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ABSTRACT
The adsorption and precipitation of cadmium ions in the presence of calcium carbonate was studied in an effort to understand the processes of Cd2+ retention in calcareous soils. Measurement of cadmium removal from solution by pure CaCO3 using a selective ion electrode indicated that the quantity of cadmium adsorbed depended upon the CaCO3 particle size. High levels of added cadmium apparently caused nucleation of CdCO3 on CaCO3 as the solutions approached saturation with respect to CdCO3. The initial chemisorption of Cd2+ on calcium carbonate was very rapid, while CdCO3 precipitation at higher cadmium concentrations was slow. Chemisorption may control Cd2+ activity in some calcareous soils, producing solubilities much lower than predicted by the solubility product of CdCO3. The surface area of soil carbonates is likely to be important in determining the levels of cadmium that can be immobilized by chemisorption. The affinity of calcite for metal ions appears to be a function of ionic radius, with divalent metal ions of the same size as Ca2+ readily substituting for Ca2+ in accessible surface sites.
1 Contribution of the Dep. of Agronomy, Cornell University, Ithaca, NY 14853. Agronomy Paper no. 1325.
2 Assistant Professor of Agronomy.
Received for publication July 9, 1979. Accepted for publication October 1, 1979.
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