Seredin Pavel, Goloshchapov Dmitry, Prutskij Tatiana, Ippolitov Yury
Department of Solid State Physics and Nanostructures, Voronezh State University, Voronezh, Russia.
Instituto de Ciencias, Benemérita Universidad Autónoma de Puebla, Puebla, Mexico.
PLoS One. 2015 Apr 22;10(4):e0124008. doi: 10.1371/journal.pone.0124008. eCollection 2015.
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.
本文的目的是通过拉曼光谱和荧光显微光谱研究裂隙龋发展过程中人类牙齿固体组织中的相变。对有裂隙龋区域的研究证实了磷酸钙磷灰石釉质与有机酸(微生物产物)之间形成弱相互作用的假设。通过拉曼光谱获得的实验结果表明,在龋裂壁脱矿区域形成了二水磷酸二钙(CaHPO₄·2H₂O)。对完整釉质和龋损釉质的结构和光谱数据进行比较分析表明,在龋病初期,出现更易溶解的相——碳酸取代羟基磷灰石是典型特征。结果表明,由于磷灰石晶体出现取向错误,龋裂中牙齿硬组织的微区比完整釉质区域具有更高的荧光产率。对于不可逆改变的有机矿物质复合体和大量矿物质成分去除的情况,即使在深度脱矿(白斑阶段)之前,这些区域也很容易被检测到。