A SYNCHROTRON X-RAY-DIFFRACTION, NEUTRON-DIFFRACTION, SI-29 MAS-NMR, AND COMPUTATIONAL STUDY OF THE SILICEOUS FORM OF ZEOLITE FERRIERITE

Citation
Re. Morris et al., A SYNCHROTRON X-RAY-DIFFRACTION, NEUTRON-DIFFRACTION, SI-29 MAS-NMR, AND COMPUTATIONAL STUDY OF THE SILICEOUS FORM OF ZEOLITE FERRIERITE, Journal of the American Chemical Society, 116(26), 1994, pp. 11849-11855
Citations number
26
Categorie Soggetti
Chemistry
ISSN journal
00027863
Volume
116
Issue
26
Year of publication
1994
Pages
11849 - 11855
Database
ISI
SICI code
0002-7863(1994)116:26<11849:ASXNSM>2.0.ZU;2-8
Abstract
The crystal structure of siliceous zeolite ferrierite has been determi ned from a combined analysis of synchrotron X-ray and neutron powder d iffraction data (space group Pmnn, a = 18.7202(1) Angstrom, b = 14.070 25(8) Angstrom, c = 7.41971(4) Angstrom, Z = 36, V = 1954.32(2) Angstr om(3), R(wp) = 12.33%, chi(2) = 3.55). The structure is subtly differe nt from several previously determined aluminosilicate analogues, which were refined in Immm, particularly in relation to the absence of a li near Si-O-Si bond angle that is now found to be 170 degrees. The energ y minimized structure is in excellent agreement with the experimental results, and the well-resolved Si-29 magic-angle spinning NMR spectrum can be assigned on the basis of a bond angle correlation that has bee n validated for other well-determined siliceous zeolite structures and a 2D INADEQUATE NMR spectrum. This assignment has provided a basis fo r interpreting the complex NMR spectra that are obtained from aluminos ilicate ferrierite samples and enabled us to estimate Si/Al ratios in this multiple T-site system.