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Simulations of Sol Gel Materials
(The following material is a brief summary of the project
description from our NSF grant "Multi-scale simulations of sol-gel
materials." - LDG)
Silica xerogels are candidate materials for
chemical sensors [1,2,3,4,5,6],
drug-delivery systems [7], and novel optical
[8,9,10,11]
and electrochromic[12,13]
applications. They are ubiquitous
in chromatography [14,15,16] and
catalysis [17,18,19],
and are widely used in studies of gas separations
[20,21]
and as a support matrix for nanocluster research
[22,23,19].
Aerogels are very high-porosity
materials [24,25,26]
used in particle detectors and as
thermal insulation [27,26],
in space probes (for comet-tail dust collection [28]),
and in many studies of fluids confined in random
media, especially helium and helium
mixtures[29,30].
Silica xerogels and aerogels prepared with
titanium[31,32],
vanadium[33,34,35], or
other metal dopants [36], or prepared from other oxides
entirely[37,38,17,11,39],
are promising materials for
catalysts and catalyst
supports[17,40,41,42]
and in electrochemical applications [38,43] and solar cells [12,44].
Thin films of xerogels
can be prepared by a variety
of processes, including spin-coating and dip-coating
[45]. Thin films
are used in sensors, electronics, optics, lubrication,
and other areas.
Templated materials arrived in 1992 with
the first preparation of
``MCM-41'' [46], demonstrating that highly regular
pore structures could be achieved on scales much larger than those
present in zeolites. Recent developments in templating
[47,48,49,50,51,52,53,54] and other micro-patterning
technologies[55] suggest the
rational design of porous media for different applications
[56,54].
A wide variety of microstructures have now been
prepared, including arrays of
simple geometries, bicontinuous networks, and hierarchical structures
[54,57].
More information on sol-gel stuff in general can be found at:
Simulations of gel processing
Simulation models, unlike experimental systems,
can be quickly and easily characterized with
many methods.
In a computational study, the systematic
optimization of synthesis conditions such as temperature and pH
to achieve a desired structure is much less time-consuming than
in the real world. Simulations also clearly
reveal why and how particular structures
appear. Thus, the design cycle would be greatly accelerated
by incorporating the predictive capacity of realistic computer modeling.
We are taking a multi-scale approach in this work, using
conventional molecular simulation at scales up to tens of
nanometers and a coarse-grained particulate model at
mesoscopic scales up to a few hundred nanometers.
The preparation and properties of xerogels[58,59] and aerogels [27,26]
have been comprehensively reviewed.
These materials are prepared through sol-gel processing,
in which precursor solutions undergo gelation,
aging and drying.
Xerogels are prepared by drying at subcritical
solvent conditions. Liquid-vapor
interfaces develop in the drying gel,
and forces due to surface tension cause substantial collapse
of the gel structure as liquid is removed. Aerogels are dried under
supercritical (or other [60])
conditions, leading to dry gels with porosity as high as 99.9%.
Consolidation, or heating at high temperatures, is used
to generate densified, non-porous materials for
optics and other applications.
Simulating the preparation of xerogels and aerogels involves
separate treatment of gelation, aging, drying, and for non-porous
materials, consolidation.
In the gelation step,
alkoxide gel precursors in aqueous solution are hydrolyzed,
and polymerize through alcohol or water producing
condensations:
The gel morphology is influenced by temperature,
the concentrations of each species (attention focuses on r,
the water/alkoxide molar ratio,
typically between 1 and 50), and
especially acidity:
- Acid catalysis generally produces weakly-crosslinked gels
which easily compact under drying conditions,
yielding low-porosity microporous (smaller than 2 nm)
xerogel structures (Figure 3a).
- Conditions of neutral to basic pH result
in relatively mesoporous xerogels after drying,
as rigid clusters a few nanometers across pack to form
mesopores. The clusters themselves may be microporous.
- Under some conditions, base-catalyzed and two-step
acid-base catalyzed gels (initial polymerization under
acidic conditions and further
gelation under basic conditions
[61,59])
exhibit hierarchical
structure and complex network topology (Figure 3c).
The initial stages of gelation,
when the average cluster size is very small, are best modeled with a purely
atomistic approach.
