GlaxoSmithKline, Weybridge, UK.
Caries Res. 2011;45(3):313-22. doi: 10.1159/000324804. Epub 2011 Jun 30.
The aim was to study the effects of zinc (Zn) and fluoride (F) on remineralisation at plaque fluid concentrations. Artificial carious lesions were created in 2 acid-gel demineralising systems (initially infinitely undersaturated and partially saturated with respect to enamel) giving lesions with different mineral distribution characteristics (high and low R values, respectively) but similar integrated mineral loss values. Lesions of both types were assigned to 1 of 4 groups and remineralised for 5 days at 37°C. Zn and F were added, based on plaque fluid concentrations 1 h after application, to give 4 treatments: 231 μmol/l Zn, 10.5 μmol/l F, Zn/F combined and an unmodified control solution (non-F/non-Zn). Subsequently remineralisation was measured using microradiography. High-R lesions were analysed for calcium, phosphorus, F and Zn using electron probe micro-analysis. All lesions underwent statistically significant remineralisation. For low-R lesions, remineralisation was in the order F(a) < non-F/non-Zn(a) < Zn(a, b) < Zn/F(b), and for high-R lesions F(a) < non-F/non-Zn(b) < Zn(b) < Zn/F(c) (treatments with the same superscript letter not significantly different, at p < 0.05). Qualitatively, remineralisation occurred throughout non-F/non-Zn and Zn groups, predominantly at the surface zone (F) and within the lesion body (Zn/F). Electron probe micro-analysis revealed Zn in relatively large amounts in the outer regions (Zn, Zn/F). F was abundant not only at the surface (F), but also in the lesion body (Zn/F). Calcium:phosphate ratios were similar to hydroxyapatite (all). To conclude, under static remineralising conditions simulating plaque fluid, Zn/F treatment gave significantly greater remineralisation than did F treatment, possibly because Zn in the Zn/F group maintained greater surface zone porosity compared with F, facilitating greater lesion body remineralisation.
目的是研究在菌斑液浓度下锌(Zn)和氟化物(F)对再矿化的影响。在 2 种酸凝胶脱矿系统(初始条件下对釉质无限过饱和度和部分饱和度)中创建人工龋齿病变,产生具有不同矿物质分布特征(高和低 R 值,分别)但具有相似整体矿物质损失值的病变。将这两种类型的病变分别分配到 4 组中的 1 组中,并在 37°C 下再矿化 5 天。根据应用后 1 小时的菌斑液浓度添加 Zn 和 F,给予 4 种处理:231 μmol/l Zn、10.5 μmol/l F、Zn/F 联合和未修饰的对照溶液(非 F/非 Zn)。随后使用显微放射照相术测量再矿化。使用电子探针微分析对高 R 值病变进行钙、磷、F 和 Zn 分析。所有病变均经历了统计学上显著的再矿化。对于低 R 值病变,再矿化顺序为 F(a)<非 F/非 Zn(a)<Zn(a,b)<Zn/F(b),对于高 R 值病变,F(a)<非 F/非 Zn(b)<Zn(b)<Zn/F(c)(处理相同上标字母之间无显著差异,p<0.05)。定性地说,再矿化发生在非 F/非 Zn 和 Zn 组中,主要在表面区(F)和病变体中(Zn/F)。电子探针微分析显示 Zn 在外部区域(Zn、Zn/F)中以相对大量存在。F 不仅在表面(F)丰富,而且在病变体(Zn/F)中丰富。钙:磷比值与羟基磷灰石相似(均)。总之,在模拟菌斑液的静态再矿化条件下,Zn/F 处理比 F 处理产生更显著的再矿化,可能是因为 Zn/F 组中的 Zn 保持了比 F 更大的表面区孔隙率,从而促进了更大的病变体再矿化。