1 TRANSFORMATION OF ZEOLITE NaY SYNTHESIZED 2 FROM RICE HUSK SILICA TO NaP DURING 3 HYDROTHERMAL SYNTHESIS 4 Supattra Khabuanchalad, Pongtanawat Khemthong, Sanchai 5 Prayoonpokarach and Jatuporn Wittayakun 6 School of Chemistry, Institute of Science, Suranaree University of Technology, Nakhon Ratchasima 30000. Tel.:0-4422-4256; Fax.: 0-4422-4185; Email: jatuporn@sut.ac.th Corresponding author 1 1 Abstract 2 Rice husk silica (RHS) powder with approximately 98% purity was used as 3 a silica source for zeolite syntheses. This study investigated the transformation of 4 zeolite NaY to zeolite NaP during hydrothermal synthesis at 100°C by fixing the 5 ratio of SiO2, Al2O3, and Na2O at 10:1:4.6, the optimum ratio for NaY synthesis. 6 The studied parameters included aging time (1, 2 and 3 days) and crystallization 7 time (1, 2, 3, 4 and 5 days). The transformation was observed by powder X-ray 8 diffraction (XRD). The aging time did not have much effect on the transformation 9 because when the crystallization time was fixed at one day, the synthesis with one 10 day aging produced pure phase NaY and that with 2 and 3 days produced only a 11 small amount of NaP. In contrast, changes of crystallization time, with fixed aging 12 time at one day, caused a significant transformation. The transformation of NaY to 13 NaP was observed in the synthesis with crystallization of 2 days and the amount of 14 NaP increased with the crystallization time. The NaY phase was not observed after 15 the crystallization time of 4 days and NaP with cleaner phase was obtained after 16 crystallization of 5 days. Consequently, the synthesis condition with aging time of 17 one day and crystallization time of five days was the optimum condition for the 18 transformation. Scanning electron micrographs at this optimum condition showed 19 narrow size distribution in the range of 7-14 µm. 20 21 Keywords : Zeolite synthesis, NaP, NaY, Rice Husk Silica, Crystallization time, 22 Aging time, Hydrothermal. 23 24 2 1 Introduction 2 Zeolite P class includes a series of synthetic zeolite phases such as cubic 3 configuration (also termed B or Pc) or tetragonal configuration (also termed P1). Its 4 conformation depends on the extra-framework ion, the state of dehydration and the 5 chemical composition (Nery et al., 2003). The zeolite P class has the typical oxide 6 formula: M2/nO·Al2O3·1.80-5.00SiO2·5H2O; where M is an n-valent cation, 7 normally an alkali metal. Crystallines of zeolite P with a Si/Al ratio from 0.9 to 8 1.33 are useful as molecular sieves and detergent builders (Huang et al., 2001). 9 Zeolite P can be synthesized from various silica sources and methods, for 10 examples, from a natural clay, Kaolinite and crystallization at 75–85°C 11 (Sathupunya et al., 2002); from coal fly ash by agitation at 120°C (Murayama et 12 al., 2002) or from sodium aluminate and sodium silicate solution by hydrothermal 13 treatment in microwave oven (Zubowa et al., 2007). 14 Sang et al. (2006) synthesized small crystals of zeolite NaY by 15 hydrothermal method and found that the crystallization at 120°C caused the 16 formation of zeolite NaP instead of zeolite NaY. Moreover, in the synthesis of 17 zeolite NaY with rice husk silica by our group, zeolite NaP was observed when the 18 crystallization at 100°C was longer than 48 hours (Wittayakun et al., 2008). Thus, 19 we investigated further to determine the synthesis conditions such as aging and 20 crystallization time that facilitated the transformation of NaY to NaP. 21 Here we report the transformation of zeolite NaY, synthesized with the 22 rice husk silica as reported previously, to NaP under different aging time (1,2 and 23 3 days) and crystallization time (1,2,3,4 and 5 days). The product from each 24 condition was characterized by X-Ray Diffraction (XRD). The sample with the 3 1 highest degree of transformation was characterized further by Fourier Transform 2 Infrared Spectroscopy (FTIR), Scanning Electron Microscopy (SEM), Laser 3 Diffraction Particle Size Analyzer (DPSA) and Simultaneous Differential Thermal 4 Analysis (TGA-DTA). 