Topotactic condensation of layer silicates with ferrierite-type layers   forming porous tectosilicates

doi:10.1039/c4dt00262h

CORC > 北京大学 > 化学与分子工程学院

	Topotactic condensation of layer silicates with ferrierite-type layers forming porous tectosilicates
	Marler, B. ; Wang, Y. ; Song, J. ; Gies, H.
刊名	dalton transactions
	2014
关键词	CRYSTAL-STRUCTURE INTERLAYER EXPANSION MOLECULAR-SIEVE ZEOLITE PRECURSOR CONVERSION SODALITE RUB-39 EU-19
DOI	10.1039/c4dt00262h
英文摘要	Five different hydrous layer silicates (HLSs) containing fer layers (ferrierite-type layers) were obtained by hydrothermal syntheses from mixtures of silicic acid, water and tetraalkylammonium/tetraalkylphosphonium hydroxides. The organic cations had been added as structure directing agents (SDA). A characteristic feature of the structures is the presence of strong to medium strong hydrogen bonds between the terminal silanol/siloxy groups of neighbouring layers. The five-layered silicates differ chemically only with respect to the organic cations. Structurally, they differ with respect to the arrangement of the fer layers relative to each other, which is distinct for every SDA-fer-layer system. RUB-20 (containing tetramethylammonium) and RUB-40 (tetramethylphosphonium) are monoclinic with stacking sequence AAA and shift vectors between successive layers 1a(0) + 0b(0) + 0.19c(0) and 1a(0) + 0b(0) + 0.24c(0), respectively. RUB-36 (diethyldimethylammonium), RUB-38 (methyltriethylammonium) and RUB-48 (trimethylisopropylammonium) are orthorhombic with stacking sequence ABAB and shift vectors 0.5a(0) + 0b(0) +/- 0.36c(0), 0.5a(0) + 0b(0) + 0.5c(0) and 0.5a(0) + 0b(0) +/- 0.39c(0), respectively. Unprecedented among the HLSs, two monoclinic materials are made up of fer layers which possess a significant amount of ordered defects within the layer. The ordered defects involve one particular Si-O-Si bridge which is, to a fraction of ca. 50%, hydrolyzed to form nests of two Si-OH groups. When heated to 500-600 degrees C in air, the HLSs condense to form framework silicates. Although all layered precursors were moderately to well ordered, the resulting framework structures were of quite different crystallinity. The orthorhombic materials RUB-36, -38 and -48, general formula SDA(4)Si(36)O(72)(OH)(4), which possess very strong hydrogen bonds (d[O center dot center dot center dot O] approximate to 2.4 angstrom), transform into a fairly or well ordered CDO-type silica zeolite RUB-37. The monoclinic materials RUB-20 and -40, general formula SDA(2)Si(18)O(36)(OH)(2)OH, possessing medium strong hydrogen bonds (d[O center dot center dot center dot O] approximate to 2.65 angstrom) are transformed into poorly ordered framework silicates. Some rules of thumb can be established concerning the successful zeolite synthesis via a topotactic condensation of layered precursors. Favourably, the precursor (i) possesses already a well ordered structure without defects, (ii) contains strong inter-layer hydrogen bonds and does not contain strong intra-layer hydrogen bonds and (iii) contains a suitable cation. The nature of the organic cation (size, geometry, flexibility, thermal stability) plays a key role in the formation of a microporous tectosilicate with well ordered structure. RUB-36 which meets these criteria yields a well ordered condensation product (RUB-37).; Chemistry, Inorganic & Nuclear; SCI(E); EI; 3; ARTICLE; bernd.marler@rub.de; 27; 10396-10416; 43
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/390567]
专题	化学与分子工程学院
推荐引用方式 GB/T 7714	Marler, B.,Wang, Y.,Song, J.,et al. Topotactic condensation of layer silicates with ferrierite-type layers forming porous tectosilicates[J]. dalton transactions,2014.
APA	Marler, B.,Wang, Y.,Song, J.,&Gies, H..(2014).Topotactic condensation of layer silicates with ferrierite-type layers forming porous tectosilicates.dalton transactions.
MLA	Marler, B.,et al."Topotactic condensation of layer silicates with ferrierite-type layers forming porous tectosilicates".dalton transactions (2014).