Larsen M J, Pearce E I, Ravnholt G
Royal Dental College, Faculty of Health Sciences, University of Aarhus, Denmark.
Arch Oral Biol. 1997 Sep;42(9):657-63. doi: 10.1016/s0003-9969(97)00043-5.
The aim was to examine the nature of enamel dissolution in aqueous suspensions with a high solid/solution ratio and in a CO2-rich atmosphere. Before experimentation, a water-saturated mixture of 95% N2-5% CO2 was passed through the acid solutions for 24 hr. Samples of 2 g of powdered enamel were suspended in 7 ml of either 5 or 10 mmol/l HClO4, with or without 2 parts/10(6) fluoride and kept gently agitated for 24 hr in the above atmosphere. The same enamel samples were repeatedly exposed to fresh acid for 26 runs. All experiments were duplicated. The aqueous phase was analysed after 20 min and 24 hr for calcium, phosphate, fluoride, chloride, sodium and magnesium. It was found that after 20 min the fluoride was invariably taken up in the enamel and the solution was supersaturated with respect to hydroxyapatite with pH ranging 6.7-5.6. During the following 24 hr pH increased further, the supersaturation remained unchanged and the concentrations of calcium and phosphate in solution decreased. In contrast, sodium, magnesium and chloride were released from enamel during the entire period. In the later runs, the supersaturation with respect to hydroxyapatite was only modest and the decrease of calcium and phosphate concentrations limited, as were the release of sodium, magnesium and chloride. It is concluded that despite a CO2-rich atmosphere, calcium, phosphate and carbonate were released from enamel and quickly established a supersaturation with respect to hydroxyapatite with a secondary reprecipitation of mineral. It indicates that within the dental caries lesion in vivo, lesion fluid cannot exist undersaturated with respect to enamel apatite.
目的是研究在高固液比的水悬浮液中以及在富含二氧化碳的气氛中牙釉质溶解的性质。实验前,将95% N₂ - 5% CO₂的水饱和混合物通入酸溶液中24小时。将2克牙釉质粉末样品悬浮于7毫升5或10毫摩尔/升的高氯酸中,添加或不添加2 ppm的氟化物,并在上述气氛中轻轻搅拌24小时。相同的牙釉质样品重复暴露于新鲜酸中26次。所有实验均重复进行。在20分钟和24小时后分析水相中的钙、磷、氟、氯、钠和镁。结果发现,20分钟后氟总是被牙釉质吸收,溶液相对于羟基磷灰石过饱和,pH值范围为6.7 - 5.6。在接下来的24小时内,pH值进一步升高,过饱和度保持不变,溶液中钙和磷的浓度降低。相比之下,钠、镁和氯在整个期间都从牙釉质中释放出来。在后期实验中,相对于羟基磷灰石的过饱和度仅适度,钙和磷浓度的降低有限,钠、镁和氯的释放也有限。得出的结论是,尽管存在富含二氧化碳的气氛,但钙、磷和碳酸盐从牙釉质中释放出来,并迅速建立了相对于羟基磷灰石的过饱和度,伴有矿物质的二次再沉淀。这表明在体内龋齿病变中,病变液相对于牙釉质磷灰石不可能处于不饱和状态。