关于 Mn2+ 交换沸石 Y(Si/Al = 1.67)中 Mn2+ 离子随温度变化的脱水和迁移的晶体学研究

IF 2.5 4区 材料科学 Q2 CHEMISTRY, APPLIED Journal of Porous Materials Pub Date : 2024-05-08 DOI:10.1007/s10934-024-01626-4
Sayantika Nath, Hu Sik Kim, Hyeon Seung Lim, Hyeonuk Choo, Bayarsaikhan Battsetseg, Woo Taik Lim
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引用次数: 0

摘要

为了研究 Mn2+ 交换沸石 Y(Si/Al = 1.67)中的 Mn2+ 离子和水分子在不同温度下的脱水行为,采用间歇法在室温下制备了 Mn2+ 交换沸石 Y 的单晶体。在动态真空条件下,分别在 297 K(晶体 1)、523 K(晶体 2)、573 K(晶体 3)、623 K(晶体 4)和 673 K(晶体 5)条件下脱水 48 小时,制备了五种 Mn2+ 交换沸石 Y 单晶。它们的晶体结构是通过单晶同步辐射 X 射线衍射技术在 100(1) K 的立方空间群 Fd \(\overline{3 }\) m 中确定的。晶体 1、2、3、4 和 5 的最终误差指数 R1/wR2 = 0.0594/0.1615、0.0450/0.1229、0.0445/0.1108、0.0447/0.1145 和 0.0418/0.1084(对于 Fo > 4σ(Fo))。在所有五种晶体中,约有 36 个 Mn2+ 离子占据五个晶体学位点。在所有结构中,Mn2+ 离子在能量上都优先位于位点 I。脱水时,Mn2+ 离子从一个位点(位点 I' 或 II')迁移到另一个可用的位点(位点 I 或 II),以更好地满足其配位要求。最后,在完全脱水的晶体 5 中,36 个 Mn2+ 离子占据了位点 I、I'、II'、IIa 和 IIb,占据率分别为 15、2、2、12 和 5。在不完全脱水晶体 1 ~ 4 中,所有与 Mn2+ 离子相关的水分子都位于钠长石空穴中。在晶体 1 的结构中,每个单位晶胞中约有 10.5 个水分子,每个水分子都与 Mn2+ 离子配位在 Mn(1'b)处。这些水分子形成的簇为 [Mn4(H2O)4]8+。随着温度的升高,在晶体 2 ~ 4 的结构中分别只发现了 5、3 和 2 个水分子。每个水分子都与 Mn(2')处的一个 Mn2+ 离子结合,形成 [MnH2O]2+。随着脱水温度的升高,水分子数量减少,沸石框架的单胞常数也随之降低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Crystallographic study of the temperature-dependent dehydration and migration of Mn2+ ions in Mn2+-exchanged zeolite Y (Si/Al = 1.67)

To study the behavior of Mn2+ ions and water molecules in Mn2+-exchanged zeolite Y (Si/Al = 1.67) at different temperatures during dehydration, single crystals of Mn2+-exchanged zeolite Y were prepared by batch method at room temperature. Five single crystals of Mn2+-exchanged zeolite Y were dehydrated at 297 K (crystal 1), 523 K (crystal 2), 573 K (crystal 3), 623 K (crystal 4), and 673 K (crystal 5), respectively, under dynamic vacuum for 48 h. Their crystal structures were determined by single-crystal synchrotron X-ray diffraction techniques in the cubic space group Fd \(\overline{3 }\) m at 100(1) K. They were refined to the final error indices R1/wR2 = 0.0594/0.1615, 0.0450/0.1229, 0.0445/0.1108, 0.0447/0.1145, and 0.0418/0.1084 (for Fo > 4σ(Fo)) for crystals 1, 2, 3, 4, and 5, respectively. In all five crystals, about 36 Mn2+ ions occupy five crystallographic sites. Mn2+ ions are energetically preferentially located at site I in all structures. The Mn2+ ions migrated from one site (sites I’ or II’) to another available site (sites I or II) to better satisfy their coordination requirements upon dehydration. Finally, in the completely dehydrated crystal 5, 36 Mn2+ ions occupy the sites I, I’, II’, IIa, and IIb with the fractional occupancies 15, 2, 2, 12, and 5, respectively. All water molecules associated with Mn2+ ions in the incompletely dehydrated crystals 1 ~ 4 were located in the sodalite cavities. In the structure of crystal 1, about 10.5 water molecules were found per unit cell, each coordinating to Mn2+ ions at Mn(1’b). These water molecules formed clusters as [Mn4(H2O)4]8+. Only 5, 3, and 2 water molecules were found in the structures of crystals 2 ~ 4, respectively, with increasing temperature. Each of these water molecules was bonded to one Mn2+ ion at Mn(2’), forming [MnH2O]2+. The unit cell constant of the zeolite framework decreased, as the number of water molecules decreased with the increasing dehydration temperature.

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来源期刊
Journal of Porous Materials
Journal of Porous Materials 工程技术-材料科学:综合
CiteScore
4.80
自引率
7.70%
发文量
203
审稿时长
2.6 months
期刊介绍: The Journal of Porous Materials is an interdisciplinary and international periodical devoted to all types of porous materials. Its aim is the rapid publication of high quality, peer-reviewed papers focused on the synthesis, processing, characterization and property evaluation of all porous materials. The objective is to establish a unique journal that will serve as a principal means of communication for the growing interdisciplinary field of porous materials. Porous materials include microporous materials with 50 nm pores. Examples of microporous materials are natural and synthetic molecular sieves, cationic and anionic clays, pillared clays, tobermorites, pillared Zr and Ti phosphates, spherosilicates, carbons, porous polymers, xerogels, etc. Mesoporous materials include synthetic molecular sieves, xerogels, aerogels, glasses, glass ceramics, porous polymers, etc.; while macroporous materials include ceramics, glass ceramics, porous polymers, aerogels, cement, etc. The porous materials can be crystalline, semicrystalline or noncrystalline, or combinations thereof. They can also be either organic, inorganic, or their composites. The overall objective of the journal is the establishment of one main forum covering the basic and applied aspects of all porous materials.
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