Okazaki M, Takahashi J, Kimura H
J Biomed Mater Res. 1986 Sep;20(7):879-86. doi: 10.1002/jbm.820200703.
Iron-containing fluoridated hydroxyapatites with various fluoride contents were synthesized at 80 degrees C and pH 7.4 using FeCl2 X nH2O as a source of iron. The Fe2+ uptake of fluoridated apatites was independent of fluoride concentration in the solution. a-Axis dimensions of Fe-containing apatites decreased with the degree of fluoridation in addition to the decrease related to the substitution of Fe2+ ions. All Fe-containing fluoridated apatites were less well crystallized than Fe-free fluoridated apatites previously reported, although with increasing degree of fluoridation, the crystallinity behavior of the former apatites appeared analogous to that of the latter apatites. In contrast to this inhibited crystallinity behavior, the apparent solubility of Fe-containing fluoridated apatites decreased more than that of Fe-free fluoridated apatites at low fluoride content.
以FeCl₂·nH₂O作为铁源,在80℃和pH 7.4的条件下合成了具有不同氟含量的含铁氟羟基磷灰石。氟磷灰石对Fe²⁺的吸收与溶液中的氟浓度无关。含铁磷灰石的a轴尺寸除了因Fe²⁺离子取代而减小外,还随着氟化程度的增加而减小。所有含铁氟磷灰石的结晶程度都不如先前报道的无铁氟磷灰石,不过随着氟化程度的增加,前者磷灰石的结晶行为似乎与后者磷灰石相似。与这种结晶行为受抑制的情况相反,在低氟含量下,含铁氟磷灰石的表观溶解度比无铁氟磷灰石下降得更多。