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Metastable equilibrium solubility behavior of bone mineral
1Department of Pharmaceutics and Pharmaceutical Chemistry, 301 Skaggs Hall, University of Utah, Salt Lake City, Utah 84112, USA.
Calcified Tissue International
|March 25, 1999
Summary
Bone mineral exhibits metastable equilibrium solubility (MES) distributions, similar to carbonated apatite (CAP). Hydroxyapatite stoichiometry governs bone mineral solubility, with age-related crystallinity changes correlating to MES values.
Area of Science:
- Biomineralization
- Bone Physiology
- Materials Science
Background:
- Carbonated apatites (CAP) display metastable equilibrium solubility (MES) distributions.
- Bone mineral's solubility behavior requires further investigation using MES concepts.
Purpose of the Study:
- Investigate bone mineral solubility using MES distributions.
- Compare bone mineral to synthetic CAP, considering crystallinity and composition.
- Identify the governing function for bone mineral and CAP dissolution.
Main Methods:
- Harvested bone samples from rats of varying ages (1, 5, 8 months).
- Deproteinated bone samples using hydrazine.
- Synthesized CAP via dicalcium phosphate dihydrate (DCPD) hydrolysis.
- Determined MES distributions by equilibrating samples in buffered solutions at various pHs.
- Calculated ion activity products for octacalcium phosphate, hydroxyapatite, and CAP stoichiometries.
Main Results:
- Bone mineral exhibits MES distribution phenomena.
- Changes in bone mineral crystallinity with age correlated with MES values.
- A synthetic CAP closely mimicked the physicochemical behavior of 8-month-old rat bone mineral.
- Hydroxyapatite stoichiometry accurately described MES results for both CAP and bone mineral.
- Surface complex with hydroxyapatite stoichiometry governs bone mineral solubility.
Conclusions:
- Bone mineral solubility behavior is governed by a surface complex with hydroxyapatite stoichiometry.
- Metastable equilibrium solubility distributions are characteristic of bone mineral.
- Synthetic CAP can serve as a model for bone mineral physicochemical properties.