Damen J J, Buijs M J, ten Cate J M
Department of Cariology, Endodontology, Pedodontology, Academic Centre for Dentistry Amsterdam (ACTA) Amsterdam, The Netherlands
Caries Res. 1998;32(6):435-40. doi: 10.1159/000016484.
Demineralization of dentin in the presence of fluoride produces lesions with a mineralized surface layer which becomes thicker and more mineralized with higher fluoride concentrations whereas the lesion depth is hardly affected. The aim of this study was to investigate the effects of the time of fluoride treatment and the amount of fluoride taken up on the properties of the mineralized layer. Discs of bovine dentin embedded in methylmethacrylate with one surface exposed were demineralized in 50 mM acetic acid, 2.2 mM CaCl2, 2.2 mM KH2PO4, pH 5.0. At the start and/or later during the demineralization period, the specimens were incubated individually for 1 or 2 days in 10 ml of the same demineralization solution supplemented with 0.5, 2.0 or 5.0 ppm fluoride, which was then assessed for changes in calcium and fluoride concentrations. After 2, 5 and 8 days, specimens were sectioned for microradiographic analysis so as to follow development of the lesions and the mineralized layers. The results were the following: While demineralization with fluoride present at the first day led to the formation of a surface layer, fluoride present only at a later day produced a subsurface layer, not at the lesion front but closer to the surface. This layer resulted from (re)precipitation and not from preservation of the original mineral. The 'integrated mineral content' of the surface layer increased linearly with the uptake of fluoride, which resulted in an apparent fluorapatite content of about 20 vol%. The profiles of the surface layers remained unchanged during continued demineralization in the absence of fluoride. It was concluded that in the presence of fluoride mineral loss is reduced as a result of the reprecipitation of dissolved mineral ions as a layer of fluoride-enriched apatite. This layer does not offer protection of underlying dentin against continued demineralization.
在有氟存在的情况下,牙本质脱矿会产生具有矿化表层的病变,随着氟浓度升高,该表层会变得更厚且矿化程度更高,而病变深度几乎不受影响。本研究的目的是调查氟处理时间和氟摄取量对矿化层性能的影响。将嵌入甲基丙烯酸甲酯且一个表面暴露的牛牙本质圆盘在50 mM乙酸、2.2 mM氯化钙、2.2 mM磷酸二氢钾、pH 5.0的溶液中脱矿。在脱矿期开始时和/或之后,将标本分别在10 ml补充有0.5、2.0或5.0 ppm氟的相同脱矿溶液中孵育1或2天,然后评估钙和氟浓度的变化。在2、5和8天后,将标本切片进行显微放射分析,以跟踪病变和矿化层的发展。结果如下:第一天存在氟时脱矿导致形成表层,而仅在稍后时间存在氟时会产生次表层,不在病变前沿,而是更靠近表面。该层是由(再)沉淀形成,而非原始矿物质的保存。表层的“综合矿物质含量”随氟摄取量线性增加,导致明显的氟磷灰石含量约为20体积%。在无氟的情况下继续脱矿期间,表层轮廓保持不变。得出的结论是,在有氟存在的情况下,由于溶解的矿物质离子重新沉淀为富含氟的磷灰石层,矿物质损失减少。该层不能保护下面的牙本质免受持续脱矿。