Rölla G, Bowen W H
Acta Odontol Scand. 1978;36(4):219-24. doi: 10.3109/00016357809004671.
The experiments showed that a part of the fluoride which was taken up by hydroxyapatite or teeth at low concentrations of fluoride at neutral pH was soluble in alkali (IN KOH, 24 h) and was thus not fluoroapatite. Calcium fluoride could not form under the present conditions because the solubility of this compound was not exceeded. It is suggested that the alkali soluble fluoride is adsorbed to calcium ions bound as counterions in the hydration layer of the hydroxyapatite or the enamel. This is consistent with previous findings in this laboratory, showing that fluoride displaced acidic proteins adsorbed to calcium receptors on the hydroxyapatite surface in the same way as other anions displace proteins. It could also be shown that polyanions and polycations adsorbed to hydroxyapatite surfaces by ionic exchange, displacing phosphate or phosphate and calcium respectively in the process. A model is suggested which differs slightly from that proposed by Bernardi.
实验表明,在中性pH值下低氟浓度时,被羟基磷灰石或牙齿吸收的一部分氟可溶于碱(在氢氧化钾中,24小时),因此不是氟磷灰石。在当前条件下不会形成氟化钙,因为该化合物的溶解度未被超过。有人提出,碱溶性氟吸附在羟基磷灰石或牙釉质水化层中作为抗衡离子结合的钙离子上。这与本实验室先前的发现一致,表明氟以与其他阴离子取代蛋白质相同的方式取代吸附在羟基磷灰石表面钙受体上的酸性蛋白质。还可以表明,聚阴离子和聚阳离子通过离子交换吸附在羟基磷灰石表面,在此过程中分别取代磷酸盐或磷酸盐和钙。有人提出了一个与贝尔纳迪提出的模型略有不同的模型。