The
structures of fully Zn2+-exchanged zeolite Y, |Zn37.5|[Si117Al75O384]-FAU (Si/Al
= 1.56), evacuated at 523, 623, 723, 773, and 823 K, were determined
at 100 K by single-crystal synchrotron X-ray diffraction in the cubic
space group Fd3̅m, a = 24.70 to 24.74 Å. At the three highest temperatures,
dehydration was complete. In those three, 26 of the 37.5 Zn2+ ions per unit cell lie directly in the planes of the two kinds of
six-rings (6Rs, rings containing six oxygen atoms and six tetrahedral
atoms (Si or Al)); other Zn2+ ions occupied positions on
either side of their 6Rs with Zn–O distances that are 0.1 to
0.3 Å longer. The number of Zn2+ ions in these planes
closely matches the number of three-Al (3Al) 6Rs calculated by simulated
annealing using MAS-NMR data. This indicates that Zn2+,
somewhat uniquely because of its ionic size and filled outer shell,
is able to lie in the 6R planes of 3Al 6Rs. It lies substantially
out of the planes of other 6Rs, predominantly 2Al 6Rs. Thus, it is
possible to count the number of 3Al 6Rs per unit cell. About 12 of
the 32 D6R 6Rs per unit cell, and 14 of the 32 S6Rs, are 3Al 6Rs.
This difference is a consequence of the “aluminum avoidance”
rule. After vacuum dehydration at 523 and 623 K, water oxygen atoms,
10 and 6, respectively, were found per unit cell, each bridging between
two Zn2+ ions in the sodalite cavities; these may be bridging
hydroxide ions. The structures (three at each dehydration temperature)
were refined using all intensities to final error indexes, R
1 for F
o > 4σ(F
o), between 0.04 at the lowest dehydration temperature
and 0.07 at the highest.