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ABSTRACT
The solubility isotherm (25°C.) for gypsum was determined in the concentration range from 1.5 x 10-2 to 6.0 x 10-2 mols of S per liter by equilibrating CaSO4 · 2H2O with H2SO4 solutions of varying concentrations. The solubility product of gypsum calculated from these data was 2.45 x 10-5. The effect of gypsum upon the solubility of dicalcium phosphate dihydrate (DCPD) was related to the pH. The percentage of calcium in solution which was derived from DCPD was 80% and 3% at pH 3.6 and 6.3, respectively. The data from exchange resin and solubility studies are consistent with a hypothesized complex in solution of the form Ca(H2PO4)+. Equilibrations of DCPD and gypsum in soil systems indicated that apparent supersaturation with respect to both salts was obtained at pH values above 5.8. This anomalous behavior was explained by the complexing of Ca by soluble organic matter. The research findings are discussed in the light of soil and fertilizer chemistry.
1 Contribution from the Soils and Fertilizer Research Branch, Division of Agricultural Department, TVA, Wilson Dam, Ala. Presented at the annual meeting of the American Society of Agronomy, Cornell University, Ithaca, New York, August 20–23, 1962.
2 Formerly Research Chemist, TVA, now Research Associate, American Dental Association Research Div., National Bureau of Standards, Washington 25, D. C.; and Analytical Chemist, TVA, respectively.
Received for publication August 8, 1962. Accepted for publication April 17, 1963.
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