Time-Resolved in Situ X-ray Powder Diffraction Study of the Formation of Mesoporous Silicates Stephen O’Brien, Robin J. Francis, Andrew Fogg, Dermot O’Hare,* ,† Nanae Okazaki, and Kazuyuki Kuroda ‡,§ Inorganic Chemistry Laboratory, University of Oxford, South Parks Road, Oxford, OX1 3QR, U.K., Department of Applied Chemistry, Waseda University, Ohkubo 3, Shinjuku-ku, Tokyo 169, Japan, and Kagami Memorial Laboratory for Materials Science and Technology, Waseda University, Nishiwaseda 2, Shinjuku-ku, Tokyo 169, Japan Received January 25, 1999. Revised Manuscript Received April 12, 1999 In situ, time-resolved energy-dispersive X-ray diffraction has been used to investigate the formation of the mesoporous silicates FSM-16 and MCM-41. The data suggest that the silica- surfactant mesophases formed are highly dependent on the reactant medium, the effect of the silica source being one of the main determining factors. Kanemite, a layered polysilicate, proves to be an excellent silicate source, giving rise to relatively ordered mesophases and subsequent highly ordered mesoporous silicate products. The time-resolved in situ X-ray diffraction data of the kanemite-alkytrimethylammonium system indicated that the silica- surfactant mesophase precursor to FSM-16 forms from a medium containing a number of intercalated silicate phases, while in contrast, the hexagonal mesophase precursor to MCM- 41 forms from a medium containing no other ordered silicate-surfactant phases detectable by in situ X-ray diffraction. Introduction The determination of mechanistic information relat- ing to solid-state reactions should ultimately lead to a more rational approach to the synthesis of microporous and mesoporous materials. Understanding how mol- ecules and ions can preferentially organize themselves under certain conditions to form extended crystalline solid structures is a well-established goal in modern inorganic chemistry. However, it is often difficult to acquire sufficient data to substantiate a particular mechanistic theory that can adequately describe het- erogeneous reactions (i.e., involving solid and liquid reagents): Such systems involve a complicated variety of species, nucleation, and crystallization processes. In situ methods can often provide invaluable insights into the nature and the rate of transformation from reac- tants to products and can therefore shed light on the stages of nucleation and the molecular species involved. 1 The mechanisms involved in the formation of meso- porous silicates are an important issue in contemporary solid-state chemistry. An additional feature to the problem of examining these reaction mechanisms is that the concept of templating is applied to aggregates, as opposed to single molecules, and involves a variety of inorganic-organic species. Some of the currently re- ported synthetic routes to silica-surfactant mesophases which are precursors to mesoporous silicates are sum- marized in Table 1. It appears that there seems to be effectively two independent routes to the synthesis these materials. The synthetic approach originally reported by Beck, Vartuli, and co-workers 2 led to the development and investigation of the M41S family of mesoporous molec- ular sieves. 3-6 The three phases obtained from the M41S synthesis methods are hexagonal (MCM-41), cubic (MCM-48), and lamellar (MCM-50), whose microscopy and diffraction data are reminiscent of surfactant/water binary systems. This has led to many extensive in situ NMR studies of the systems, 7-9 and prompted Beck et al. to initially propose a liquid crystal template (LCT) mechanism. 3 Beck et al. describes the process as the formation of liquid crystals by the surfactants, followed by condensation of the silicate framework around the University of Oxford. Department of Applied Chemistry, Waseda University. § Kagami Memorial Laboratory for Materials Science and Technol- ogy, Waseda University. (1) Cheetham, A. K.; Mellot, C. F. Chem. Mater. 1997, 9, 2269- 2279. (2) Kresge, C. T.; Leonowicz, M. E.; Roth, W. J.; Vartuli, J. C.; Beck, J. S. Nature 1992, 359, 710-712. (3) Beck, J. S.; Vartuli, J. C.; Roth, W. J.; Leonowicz, M. E.; Kresge, C. T.; Schmitt, K. D.; Chu, C. T. W.; Olson, D. H.; Sheppard, E. W.; Mccullen, S. B.; Higgins, J. B.; Schlenker, J. L. J. Am. Chem. Soc. 1992, 114, 10834-10843. (4) Beck, J. S.; Vartuli, J. C.; Kennedy, G. J.; Kresge, C. T.; Roth, W. J.; Schramm, S. E. Chem. Mater. 1994, 6, 1816-1821. (5) Vartuli, J. C.; Schmitt, K. D.; Kresge, C. T.; Roth, W. J.; Leonowicz, M. E.; Mccullen, S. B.; Hellring, S. D.; Beck, J. S.; Schlenker, J. L.; Olson, D. H.; Sheppard, E. W. Chem. Mater. 1994, 6, 2317-2326. (6) Kresge, C. T.; Vartuli, J. C.; Roth, W. J.; Leonowicz, M. E.; Beck, J. S.; Schmitt, K. D.; Chu, C. T. W.; Olson, D. H.; Sheppard, E. W.; Mccullen, S. B.; Higgins, J. B.; Schlenker, J. L. Stud. Surf. Sci. Catal. 1995, 92, 11. (7) Chen, C.-Y.; Burkett, S. L.; Davis, M. E.; Li, H. X. Microporous Mater. 1993, 2, 27-34. (8) Steel, A.; Carr, S. W.; Anderson, M. W. J. Chem. Soc., Chem. Commun. 1994, 1571-1572. (9) Firouzi, A.; Atef, F.; Oertli, A. G.; Stucky, G. D.; Chmelka, B. F. J. Am. Chem. Soc. 1997, 119, 3596-3610. 1822 Chem. Mater. 1999, 11, 1822-1832 10.1021/cm990044a CCC: $18.00 © 1999 American Chemical Society Published on Web 06/04/1999