E. Suzuki et al., MODIFICATION OF CRYSTAL-STRUCTURE OF AMMONIUM ROCHELLE SALT [NANH4(-C(4)H(4)O(6.)4H(2)O] OWING TO THE REPLACEMENT OF NH4 IONS WITH K IONS()), Acta crystallographica. Section B, Structural science, 52, 1996, pp. 296-302
The crystal structures of NaK1-x(NH4)(x)(+)-C4H4O6.4H(2)O (RS(1-x)ARS(
x), x=0.90, 0.94 and 1.00) have been determined in the paraelectric ph
ase (T=294K). The crystal data for ARS, orthorhombic, P2(1)2(1)2, R=0.
038, wR-0.032, no of reflections=3373, a-12.206(7) b=14,451(6), c=6.25
0(4)Angstrom, V=1102(1)Angstrom(3), D-x=1.573 g cm(-3), lambda(Mo-kapp
a-alpha(1))=0.70926Angstrom, F(000)=552.00; for RS(0.06)ARS(0.94), ort
horhombic, P2(1),2(1),2, R=0.0040, wR=0.030, no of reflections=2446, a
=12.172(4), b=14.421(4), c=6.239(2)Angstrom, V=1095.2(6)Angstrom(3), Z
=4, D-x=1.5292 g cm(-3), lambda(Mo-kappa-alpha(1))=0.70926Angstrom, F(
000)=553.92; for RS(0.10)ARS(0.090), orthorhombic, P2(1)2(1)2, R=0.036
, wR=0.0027, no of reflections=1898, a=12.165(9), b=14.420(7), c=6.239
(4)Angstrom, V=1094(1)Angstrom(3), Z=4, D-x=1.598 g cm(-3), lambda(Mo-
kappa-alpha(1))=0.70926Angstrom, F(000)=555.20. In the crystals there
are two crystallographically non equivalent cation sites occupied by K
/NH4 ions. The accommodation ratios of sites (1)[(2A) by the Wyckoff n
otation] and (2) [(2b)] are 0.94(1)and 0.92(1), respectively, in RS(0.
094)ARS(0.94), 0.90(1) and 0.93(1), respectively, in RS(0.10)ARS(0.90)
. As x increases, the location site (2) displaces towards the origin.
The hydrogen bonds around sites (1) and (2) are classified into two ty
pes: one is that the distances become longer as x increases, due to th
e differences in the ionic radii of K and NH4 ions, while the other is
that the distances are equal. Comparing the crystal structure of ARS
to that of RS, the following differences occur: the position of site (
2), the interatomic distances between cations of sites (1) and (2) and
oxygens, the form of the tartrate molecule and the position of some w
ater molecules. These differences seem to be mainly caused by the repl
acement of NH4 ions by K.