Achieving controls on the self-assembly
of cationic and block copolymer
micelles has significant implications for advancing novel material
systems for energy, environmental, and biological applications and
for tuning fluid flow behavior in subsurface geologic environments.
While it is known that the aggregation of micelles is influenced by
the composition of the surrounding fluid, the influence of a solid
interface has been less explored. In this study, we probe the organization
of cetyltrimethylammonium bromide (CTAB) micelles in the absence and
presence of the Pluronic P123 block copolymer and quartz substrate
using transmission and grazing-incidence small-angle X-ray scattering
measurements and classical molecular dynamics (MD) simulations. In
the absence of the quartz interface, CTAB with and without P123 molecules
assemble as ellipsoid core–shell micelles. Densification of
the core on adding P123 is noted from the decrease in the core radius
from 15.9 to 14.6 Å. The presence of a quartz substrate causes
the micelles to elongate, which is noted by the emergence of a power-law
slope in the low q region (<0.02 Å–1). Moreover, in the presence of both P123 and the quartz substrate,
the micelle shape changes from ellipsoid core–shell to cylindrical
core–shell, and a significantly higher number of aggregates
are formed. The higher number of aggregates, and faster aggregation
kinetics are linked to the organization of the solvent structures
as noted from the MD simulations. These findings demonstrate the effects
of adding a block copolymer and including a quartz substrate on the
self-assembly of cationic (CTAB) micelles, which can be used to inform
the design of functional material systems that harness surfactant
chemistries.