New anion exchangeable layered basic salts were prepared and their ion-exchange properties were studied. Basic copper acetate, Cu
2 (OH)
3 (OCOCH
3) ⋅ H
2O has a layer structure of the botallackite type. The acetate ions are located between the positively charged copper hydroxide layers and exchangeable with various anions. The exchanged product, Cu
2 (OH)
3 (MnO
4), was thermally decomposed to an amorphous mixture of CuO and CuMn
2O
4, which showed a high catalytic activity towards the oxidation of carbon monoxide. Another basic salt with a composition of Ni
1-xZn
2x (OH)
2 (OCOCH
3)
2x⋅ nH
2O (0.15<x<0.25) was prepared by hydrothermal hydrolysis of Ni-Zn mixed acetate solutions. The structure is of zinc basic salts such as Zn
5 (OH)
8Cl
2⋅ nH
2O and Zn
5 (OH)
8 (NO
3)
2⋅2H
2O; nickel ions form brucite-type hydroxide layers with vacancies, Ni
1-x (OH)
2, and zinc ions occupy the tetrahedral sites above and below the vacant sites outside the hydroxide layers. Acetate ions are weakly bound to the Zn
2+ ions, completing the tetrahedra, and easily exchanged with most of inorganic as well as organic anions. The reactions are reversible. Exchange with [Si
8O
20]
8- ions resulted in the formation of two-dimensional silicate layers analogous to those of 2: 1 type clay minerals.
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