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.
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1822 Chem. Mater. 1999, 11, 1822-1832
10.1021/cm990044a CCC: $18.00 © 1999 American Chemical Society
Published on Web 06/04/1999