Single crystals (up to 580 × 480 × 20 μm) of highly silicious ferrierite (Si-FER, 1 ), suitable for single-crystal X-ray investigations, are synthesized under organothermal conditions. The structures of the as-synthesized ( 1a ) and the calcined ( 1b ) Si-FER are determined at room temperature. Both structures are refined in the orthorhombic space group Pnnm (No. 58, standard setting) with a = 743.0(1) pm, b = 1409.2(2) pm, c = 1882.0(2) pm, V = 1970.5(4) × 10 6 pm 3, Z = 1, R = 0.041 ( 1a ) and a = 741.8(1) pm, b = 1407.0(2) pm, c = 1871.3(2) pm, V = 1953.1(4) × 10 6 pm 3, Z = 1, R = 0.037 ( 1b ). The structure solution when combined with chemical analysis and 1 H and 13 C MAS NMR gives a unit cell content of [Si 36 O 72 ]{py (4 - x ) ap x } ( x = 0−1, py = pyridine, ap = 1-amino- n -propane) and [Si 36 O 72 ] for 1a and 1b, respectively. The structure of 1a shows only weak host−guest interactions between the { 3 ∞ }[SiO 4/2 ] framework and the occluded, orientationally disordered pyridine molecules by means of relatively long organic-to-framework distances, d (C py ···O) ≥ 354(2) pm. 29 Si MAS NMR spectra from the organic-containing Si-FER 1a and the organic-free form 1b are in good agreement with the crystallographic results in that they conform to the well-known linear relationship between the cosine expression of the T−O−T angles and the chemical shift of the respective tetrahedral sites (T-sites). A new modification of this relationship is presented here and offers an improved linear correlation between the X-ray and NMR data for 1a and 1b, as well as for other high-silica microporous materials. Application of this new correlation to denser SiO 2 compounds is discussed.
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Lewis et al. (1996) studied this question.
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