R. Vomscheid et al., THE ROLE OF THE TEMPLATE IN DIRECTING THE SI DISTRIBUTION IN SAPO ZEOLITES, Journal of physical chemistry, 98(38), 1994, pp. 9614-9618
X-ray diffraction and Al-27 and Si-29 MAS NMR are used to study the in
teraction of the templates (morpholine or TEAOH) with the SAPO-34 fram
ework (chabasite structure) and to characterize the distribution of Si
in the lattice. The interaction of the template with Si-O-Al bonds su
ggests the formation of penta- and hexacoordinated Al. Specific limits
of Si contents (x(Si)) determine areas where Si(4A1) species are isol
ated (Si(4Al,9P)) or nonisolated (Si(4Al,nP,mSi)) or where Si forms is
lands. The two main parameters involved are the upper charge introduce
d by the template (b) and the upper x(Si) values (d) derived from topo
logy, to have isolated Si, Two main cases of the distribution of Si ar
e whether b < d or b > d. The results obtained for SAPO-34 are extende
d to any other SAPO.