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Published in Soil Sci Soc Am J 43:866-870 (1979)
© 1979 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Zinc and Copper Solubility as a Function of pH in an Acid Soil1

M. B. McBride and J. J. Blasiak2

ABSTRACT

Studies of the effect of pH and competing cations on Zn2+ and Cu2+ solubility in an acid mineral soil indicate the probable involvement of hydrous oxides of iron, aluminum, or manganese in the adsorption process. Adsorption on permanent charge sites of clays, or complexation with organic matter could not account for the apparent fixation of Zn2+ in a nonexchangeable form in the pH range of 5 to 7. Nucleation of Zn hydroxide on clay mineral surfaces may have produced the strongly pH-dependent retention in the soil; however, Cu2+ showed more evidence of being controlled by organic complexation mechanisms. All soil solutions were undersaturated with respect to the least soluble hydroxides and carbonates of Cu2+ and Zn2+, at least at pH values below 7, indicating that simple precipitation was not involved in metal retention in the soil.


NOTES

1 Contribution of the Dep. of Agronomy, Cornell Univ., Ithaca, NY 14853. Agronomy Paper no. 1317.

2 Assistant Professor of Agronomy and Senior Undergraduate Agronomy Major, respectively.

Received for publication February 9, 1979. Accepted for publication April 18, 1979.




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Copyright © 1979 by the Soil Science Society of America.