Sayantika Nath, Hu Sik Kim, Hyeon Seung Lim, Hyeonuk Choo, Bayarsaikhan Battsetseg, Woo Taik Lim
{"title":"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","authors":"Sayantika Nath, Hu Sik Kim, Hyeon Seung Lim, Hyeonuk Choo, Bayarsaikhan Battsetseg, Woo Taik Lim","doi":"10.1007/s10934-024-01626-4","DOIUrl":null,"url":null,"abstract":"<div><p>To study the behavior of Mn<sup>2+</sup> ions and water molecules in Mn<sup>2+</sup>-exchanged zeolite Y (Si/Al = 1.67) at different temperatures during dehydration, single crystals of Mn<sup>2+</sup>-exchanged zeolite Y were prepared by batch method at room temperature. Five single crystals of Mn<sup>2+</sup>-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 <i>Fd</i> <span>\\(\\overline{3 }\\)</span> <i>m</i> at 100(1) K. They were refined to the final error indices <i>R</i><sub>1</sub>/<i>wR</i><sub><i>2</i></sub> = 0.0594/0.1615, 0.0450/0.1229, 0.0445/0.1108, 0.0447/0.1145, and 0.0418/0.1084 (for F<sub>o</sub> > 4σ(F<sub>o</sub>)) for crystals 1, 2, 3, 4, and 5, respectively. In all five crystals, about 36 Mn<sup>2+</sup> ions occupy five crystallographic sites. Mn<sup>2+</sup> ions are energetically preferentially located at site I in all structures. The Mn<sup>2+</sup> 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 Mn<sup>2+</sup> 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 Mn<sup>2+</sup> 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 Mn<sup>2+</sup> ions at Mn(1’b). These water molecules formed clusters as [Mn<sub>4</sub>(H<sub>2</sub>O)<sub>4</sub>]<sup>8+</sup>. 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 Mn<sup>2+</sup> ion at Mn(2’), forming [MnH<sub>2</sub>O]<sup>2+</sup>. The unit cell constant of the zeolite framework decreased, as the number of water molecules decreased with the increasing dehydration temperature.</p></div>","PeriodicalId":660,"journal":{"name":"Journal of Porous Materials","volume":"31 5","pages":"1711 - 1725"},"PeriodicalIF":2.5000,"publicationDate":"2024-05-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Crystallographic study of the temperature-dependent dehydration and migration of Mn2+ ions in Mn2+-exchanged zeolite Y (Si/Al = 1.67)\",\"authors\":\"Sayantika Nath, Hu Sik Kim, Hyeon Seung Lim, Hyeonuk Choo, Bayarsaikhan Battsetseg, Woo Taik Lim\",\"doi\":\"10.1007/s10934-024-01626-4\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>To study the behavior of Mn<sup>2+</sup> ions and water molecules in Mn<sup>2+</sup>-exchanged zeolite Y (Si/Al = 1.67) at different temperatures during dehydration, single crystals of Mn<sup>2+</sup>-exchanged zeolite Y were prepared by batch method at room temperature. Five single crystals of Mn<sup>2+</sup>-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 <i>Fd</i> <span>\\\\(\\\\overline{3 }\\\\)</span> <i>m</i> at 100(1) K. They were refined to the final error indices <i>R</i><sub>1</sub>/<i>wR</i><sub><i>2</i></sub> = 0.0594/0.1615, 0.0450/0.1229, 0.0445/0.1108, 0.0447/0.1145, and 0.0418/0.1084 (for F<sub>o</sub> > 4σ(F<sub>o</sub>)) for crystals 1, 2, 3, 4, and 5, respectively. In all five crystals, about 36 Mn<sup>2+</sup> ions occupy five crystallographic sites. Mn<sup>2+</sup> ions are energetically preferentially located at site I in all structures. The Mn<sup>2+</sup> 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 Mn<sup>2+</sup> 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 Mn<sup>2+</sup> 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 Mn<sup>2+</sup> ions at Mn(1’b). These water molecules formed clusters as [Mn<sub>4</sub>(H<sub>2</sub>O)<sub>4</sub>]<sup>8+</sup>. 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 Mn<sup>2+</sup> ion at Mn(2’), forming [MnH<sub>2</sub>O]<sup>2+</sup>. The unit cell constant of the zeolite framework decreased, as the number of water molecules decreased with the increasing dehydration temperature.</p></div>\",\"PeriodicalId\":660,\"journal\":{\"name\":\"Journal of Porous Materials\",\"volume\":\"31 5\",\"pages\":\"1711 - 1725\"},\"PeriodicalIF\":2.5000,\"publicationDate\":\"2024-05-08\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Porous Materials\",\"FirstCategoryId\":\"88\",\"ListUrlMain\":\"https://link.springer.com/article/10.1007/s10934-024-01626-4\",\"RegionNum\":4,\"RegionCategory\":\"材料科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"CHEMISTRY, APPLIED\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Porous Materials","FirstCategoryId":"88","ListUrlMain":"https://link.springer.com/article/10.1007/s10934-024-01626-4","RegionNum":4,"RegionCategory":"材料科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"CHEMISTRY, APPLIED","Score":null,"Total":0}
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.
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.