Influence of framework silicon to aluminium ratio on aluminium coordination and distribution in zeolite Beta investigated by 27Al MAS and 27Al MQ MAS NMR

被引:101
作者
Abraham, A [1 ]
Lee, SH
Shin, CH
Hong, SB
Prins, R
van Bokhoven, JA
机构
[1] ETH, Swiss Fed Inst Technol, Inst Chem Engn & Bioengn, CH-8093 Zurich, Switzerland
[2] Hanbat Natl Univ, Div Chem Engn, Taejon 305719, South Korea
[3] Chungbuk Natl Univ, Dept Chem Engn, Chungbuk 361763, South Korea
关键词
D O I
10.1039/b401235f
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Al-27 magic-angle spinning (MAS) and triple quantum (3Q) MAS NMR spectroscopic techniques were used to characterise zeolite Beta samples with framework Si/Al ratios between 9 and 215, obtained by synthesis in fluoride medium. A carefully controlled stepwise calcination procedure was adopted to obtain H-Beta. A partial resolution of the T-sites was observed in the Al-27 MAS NMR spectra, the resolution increasing with increasing the Si/Al ratios. The relative intensity of these peaks varied gradually, with Si/Al ratio showing that the relative occupancy of the crystallographic T-sites changes with Si/Al ratio. The tetraethylammonium cation, used as an organic structure-directing agent in Beta synthesis, affects the average chemical shift of aluminium atoms in different T-sites. In H-Beta, octahedrally coordinated framework-associated aluminium atoms that could be quantitatively reverted into tetrahedral coordination were observed. The amount of this octahedral aluminium species decreases with increasing Si/Al ratio and it was absent for the two high-silica H-Beta samples with Si/Al = 110 and 215. Specific framework tetrahedral T-sites tend to convert to framework-associated octahedral sites during calcination It is suggested that two aluminium T-sites, which are adjacent or close to each other, obeying the Loewenstein's rule (i.e., no Al-O-Al linkage), are required for the hydrolysis of a Si-O-Al bond for the formation of octahedrally coordinated aluminium. The distribution of aluminium in zeolite Beta is a function of the Si/Al ratio and is non-uniformly distributed over the crystallographic T-sites.
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页码:3031 / 3036
页数:6
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