Chemisorption of Cu(II) and Co(II) on Allophane and Imogolite

C. J. Clark1 and M. B. McBride
Department of Agronomy, Cornell University Ithaca, New York 14853
1 Present address: Ruakura Soil and Plant Research Station, Hamilton, New Zealand.

Abstract: Adsorption of Cu2+ and Co2+ by synthetic imogolite, synthetic allophanes with a range of SiO2/Al2O3 ratios, and allophanic clay fractions from volcanic ash soils was measured in an ionic medium of 0.05 M Ca(NO3)2. The effect of pH (and metal concentration) on adsorption was qualitatively similar for the synthetic and natural allophanes with relatively minor changes in behavior caused by variable SiO2/Al2O3 ratios. Cu and Co were chemisorbed by allophane at pH 5.0–5.5 and 6.9–7.2 (pH values for 50% adsorption level), respectively, with concomitant release of 1.6–1.9 protons/metal ion adsorbed. Quantitatively, adsorption by imogolite was less than that by the allophanes, presumably because of fewer sites available for chemisorption on the tubular structure of imogolite. Electron spin resonance studies of the imogolite and allophanes revealed that Cu2+ was adsorbed as a monomer on two types of surface sites. The preferred sites were likely adjacent AlOH groups binding Cu2+ by a binuclear mechanism; weaker bonding occurred at isolated AlOH or SiOH groups. These chemisorbed forms of Cu2+ were readily extracted by EDTA, CH3COOH, and metals capable of specific adsorption, but were not exchangeable. In addition, the H2O and/or OH- ligands of chemisorbed Cu2+ were readily displaced by NH3, with the formation of ternary Cu-ammonia-surface complexes.

Key Words: Allophane • Chemisorption • Cobalt • Copper • Electron spin resonance • Imogolite • SiO2/Al2O3

Clays and Clay Minerals; August 1984 v. 32; no. 4; p. 300-310; DOI: 10.1346/CCMN.1984.0320408
© 1984, The Clay Minerals Society
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