Influence of the source of silicon and aluminium in the hydrothermal synthesis of sodalite
Abstract
The synthesis of sodalite from aluminium hydroxide, aluminium isopropoxide and pseudo-boehmite (Catapal alumina) as the source of Al, and fumed silica and sodium silicoglycolate (Na-SiV) as the source of Si has been monitored by solid-state NMR, X-ray diffraction (XRD) and IR spectroscopy. The use of Na-SiV does not affect the crystallization time, but considerably shortens the preparation of the synthesis gel. Aluminium is not significantly incorporated into the sodalite structure when Al(OH)3 is used. Pseudo-boehmite gives multi-phasic products in which purely siliceous sodalite is always accompanied by (Si,Al)-sodalites. Some of the Al occupies non-framework positions, and parent gels with Si : Al = 5.0, 2.0 and 1.0 gave solids with AlIV : AlVI= 0.73, 1.3 and 3.0, respectively. Only aluminium isopropoxide leads to phase-pure products in which all the AI is four-coordinate and Si : Al = 3.49 and 3.13 with fumed silica and Na-SiV, respectively. The formula NAI= 51.855 – 0.0465vas(Si—O—T) allows the Si : Al ratio to be calculated directly from the FTIR spectrum. With the exception of the material with Si : Al = 1.0 and a0= 8.94 ± 0.1 Å, the unit cell parameter of sodalites is 8.83 ± 0.1Å irrespective of the Al content.