The product of the reaction of HgCl2 vapor with fully dehydrated fully NH4
+-exchanged zeolite X at 115 °C,
ca. Hg44Cl64(NH4)68−Si100Al92O384 per unit cell, was studied by single-crystal X-ray diffraction techniques at
23 °C (R
1 = 0.121) in the cubic space group Fd3̄ (a
0 = 25.094(8) Å). Hg2+ ions are found at seven
nonequivalent sites, a surprisingly large number. Hg2+ ions at sites I and II each coordinate only to framework
oxygens; this is the first observation of Hg2+ ions at conventional ionic sites in a zeolite, and of very nearly
regular octahedral Hg(II), and of three-coordinate trigonal Hg(II). Hg2+ ions at two general site III‘ positions
form (HgCl2)3(NH4
+)2 and (HgCl2)3(NH4
+) clusters, respectively, in 12-rings with each Hg2+ ion bonding to
one framework oxygen. The Hg2+ ions at another two general site III‘ positions form (HgCl2)6(NH4
+)2 clusters,
also in 12-rings with each Hg2+ ion bonding to two framework oxygens. These two clusters could bridge
through Cl- ions to form a supercluster that contains as alternative subunits Hg12Cl12 rings each of which
wraps around a double six-ring. Site II is full with two Hg2+ and 30 NH4
+ ions. In each sodalite cage, an
NH4
+ ion at site I‘ bonds to three framework oxygens. Two Hg2+ ions per unit cell are seen near supercage
centers; each coordinates to three Cl- ions that bridge to other Hg2+ ions. The desired reaction of NH4-X
with HgCl2 vapor did not go to completion. Substantial amounts of HgCl2 were sorbed and cationic superclusters
of Hg(II) and Cl- have formed. This is the first observation of cationic halomercuric species.