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表面软化过程中氟化物与矿物质在牛牙釉质最外层的再沉积

Fluoride and mineral redeposition in outermost layers of bovine enamel during surface softening.

作者信息

Rentsch H, Merte K, Zschau H E, Plier F, Otto G, Vogt J

机构信息

Department of Conservative Dentistry, Karl-Marx-University of Leipzig, GDR.

出版信息

Caries Res. 1990;24(2):97-100. doi: 10.1159/000261247.

Abstract

Mineral and fluoride concentration changes in the outermost layers of bovine enamel (depth less than 1 micron) were measured after demineralization in unbuffered hydroxyethylcellulose gels of pH = 5.4 with an intrinsic fluoride concentration of about 0.02 ppm. A combination of two nuclear analytical techniques, Rutherford backscattering spectrometry (RBS) and proton-induced gamma ray emission spectrometry (PIGE) was applied to determine the Ca/P molar ratios and F depth profiles, respectively. When compared to deeper layers, a reduced loss of mineral content is observed for the depth range of about 0-0.1 micron corresponding well with a F concentration increase from about 500 to about 5,000 ppm in the same range. These findings are interpreted as a fluoride-induced partial remineralization of the superficial surface layer during an overall demineralization process.

摘要

在pH = 5.4、固有氟浓度约为0.02 ppm的无缓冲羟乙基纤维素凝胶中脱矿后,测量了牛牙釉质最外层(深度小于1微米)的矿物质和氟浓度变化。结合使用两种核分析技术,即卢瑟福背散射光谱法(RBS)和质子诱导γ射线发射光谱法(PIGE),分别测定Ca/P摩尔比和氟深度分布。与较深层相比,在约0 - 0.1微米的深度范围内观察到矿物质含量损失减少,这与同一范围内氟浓度从约500 ppm增加到约5000 ppm的情况良好对应。这些发现被解释为在整体脱矿过程中氟诱导的表层部分再矿化。

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