite membrane||6.6°|
|Monovalent cation||Li+ exchanged NaA zeolite membrane||46.5°|
|K+ exchanged NaA zeolite membrane||43.0°|
|Ag+ exchanged NaA zeolite membrane||99.6°|
|Divalent cation||Zn2+ exchanged NaA zeolite membrane||72.6°|
|Mg2+ exchanged NaA zeolite membrane||18.3°|
|Ca2+ exchanged NaA zeolite membrane||46.2°|
|Ba2+ exchanged NaA zeolite membrane||33.5°|
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