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Enamel hydroxyapatite lattice hydroxyl sites represent the specific chemical positions within the crystalline structure of tooth enamel where hydroxyl (OH-) ions reside. These sites are fundamental to the mineral's stability and are the primary focus of preventive dentistry (Featherstone, 2000). In the oral environment, bacterial acids can cause the dissociation of these ions, leading to the breakdown of the enamel matrix known as demineralization (Aoba, 1997). Therapeutic agents like fluoride target these sites through an ion-exchange mechanism, replacing the hydroxyl group with fluoride to form fluorapatite, a more chemically stable and acid-resistant mineral phase (Robinson, 2014). This process not only halts the progression of dental caries but also facilitates the remineralization of early-stage lesions. Consequently, these lattice sites are critical for maintaining the structural integrity of teeth against chemical and mechanical wear (NIH, 2023). Beyond fluoride, other remineralizing agents like casein phosphopeptide-amorphous calcium phosphate (CPP-ACP) also interact with these sites to promote mineral deposition (Reynolds, 2008). Understanding the chemistry of these sites is essential for developing next-generation dental materials that mimic natural enamel properties.
Ion substitution where fluoride ions replace hydroxyl ions in the crystal lattice to form fluorapatite, which has a lower solubility product and higher acid resistance.
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