5 6 Experimental 7 Materials 8 Chemicals for the preparation of rice husk silica (RHS) and zeolite 9 synthesis were hydrochloric acid (37% HCl, Carlo-Erba), sodium aluminate (~55 – 10 56% of NaAlO2, Riedel-de Haën), sodium hydroxide (97% NaOH, Carlo-Erba), 11 and rice husk (local rice mill in Lampang, Thailand). The standard zeolites were 12 NaY with Si/Al molar ratio 5.7 (JRC with Tosoh Crop) and NaP (Fluka). 13 RHS was prepared by acid-leaching method reported previously 14 (Khemthong et al., 2007). Briefly, rice husk was washed and dried at 100°C 15 overnight; refluxed with 3 N HCl for 6 hours; filtered and washed again with water 16 until the filtrate was neutral and dried at 100°C overnight before the pyrolysis in a 17 furnace (Carbolite, CWF1200) at 550°C for 6 hours to remove the hydrocarbon 18 and volatile organic compounds. The obtained RHS contain amorphous silica with 19 approximately 98%wt purity. This RHS was dissolved in 3.5M NaOH solution to 20 produce Na2SiO3 for further zeolite synthesis. 21 Transformation of zeolite NaY to NaP 22 The transformation was investigated with the synthesis gel of zeolite NaY 23 prepared similarly to that of a previous work by Khemthong et al. (2008) by 24 mixing a seed gel and feedstock gel. The seed gel was prepared by dissolving 4 1 NaOH and NaAlO2 in DI water followed by the addition of Na2SiO3 solution and 2 kept at room temperature for 1 day. The feedstock gel was prepared with similar 3 method to that of the seed gel except that it was used immediately without aging. 4 In the synthesis, both gels were mixed to form overall gel, aged (kept undisturbed) 5 at room temperature, and crystallized at 100oC. After the crystallization step, the 6 resulting white powder was separated by filtration, washed and dried at 100oC. 7 The transformation of zeolite NaY to NaP was investigated by changing 8 aging time or crystallization time. In the first set, the overall gel were aged at 9 various time (1, 2, and 3 days) and crystallized for 1 day. These conditions were 10 chosen because the aging time of 1 day and the crystallization of 1 day was the 11 optimum condition for the synthesis of NaY. Another set of the experiment, the 12 effect of crystallization time was investigated by fixing the aging time at one day 13 and vary the crystallization time to 1, 2, 3, 4 and 5 days. 14 The product from each condition was characterized by XRD with nickel 15 filter Cu Kα radiation scanning from 4 to 50°. The XRD pattern was compared 16 with that of standard NaY and NaP. A product with the highest degree of 17 transformation was characterized further by Fourier Transform Infrared 18 Spectroscopy (FTIR) (Spectrum GX, Perkin-Elmer) using KBr as a medium. IR 19 spectra were scanned in the range of 4,000 cm-1 to 400 cm-1 with a resolution of 4 20 cm-1. Crystallite size and morphology were studied by Scanning Electron 21 Microscopy (SEM) with a JEOL JSM-6400 with applied potential 10 - 20 kV. 22 Particle size distribution of zeolites was determined by Laser Diffraction Particle 23 Size Analyzer (DPSA ) (Malvern Instruments, Mastersizer 2000) with the sample 24 dispersed in distilled water and analyzed by He-Ne laser. The standard volume 5 1 percentiles at 10, 50, and 90, or denoted as d(0.1), d(0.5), and d(0.9), respectively, 2 were recorded from the analysis and used to calculate the width of the distribution. 3 4 The width was calculated from the equation below: d (0.9) d(0.1) d (0.5) 5 Thermal stabilities were investigated by TGA on a Simultaneous 6 Differential Thermal Analysis (SDT 2690) by heating from 0oC to 1000°C with a 7 heating rate of 10°C/min in nitrogen flow (100 ml/min). 8 9 10 Results and Discussion Effect of aging time on transformation of NaY to NaP 11 The XRD patterns of the sample prepared at aging time of 1,2 and 3 days 12 were compared with that of NaY and NaP standards in Fig.1. The spectrum of one- 13 day aging sample was similar to that of standard zeolite Y without any other peaks 14 indicating that pure phase of NaY was obtained. With increased aging time, the 15 peaks at 12.5, 21.6 and 28.1 degree with low intensity emerged in the products 16 from two- and three-day aging time. The positions of those extra peaks were the 17 characteristic peaks of NaP, indicating that longer aging time than 1 day cause the 18 transformation of NaY to NaP. The transformation was not significant at these 19 conditions. It was found in the next section that the transformation occurred faster 20 at higher temperature. Thus, this transformation is endothermic. 