Copper(II) Interactions with Kaolinite: Factors Controlling Adsorption
- 1 April 1978
- journal article
- Published by Cambridge University Press (CUP) in Clays and Clay Minerals
- Vol. 26 (2) , 101-106
- https://doi.org/10.1346/ccmn.1978.0260204
Abstract
The adsorption of Cu2+ on kaolinite was studied at different ionic strengths following various treatments of the mineral surface in order to evaluate the conditions influencing adsorption. The data indicate a strong preference of the Na+ exchange form of kaolinite for Cu2+ but a weak affinity of the natural kaolinite for Cu2+. Protons are generated by Cu2+ adsorption, a result of the exchange of surface protons, and possibly the enhancement of Cu2+ hydrolysis at the kaolinite surfaces. The exchange of Na+ by Cu2+ on the kaolinite is not described by the mass-action equation, but can be interpreted in terms of permanent charge sites on the surfaces when the additional factors of Na+-H3O+ exchange and blockage of sites by Al ions are considered.Keywords
This publication has 10 references indexed in Scilit:
- Origin and Position of Exchange Sites in Kaolinite: An ESR StudyClays and Clay Minerals, 1976
- The sorption of copper species by clays. I. KaoliniteAustralian Journal of Chemistry, 1976
- Surface charge on kaolinites in aqueous suspensionSoil Research, 1976
- Exchangeable aluminium on kaoliniteSoil Research, 1976
- The exchange capacities of kaolinite and the preparation of homoionic claysJournal of Colloid and Interface Science, 1975
- THE RETENTION OF AMORPHOUS, COLLOIDAL ‘FERRIC HYDROXIDE’ BY KAOLINITESEuropean Journal of Soil Science, 1965
- FACTORS AFFECTING THE SOLUBILITY OF Al(OH)3 PRECIPITATED IN THE PRESENCE OF MONTMORILLONITESoil Science, 1965
- Effect of Iron Oxides on Positive and Negative Charges in Clays and SoilsClay Minerals, 1963
- Ion Exchange Equilibria Involving AluminumSoil Science Society of America Journal, 1961
- Mechanism of Sorption of Hydroxy Cupric Ion by ClaysSoil Science Society of America Journal, 1951