The preparation of metastable zeolites is often restricted
to a
limited range of synthesis conditions, which is exemplified in commercial
syntheses lacking organics to stabilize the crystal structure. In
the absence of an organic structure-directing agent, interzeolite
transformation is a common phenomenon that can lead to undesirable
products or impurities. Many studies have investigated the substitution
of Si and Al in zeolite frameworks with alternative elements (heteroatoms)
as a means of tailoring the properties of zeolites; however, relatively
few studies have systematically explored the impact of heteroatoms
on interzeolite transformations and their concomitant effects on zeolite
crystallization. In this study, we examine methods to prepare isostructures
of faujasite (FAU), which is one of the most commercially relevant
zeolites and also a thermodynamically metastable structure. A survey
of multivalent elements revealed that zinc is capable of stabilizing
FAU at high temperatures and inhibiting its frequent transformation
to zeolite gismondine (GIS). Using combined experimental and computational
studies, we show that zinc alters the chemical nature of growth mixtures
by sequestering silicates. Zinc heteroatoms incorporate in the FAU
framework with a loading-dependent coordination. Our collective findings
provide an improved understanding of driving forces for the FAU-to-GIS
interzeolite transformation where we observe that heteroatoms (e.g.,
zinc) can stabilize zeolite FAU over a broad range of synthesis conditions.
Given the growing interest in heteroatom-substituted zeolites, this
approach to preparing zinc-containing FAU may prove applicable to
a broader range of zeolite structures.