Pearce E I, Hancock E M, Gallagher I H
Arch Oral Biol. 1984;29(7):521-7. doi: 10.1016/0003-9969(84)90073-6.
Plaque grown on terylene gauze in the mouths of 5 volunteers was treated with a mineralizing solution intermittently for 4 days to deposit fluorhydroxyapatite. Control plaque grown simultaneously was not treated. Sixteen hours after the last treatment, plaque gauzes were incubated in 0.28 M glucose under N2 at 37 degrees C. The mean pH, reached by the 5 mineralized plaques after 30 min, (4.78) was significantly higher than the mean pH reached by control plaques (4.13), a difference that was due neither to unequal microbial mass nor to unequal acid concentrations. Acid neutralization following the dissolution of apatite was probably mainly responsible for the pH differences although a small antiglycolytic effect from leached F could not be ruled out. Mineralized plaque lost on average 24 per cent of its Ca, 25 per cent of its P and 16 per cent of its F, resulting in 0.868 mM Ca, 0.676 mM P and 0.075 mM F in the supernatant. Test plaque fluid was saturated with respect to fluorapatite and only moderately undersaturated with respect to hydroxyapatite at the end of the incubation period; this could explain the pronounced caries-protective effect of plaque fluorhydroxyapatite shown previously.
在5名志愿者口腔中的涤纶纱布上生长的菌斑,用矿化溶液间歇处理4天以沉积氟羟基磷灰石。同时生长的对照菌斑未作处理。在最后一次处理16小时后,将菌斑纱布在37℃、氮气环境下于0.28M葡萄糖中孵育。5个矿化菌斑在30分钟后达到的平均pH值(4.78)显著高于对照菌斑达到的平均pH值(4.13),这种差异既不是由于微生物量不等,也不是由于酸浓度不等。磷灰石溶解后的酸中和可能是造成pH差异的主要原因,尽管不能排除浸出氟产生的微小抗糖酵解作用。矿化菌斑平均损失了其24%的钙、25%的磷和16%的氟,导致上清液中钙为0.868mM、磷为0.676mM、氟为0.075mM。在孵育期结束时,测试菌斑液相对于氟磷灰石饱和,而相对于羟基磷灰石仅适度不饱和;这可以解释先前显示的菌斑氟羟基磷灰石显著的防龋作用。