44 Ca doped remineralization study on dentin by isotope microscopy
44 Ca doped remineralization study on dentin by isotope microscopy
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同位素显微镜下44 Ca掺杂牙本质再矿化研究
DOI:
10.1016/j.dental.2018.01.022
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发表时间:
2018
期刊:
影响因子:
5
通讯作者:
Tagami J.
中科院分区:
文献类型:
--
作者:
Hiraishi N.;Kobayashi S.;Yurimoto H.;Tagami J.
ObjectiveThe dental caries is developed as a result of an alternative course of mineral gain and loss. In order to distinguish between intrinsic Ca (tooth-derived mineral) and extrinsic Ca (solution-derived mineral) uptakes, a44Ca doped pH-cycling was performed using44Ca (a stable calcium isotope) remineralization solution.MethodsThe natural abundance of40Ca and44Ca is 96.9% and 2.1%, respectively. The remineralization solution was prepared using44Ca to contain 1.5 mmol/L CaCl2(44Ca), 0.9 mmol/L KH2PO4,130 mmol/L KCl, 20 mmol/L HEPES at pH 7.0. The pH-cycling was conducted on bovine root dentin daily by demineralization (pH 5.0) for 2 h, incubation in 0% (control) and 0.2% NaF (900 ppm fluoride) for 2 h and44Ca doped remineralization for 20 h. After 14 days pH-cycling, the specimens were sectioned longitudinally. On the sectioned surface, isotope imaging of40Ca and44Ca labeled mineral distribution was observed by a high mass-resolution stigmatic secondary ion 77 (Camera IMS 1270, Gennevilliers Cedex, France).ResultsUptake of44Ca was greater in intensity for the 0.2% fluoride group than the control, especially in the superficial lesions. The control group showed40Ca (intrinsic) distribution in the subsurface lesions and in the superficial lesions, meanwhile the fluoride group showed40Ca distribution limited in subsurface lesions. The total Ca (44Ca +40Ca) image revealed more homogeneously for the control than the fluoride group.SignificanceSince the fluoride-treated surface is more acid-resistant than intrinsic dentin, alternative minerals were dissolved from the intact intrinsic lesion in the demineralization cycle.