Ishikawa K, Eanes E D, Tung M S
National Institute of Dental Research, Bone Research Associate Program, National Institute of Standards and Technology, Gaithersburg, Maryland 20899.
J Dent Res. 1994 Aug;73(8):1462-9. doi: 10.1177/00220345940730081101.
The importance of supersaturation in the dynamics of apatite precipitation from aqueous solutions is well-established. To determine whether this parameter has a comparable impact on the concomitant development of the textural properties of this phase, such as crystal size and shape, we investigated mineral accretion in synthetic solutions seeded with 0.67 g/L apatite over a range of supersaturations at pH 7.4 and 37 degrees C. A dual specific-ion electrode-controlled titration method was used to maintain the seeded reactions under the following solution conditions: 1.0 to 1.8 mmol/L Ca2+, 0.67 to 1.2 mmol/L total phosphate (PO4), Ca/PO4 (initial) = 1.5, 143 mmol/L KNO3, and 10 mmol/L HEPES. Samples were collected for chemical and textural analyses when the seed apatite was reduced by new accretions to 1/2, 1/4, 1/8, 1/16, and 1/32 of the total solids in suspension. All new accretions were found to be apatitic. At the lowest supersaturation, accretion occurred primarily by growth of the seed crystals. However, at the highest supersaturation examined, the crystals at the end of the experiments were actually smaller, on average, than the original seeds, even though the total mass increased 32-fold. The results suggest that proliferation of new crystals supplanted growth of the seed crystals as supersaturation was increased. The results also suggest that differences in tissue fluid supersaturation may contribute to the large disparity in dimensions between dentin and enamel apatite crystals.
过饱和度在水溶液中磷灰石沉淀动力学中的重要性已得到充分证实。为了确定该参数是否对该相的结构性质(如晶体大小和形状)的伴随发展具有类似影响,我们在pH 7.4和37摄氏度的一系列过饱和度条件下,研究了在含有0.67 g/L磷灰石晶种的合成溶液中的矿物生长。采用双特定离子电极控制滴定法,在以下溶液条件下维持晶种反应:1.0至1.8 mmol/L Ca2+、0.67至1.2 mmol/L总磷酸盐(PO4)、Ca/PO4(初始)= 1.5、143 mmol/L KNO3和10 mmol/L HEPES。当晶种磷灰石因新生长物而减少至悬浮液中总固体的1/2、1/4、1/8、1/16和1/32时,收集样品进行化学和结构分析。所有新生长物均被发现为磷灰石质。在最低过饱和度下,生长主要通过晶种晶体的生长发生。然而,在研究的最高过饱和度下,尽管总质量增加了32倍,但实验结束时的晶体平均实际上比原始晶种小。结果表明,随着过饱和度增加,新晶体的增殖取代了晶种晶体的生长。结果还表明,组织液过饱和度的差异可能导致牙本质和釉质磷灰石晶体在尺寸上的巨大差异。