Electron crystallography of zeolites - the MWW family as a test of direct 3D structure determination

被引:47
作者
Dorset, DL
Roth, WJ
Gilmore, CJ
机构
[1] ExxonMobil Res & Engn Co, Corp Strateg Res, Annandale, NJ 08801 USA
[2] Univ Glasgow, Dept Chem, Glasgow G12 8QQ, Lanark, Scotland
来源
ACTA CRYSTALLOGRAPHICA A-FOUNDATION AND ADVANCES | 2005年 / 61卷
关键词
D O I
10.1107/S0108767305024670
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The efficacy of direct methods for solving the crystal structures of zeolites from electron diffraction data is evaluated for a series of related materials, i.e. MCM-22, MCM-49 and ITQ-1. First, it is established by tilting experiments that all materials share the same MWW framework. The calcined product of a delaminated MCM-22 precursor, ITQ-2, also shares this framework structure within the limited number of stacked unit cells. For all materials, the underlying space group is P6/mmm where a similar or equal to 14.21, c similar or equal to 24.94 angstrom. Traditional direct methods are useful for determining the projected structure down the hexagonal axis but are not very effective for finding the three-dimensional structure. On the other hand, maximum-entropy and likelihood approaches are effective for determining either 2D projections or 3D frameworks. The major restriction to 3D determinations by direct methods is the limited goniometric tilt range of the electron microscope, hence the 'missing cone' of information. Potential maps from the most accurate phase sets are, therefore, observed as continuous density envelopes to the true structure. Some improvement is found when the Sayre equation predicts missing amplitudes and phases but it is clear that better specimen preparation methods are required to include projections containing the c* axis of the reciprocal lattice.
引用
收藏
页码:516 / 527
页数:12
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