Considerable effort has already gone into
developing potential models
for this, with convincing results
[62,63,64,65,66,67,68].
Hierarchically structured gels and low-density
gels cannot be directly treated
with molecular models; a meso-scale approach must be used in this case.
Relatively dense gels can be modeled with either atomistic
simulations or coarse-grained simulations.
Schematic wet and dry gel morphologies and representative
transmission electron micrographs. (Adapted from
Brinker and Scherer,
Sol Gel Science, chapter 9, figures 3a-3d.
[58].)
Gel aging is an extension of the gelation step
in which the gel network is reinforced through further polymerization,
possibly at different temperature and solvent conditions.
Syneresis, the expulsion
of solvent due to gel matrix shrinkage, can occur during gel
aging.
Simulating aging requires the use of an approach
which can access long time scales. The ``activation-relaxation technique'' (ART)
[69,70,71]
is being implemented for this purpose. In
this method the system is repeatedly moved onto saddle-points in the
potential energy hypersurface (e.g., ``activation'') and then relaxed,
efficiently sampling many potential minima. These methods have
been successfully applied to amorphous silica
[70,71] and can be
implemented as an extension of a molecular
dynamics code. The relaxation step can be accomplished either by
numerical optimization or with molecular dynamics.
The gel drying process consists of removal
of water from the gel system, with simultaneous collapse of the gel structure,
under conditions of constant temperature, pressure, and humidity.
In the coarse-grained model (below) the equation of state is trivially calculable,
and drying is easily modeled by
choosing the solvent chemical potential to favor the vapor
phase and allowing the particle positions and
cell volume to slowly relax under the influence of solvent
capillary forces.
At the molecular scale, we can
model this process using an extension of the
``Gibbs Ensemble Monte Carlo'' technique for binary mixtures
[72,73,74],
where the mixture consists of water and atmosphere. The atmosphere will be
modeled as a single-component gas.
In this technique,
two simulation cells are coupled by mass-exchange moves, in which
molecules in one cell are transferred into the other cell. The volumes of the
cells fluctuate independently,
allowing specification of the pressure.
To model constant
humidity, the water content in the ``atmosphere''
cell will be controlled
by periodic removal of water molecules from the simulation. This is analogous
to using dehumidification in an experimental setup, and has the added benefit
of requiring only a relatively small ``atmosphere'' cell.
Xerogels are higher in free energy than conventional
amorphous silica (glass) and crystalline silica, as they have
a substantial internal surface area and associated surface
tension. During heating to temperatures above at least
700 C,
the dry gel shrinks substantially and becomes
similar to a melt-prepared glass.
Many such sintering experiments are done at
constant heating rate, which
hastens the densification [59,58].
Simulations of consolidation will use molecular models.
Both isothermal conditions and constant heating rates
can be accessed with standard molecular
dynamics simulations and ART as above.
Aerogels can be simulated using the same basic
techniques as xerogels,
except that the conditions during drying must be chosen
above the critical point of the water model.
Aerogel systems do not collapse (much)
under drying conditions, and supercritical gel drying will be
easier to simulate than the subcritical process.
High-porosity aerogels are only accessible
via the meso-scale model.
Experimental studies involving sol-gel nanocoating have
been reviewed recently by Caruso and
Antonietti[54]. The deposition of a
gel of several nanometers' thickness upon a surface or nanoparticle
allows one to generate novel nanostructured silica materials
(via templating, below), or to modify the surface
properties of the system.
Simulating such processes requires
the introduction of the surface or nanoparticle into the simulation
cell and suitable intermolecular potentials. For
deposition on planar surfaces, as in spin-coating, the concentration
of the sol increases as the solvent evaporates, which
can be accounted for using the drying methodology
discussed above.
When a gel is formed around a template which
is then removed, the process is known as casting, and
is the most commonly used templating strategy. One may
apply casting twice, generating a final material
with the same structure as the original template; this
is reminiscent of the ``lost-wax'' method of bronze
casting[75].
For gelation around a template, suitable
models for the template must be introduced.
Our exploratory simulations
in this area will focus on two systems with stiff and
soft templates, respectively: rigid
nanotubes [76],
which are easily modeled for these purposes,
and the quaternary ammonium surfactants used in preparation
of MCM-41 [46], parameterized using the
AMBER force field [77].
