Liancheng Binga,
Guangjian Wang*a,
Fang Wanga,
Xiufeng Liub and
Baoquan Zhang*b
aSchool of Chemical Engineering, Qingdao University of Science and Technology, Qingdao, Shandong 266042, China. E-mail: wgjnet@126.com; Tel: +86 532 85889106
bState Key Laboratory of Chemical Engineering, School of Chemical Engineering and Technology, Tianjin University, Tianjin 300072, China. E-mail: bqzhang@tju.edu.cn; Tel: +86 22 27408785
First published on 6th June 2016
Piece-like SAPO-34 crystals were directly assembled into a highly oriented seed layer on the α-Al2O3 substrate by using spin-coating, and then a preferentially oriented SAPO-34 membrane with no large defects was prepared on an oriented SAPO-34 seed layer by secondary hydrothermal microwave growth. The synthesized membrane exhibited a high CO2 permeance of 1.57 × 10−6 s−1 Pa−1 at 302 K and 138 kPa pressure drop, with a CO2/CH4 separation selectivity of 109.
Oriented zeolite membranes exhibit superior performance compared to randomly oriented ones. For example, appropriate orientation of crystals can effectively enhance the mass transport and mechanical stress of the membranes which related to membrane separation and chemical sensors.10 Despite great effort over the past several years, challenges still exist to fabricate high-quality oriented zeolite membranes. Compared with other methods, including in situ hydrothermal synthesis, the secondary growth method is more reliable for achieving preferentially oriented membranes because the membrane microstructure (i.e., thickness, grain size, crystal orientation) can be easier controlled by decoupling the nucleation and crystal growth steps during membrane formation.
In the preparation of oriented zeolite membranes by secondary growth starting from randomly oriented seed layers, grains grow out rapidly along their fastest growth direction, while grains in other orientations grown slower will be gradually buried by faster grains. The final membrane orientation is attributed to the competitive growth of grains along different crystallographic directions. During secondary growth, the orientation of the seed layer is critical for the preparation of membranes with the same orientation and often enhances their separation performance by providing desired pore channels perpendicular to the membrane surface. Tsapatsis and co-workers prepared oriented ZSM-5 membranes by secondary growth of b-oriented monolayers. Compared with c-oriented membranes synthesized under the same conditions except for the use of randomly oriented seed layers, these b-oriented membranes are thinner, less defective and more robust to crack formation.11 Huang et al. reported that an oriented AlPO4 LTA zeolite membrane prepared using a highly oriented AlPO4 LTA monolayer showed superior gas separation performances compared to a random AlPO4 LTA membrane.12 SAPO-34 has a CHA framework topology and a three-dimensional 8-ring channel system with a pore diameter of 0.38 nm. The pores in SAPO-34 are essentially the same size as the kinetic diameter of CH4 (0.38 nm), so the small-pore SAPO-34 favors the diffusion of CO2 (0.33 nm) over CH4. Besides, SAPO-34 adsorbs CO2 more strongly than CH4, which could improve separation performance in CO2/CH4 binary mixtures when it is used as a membrane. SAPO-34 has straight channels with an estimated pore opening of 0.38 nm × 0.38 nm along its a-axis (Scheme 1), so the growth of a-oriented crystals in a membrane can effectively reduce the mass transport resistance and control the thermal stress when related to gas separation. Zhu et al.13 synthesized an a-oriented SAPO-34 membrane on a macroporous stainless-steel-net. This oriented membrane displayed CO2/CH4 separation selectivity of less than 10, although CO2 permeance was as high as 2.5 × 10−6 mol m−2 s−1 Pa−1.
Das and co-workers14–16 prepared preferentially oriented SAPO-34 membranes on clay-Al2O3 supports by selective deposition of oriented seed crystals, followed by epitaxial secondary growth. In this procedure, cubic SAPO-34 particles (thicker than 1 mm) were used as seeds, and the membrane thickness was found to be about 25 μm. Considering the shortest dimension perpendicular to the large basal plane in piece-like particles would be beneficial in the formation of an oriented layer, Choi et al.17 selectively deposited piece-like Si-CHA particles onto the α-Al2O3 disk by a sonication-assisted method with the successful formation of uniform h0h-out-of-plane-oriented Si-CHA layers. Furthermore, compared with the cubic crystals, the nanosized piece-like crystals would be beneficial in decreasing the thickness of the membrane. Unlike other strategies, including in situ growth, seed growth, convective assembly and electric-field-driven assembly, spin-coating is a simple, quick, effective and highly reproducible strategy to prepared zeolite layer. In the present work, an oriented SAPO-34 seed layer was prepared by spin-coating the α-Al2O3 substrate with piece-like SAPO-34 crystals, and then a preferentially SAPO-34 membrane was prepared on an oriented SAPO-34 seed layer under microwave irradiation, and was used for the separation of equimolar CO2/CH4 gas mixtures.
The SAPO-34 crystals were synthesized by using a microwave irradiation method and the synthesis procedure was similar to that described previously.18 After hydrothermal treatment at 453 K for 2 h, pure SAPO-34 crystals with high crystallinity are formed (Fig. 1). The SAPO-34 crystals that are used as seeds for membrane preparation are piece-like with the approximate dimension of 400 × 400 × 40 nm (Fig. 2a). An a-oriented SAPO-34 seed layer was prepared as follows. The seed suspension with a concentration of 0.5 wt% in ethanol was irradiated with ultrasound for 1 h. The suspension was then spin-coated onto the treated α-Al2O3 substrate with a spinning rate of 1280 rpm for 40 s. After dried at 333 K overnight, uniform layer was obtained. Fig. 2b shows the SEM top view of the SAPO-34 seed layer deposited by spin-coating. The porous α-Al2O3 support surface is completely covered by uniform SAPO-34 crystals, and the seed layer is preferentially oriented. XRD pattern further verifies the formation of a preferentially a-oriented SAPO-34 seed layer on the α-Al2O3 support surface (Fig. 1). Compared with the randomly oriented XRD pattern of SAPO-34 zeolite powder, the oriented SAPO-34 seed layer shows only (100) peak besides the α-Al2O3 signals from the substrate.
