Zeolite crystallization occurs by complex processes involving
a
variety of possible mechanisms. The sol gel media used to prepare
zeolites leads to heterogeneous mixtures of solution and solid states
with diverse solute species. At later stages of zeolite synthesis
when growth occurs predominantly from solution, classical two-dimensional
nucleation and spreading of layers on crystal surfaces via the addition
of soluble species is the dominant pathway. At earlier stages, these
processes occur in parallel with nonclassical pathways involving crystallization
by particle attachment (CPA). The relative roles of solution- and
solid-state species in zeolite crystallization have been a subject
of debate. Here, we investigate the growth mechanism of a commercially
relevant zeolite, faujasite (FAU). In situ atomic force microscopy
(AFM) measurements reveal that supernatant solutions extracted from
a conventional FAU synthesis at various times do not result in growth,
indicating that FAU growth predominantly occurs from the solid state
through a disorder-to-order transition of amorphous precursors. Elemental
analysis shows that supernatant solutions are significantly more siliceous
than both the original growth mixture and the FAU zeolite product;
however, in situ AFM studies using a dilute clear solution with a
lower Si/Al ratio revealed three-dimensional growth of surfaces that
is distinct from layer-by-layer and CPA pathways. This unique mechanism
of growth differs from those observed in studies of other zeolites.
Given that relatively few zeolite frameworks have been the subject
of mechanistic investigation by in situ techniques, these observations
of FAU crystallization raise the question whether its growth pathway
is characteristic of other zeolite structures.