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羟基磷灰石在简单无机溶液中的溶解度。

Hydroxyapatite solubility in simple inorganic solutions.

作者信息

Chen Z-F, Darvell B W, Leung V W-H

机构信息

Guanghua College of Stomatology, Sun Yat-Sen University, Guangzhou, China.

出版信息

Arch Oral Biol. 2004 May;49(5):359-67. doi: 10.1016/j.archoralbio.2003.12.004.

Abstract

OBJECTIVE

To use solid titration and laser-scattering end-point detection to determine the hydroxyapatite (HAP) solubility isotherm at 37 degrees C in a plain KCl solution, with CO(2) present, and with additional phosphate.

DESIGN

Pulverised HAP solid was used to perform a titration to saturation. A very sensitive detector capable of detecting the light scattered at small forward angles from a laser beam was adopted to monitor the onset of precipitation (or failure to dissolve) near the equilibrium point. Each addition of HAP solid caused a step increase in scattered light and this signal decreased quasi-exponentially with time. When a steady but elevated scattering was obtained, small portions of 1M HCl were added to lower the pH by about 0.5-2 units, according to need, to dissolve excess solid and allow a further titration. The scatter signal and pH data, plotted against the amount of HAP added, were used to estimate the actual end-point by interpolation and thus construct each point on the solubility isotherm.

RESULTS

The solubility isotherm for HAP in plain KCl solution in the absence of CO(2) obtained now differs substantially from the results of previous solubility studies (i.e. much lower). The increase in solubility due to CO(2) reported earlier was confirmed, while the effect of excess phosphate was found to be to increase the apparent solubility of HAP, contrary to elementary mass-action expectations.

CONCLUSIONS

The solid titration method is a more reliable approach than that of conventional excess solid method with respect to the determination of the HAP-carrying capacity. The solubility of HAP appears to be substantially lower than previously reported, and a reconsideration of all aspects of the system is warranted.

摘要

目的

采用固体滴定法和激光散射终点检测法,在37℃下,于普通氯化钾溶液中、存在二氧化碳以及添加额外磷酸盐的情况下,测定羟基磷灰石(HAP)的溶解度等温线。

设计

使用粉碎的HAP固体进行滴定至饱和。采用一种非常灵敏的探测器,该探测器能够检测从激光束向前小角度散射的光,以监测平衡点附近沉淀的开始(或溶解失败)。每次添加HAP固体都会导致散射光呈阶梯式增加,且该信号随时间呈准指数下降。当获得稳定但升高的散射时,根据需要加入小份1M盐酸,将pH值降低约0.5 - 2个单位,以溶解过量固体并允许进一步滴定。将散射信号和pH数据与添加的HAP量作图,通过插值法估计实际终点,从而构建溶解度等温线上的每个点。

结果

现在获得的在无二氧化碳的普通氯化钾溶液中HAP的溶解度等温线与先前溶解度研究的结果有很大不同(即低得多)。早期报道的由于二氧化碳导致的溶解度增加得到证实,而发现过量磷酸盐的作用是增加HAP的表观溶解度,这与基本的质量作用预期相反。

结论

在测定HAP承载能力方面,固体滴定法比传统的过量固体法更可靠。HAP的溶解度似乎比先前报道的要低得多,因此有必要重新考虑该体系的各个方面。

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