The formation and growth of tetrapropylammonium-templated crystal
nuclei of silicalite from a clear
homogeneous solution was recorded in situ as a function of time at
temperatures between 90 and 115 °C
using small-angle X-ray scattering (SAXS). The kinetics of the
nucleation process was studied and give an
apparent activation energy of 70 kJ mol-1.
A small-angle neutron scattering (SANS) contrast variation
study
confirms that the nuclei contain the tetrapropylammonium template in
the expected stoichiometry of the
completed crystal. Infrared spectroscopy provides evidence that
the silicalite framework structure is present
in the nuclei. Our SAXS and SANS data both show that a cylindrical
form factor gave the best fit to the
measured scattering functions for the particles that developed from
nucleation to the end of the induction
period. Dynamic light scattering measurements were used to follow
the crystal growth in the 100−6000 Å
size domain, beyond the range of the SAXS measurements. Scanning
electron microscopy was also used to
determine crystal morphology and particle sizes of sedimented crystals
and freeze-dried solutions. We have
proposed a detailed model for the nucleation and crystallization
processes wherein cylindrical primary nuclei,
2 × 2 unit cells in cross section, form very quickly upon heating and
then assemble end-to-end along the
crystal c axis into 330 Å long primary crystallites during
an extended induction period, followed by the
aggregation of the primary crystallites into polycrystalline ellipsoids
of length 6000 Å.
Protolytic cracking of ethane in zeolites has been investigated using quantum-chemical techniques and a
cluster model of the zeolite acid site. An aluminosilicate cluster model containing five tetrahedral (Si, Al)
atoms (5T) was used to locate all of the stationary points along a reaction path for ethane cracking at the
HF/6-31G(d), B3LYP/6-31G(d), and MP2(FC)/6-31G(d) levels of theory. The cracking reaction occurs via a
protonated structure that is a carbonium-like ion and is a transition state on the potential energy surface. The
activation barrier for cracking calculated at each level of theory was refined by including (i) vibrational
energies at the experimental reaction temperature of 773 K, (ii) electron correlation and/or an extended basis
set at the B3LYP/6-311+G(3df,2p) or MP2(FC)/6-311+G(3df,2p) levels, and (iii) the influence of the
surrounding zeolite lattice from a 58T cluster model of the zeolite H-ZSM-5. The barrier is especially sensitive
to the long-range electrostatic effect of the lattice, which reduces it by 14.5 kcal/mol from the value obtained
with the 5T cluster. The final calculated barrier of 54.1 kcal/mol at the MP2(FC)/6-311+G(3df,2p)//MP2(FC)/6-31G(d) level, including corrections, is significantly smaller than values obtained by previous theoretical
studies and is in reasonable agreement with typical experimental values for short alkanes. The other levels of
theory give similar values for the barrier.
A critical analysis is given of the EPR spectrum exhibited by the rare-earth S-state ions, Gd3+ and Eu2+, in glassy and disordered polycrystalline materials. The analysis of this spectrum and of its previous interpretations is based on (a) a set of criteria derived from a wide range of experimental EPR and optical data, and (b) a first principles computer simulation method which explicitly incorporates broad distributions in the crystal field interaction parameters. It is found that all four previous interpretations of the glassy spectrum are unsatisfactory, each failing to satisfy two or more of the criteria imposed by the full range of data. The correct general solution to the spectrum is unequivocally established and shown to be a convolution of (a) a broad and essentially unimodal distribution of second-order crystal field parameters, b02, with a maximum in the approximate range 0.051≲b02 ≲0.056 cm−1, and (b) a broad distribution of asymmetry parameters, λ′=b22/b02, with appreciable probability over the whole range 0.0≤ λ′≤1.0. The prominent features in the X-band spectrum at g∼6.0 and 2.8 are found to be the result of specific EPR transitions that are stationary with respect to b02, λ′, and the orientation angles of the applied field H over a wide range. The quantitive results indicate that the site symmetries of the RE ions are essentially very low and disordered, and are best characterized by a single low-symmetry ‘‘glassy type’’ site.
Ab initio molecular orbital calculations using Hartree−Fock
theory and Møller−Plesset perturbation theory
have been used to study the interaction of H2O with the
Brønsted acid site in the zeolite H-ZSM-5.
Aluminosilicate clusters with up to 28 T atoms (T = Si, Al) were
used as models for the zeolite framework.
Full optimization of a 3 T atom cluster at the MP2/6-31G(d)
level indicates that the “ion-pair” structure,
Z-···HOH2
+, formed
by proton transfer from the acid site of the zeolite (ZH) to the
adsorbed H2O molecule,
is a transition state, while the “neutral” adsorption structure,
ZH···OH2, is a local energy minimum.
Partial
optimization of a larger 8 T cluster at the HF/6-31G(d) level also
gave results suggesting that the ion-pair
structure is a transition state. Calculations were carried out to
obtain corrections for high levels of theory,
zero-point energies, and larger cluster size. The resulting energy
difference between the neutral and ion-pair
structure is small (less than 5 kcal/mol and possibly close to zero).
The interaction energy of ZH···OH2
is
13−14 kcal/mol, in agreement with experiment. We find that
addition of a second H2O molecule
to
Z-···HOH2
+ in the 3
T atom cluster stabilizes the ion-pair structure,
Z-···H(OH2)2
+,
making it a local energy
minimum. Finally, calculated vibrational frequencies for a 3 T
atom cluster are used to help interpret
experimental IR absorption spectra.
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