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Published in Soil Sci Soc Am J 58:1628-1632 (1994)
© 1994 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Solute Partitioning in a Calcium Carbonate-Phosphoric Acid-Water System

Yigal Salingar*

Keren Kayemeth LeIsrael (JNF), Land Development Authority, Soil Reclamation Dep., P.O. Box 45, 26103 K. Hayim, Israel

Malik Kochva

Faculty of Agricultural Engineering, Technion-Israel Institute of Technology, 32000 Haifa, Israel

* Corresponding author.

ABSTRACT

A range of Ca phosphates form in a time-dependent process, when calcite interacts with a dilute orthophosphate solution. This study was conducted to ascertain the possible formation of a stable CaCO3-PO4 compound on calcite surfaces and to characterize its precursors. The solution's ionic speciation provided evidence of the formation of a CaHCO3-PO4 compound (CBP) with a stoichiometric Ca/P ratio of 3 and a solubility product, Ksp, of (Ca2+)3(HCO3)3(PO3–4) = 10–28.36. This hypothesis was also supported by electron spectroscopy analyses of the surface layers of the final solid product and scanning electron microscopy (SEM). Prior to the CBP formation, either a compound with the same Ca/P ratio as dicalcium phosphate (DCP, CaHPO4) formed, or CBP was in quasi-equilibrium at a Ca/P ratio of 1.5 to 2.3. Another possibility is that a poorly crystalline or amorphous Ca phosphate solid phase was formed. Finally, the newly formed CBP converted to hydroxyapatite (HAP, Ca5 (PO4)3OH).


NOTES

This study conducted at Technion-Israel Inst. of Technology.

Received for publication January 14, 1992.





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