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Fig. 1 XRD patterns of (a) SAPO-34 crystals, (b) α-Al2O3 substrate, (c) SAPO-34 seed layer and (d) SAPO-34 membrane. The asterisk (*) indicates the XRD peaks of a bare α-Al2O3 support. |
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Fig. 2 SEM images of (a) SAPO-34 seeds, (b) top-view of SAPO-34 seed layer, (c) top-view and (d) cross-section of SAPO-34 membrane. |
Zhu and co-workers prepared a-oriented SAPO-34 membrane by using conventional heating.13 In contrast to this traditional method, the use of microwave heating allows faster crystal nucleation and crystal growth in the form of powders or membranes. Fig. 2c shows the SEM top view of the preferentially oriented membrane prepared by microwave-assisted secondary growth. After microwave-assisted secondary growth for 4 h, zeolite seeds on the surface have grown bigger and merged with each other, and no visible cracks and grain boundary defects are observed. Meanwhile, the SAPO-34 membrane still keeps preferentially oriented. From the cross section shown in Fig. 2d, the membrane is dense through the whole membrane thickness, and the thickness is about 4 μm. The XRD pattern of SAPO-34 membrane is shown in Fig. 1. As clearly seen in the figure, the peak at 9.4° corresponding to the (100) peak is still observed with an enhancement in the peak intensity. It suggests that the SAPO-34 membrane retains the preferred orientation, which is in good agreement with the result of the SEM images.
The FT-IR spectra of the oriented SAPO-34 membrane before and after calcination are shown in Fig. 3. The bands at around 2800–3200 and 1300–1500 cm−1 are attributed to the template TEAOH, which disappeared after calcinations at 390 °C in flowing air.19 The low defect concentration of the SAPO-34 membrane could be confirmed by measuring the single gas permeance for i-C4H10.20 Fig. 4 shows the single gas permeances through the oriented membrane as a function of molecular kinetic diameter at 302 K with a 0.4 MPa pressure difference. After template removal from SAPO-34 membrane, the single gas permeances of molecules larger than CO2 decrease with the increase in kinetic diameter, which indicates that the SAPO-34 membrane has a relatively narrow pore size distribution and its gas permeation behavior can be controlled by zeolitic pores. Therefore, CH4 molecules can permeate through SAPO-34 membrane to only a small extent, and n-C4H10 and i-C4H10 (0.43 and 0.50 nm, respectively) hardly at all, which indicates that the SAPO-34 membrane prepared in this study had no large defects. As shown in Fig. 4, CO2 permeance is higher than those of He and H2, although the kinetic diameter of CO2 is larger than that of He (0.26 nm) and H2 (0.29 nm). Because CO2, He and H2 are smaller than SAPO-34 pores, the size difference among CO2, He and H2 has a small effect on determining the order of their permeances. Thus, differences in adsorption are more important in determining permeance. According to the adsorption isotherms on SAPO-34 power reported by Noble and co-workers,21–23 SAPO-34 crystals adsorb CO2 much more strongly than He and H2. So the single-gas permeation of CO2 is more than that of He and H2 though CO2 is the larger molecule.
The separation performance of the SAPO-34 membrane with a thickness of 4 μm was measured by separating the equimolar CO2/CH4 binary gas mixture after organic templates were removed. As shown in Table 1, the CO2/CH4 selectivity and CO2 permeance are 109 and 1.57 × 10−6 mol m−2 s−1 Pa−1 respectively at 138 kPa pressure drop and 302 K. Table 1 also lists the CO2/CH4 separation of the SAPO-34 membranes in previous studies.13,18,24,25 The synthesized thick membrane shows a relatively high CO2 permeation as compared to previously reported SAPO-34 membranes with random orientations. For a preferentially oriented membrane, the pores are more aligned and the mass transport resistance through the aligned channel is less than that of the zig–zag path of the non-aligned randomly oriented pores. As a result, CO2 permeance through the membrane is enhanced. Lower CO2 permeance but higher CO2/CH4 selectivity compared to membrane reported in the literature13 is due to the use of the homogeneous and dense SAPO-34 membrane in this study.
Membrane | Orientation | Thickness (μm) | Temperature (K) | Pressure drop (kPa) | CO2 permeance (10−6 mol m−2 s−1 Pa−1) | CO2/CH4 selectivity | References |
---|---|---|---|---|---|---|---|
SAPO-34 | Random | 2.5 | 295 | 138 | 0.40 | 115 | 24 |
SAPO-34 | Random | 3 | 303 | 100 | 1.20 | 95 | 25 |
SAPO-34 | Random | 2.5 | 302 | 138 | 0.91 | 130 | 18 |
SAPO-34 | a | 10–20 | Room temp | 120 | 2.52 | 9.3 | 13 |
SAPO-34 | a | 4 | 302 | 138 | 1.57 | 109 | This work |
Footnote |
† Electronic supplementary information (ESI) available: Experimental and characterization details. See DOI: 10.1039/c6ra09018d |
This journal is © The Royal Society of Chemistry 2016 |