超饱和度对羟基磷灰石沉淀大小和形态的影响

K. Prakash, C. Ooi, R. Kumar, K. Khor, P. Cheang
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引用次数: 11

摘要

羟基磷灰石(HA)是在40℃、80℃和100℃的氢氧化钙水溶液中加入正磷酸水溶液,通过酸碱反应合成的。x射线衍射结果表明,在所有温度下析出相均以羟基磷灰石为主,颗粒形貌由40℃时的针状变为100℃时的球形。考虑了HA析出的驱动力以及Ca2+和po43离子相对于HA的超饱和水平,分析了形貌随温度的变化。与过饱和水平相比,温度对形貌的影响似乎不那么明显。分析还表明,反应物的过饱和水平,特别是Ca2+离子的浓度,对这一经典酸碱反应的沉淀形态起主导作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effect of Super Saturation Level on the size and morphology of Hydroxyapatite precipitate
Hydroxyapatite (HA) is synthesized through acid-base reaction by adding an aqueous solution of orthophosphoric acid to an aqueous solution of calcium hydroxide maintained at 40, 80 and 100°C. X-ray diffraction of the precipitate particles revealed HA as the predominant phase in all the temperatures and that the morphology of the particles changed from needle-shaped at 40°C to spheroid at 100°C. The changes in the morphology with temperature were analyzed taking into account the driving force for the HA precipitation and the super saturation level of Ca2+and PO43-ions with respect to HA. It appears that the effect of temperature on morphology is less pronounced compared to that of super saturation level. The analysis also indicated that the super saturation level of the reactants, especially the concentration of Ca2+ions, played a predominant role on the precipitate morphology for this classical acid-base reaction.
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