The mechanisms of formation of organically modified (phenyl,
vinyl,
and methyl) silica materials with cubic Pm3̅n and hexagonal p6m periodic
mesostructures obtained in one step in the presence of the cetyltrimethylammonium
bromide (CTA+B) surfactant are reported in this study.
Understanding the way these complex materials form is difficult but
undoubtedly necessary for controlling the material structure and its
properties because of the combined presence of surface organic groups
and large surface areas. Here, the mechanism of formation is clarified
on the basis of the modeling of time-resolved in situ small angle
X-ray scattering (SAXS) experiments, with a specific focus on the
micelle evolution during material formation. Their fast self-assembly
is followed for the first time with a quick temporal resolution of
a few seconds using a third-generation synchrotron radiation source.
To better understand the behavior of the complex organic-containing
mesostructure, we perform a comparative study with the corresponding
organo-free, isostructural materials obtained from three different
surfactants (CTA+, CTEA+, and CTPA+) having a constant chain length (C16) and an increasing
polar head volume (met-, et-, and prop-). Numerical modeling of SAXS
data was crucial to highlighting a systematic sphere-to-rod micellar
transition, otherwise undetected, before the formation of the 2D hexagonal
phase in both organo-free and organo-containing systems. Then, two
different pathways were found in the formation of the cubic Pm3̅n mesostructure: either an ordering
transition from concentrated flocs of spherical micelles (from CTEA+ or CTPA+) for pure TEOS systems or a structural
transformation from an intermediate 2D hexagonal mesophase in organosilane
systems (from CTA+). Combining the comparison between organo-free
and organo-containing systems with numerical modeling, we find that
the hexagonal-to-cubic phase transition in the organically modified
materials seems to be strongly influenced not only by the obvious
presence of the organic group but also by the quicker and more massive
condensation kinetics of silicate oligomers on the CTA+ micellar surface. Finally, quite unexpectedly, we find a wormlike-to-sphere
micellar transition in the CTPA+ system.