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体液、血浆和尿液相对于生物羟基磷灰石的过饱和状态。

Supersaturation of body fluids, plasma and urine, with respect to biological hydroxyapatite.

作者信息

Söhnel Otakar, Grases Felix

机构信息

Faculty of Enviromental Studies, University of J. E. Purkyne, Usti n.L., Czech Republic.

出版信息

Urol Res. 2011 Dec;39(6):429-36. doi: 10.1007/s00240-011-0387-5. Epub 2011 May 14.

Abstract

Supersaturation of body fluids, specifically of plasma and urine, with respect to biological hydroxyapatite was evaluated taking into account calcium complexation, fraction of total phosphorus present as hydrogen phosphate ions, solubility of carbonated hydroxyapatite and the size dependency of equilibrium solubility. Plasma is always supersaturated with respect to apatitic solid phase and thus calcific deposits are formed unless a sufficient quantity of potent inhibitors is present. When urinary pH is lower than 6.3 for normal urine hydroxyapatite cannot appear in renal stones, at higher pH apatitic renal stones can be formed. Predictions based on supersaturation calculated for different conditions correspond well with clinical observations.

摘要

考虑到钙络合、以磷酸氢根离子形式存在的总磷比例、碳酸化羟基磷灰石的溶解度以及平衡溶解度的尺寸依赖性,对体液(特别是血浆和尿液)相对于生物羟基磷灰石的过饱和度进行了评估。血浆相对于磷灰石固相始终处于过饱和状态,因此除非存在足够量的有效抑制剂,否则会形成钙化沉积物。对于正常尿液,当尿液pH值低于6.3时,肾结石中不会出现羟基磷灰石,而在较高pH值时,则会形成磷灰石肾结石。基于不同条件下计算出的过饱和度所做的预测与临床观察结果非常吻合。

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