Synthesis and characterization of the new cyclosilicate hydrate (hexamethyleneimine)4•[Si8O16(OH)4]•12H2O

被引:7
作者
Verlooy, Pieter L. H. [1 ]
Robeyns, Koen [2 ]
Van Meervelt, Luc [2 ]
Lebedev, Oleg I. [3 ]
Van Tendeloo, Gustaaf [3 ]
Martens, Johan A. [1 ]
Kirschhock, Christine E. A. [1 ]
机构
[1] Catholic Univ Louvain, Ctr Surface Chem & Catalysis, B-3001 Heverlee, Belgium
[2] Catholic Univ Louvain, Dept Chem, B-3001 Heverlee, Belgium
[3] Univ Antwerp, Dept Phys, EMAT, B-2020 Antwerp, Belgium
关键词
Cyclosilicate hydrate; Hydrogen bonds; Cubic silicate octamer; Hexamethyleneimine; Microporous material; X-RAY-DIFFRACTION; TRIETHYL-(2-HYDROXYETHYL)AMMONIUM SILICATE SOLUTIONS; NUCLEAR-MAGNETIC-RESONANCE; DOUBLE-RING SILICATE; CLATHRATE HYDRATE; CRYSTAL-STRUCTURE; TETRAMETHYLAMMONIUM SILICATE; STRUCTURAL LINKS; ZEOLITE-TYPE; CONSTITUTION;
D O I
10.1016/j.micromeso.2009.10.006
中图分类号
O69 [应用化学];
学科分类号
081704 ;
摘要
A new cyclosilicate hydrate with composition (C6H14N)(4)center dot[Si8O16(OH)(4)]center dot 12H(2)O was crystallized and the structure determined by single-crystal X-ray diffraction. The structure, described by the tetragonal space group I4(1)/a, with unit cell dimensions of a = 39.2150(2) angstrom and c = 14.1553(2) angstrom, contains columns of hydrogen-bonded cubic octamer silicate anions. The space between silicate columns holds hydrogen-bonded water and protonated hexamethyleneimine molecules compensating the negative charge of the silicate. The crystal water can be removed resulting in a rearrangement of the columns into ortho-rhombic symmetry. Removal of the organic moiety causes amorphisation. Flash evacuation results in a new microporous material with pore volumes typical of a zeolite. (C) 2009 Elsevier Inc. All rights reserved.
引用
收藏
页码:14 / 20
页数:7
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