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Studies of fluorapatite: II. The solubility behavior
Journal of Dental Research
|March 1, 1975
Summary
The solubility product of fluorapatite was determined in KCl solutions. Below pH 6, fluorite solubility, not fluorapatite, controlled the experimental conditions.
Area of Science:
- Geochemistry
- Environmental Science
Background:
- Fluorapatite is a key mineral in geological and biological systems.
- Understanding its solubility is crucial for environmental and geochemical modeling.
Purpose of the Study:
- To determine the solubility product of fluorapatite.
- To investigate the influence of ionic strength on fluorapatite solubility.
- To identify the dominant solubility control under acidic conditions.
Main Methods:
- Equilibration of a pure fluorapatite mineral specimen.
- Experiments conducted in potassium chloride (KCl) solutions.
- Varying ionic strengths up to 0.1 M were employed.
Main Results:
- The solubility product of fluorapatite was determined under specific conditions.
- At pH values below 5.0 to 6.0, fluorite solubility governed the system.
- This indicates that fluorapatite solubility is not the limiting factor in acidic environments.
Conclusions:
- Fluorapatite solubility is influenced by solution chemistry.
- Fluorite precipitation/dissolution is the primary control on mineral saturation in acidic conditions.
- These findings have implications for understanding mineral behavior in natural waters.