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ABSTRACT
When a granule of monocalcium phosphate monohydrate, Ca(H2PO4)2 · H2O, dissolves in a soil system, the fraction, f, of the phosphate left at the site of the granule as a dicalcium phosphate, CaHPO4 or CaHPO4 · 2H2O, is shown by the relation
f = (1 – R)/(2 – R)
where R, the mole ratio of CaO/P2O5 in the composite solution removed from the granule, can be determined experimentally or estimated from phase-rule data for the system CaO-P2O5-H2O. The composition of the solution leaving the granule approximates the invariant-point solution in equilibrium with Ca(H2PO4)2 · H2O and either CaHPO4 (the stable invariant point) or CaHPO4 · 2H2O (a metastable invariant point).
Equilibrium data from the literature suggest that a residue of CaHPO4 will contain some 28% of the P. Experimental data are presented from which a residue of CaHPO4 · 2H2O is predicted to contain about 21% of the P.
Reaction of some of the solute phosphate with cations such as iron and aluminum can cause precipitation of additional calcium phosphate.
1 Contribution of the Research Branch, Division of Chemical Development, TVA, Wilson Dam, Ala. Presented before Div. II, Soil Science Society of America, Cincinnati, Ohio, Nov. 15, 1956.
2 Research Chemists. Inez Jenkins Murphy and J. W. Williard made the chemical analyses.
Received for publication May 15, 1958. Accepted for publication August 13, 1958.
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