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
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.