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Modeling of zeolite L crystallization using continuum time Monte Carlo simulations

机译:使用连续时间蒙特卡洛模拟法对L型沸石结晶进行建模

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摘要

A model to investigate a gel-to-zeolite transformation as a possible growth mechanism through association and rearrangements of extended precursor structures is developed and solved via continuum time lattice Monte Carlo simulations. The model is used to study the morphology of zeolite L nanocrystals grown from an initial amorphous microporous precursor gel. The model considers gel dissolution to release growth precursor extended structures, precursor migration, precursor-precursor association, precursor incorporation into zeolite nanoparticles, and zeolite dissolution. It is shown that the gel-to-zeolite transformation can occur when dissolved precursor migration is slow compared to precursor incorporation and zeolite dissolution. Under these conditions, the initial gel microstructure (intraparticle porosity) has a significant effect on the zeolite morphology and on the crystallization kinetics. This transformation proceeds in two stages: A zeolitic framework forms initially without long-range order, followed by slow rearrangement of building units into nanocrystalline particles with possible defects. Finally different growth modes are identified as a function of microkinetic parameters and gel morphology.
机译:通过连续时间点阵蒙特卡洛模拟,开发并解决了一个模型,该模型通过扩展的前体结构的缔合和重排来研究凝胶向沸石的转变作为可能的生长机理。该模型用于研究从初始无定形微孔前体凝胶生长的沸石L纳米晶体的形貌。该模型考虑了凝胶溶解以释放生长的前驱物延伸结构,前驱物迁移,前驱物-前体缔合,前驱物掺入沸石纳米颗粒中以及沸石溶解的情况。结果表明,与前驱物掺入和沸石溶解相比,当溶解的前驱物迁移较慢时,可能会发生凝胶向沸石的转化。在这些条件下,初始的凝胶微结构(颗粒内孔隙率)对沸石的形态和结晶动力学具有重要影响。这种转变分为两个阶段:最初形成的沸石骨架没有长程有序,然后缓慢将建筑单元重排成具有可能缺陷的纳米晶体颗粒。最终,根据微动力学参数和凝胶形态来确定不同的生长模式。

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