Abstract
MCM-22 is a synthetic high-silica zeolite which crystallizes as very thin plates. Its internal structure contains two independent internal pore systems accessible through 10-ring apertures. A high concentration of external zeolitic pockets, with 12-ring openings and having an approximate depth of 7 Å, covers the hexagonal faces of the thin crystals. Evidence for the presence of these pockets was established by high-resolution electron microscopy. Experimental evidence to support this was obtained from ion-exchange studies using tetramethylammonium and tetraethylammonium ions, and from dynamic sorption studies using n-heptane and 2,2,4-trimethylpentane. The results suggest that the surface pockets unique to the MCM-22 structure have zeolitic characteristics and may play a significant role in certain catalytic processes.
Author supplied keywords
Cite
CITATION STYLE
Lawton, S. L., Leonowicz, M. E., Partridge, R. D., Chu, P., & Rubin, M. K. (1998). Twelve-ring pockets on the external surface of MCM-22 crystals. Microporous and Mesoporous Materials, 23(1–2), 109–117. https://doi.org/10.1016/S1387-1811(98)00057-2
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.