The physical properties of a series of layer double hydroxides (LHD) of the
farm [(CO3)(0.195(1-x))Cl-0.39x(H2O)(y)]:[Zn0.61Al0.39(OH)(2)], 0 less tha
n or equal to x less than or equal to 1, 0 less than or equal to y less tha
n or equal to(0.4+0.2x) have been studied. The hydration dynamics of these
materials indicate that the guest layer water molecules form a hydration ri
ng which defines the height of the solvated, nested Cl anion. The water mol
ecules can tilt around their Ct, axis such that the height of the solvated
Cl ion is a function of the number of molecules forming the hydration ring.
The composition dependence of the basal spacing, determined from x-ray-dif
fraction powder patterns measured as a function of humidity and temperature
for these materials, is a function of both the Cl concentration (x) and th
e number of guest layer water molecules (y). Distinct basal spacing curves
are observed for fully hydrated, partially hydrated, and dehydrated materia
ls. At x = 1 the Cl end-member material exhibits a change in stacking seque
nce from a 3R polytype to a 2H polytype upon dehydration. The dehydrated fa
rm of this material also exhibits a (root 3 x root 3)R30 degrees superlatti
ce ordering of the Cl ions. Due to the nesting of the Cl ion and the active
nature of the water molecules, the basal spacing vs x curve for the dehydr
ated materials is the only curve that can be fit by the discrete finite lay
er rigidity model. The interlayer rigidity parameter for LDH materials has
been determined to be p = 4.84+/- 0.06 indicating that these materials are
stiffer than class-II layered solids but not as stiff as class-III layered
solids.