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ABSTRACT
At least three groups of compounds were found to complex Zn2+ and Cu2+ in soil solution from the A horizon of a Williamson silt loam. A nondialyzable fraction of soil solution ligands had a poorly defined acid dissociation, pKa, ranging from 3 to 4.7. The dialyzable fraction had acid dissociation constants of 4.5 and 9.5, which were attributed to aliphatic and amino acids, respectively. The equivalent concentration of the nondialyzable acid fraction was only 1/40 that of the dialyzable fraction, but was more effective in complexing Zn and Cu in the soil solution. The average metal/ligand ratio was equal to unity in complexes of both the dialyzable and nondialyzable fractions with Zn2+ and Cu2+. Estimated, log10 (average formation constants) of the nondialyzable-metal complexes were calculated on the basis of titratable acidity as 4.3 ± 0.1 and 5.5 ± 0.1 for Zn2+ and Cu2+, respectively.
1 Contribution from the US Plant, Soil and Nutrition Laboratory, SWC, ARS, USDA, Ithaca, N.Y., in cooperation with the Department of Agronomy, New York State College of Agriculture, Ithaca.
2 Research Associate and Soil Scientist, respectively. Second author is also Associate Professor at Cornell University.
Received for publication May 3, 1968. Accepted for publication July 31, 1968.
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