Interzeolite transformation (IZT) is a powerful method for controlling the framework type, aluminum distribution, and hierarchical structures of zeolite. However, the in-depth mechanisms underlying IZT remain unexplored. In this study, we reveal a distinctive nucleation pathway and structural evolution of zeolite SSZ-13 during IZT that is different from the traditional hydrothermal synthesis methods. Utilizing two aluminum sources—al-rich zeolite analcite and aluminum sulfate—we accelerated the crystallization process with SSZ-13 seed crystals and TMAda-OH. Our findings indicate that the Al content, representing the charge density of the nucleation micro-environment, plays a critical role in shaping the framework and nucleation pathway. Nucleation occurred at the interface between analcite and the silica solution during IZT, characterized by a high-silica micro-environment with low charge density. In this environment, the precursor predominantly replicated the double six rings (D6R) of SSZ-13 seed fragments, forming double four rings (D4R) and CHA cages which resulted in a short induction period, fewer nucleation sites, and larger crystals size (∼1.5 μm). Conversely, when aluminum sulfate was mixed with silica sol, a uniform, Al-rich nucleation micro-environment with high negative charge density was established. the precursor primarily interacted with TMAda+ ions for charge compensation rather than with seed fragments. This slow interaction promoted the formation of CHA cages instead of D6R and D4R, leading to a longer induction period, increased nucleation sites, and smaller SSZ-13 crystal sizes (∼150 nm). This study elucidates how the charge density of micro-environment mediated interaction between precursors, organic structure-directing agent, and seed, providing valuable insights into the crystallization kinetics of IZT.
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