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通过元素组成控制各向异性沸石的晶体形态

Controlling Crystal Morphology of Anisotropic Zeolites with Elemental Composition.

作者信息

Veselý Ondřej, Shamzhy Mariya, Roth Wiesław J, Morris Russell E, Čejka Jiří

机构信息

Faculty of Sciences, Charles University, Hlavova 8, 128 43 Prague 2, Czech Republic.

Faculty of Chemistry, Jagiellonian University, Gronostajowa 2, 30-387 Krakow, Poland.

出版信息

Cryst Growth Des. 2024 Mar 8;24(6):2406-2414. doi: 10.1021/acs.cgd.3c01312. eCollection 2024 Mar 20.

DOI:10.1021/acs.cgd.3c01312
PMID:38525100
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10958493/
Abstract

The morphology of zeolite crystals strongly affects their textural, catalytic, and mechanical attributes. However, controlling zeolite crystal morphology without using modifiers or structure-directing agents remains a challenging task because of our limited understanding of the relationships between zeolite crystal shape, crystallization mechanism, and composition of the starting synthesis mixture. In this study, we aimed at developing a general method for controlling the morphology of zeolites by assessing the impact of the Si/T molar ratio of the synthesis gel on the growth rate of zeolite crystals in various crystallographic directions and on the final crystal morphology of the germanosilicate with a 2D system of intersecting 14- and 12-ring pores. Our results showed that flat crystals progressively thicken with the Si/Ge molar ratio, demonstrating that Ge concentration controls the relative rate of crystal growth in the perpendicular direction to the pore system. The morphology of other zeolites and zeotypes with an anisotropic structure, including (12R), (12R), (10-10R), and (12-10-8R), can also be predicted based on their Si/T ratio, suggesting a systematic pattern across zeolite structures and in a wide range of zeolite framework elements. Combined, these findings introduce a facile and cost-efficient method for directly controlling crystal morphology of zeolites with anisotropic structures with a high potential for scale-up while providing further insights into the role of elemental composition in zeolite crystal growth.

摘要

沸石晶体的形态强烈影响其纹理、催化和机械属性。然而,在不使用改性剂或结构导向剂的情况下控制沸石晶体形态仍然是一项具有挑战性的任务,因为我们对沸石晶体形状、结晶机制和起始合成混合物组成之间的关系了解有限。在本研究中,我们旨在开发一种通用方法来控制沸石的形态,通过评估合成凝胶的Si/Ge摩尔比对具有二维交叉14环和12环孔系统的锗硅酸盐沸石晶体在不同晶体学方向上的生长速率以及最终晶体形态的影响。我们的结果表明,扁平晶体随着Si/Ge摩尔比逐渐变厚,这表明Ge浓度控制了与孔系统垂直方向上晶体生长的相对速率。其他具有各向异性结构的沸石和沸石型材料,包括(12R)、(12R)、(10 - 10R)和(12 - 10 - 8R),其形态也可以根据它们的Si/Ge比来预测,这表明在沸石结构和广泛的沸石骨架元素中存在一种系统模式。综合起来,这些发现引入了一种简便且经济高效的方法,用于直接控制具有各向异性结构的沸石晶体形态,具有很高的放大潜力,同时为元素组成在沸石晶体生长中的作用提供了进一步的见解。

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