Sv. Borisov et al., CLASSIFICATION OF HEAVY-METAL FLUORIDES - FLUORIDES WITH HIGH WATER CONTENTS, Journal of structural chemistry, 36(3), 1995, pp. 439-444
Five fluoride structures differing in the character of linkage of cati
onic polyhedra and in relative water contents are considered. The cati
onic sublattice is four-layered (ABAC) in K2Cu(ZrF6)(2) . 6H(2)O, face
-centered (F-type, ABC) in CuZrF6 . 4H(2)O, primitive cubic (P-type) i
n Cu-3(ZrF7)(2) . 16H(2)O, hexagonal one-layered (AA) in Cu2ZrF8 . 12H
(2)O, and hexagonal two-layered (AB) in Zr2F8 . 6H(2)O. Some structure
s have considerably distorted symmetries of cationic sublattices compa
red to anhydrous structures because of the anisotropy of cation surrou
ndings in the first, second, and third spheres, bur all characteristic
close-packed cation planes of the corresponding structural types are
retained. In structures with cation-cation distances of similar to 3.5
Angstrom, dimeric cations are arranged as single fragments for planes
with d(hkl) > 3.5 Angstrom or as separate fragments for planes with s
maller d(hkl).