It has been shown that biominerals such as dental enamel and bone demonstrate a non-thermodynamic equilibrium state following initial dissolution where no further mineral dissolution or precipitation occurs; this state is termed metastable equilibrium solubility (MES). Furthermore, these minerals are composed of a distribution of domains each with their own MES. Recent studies have also demonstrated a linear relationship between crystallinity and the mean MES of these minerals, with solubility decreasing with increasing crystallinity. This study investigates the effect of age on the MES and crystallinity of rat bone mineral. The bone mineral samples were prepared by protein extraction with a series of hydrazine and alcohol solutions. The MES distributions of the bone mineral were measured by exposure to 0.1 M acetate buffers containing a range of calculated amounts of calcium (Ca) and phosphate for 48 h. The amount of mineral dissolved in each solution was determined from Ca and phosphate analyses of the undissolved residue. The full width of the half maximum (FWHM) of the 002 reflection of the X-ray powder diffraction was used as an indicator of crystallinity. The MES of mineral from bone of rats of different ages (1-25 months) were compared. Results of this study indicate that (l) there is a difference in the mean MES of bone mineral from rats of different ages, with older bone mineral being less soluble and more crystalline than bone mineral from younger rats; (2) the nature of the solubility distribution changes from a narrow to a broader distribution with age; and (3) all of the bone samples demonstrated an inverse-linear correlation between crystallinity and mean MES value consistent with previous results obtained with synthetic apatites and dental enamel.

The purpose of this research was to address the following question: How is the solubility of fluoride-pretreated carbonated apatite (CAP) in aqueous acidic media related to the equilibrium solution fluoride and/or the CAP adsorbed fluoride levels? A CAP sample prepared by a precipitation method at 70 degrees C containing approximately 6% carbonate was fluoride-treated (F adsorption from neutral aqueous solutions) to yield a approximately 1000 ppm F CAP and a approximately 3300 ppm F CAP. Metastable equilibrium solubility distributions were determined in acetate buffers at pH 5.0. Solution fluoride, calcium, phosphate, and pH were determined from the equilibrated solutions. The equilibrium solution fluoride levels were extremely low, e.g., as low as approximately 0.10 ppb to approximately 0.30 ppb at 50% dissolved for the two CAP preparations. The approximately 3300 ppm F CAP yielded a lower solubility than the approximately 1000 ppm F CAP (shift in the mean pKHAP value of 1.5-2 units). This can be attributed to the lower solution F(-) for the sample containing approximately 1000 ppm fluoride compared with the approximately 3300 ppm fluoride-containing CAP. These important findings suggest that a fluoride treatment simply may provide an adsorption fluoride depot for subsequent release, providing a solution fluoride effect upon the CAP solubility and not necessarily any intrinsic alteration of the mineral solubility.

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