S. Che et al.
A zone around C14GluA/NaOH/TMAPS 0.2:0.3:0.5 in the
diagram gives rise to a undefined cage-type mesophase,
which was formed at a pH of 6.2–7.4. The hydrolysis of
TMAPS and silica source TEOS was very low within this
range of pH, which hindered the self-organization of the or-
ganic/inorganic species and the formation of stable ordered
mesophases. The mesophase formed is unstable and easily
collapses during the thermal treatment at 5508C. The struc-
ture is not fully understood and is under further investiga-
tion. (see the HRTEM images in Figure S4 of the Support-
ing Information)
a line in direction c in the diagram, and the structure of the
mesoporous silica obtained changes from bicontinuous cubic
¯
¯
Pn3m to 2D hexagonal p6mm, cubic Fd3m, an undefined
¯
cage-type phase, and cubic Fm3m; from 2D hexagonal
p6mm to cubic Pm3n and tetragonal P42/mnm. These
¯
changes of mesophases show a dramatic mesopore geometry
change from bicontinuous to cylindrical and further cage-
types, with an increase of the organic/inorganic interface
curvature.
Mesophase formation dominated by the organic/inorganic
interface curvature: As a conclusion of the above discus-
sions, the bicontinuous cubic phase, which has a low organ-
ic/inorganic-interface curvature (1/2<g<1), has been ob-
tained in the zones with low surfactant ionization degree
(NaOH/C14GluA=0.45–0.62) showing an initial pH of 5.0–
5.2. The 2D-hexagonal phase, whose organic/inorganic-inter-
face curvature (g=1/2) is larger than bicontinuous cubic,
was synthesised in the zones with a moderate ionization
degree of surfactant (NaOH/C14GluA=0.62–0.86), with an
initial pH of 5.2–5.6. Increasing the ratio of NaOH/C14GluA
to 0.86–2.7, or increasing the pH of synthesis system to 5.6–
11.0 lead to the formation of cage-type mesophases with the
largest organic/inorganic-interface curvature (g=1/3).
Notably, in Figure 1, composition points in zone a gives
¯
¯
¯
rise to a coexistence of Fd3m, Pm3n, P42/mnm, and Fm3m
(Supporting Information, Figure S5); composition points in
zone b give a mixture of cubic and 2D-hexagonal phase
(Supporting Information, Figure S6); and a mixed phase
¯
comprising bicontinuous cubic Pn3m and 2D hexagonal
p6mm could be found in zone g (Supporting Information,
Figure S7). However, in the zones d, e, or z, mesoporous sili-
cas could not be formed because the mole fraction of
NaOH, C14GluA or TMAPS, respectively, was too high.
The diverse mesophases, as have been described above,
were achieved in the same synthesis system but different
composition ratios. It proved the versatility of the meso-
phase formation by using the diprotic anionic surfactant
CnGluA as the SDA by means of the co-structure-directing
method. On the other hand, the diverse mesophases formed
in the same system make it possible for the study on the
structure occurrence, dependence, and formation mecha-
nism.
In our earlier works[13,19] we have described that in the
synthesis of AMS, higher alkalinity favours the formation of
mesophases with high organic/inorganic-interface curvature,
owing to the lager ionization degree of the anionic surfac-
tant. From the full-scaled synthesis-field diagram shown in
Figure 1, this change of mesophase from bicontinuous cubic
to 2D hexagonal and further cage-type, triggered by the in-
crease of the ionization degree of the surfactant, proves the
dominating rule of the organic/inorganic-interface curvature
on the mesophase determination.
Effect of the synthesis composition on the mesostructure:
From the diagram shown in Figure 1, it can be inferred that
the phase fields are strip-like, lie in the sector zones, and
employ C14GluA/NaOH/TMAPS 0:0:1 as the vertex (as the
shadow zones in Figure 1 shows). It is known that when
changing the composition point down a line, starting at the
point C14GluA/NaOH/TMAPS 0:0:1 in the synthesis-field
diagram, the ratio of NaOH/C14GluA is kept constant and
the ratios of TMAPS/NaOH and TMAPS/C14GluA are de-
creasing. Therefore, the strip-like distribution of the meso-
phases in the diagram indicates that the determining factor
of the mesophase formation is the ionization degree of the
surfactant (NaOH/C14GluA); the effect of the amount of
TMAPS in the synthesis gel on the mesophase formation is
not prominent. The change in the fraction of TMAPS in the
synthesis gel could not dramatically change the mesophase
obtained, especially in the zones of bicontinuous cubic and
2D hexagonal. Notably, the mesophase changes could be
also observed in the zones of the cage-type mesophase from
tetragonal P42/mnm to an undefined cage-type phase and
Mesophase formation affected by the mesocage–mesocage
electrostatic interactions: The organic/inorganic-interface
curvature dominates the change of mesophase from bicon-
tinuous cubic to 2D hexagonal and further cage-type; how-
ever, it cannot explain the packing manner of the mesocages
in the cage-type zone and the formation mechanism of dif-
ferent 3D mesostructures, which has been long pursued by
scientists. Our system affords various cage-type mesostruc-
tures by simply varying the mole fraction, which provides
experimental foundations to propose a possible formation
mechanism as described in Scheme 1.
In the formation of cage-type mesostructures anionic sur-
factant molecules form micelles to reduce the free energy,
which makes a negatively charged surface. On the outside of
this surface, to balance the negative charge, positively
charged CSDA distributes in both the Stern layer in which
immobile CSDA cations are tightly bonded to the surface
and the diffuse layer in which mobile CSDA cations weakly
interact with the charged surface (Scheme 1). The micelles
and the inorganic species in the Stern layer, which together
are defined as a “mesocage”, are then packed by certain
means with the hydrolyzed TEOS to form the mesostruc-
¯
¯
from cubic Pm3n to cubic Fd3m, as a result of an increase
of the mole fraction of TMAPS in the C14GluA/TMAPS/
NaOH tri-component system.
When keeping the mole fraction of TMAPS constant in
the C14GluA/TMAPS/NaOH system and increasing the
NaOH/C14GluA ratio, the composition point changes down
11426
ꢀ 2008 Wiley-VCH Verlag GmbH & Co. KGaA, Weinheim
Chem. Eur. J. 2008, 14, 11423 – 11428