Abstract
The sorption of cobalt ion on calcium-montmorillonite was studied by the radioisotopic tracer method at different pH values. In dilute solutions the reaction has to be treated as a ternary exchange of cobalt, calcium, and hydrogen ions because of the high affinity of hydrogen ion to montmorillonite. Equilibrium constant for calcium-hydrogen exchange was determined.
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Schedule a callMore From: Colloids and Surfaces A: Physicochemical and Engineering Aspects
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