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Microbeam x-ray diffraction analysis of dental calculus
Journal of Dental Research
|February 1, 1983
Summary
Human dental calculus contains hydroxyapatite and octacalcium phosphate in porous areas, and whitlockite in dense regions. Brushite is rare, with a proposed formation mechanism involving plaque calcification transformation.
Area of Science:
- Crystallography
- Biomineralization
- Dental Science
Background:
- Dental calculus, a hardened form of plaque, significantly impacts oral health.
- Understanding its crystalline composition is crucial for dental research and treatment.
- Previous studies have identified various mineral phases, but their distribution and formation pathways require further clarification.
Purpose of the Study:
- To identify the crystalline components of human dental calculus.
- To analyze the distribution of these components based on calculus structure.
- To elucidate the formation mechanism of dental calculus.
Main Methods:
- Microbeam X-ray diffraction analysis was employed to determine the crystalline phases present.
- Samples were analyzed based on their structural characteristics (porous/zonal vs. homogeneous/highly calcified).
Main Results:
- Hydroxyapatite and octacalcium phosphate were predominant in porous, zonal calculus.
- Whitlockite was the main component in homogeneous, highly calcified calculus.
- Brushite was found to be rare, and calcite was not detected.
Conclusions:
- The crystalline composition of dental calculus varies with its structural morphology.
- A proposed formation mechanism suggests initial calcification involves octacalcium phosphate or brushite.
- These initial phases are subsequently hydrolyzed and transformed into hydroxyapatite and/or whitlockite.