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ABSTRACT
The Mn2+ concentrations in control and autoclaved suspensions of nine acid and alkaline soils in 0.01M CaCl2 differed widely from the Mn2+ concentrations calculated from models which either require measurement of Eh or assume Eh to be fixed by another redox couple. An alternative model is proposed which expresses the equilibrium solubility of the manganese compounds in terms of pH —
pMn. The values of pH —
pMn measured in the suspensions of all the soils tested correspond to the solubility of MnO2.
1 Contribution of the Department of Agricultural Chemistry & Soils, University of Arizona, Tucson, 85721. Journal Paper no. 1521 of the Arizona Agr. Exp. Sta.
Received for publication July 22, 1969. Accepted for publication December 2, 1969.
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