Daculsi G, Menanteau J, Kerebel L M, Mitre D
Calcif Tissue Int. 1984 Sep;36(5):550-5. doi: 10.1007/BF02405364.
An original method for fractionating and preparing isolated crystals of homogeneous size was developed. It was demonstrated that enamel apatite crystals are at least 100 micron long. The flexibility of the very long crystallites was demonstrated. Crystal curvatures, accounting for the irregular course of the prisms through the enamel thickness, were visualized and measured. It was shown that in the deep forming enamel layer, lateral branches may grow out of the crystals and crystal fusing often occurs, inducing the crystallites to assume pyramidal shapes with their wide bases pointing toward the dentino-enamel junction and one or two tops toward Tomes' processes. During the maturation process, the two tops of the still immature crystals also fuse so that the mature crystals acquire a rodlike aspect, with parallel faces and steplike graduations along the c axis, allowing a close contact between the crystals. These results support the hypothesis that the crystallites would be continuous from the dentino-enamel junction to the surface.
开发了一种用于分离和制备尺寸均匀的孤立晶体的原始方法。结果表明,牙釉质磷灰石晶体至少有100微米长。证明了非常长的微晶具有柔韧性。观察并测量了晶体曲率,这些曲率解释了棱柱在牙釉质厚度方向上的不规则走向。结果表明,在深层形成的牙釉质层中,晶体可能会长出侧枝,并且经常发生晶体融合,导致微晶呈现出金字塔形状,其宽基底指向牙本质-牙釉质交界处,一个或两个顶部指向托姆斯突。在成熟过程中,仍未成熟的晶体的两个顶部也会融合,从而使成熟的晶体呈现出棒状外观,具有平行面且沿c轴有阶梯状渐变,使得晶体之间能够紧密接触。这些结果支持了微晶从牙本质-牙釉质交界处到表面是连续的这一假设。