Aoba T, Collins J, Moreno E C
Forsyth Dental Center, Boston, Massachusetts 02115.
J Dent Res. 1989 Jul;68(7):1162-8. doi: 10.1177/00220345890680070501.
The present study was undertaken to elucidate the mechanism of fluoride incorporation into secretory enamel mineral, with porcine enamel used as a model. Although the fluoride content in the enamel varied greatly among the animals, we observed that the fluoride-to-calcium ratio in the enamel tissue was maximal at the beginning of the secretory stage; the F/Ca ratio decreased (and leveled off) with the advancement of mineralization. In vitro work showed that some of the fluoride in the secretory enamel tissue was removed with the extraction of organic matter, mostly amelogenins. Furthermore, coating hydroxyapatite crystals with enamel matrix proteins resulted in a retardation of fluoride incorporation into the crystals when exposed to fluoride solutions, as a result of an inhibition of apatite reprecipitation. We also confirmed that the growth kinetics of fluoridated apatite onto HA seeds decreased with increasing coverage of the seed surface with the enamel proteins. All the results of the present study strongly suggest that the fluoride incorporation into enamel mineral during the secretory stage may be regulated by the kinetics of mineralization, which is highly dependent on the driving force for precipitation and the presence of proteinaceous inhibitors, mainly amelogenins.
本研究以猪牙釉质为模型,旨在阐明氟化物掺入分泌期釉质矿物的机制。尽管动物牙釉质中的氟含量差异很大,但我们观察到,在分泌期开始时,牙釉质组织中的氟钙比最大;随着矿化进程,F/Ca 比下降(并趋于平稳)。体外研究表明,分泌期牙釉质组织中的一些氟化物会随着有机物(主要是釉原蛋白)的提取而去除。此外,用牙釉质基质蛋白包被羟基磷灰石晶体,当暴露于氟溶液时,由于抑制了磷灰石的再沉淀,导致氟化物掺入晶体的过程受阻。我们还证实,随着牙釉质蛋白对种子表面覆盖率的增加,氟化磷灰石在 HA 晶种上的生长动力学降低。本研究的所有结果强烈表明,分泌期牙釉质矿物中氟化物的掺入可能受矿化动力学的调节,而矿化动力学高度依赖于沉淀驱动力和蛋白质抑制剂(主要是釉原蛋白)的存在。