Abstract
A series of multiple-pulse nuclear magnetic resonance (NMR) techniques have been applied to the study of the adsorbed state of formic acid on ammonium-Y (NH 4Y) and ultrastable hydrogen-Y (HY) zeolites. It is determined that the formic acid is adsorbed on the zeolites in two different forms: as unidentate and bidentate formate species, which can be distinguished by the symmetry of the 13C chemical shift powder patterns. Cross-polarization NMR techniques exploit differences in the 13C 1H dipolar couplings to separate the two groups. The ratio of bidentate to unidentate species is about 52:48 on the NH 4Y zeolite and about 83:17 on the ultrastable HY zeolite at a coverage of 0.3 monolayer. The strength of the 13C 27Al dipolar interaction suggests that the bidentate formate ions are bonded to the Al atoms of the zeolites. The 1H NMR spectrum of the carbonyl hydrogen, isolated by a dipolar-difference technique, is shifted downfield from that of neat formic acid, indicating that the hydrogen has become more acidic.
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