Driessens F C, Verbeeck R M
Calcif Tissue Int. 1985 Jul;37(4):376-80. doi: 10.1007/BF02553705.
A solid-state chemical model is derived to estimate the solubility of dolomites having different degrees of cation ordering. It is shown that the solubility of dolomites formed by precipitation at ordinary temperatures is such that it allows for the formation of dolomite in tooth enamel during in vivo mineralization.
推导了一个固态化学模型来估算具有不同阳离子有序度的白云石的溶解度。结果表明,常温下通过沉淀形成的白云石的溶解度使得其在体内矿化过程中能够在牙釉质中形成。