Publication | Open Access
Preparation and solubility of hydroxyapatite
244
Citations
8
References
1968
Year
Two portions of a synthetic hydroxyapatite (HA), Ca<sub>5</sub>OH(PO<sub>4</sub>)<sub>3</sub>, fully characterized by x-ray, infrared, petrographic, and chemical analyses, were heated at 1,000 °C in air and steam atmospheres, respectively. Solubility isotherms for these two samples in the system Ca(OH)<sub>2</sub>-H<sub>3</sub>PO<sub>4</sub>-H<sub>2</sub>O were determined in the <i>p</i>H range 5 to 7 by equilibrating the solids with dilute H<sub>3</sub>PO<sub>4</sub> solutions. Both samples of HA dissolved stoichiometrically. The activity products <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:mrow> <mml:msup> <mml:mrow><mml:mrow><mml:mo>(</mml:mo> <mml:mrow> <mml:msup><mml:mrow><mml:mtext>Ca</mml:mtext></mml:mrow> <mml:mrow><mml:mo>+</mml:mo> <mml:mo>+</mml:mo></mml:mrow> </mml:msup> </mml:mrow> <mml:mo>)</mml:mo></mml:mrow> </mml:mrow> <mml:mn>5</mml:mn></mml:msup> <mml:mrow><mml:mo>(</mml:mo> <mml:mrow> <mml:msup><mml:mrow><mml:mtext>OH</mml:mtext></mml:mrow> <mml:mo>-</mml:mo></mml:msup> </mml:mrow> <mml:mo>)</mml:mo></mml:mrow> <mml:msup> <mml:mrow><mml:mrow><mml:mo>(</mml:mo> <mml:mrow> <mml:msubsup><mml:mrow><mml:mtext>PO</mml:mtext></mml:mrow> <mml:mn>4</mml:mn> <mml:mo>≡</mml:mo></mml:msubsup> </mml:mrow> <mml:mo>)</mml:mo></mml:mrow> </mml:mrow> <mml:mn>3</mml:mn></mml:msup> </mml:mrow> </mml:math> and their standard errors-obtained by a least squares adjustment of the measurements (Ca and P concentrations and <i>p</i>H of the saturated solutions) subject to the conditions of electroneutrality, constancy of the activity product, and stoichiometric dissolution - were 3.7<sub>3</sub> ± 0.5 × 10<sup>-58</sup> for the steam-heated HA and 2.5<sub>1</sub> ± 0.4 × 10<sup>-55</sup> for the air-heated HA. Allowance was made in the calculations for the presence of the ion pairs [CaHPO<sub>4</sub>]<sup>0</sup> and [CaH<sub>2</sub>PO<sub>4</sub>]<sup>+</sup>. The higher solubility product for the air-heated HA is ascribed either to a change in the heat of formation brought about by partial dehydration or to a state of fine subdivision resulting from a disproportionation reaction. The solubility product constants were used to calculate the points of intersection (i.e., singular points) of the two HA solubility isotherms with the isotherms of CaHPO<sub>4</sub> · 2H<sub>2</sub>O and CaHPO<sub>4</sub>; it was found that the <i>p</i>H's of the singular points for the air-heated HA were a full unit higher than those of the steam-heated preparation. Conditions are described for the precipitation of HA crystals suitable for solubility measurements.
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