Abstract
The formation of 10750oxy-apatite may be a major determinant of the concentration of dissolved orthophosphate in many natural hard fresh waters. Tests of this hypothesis require knowledge of the precision and accuracy of the calculated ionic product [Ca2+]5 [PO sup3−inf4 ]3 [OH−]. In routine analyses the largest contribution to overall error is probably that of pH: precision and bias better than 0.02 units are desirable. There is also a large uncertainty present in the possible bias of the third ionisation ‘constant’ of ortho-phosphoric acid.
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References
Bjerrum & Unmack, 1929. K. Danske Vidensk. Selsk., Mat-Pys Medd. 9(1).
Ghosh, A. K., J. C. Ghosh & B. Prasad, 1980. Third dissociation constant of phosphoric acid from 283.15 K to 323.15 K. J. Indian Chem. Soc. 57: 1194–1199.
Golterman, H. L. & L. Meyer, 1985. the geochemistry of two hard water rivers, the Rhine and the Rhone, 4. The apparent solubility product of 10750oxy-apatite. 10750obiologia 126: 25–30.
Mesmer, R. E. & C. F. Baes, 1974. Phosphoric acid dissociation equilibria in aqueous solutions to 300°C. J. Solution Chem. 3: 307–332.
Nelder, J. A. & R. Mead, 1965. A simplex method for function minimization. Computer J. 7: 308–313.
Perrin, D. D., 1982. Ionisation Constants of Inorganic Acids and Bases in Aqueous Solution. 2nd Edn. Pergamon Press, N.Y., Oxford, Lond., Edinb., Paris, Frankfurt.
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Clymo, R.S., Golterman, H.L. Precision and accuracy of the determination of the ionic product of 10750oxy-apatite. Hydrobiologia 126, 31–34 (1985). https://doi.org/10.1007/BF00008384
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DOI: https://doi.org/10.1007/BF00008384