21 22 6 1 Effect of crystallization time on the transformation of NaY to NaP 2 The effect of crystallization time on the transformation of NaY to NaP was 3 investigated with the aging time of 1-day because it showed no effect on the 4 transformation. The XRD patterns of products with crystallization time from one 5 to five days are displayed in Fig.2 along with that of standard zeolites. Only the 6 sample with 1-day crystallization time showed pure phase of NaY with the first 4 7 peaks at 6.5, 10.1, 15.6 and 23.7 degree. Characteristic peaks of NaP started to 8 emerge in the sample with 2-day crystallization and the intensities of those peaks 9 increased with longer crystallization time. The main peak of NaY was not 10 observed after crystallization for 4 days and NaP became a major component. 11 Because there was another phase along with NaP, this condition was not suitable 12 for the synthesis of zeolite P. 13 The first peak of NaP (2 = 12.5) from this study splitted into 2 peaks but 14 the position was similar to that of the standard NaP. It was possible that there 15 were two types of NaP in this sample and this was confirmed by SEM in the next 16 section. From literatures, the position of this peak of NaP with different 17 morphology was slightly different (within 0.5 degree) (Sathupunya et al. 2002), 18 Zubowa et al. 2007). 19 Characterization of product with 5- day crystallization. 20 The product obtained after 5-day crystallization contained NaP as major 21 component. It was further characterized by FTIR, SEM, DPSA, and TGA-DTA. 22 The FTIR spectrum in transmittance mode in Fig. 3 shows peaks at 3487, 1638, 23 1002, 773, 690, 571 and 465 cm-1. These peaks were similar to those of zeolite P 7 1 reported by Flanigen et al. (1971). The peaks at 571-460 cm-1 and 1002 cm-1 were 2 assigned to T-O (T = Si, Al) bending and Si-O, Al-O tetrahedral vibration, 3 respectively. The appearance of the peaks at 690, 1638 and 3487 cm -1 was 4 attributed to the double ring external linkage, vibration of water molecule and OH 5 stretching, respectively (Albert et al., 1998). 6 SEM micrograph in Fig. 4 illustrates the morphology of product from the 7 crystallization of 5 days. There were two types of particles: spherical and 8 multifaceted. The spherical shape was similar to that of NaP reported by 9 Sathupunya et al. (2002) and the multifaceted shape was similar to that of NaP 10 reported by Zubowa et al. (2007). The mixed morphology might be the reason that 11 the XRD peak at 12.5 degree (Fig. 2) splitted into two peaks. 12 Particle size distribution of the product with 5-day crystallization obtained 13 from DPSA is showed in Fig. 5. The major population had particle size in the 14 range of 4-25 µm with a small population with the size in the range of 0.7-3 µm. 15 Note that the particle size from DPSA were the size and distribution of bulk 16 particles which might composed of several small particles aggregated together, 17 and thus were different from the results from SEM which displayed images of 18 isolate crystals. 19 Thermal stability of the product with 5-day crystallization obtained from 20 TGA-DTA experiment is showed in Fig. 6. The weight loss during heating was 21 approximately 17% up to 400°C, accompanied by three endothermic peaks at 22 about 60, 100 and 150°C which attributed to the loss of water (Zubowa et al., 23 2007). Further weak endothermic peaks were observed at about 200, 300 and 24 600°C. These three peaks were resulted from a three step endothermic water loss 8 1 and at 900°C at which the zeolite P was irreversibly converted into nepheline, a 2 dense NaAlSiO4 phase (Albert et al., 1998). 3 4 Conclusions 5 Two parameters that affected the transformation of zeolite NaY to zeolite 6 NaP were aging time and crystallization time. When the crystallization time was 7 fixed at 1 day, the aging time of 1 day was suitable to produce pure phase of 8 zeolite NaY whereas 2 and 3 days aging time produced a small amount of NaP. 9 The crystallization time showed more significant effect on the transformation. The 10 phase of NaY was not observed after crystallization for 4 days and crystallization 11 time of 5 days, NaP was a major product. 