Okazaki M
Department of Dental Technology, Osaka University, Faculty of Dentistry, Japan.
Magnesium. 1988;7(3):148-53.
Fluorapatites with various magnesium contents (Mg-FAp) were synthesized at pH 7.4 and 80 degrees C. The contraction of their c-axis dimensions observed in X-ray diffraction analysis, together with the results of chemical analyses, suggested that Mg2+ ions may substitute into the apatite crystals to a limited extent. The apatites became less well crystallized with increase in magnesium content. At any given magnesium-calcium feed-in molar ratio (Mg/Ca)f, the magnesium uptake by Mg-FAp was higher than that by the corresponding F- -free Mg-HAp. Therefore, the former became amorphous at lower (Mg/Ca)f than the latter. However, in terms of crystallographic considerations, the Mg-FAp synthesized at high (Mg/Ca)f revealed its apatitic features after pyrolysis at 1,000 degrees C, while Mg-HAp displayed the tricalcium phosphate X-ray pattern.
在pH值为7.4、温度为80摄氏度的条件下合成了具有不同镁含量的氟磷灰石(Mg-FAp)。X射线衍射分析中观察到的其c轴尺寸收缩,以及化学分析结果表明,Mg2+离子可能在有限程度上替代进入磷灰石晶体。随着镁含量的增加,磷灰石的结晶度变差。在任何给定的镁钙进料摩尔比(Mg/Ca)f下,Mg-FAp对镁的吸收高于相应的无氟Mg-HAp。因此,前者在比后者更低的(Mg/Ca)f下就变成了非晶态。然而,从晶体学角度考虑,在高(Mg/Ca)f下合成的Mg-FAp在1000摄氏度热解后显示出其磷灰石特征,而Mg-HAp则呈现出磷酸三钙的X射线图谱。