氟离子与磷灰石在牙釉质中的再结晶。

Prakticke zubni lekarstvi Pub Date : 1990-02-01
O Brázda, R Zahradník
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引用次数: 0

摘要

本文讨论了碱基氟化原理的基本过程。珐琅质羟基磷灰石中F-离子与OH-基团的相互交换。评估羟基磷灰石和F-、氟磷灰石和OH-基团之间能量差的模型研究表明,氟磷灰石倾向于稳定释放氟离子并转变为羟基磷灰石。从预防龋齿的角度来看,这种趋势显然是不合时宜的,但它却保证了牙釉质表面上的氟含量永远很低。氟离子的存在促进了磷灰石在龋齿初期的再结晶。本研究试图从分子水平的理论化学角度,对实施防氟措施的重要途径之一——再矿化的机理进行新的探讨。
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[Fluoride ions and apatite recrystallization of apatite in enamel].

The authors discuss the basic process on which the principle of fluoridation in based--i.e. the mutual exchange of F- ions and the OH- group in hydroxyapatite of enamel. Model investigations assessing the energy difference between hydroxyapatite and F- and fluorapatite and the OH- group indicate that fluorapatite tends to release steadily fluoride ions and to change into hydroxyapatite. This tendency, apparently inopportune from the aspects of caries prevention, ensures, however, a permanent low F- level above the enamel surface. The presence of F- ions facilitates recrystalization of apatite in the initial caries stage. The investigation tries to throw new light, from the point of view of theoretical chemistry at a molecular level, on the mechanism of remineralization, one of the most important ways which implements the preventive action of fluoride.

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