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Fluorine uptake into human enamel around a fluoride-containing dental material during cariogenic pH cycling

机译:在致龋pH循环过程中,含氟牙科材料周围的牙釉质吸收氟

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Using PIGE (TIARA, JAPAN) technique, we measured fluorine (F) uptake into the tooth enamel around a fluoride-containing material during caries progression using pH cycling. Class Ⅰ cavities in the buccal surfaces of 6 extracted human teeth were drilled and filled with fluoride-containing material; a glass ionomer cement (Fuji IX(GC)). Three 300 μm sections through the material were obtained from each tooth. Two of these specimens were utilized to measure the F distribution in enamel adjacent to the material. A 1.7 MeV proton beam accelerated by the TIARA single-ended accelerator was delivered to a micro-beam apparatus. The beam spot size was about 1 μm with a beam current of about 100 pA. A nuclear reaction, ~(19)F(p, αγ)~(16)0, was used to measure the F concentration and the gamma-rays from this reaction were detected with a 4″ Nal detector. X-rays induced by proton were detected with a Si(Li) detector to measure calcium concentration and the beam intensity was monitored with the X-ray yield from a copper foil for quantitative analysis. After measurement of F uptake, all specimens were polished to a thickness of 120 μm. In order to simulate daily acid challenges occurring in the oral cavity, the pH cycling (pH6.8-pH4.5) was carried out for 1, 3 and 5 weeks, separately. The duration that the solution remained below pH 5.5 was 37 min per cycle. The cycles were repeated 6 times per day with 2 h interval between cycles, and the specimens were kept in remineralizing solution for the rest of pH cycle. After pH cycling, F and calcium distribution of each specimen was evaluated using PIGE technique. The F distribution of the specimens before pH cycling clearly showed the F uptake from fluoride-containing material into enamel adjacent to the material. After pH cycling, the caries progression in all specimens was observed by the image of transverse microradiography (TMR). The depth of caries and mineral loss progressed with increasing the duration of pH cycling, although the enamel adjacent to the material remained a caries inhibition zone due to low rate of demineralization. With caries progression, fluorine accumulated in the subsurface of the caries lesion, while the outermost surface of the caries lesion gradually dissolved under increasing pH cycling. The data obtained using PIGE (TIARA, JAPAN) technique were useful to understand the fluorine benefit for preventing dental caries by means of fluoride-containing dental materials.
机译:使用PIGE(TIARA,JAPAN)技术,我们使用pH循环测量了龋齿进展过程中氟在含氟物质周围的牙釉质中的摄取。在6颗拔出的人类牙齿的颊面钻出Ⅰ类腔,并用含氟物质填充;玻璃离聚物水泥(Fuji IX(GC))。从每个牙齿上获得三个300μm的材料截面。这些样品中的两个被用来测量与材料相邻的搪瓷中的F分布。由TIARA单端加速器加速的1.7 MeV质子束被传送到微束设备。束斑大小约为1μm,束电流约为100 pA。用〜(19)F(p,αγ)〜(16)0核反应测量F浓度,并用4“ Nal检测器检测该反应产生的伽玛射线。用Si(Li)检测器检测质子诱导的X射线,以测量钙浓度,并用铜箔的X射线产率监测射线强度,以进行定量分析。在测量F吸收之后,将所有样品抛光至120μm的厚度。为了模拟口腔中每天发生的酸刺激,分别进行了1、3和5周的pH循环(pH6.8-pH4.5)。溶液保持低于pH 5.5的持续时间为每个循环37分钟。每天重复进行6次循环,每次循环之间间隔2小时,然后在其余的pH循环中将样品保存在矿化溶液中。 pH循环后,使用PIGE技术评估每个样品的F和钙分布。 pH循环之前样品的F分布清楚地表明F从含氟材料吸收到与该材料相邻的瓷釉中。 pH循环后,通过横向显微X射线摄影(TMR)的图像观察到所有标本中的龋病进展。龋齿的深度和矿物质流失随着pH循环持续时间的增加而发展,尽管由于低矿化率,与该材料相邻的瓷釉仍保留了龋齿抑制区。随着龋病的进展,氟在龋病灶的亚表面积累,而随着pH循环的增加,龋病灶的最外表面逐渐溶解。使用PIGE(TIARA,JAPAN)技术获得的数据有助于了解氟通过含氟牙科材料预防龋齿的益处。

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