Science. 1967 Mar 17;155(3768):1409-11. doi: 10.1126/science.155.3768.1409.
Carbonate is a substituent in the apatite structure; when present, it limits the size of the growing apatite crystals and so influences their shape that they grow more equiaxed than needle-like. The tendency for carbonate apatites to be equiaxed is related to the nature of the chemical bonds formed in the crystal. The interference of carbonate with the good crystallization of apatite, and its weakening effect on the bonds in the structure, increase the dissolution rate and the solubility, thereby presumably contributing to the susceptibility to caries of dental apatites containing carbonate.
碳酸盐是磷灰石结构中的取代基;当存在时,它限制了磷灰石晶体的生长,从而影响了晶体的形状,使其生长得更等轴而不是针状。碳酸盐磷灰石具有等轴倾向与其晶体中形成的化学键的性质有关。碳酸盐对磷灰石的良好结晶的干扰及其对结构中键的削弱作用,增加了溶解速率和溶解度,从而可能导致含有碳酸盐的牙磷灰石对龋齿的敏感性增加。