J. Datka et al., PHYSICOCHEMICAL AND CATALYTIC PROPERTIES OF HZSM-5 ZEOLITES DEALUMINATED BY THE TREATMENT WITH STEAM, Journal of physical chemistry, 100(34), 1996, pp. 14451-14456
We studied the physicochemical properties (by Al-27 MAS NMR, XPS, and
IR spectroscopy) and catalytic activity (in n-heptane cracking) of a s
eries of HZSM-5 zeolites treated at 770 K with water vapor at various
partial pressures (0, 7, 13, 40, and 93 kPa). The treatment with steam
removed Al from framework tetrahedral positions (as evidenced by Al-2
7 MAS NMR studies) and yielded a decrease in the amount of acidic Si-O
H-Al groups. Quantitative IR studies of pyridine sorption showed that
the amount of Si-OH-Al in parent and in dealuminated zeolites was very
close to the amount of tetrahedral Al which remained in the framework
. The Al atoms removed from the tetrahedral positions migrated (as giv
en by XPS) to the surface. Only a small amount of these removed Al cre
ated Lewis acid sites. IR studies suggested that the vacancies created
by removal of Al were filled with Si atoms migrating from other place
s in the zeolite. From IR studies of the desorption of ammonia it was
concluded that mild dealumination (with 7 kPa of H2O) increased the ac
idic strength of Si-OH-Al groups. The experiments of chlorobenzene sor
ption suggested that this increase was in the first order due to remov
al (by steam treatment) of the less acidic hydroxyls. The more severe
dealumination decreased the acidic strength of Si-OH-Al groups. The re
sults of catalytic tests of n-heptane cracking agreed well with the IR
results concerning acidity. The mild dealumination resulted in an inc
rease in the catalytic activity which can be related to the increase i
n the acidic strength of Bronsted sites which compensate the decrease
in the number of sites. The further decrease in the cracking activity
(for more severely dealuminated zeolites) may be explained by the decr
ease in both concentration and acidic strength of Bronsted sites. The
cracking activity of our HZSM-5 zeolites was higher when hydrogen was
used (instead of nitrogen) as the carrier gas This indicates that hydr
ogen transfer plays an important role in n-heptane cracking.