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Thermal decomposition of human tooth enamel
Calcified Tissue International
|January 1, 1980
Summary
Heating human tooth enamel (TE) reveals early carbonate loss, impacting treatments. Structural water loss and carbonate migration influence enamel
Area of Science:
- Materials Science
- Biomineralization
- Crystallography
Background:
- Human tooth enamel (TE) is a biomineral with a complex structure.
- Understanding the thermal behavior of TE components is crucial for various applications.
- Previous studies recognized some thermal degradation pathways but lacked detailed insights.
Purpose of the Study:
- To investigate the thermal decomposition of human tooth enamel (TE).
- To quantify the loss and transformation of key components like carbonate, hydroxyl, and water.
- To correlate these changes with alterations in the enamel's crystal lattice structure.
Main Methods:
- Heating TE in N2 or vacuum from 25-1000°C.
- Utilizing quantitative infrared spectroscopy.
- Employing lattice parameter and thermogravimetric analysis.
Main Results:
- Carbonate loss begins at lower temperatures (around 100°C) than previously thought.
- Structural hydroxyl content increases significantly up to 400°C.
- A sharp loss of structural water around 250-300°C correlates with lattice parameter contraction and reordering.
Conclusions:
- Early carbonate loss has implications for in vitro and in vivo treatments.
- Carbonate migration between A and B sites suggests interconnectedness relevant to biological conditions.
- Structural water plays a key role in the lattice expansion of TE compared to pure hydroxyapatite.