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Phase Transformations in a Human Tooth Tissue at the Initial Stage of Caries

机译:龋初期人牙组织中的相变

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摘要

The aim of the paper is to study phase transformations in solid tissues of the human teeth during the development of fissure caries by Raman and fluorescence microspectroscopy. The study of the areas with fissure caries confirmed the assumption of the formation of a weak interaction between phosphate apatite enamel and organic acids (products of microorganisms). The experimental results obtained with by Raman microspectroscopy showed the formation of dicalcium phosphate dihydrate - CaHPO4-2H2O in the area of mural demineralization of carious fissure. A comparative analysis of structural and spectroscopic data for the intact and carious enamel shows that emergence of a more soluble phase - carbonate-substituted hydroxyapatite - is typical for the initial stage of caries. It is shown that microareas of dental hard tissues in the carious fissure due to an emerging misorientation of apatite crystals have a higher fluorescence yield than the area of the intact enamel. These areas can be easily detected even prior to a deep demineralization (white spot stage) for the case of irreversibly changed organomineral complex and intensive removal of the mineral component.
机译:本文的目的是通过拉曼光谱和荧光显微技术研究裂痕龋形成过程中人牙齿实体组织中的相变。对裂隙龋齿区域的研究证实了以下假设:磷酸盐磷灰石搪瓷与有机酸(微生物的产物)之间形成了弱相互作用。用拉曼光谱法获得的实验结果表明在龋裂的壁脱矿质区域中形成了磷酸二钙二水合物CaHPO4-2H2O。对完整和龋齿珐琅质的结构和光谱数据的比较分析表明,在龋齿的初始阶段,典型的出现是可溶性更强的相(碳酸盐取代的羟基磷灰石)的出现。结果表明,由于新出现的磷灰石晶体取向不正确,导致龋齿裂隙中牙齿硬组织的微区域的荧光产量高于完整牙釉质的面积。对于不可逆转的有机矿物配合物和大量去除矿物成分的情况,即使在深度脱矿质(白点阶段)之​​前,也可以轻松检测到这些区域。

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