MCM-22 is a synthetic high-silica zeolite which crystallizes as very t
hin plates. Its internal structure contains two independent internal p
ore systems accessible through 10-ring apertures. A high concentration
of external zeolitic pockets, with 12-ring openings and having an app
roximate depth of 7 Angstrom, covers the hexagonal faces of the thin c
rystals. 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 sur
face pockets unique to the MCM-22 structure have zeolitic characterist
ics and may play a significant role in certain catalytic processes. (C
) 1998 Elsevier Science B.V. All rights reserved.