Abstract
The effect of pH changes
and the presence of ligands on the uptake of lead and cadmium ions by three
types of clay mineral (kaolinite, illite and montmorillonite) has been
investigated. ��� In the absence of ligands, metal ion
adsorption increases gradually with increasing pH until a threshold pH value is
exceeded, whereupon total precipitation/sorption (attributed to formation of
hydroxy species) occurs. With ligands present, the threshold point tends to
shift to higher pH values, the magnitude of the effect depending on the
stability of the metal complex formed. Adsorption of cationic metal complexes
is subject to competition from charged protonated ligand species; anionic
complexes are not sorbed.
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