Meso-scale particulate model and simulations
We are investigating a coarse-grained model for sol-gel materials
which replaces each cluster with a single ``gel particle'',
while accounting for size variation of
clusters, aggregation through condensation reactions, and solvent effects.
The
particle-particle interaction will be relatively short-ranged and of a
shifted-center Lennard-Jones type,
this approximates particle-particle interactions by
the van der Waals interactions between atoms on their surfaces.
Particles may also form bonds upon contact, which are described
with Morse-type potentials. Particle sizes of 1-3 nm are appropriate.
The development of a solvent model suitable for drying simulations
is not trivial, and will be a major methodological contribution of the
proposed work. The solvent in the coarse-grained approach must (a)
possesses a liquid-vapor phase diagram and reasonable interfacial
properties, (b) be computationally inexpensive to solve, and (c) be
sufficiently general that solvent properties and solvent-gel
interactions can be fit to molecular simulation results.
These requirements can be met with a lattice-gas model
solved in the mean field approximation[78].
The fluid-fluid and fluid-gel interactions will be chosen to
mimic atomistic potentials, truncated at a few grid spacings,
and parameterized as necessary.
Solvent-particle interactions are
pairwise-additive, and within the
mean-field approximation are simply given by a summation over forces
exerted from lattice points within range of a given particle,
weighted by the mean-field solution of the densities at those
points. In drying simulations, constant
pressure can be modeled with volume-change
moves in which the simulation cell expands or contracts by one or
more lattice spacings.
In strongly inhomogeneous systems, large parts of the simulation
cell will be filled with bulk-like water or water vapor.
These lattice points can be simply fixed at
the appropriate equilibrium densities.
This will substantially speed up solution of the model.
Specifically, only lattice points within some
threshold distance of a gel particle will be considered ``active''.
As long as the pressure is either above condensation or
substantially below it, this
distance can be as small as several nanometers.
The use of more sophisticated multi-scale ``multigrid'' techniques
[79] to improve the
performance of the model will be investigated
and applied if possible.
Integration of molecular and meso-scale models
Integration of these two approaches requires two types of ``translation''.
The first is the use of the small-scale model to parameterize the large-scale
one. [The molecular model parameters could be determined, in
principle, ab initio, which would introduce a third,
subatomic, scale!] The second type
of translation moves in the other direction - once the meso-scale model
has been used to generate a structure, how can an atomic-scale
description of (part of) that structure be regenerated? This
fine-graining is necessary for simulations of molecular-scale processes
occurring within a mesoscopic system.
Dense xerogels, which can be treated with both
types of simulation, will be used to
parameterize the meso-scale model.
The initial stages of gelation in the molecular model can
be analyzed to create an ensemble of gel particles
by tabulation of the size distribution and dispersion of bonding sites.
Simulations of the meso-scale model can then be initiated,
and its parameters adjusted
to obtain agreement of the global structural
properties described above.
To reverse the process, one must replace a collection of
gel particles with atomistically modeled silica.
This is a non-trivial task, since it requires adding
atomic-scale information to the system, rather than removing it.
Two strategies will be employed. In the first, the particle configuration
will be used as a template for ``carving'' the atomistic model from
a block of amorphous silica, modeled separately. Such
templating schemes have been effectively used for
MCM-41 type materials [80], with
molecular simulation used to equilibrate the unrelaxed surfaces.
In the second approach, an ensemble of molecular clusters
can be extracted from molecular simulations
and used to replace gel particles in the
coarse-grained model, matched according to size
and arrangement of bonding sites. This would result in a molecular
model where only inter-cluster interactions are unrelaxed;
molecular dynamics can then be used to achieve mechanical stability.
Thus, in modeling the synthesis of a hierarchically structured
or low-density material, we begin with molecular simulations
of the gelation step. When the length-scale of aggregation in
this simulation exceeds a threshold fraction of the cell size,
the simulation would switch over to a coarse-grained model
with equivalent statistical properties, in a much larger
cell. This would be used for the remainder of gelation, aging,
and drying. For characterizations by
gas adsorption or surface structural analysis,
a molecular model could be regenerated from
the final coarse-grained configuration.
For small-angle scattering or network analysis, either
regenerated molecular models or
meso-scale models could be used.
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