Department of Chemical System Engineering, The University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-8656, Japan.
Japan Synchrotron Radiation Research Institute (JASRI), Kouto 1-1-1, Sayo-cho, Sayo-gun, Hyogo 679-5198, Japan.
J Phys Chem Lett. 2023 Apr 13;14(14):3574-3580. doi: 10.1021/acs.jpclett.3c00432. Epub 2023 Apr 5.
To understand the crystallization mechanism of zeolites, it is important to clarify the detailed role of the structure-directing agent, which is essential for the crystallization of zeolite, interacting with an amorphous aluminosilicate matrix. In this study, to reveal the structure-directing effect, the evolution of the aluminosilicate precursor which causes the nucleation of zeolite is analyzed by the comprehensive approach including atom-selective methods. The results of total and atom-selective pair distribution function analyses and X-ray absorption spectroscopy indicate that a crystalline-like coordination environment gradually forms around Cs cations. This corresponds to the fact that Cs is located at the center of the units in the RHO structure whose unit is unique in this zeolite, and a similar tendency is also confirmed in the ANA system. The results collectively support the conventional hypothesis that the formation of the crystalline-like structure before the apparent nucleation of the zeolite.
为了理解沸石的结晶机制,阐明结构导向剂的详细作用非常重要,结构导向剂对于沸石的结晶是必不可少的,它与无定形的硅铝酸盐基质相互作用。在这项研究中,为了揭示结构导向效应,通过包括原子选择性方法在内的综合方法,分析了导致沸石成核的硅铝酸盐前体的演变。全原子选择性配分函数分析和 X 射线吸收光谱的结果表明,Cs 阳离子周围逐渐形成了类似结晶的配位环境。这与 Cs 位于 RHO 结构的单元中心相对应,该单元在这种沸石中是独特的,在 ANA 体系中也证实了类似的趋势。这些结果共同支持了这样的传统假设,即在沸石明显成核之前,就已经形成了类似结晶的结构。