TenHuisen K S, Brown P W
Materials Research Laboratory, Pennsylvania State University, University Park 16802, USA.
J Biomed Mater Res. 1997 Sep 5;36(3):306-14. doi: 10.1002/(sici)1097-4636(19970905)36:3<306::aid-jbm5>3.0.co;2-i.
Calcium-deficient hydroxyapatite (HA) with a Ca/P molar ratio of 1.50 was synthesized in various concentrations (0.01-75 mM) of MgCl2 at 37.4 degrees C by reaction between particulate CaHPO4.2H2O and Ca4(PO4)2O. The effects of magnesium on the kinetics of HA formation were determined using isothermal calorimetry. All reactions completely consumed the precursor phases as indicated by X-ray diffraction analysis and a constant enthalpy of reaction (240 kJ/mol). Magnesium concentrations below 1 mM had no effect on the kinetics of HA formation. Magnesium concentrations between 1 and 2.5 mM affected the reaction path but did not affect the time required for complete reaction. Higher concentrations extended the times of complete reaction due to magnesium adsorption on the precursor phase(s) and HA nuclei, and stabilization of a noncrystalline calcium phosphate (NCP). HA formation in the presence of magnesium resulted in separation of the following two events: initial formation of HA nuclei and NCP, and consumption of CaHPO4.2H2O. This was indicated by the appearance of an additional calorimetric peak. Variations in calcium, magnesium, and phosphate concentrations and pH with time were determined. Increasing the magnesium concentration resulted in elevated calcium concentrations. After an initial decrease in magnesium owing to its adsorption onto HA nuclei and precursor(s), a period of slow reaction at constant magnesium concentration was observed. Both the magnesium concentration in solution and the proportions of precursors present decreased prior to any evidence of a crystalline product phase. This is attributed to the formation of NCP capable of incorporating magnesium. This noncrystalline phase persisted for more than 1 year for reactions in magnesium concentrations about 2.5 mM. Its conversion to HA resulted in the release of magnesium to the solution.
通过颗粒状CaHPO₄·2H₂O与Ca₄(PO₄)₂O之间的反应,在37.4℃下于各种浓度(0.01 - 75 mM)的MgCl₂中合成了钙磷摩尔比为1.50的缺钙羟基磷灰石(HA)。使用等温量热法测定了镁对HA形成动力学的影响。如X射线衍射分析和恒定反应焓(240 kJ/mol)所示,所有反应均完全消耗了前驱体相。低于1 mM的镁浓度对HA形成动力学没有影响。1至2.5 mM之间的镁浓度影响反应路径,但不影响完全反应所需的时间。更高的浓度延长了完全反应的时间,这是由于镁吸附在前驱体相和HA核上,以及非晶态磷酸钙(NCP)的稳定化。在镁存在下HA的形成导致以下两个事件分离:HA核和NCP的初始形成,以及CaHPO₄·2H₂O的消耗。这由一个额外的量热峰的出现表明。测定了钙、镁、磷酸盐浓度和pH随时间的变化。镁浓度增加导致钙浓度升高。由于镁吸附到HA核和前驱体上,镁最初有所下降,之后观察到在恒定镁浓度下有一段缓慢反应期。在有结晶产物相的任何证据出现之前,溶液中的镁浓度和存在的前驱体比例均下降。这归因于能够结合镁的NCP的形成。对于镁浓度约为2.5 mM的反应,这种非晶态相持续了一年多。它向HA的转化导致镁释放到溶液中。