通过In Situ高能X射线总散射测量与对分布函数分析追踪岩合成中的纳米级结构演变
Ayano Minami1, Peidong Hu1,2, Yuki Sada1
1Department of Chemical System Engineering, The University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo113-8656, Japan.
Journal of the American Chemical Society
|December 16, 2022
概括
研究人员使用现场X射线散射揭示了石SSZ-13结晶机制. 早期形成有序的四个环, 引导更大的结构和晶体生长.
科学领域:
- 材料科学
- 晶体学
- 纳米技术
背景情况:
- 由于在合成条件下对无形前体的特征有局限性,因此对石的结晶机制的了解很少.
- 石是具有多种工业应用的微孔材料,需要对其形成途径有更深入的了解.
研究的目的:
- 为了阐明 SSZ-13 石合成过程中的实时亚纳米级无形转化.
- 研究前体结构在指导石结晶中的作用.
主要方法:
- 在现场使用高能X射线总散射测量.
- 采用对分布函数分析来追踪水热合成过程中的结构演变.
- 实时研究了子纳米级结构单元的形成.
主要成果:
- 在诱导期内确定了有序的四个环 (4Rs) 的主导形成.
- 在晶体生长过程中观察到六个和八个环 (6Rs和8Rs) 的随后增加.
- 证明预先形成的4Rs促进了d6r和cha复合结构单元的形成,导致胚胎晶体.
结论:
- 这项研究揭示了由预制的4Rs启动的SSZ-13热结晶的粒子附着路径.
- 这些发现为热带石形成机制提供了关键的见解,推动了材料合成领域的发展.
- 这项工作增强了研究热结晶途径的分析工具.
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