12 13 With 5-day crystallization time, NaP was a major product with trace amount of NaY. 14 15 Acknowledgements 16 Research Funding for this research was from Suranaree University of 17 Technology Research Fund, SUT Scholarship for Outstanding Students and 18 Scholarship from Commission on Higher Education, Ministry of Education for S. 19 Khabuanchalad. 20 21 9 1 References 2 Albert, B.R., Cheetham, A.K., Stuart, J.A., and Adams, C.J. (1998). Investigation 3 on P zeolites:Synthesis, characterization and structure of highly crystalline 4 low-silica NaP. Microporous and Mesoporous Materials., 21:133-142. 5 6 7 8 Flanigen, E.M., Khatami, H., and Szymanski, H.A. (1971). Molecular sieve zeolites. Advances in Chemistry Series., 101:201-228. Huang, S., Jing, S., Wang, J., Wang, Z., and Jin, Y. (2001). White silica obtained from rice husk in fluidized propellant bed. Powder Technology., 117:232-238. 9 Khemthong, P., Prayoonpokarach, S., Wittayakun, J. (2007). Synthesis and 10 Characterization of Zeolite LSX from Rice Husk Silica, Suranaree Journal of 11 Science and Technology, 12(4), in press. 12 Murayama, N., Yamamoto, H., and Shibata, J. (2002). Mechanism of zeolite 13 synthesis from fly ash by alkali hydrothermal reaction. International Journal of 14 Mineral Processing., 64:1-17. 15 Nery, J.G., Mascarenhas, Y.P., and Cheetham, A.K. (2003). A study of highly 16 crystalline, low-silica, fully hydrated zeolite P ion exchanged with (Mn2+, 17 Cd2+, Pb2+, Sr2+, Ba2+) cations. Microporous and Mesoporous Materials., 18 57:229-248. 19 Sathupunya, M., Gularib, E., and Wongkasemjit, S. (2002). ANA and GIS zeolite 20 synthesis directly from alumatrane and silatrane by sol-gel process and 21 microwave technique. Journal of the European Ceramic Society., 22:2305– 22 2314. 10 1 Wittayakun, J., Khemthong, P., Prayoonpokarach, S., (2008). Synthesis and 2 Characterization of Zeolite NaY from Rice Husk Silica, Korean Journal of 3 Chemical Engineering, 25(4), in press. 4 Zubowa, H.L., Kosslick, H., Muller, D., Richter, M., Wilde, L., and Fricke, R. 5 (2007). Characterization of phase-pure zeolite NaP from MCM-22-type gel 6 compositions under microwave radiation. Microporous and Mesoporous 7 Materials., “Article in press”. 8 9 11 1 List of Figures 2 Figure 1 Normalized XRD patterns of zeolite synthesized with different aging time 3 compared to the patterns of standard zeolite Y and zeolite P 4 Figure 2 Normalized XRD patterns of zeolite synthesized with different 5 crystallization time compared to the patterns of standard zeolite Y and 6 zeolite P 7 8 9 10 11 12 13 14 Figure 3 FTIR spectrum of product obtained from 1-day aging and 5-day crystallization time Figure 4 SEM image of products obtained from 1-day aging and 5-day crystallization time Figure 5 Particle size distribution of product obtained from 1-day aging and 5-day crystallization time Figure 6 TGA-DTA thermogram of product obtained from 1-day aging and 5-day crystallization time 15 16 12 1 2 3 5 6 7 Intensity (Arbitrary Unit) 4 standard zeolite P 3 days 2 days 1 day 8 standard zeolite Y 9 0 5 10 15 20 25 30 35 40 10 2 Theta 11 12 Figure 1 Normalized XRD patterns of zeolite synthesized with different aging 13 time compared to the patterns of standard zeolite Y and zeolite P 14 15 16 13 1 2 4 5 6 Intensity (Arbitrary Unit) 3 standard zeolite P 5 days 4 days 3 days 2 days 1 day 7 standard zeolite Y 8 9 0 5 10 15 20 25 30 35 40 2 Thata 10 11 Figure 2 Normalized XRD patterns of zeolite synthesized with 12 different crystallization time compared to the patterns of standard zeolite Y 13 and zeolite P 14 15 14 1 2 3 5 6 7 Transmittance (%) 4 1,638 773 690 571 3,487 465 8 1,002 9 10 11 12 4,000 3,600 3,200 2,800 2,400 2,000 1,600 1,200 800 400 Wave number (cm-1) 13 14 Figure 3 FTIR spectrum of product obtained from 1-day aging and 5-day 15 crystallization time 16 17 15 1 2 3 4 Figure 4 SEM image of products obtained from 1-day aging and 5-day 5 crystallization time 6 7 16 1 Volume (%) 30 100 90 80 70 20 60 50 40 10 30 20 10 0 0.01 2 0 0.1 1.0 10.0 100.0 1000.0 Particle Diameter (µm.) 3 4 Figure 5 Particle size distribution of product obtained from 1-day aging and 5 5-day crystallization time 6 7 17 1 2 Figure 6 TGA-DTA thermogram of product obtained from 1-day aging and 3 5-day crystallization time 4 18