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ABSTRACT
At very low concentrations of Ca2+ in solution both H+ and Cu2+ retarded Zn2+ absorption through two distinct effects—toxicity and inhibition. Concentrations of 350µM Ca2+ overcame toxic effects of H+ at pH 3 but even 500µM Ca2+ did not prevent toxicity of Cu2+ at 10µM.
At Ca2+ concentrations commonly encountered in soil solutions no toxicities appeared. Copper inhibited Zn2+ absorption strongly and competitively, Co2+ competitively but weakly, and Mn2+ and Fe2+ had no effect. Also, Ca2+ had no effect on Cu2+ inhibition.
Increasing H+ concentration from pH 7 to 3 in the presence of 350µM, 10mM, or 50mM Ca2+ severely inhibited Zn2+ absorption. Hydrogen ions inhibited Zn2+ absorption by two mechanisms—one Ca2+-sensitive, the other Ca2+-insensitive. The Ca2+-sensitive mechanism only operated at very low Ca2+ or under very acid conditions. At the usual H+ and Ca2+ concentrations of soil solutions, H+ inhibited Zn2+ absorption only by the Ca2+ insensitive mechanism; in this mechanism H+ was non-competitive with Zn2+.
In soils the effects of Ca2+, Cu2+, and of H+ would be additive. However the effects of Cu2+ and especially of H+ on soil chemical reactions may operate in the opposite direction to their effects on Zn2+ absorption. More information is needed on the behavior of chelating compounds before the effects of Cu2+ on Zn2+ absorption from soils can be assessed.
1 Contribution from the Department of Soil Science & Plant Nutrition, Institute of Agriculture, University of Western Australia, Nedlands 6009. This work was supported by the West Australian Wheat Research Committee and by the grant of a Colombo Plan Studentship to the senior author.
2 Ph.D. student and Associate Professor in Plant Nutrition, respectively. Present address of the senior author, Radiation Genetics Institute, Atomic Energy Commission, Lyallpur, West Pakistan.
Received for publication June 18, 1971. Accepted for publication November 9, 1971.
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