生物磷酸钙及其在骨和牙组织生理中的作用。磷酸钙的组成和溶解度。

F C Driessens, J W van Dijk, J M Borggreven
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引用次数: 65

摘要

骨和牙齿矿物组成的变化与成分是混合微晶磷灰石(AP)-八磷酸钙(OCP)样相和无定形或亚微晶磷酸钙(ACP)样相的模型是一致的,这些相可以以不同的比例出现。描述磷灰石相的可变组成和溶解度行为的适当模型由公式(公式:见文本)给出,其中组成参数x, y, z和u分别说明一种缺陷机制。少量离子如Cl-、K+和F-的掺入也会形成其它点缺陷;在体内条件下,许多微量元素可以替代Ca2+离子。这表明,离子的掺入或从晶体损失与水溶液接触是可逆的。文献数据被用来显示方向,其中溶解度产物的磷灰石相移的结合不同的生理相关离子。对现有文献数据的定量评价表明,Na+和CO3=的掺入是导致生物磷灰石溶解度变化的主要原因。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Biological calcium phosphates and their role in the physiology of bone and dental tissues I. Composition and solubility of calcium phosphates.

Variations in the composition of bone and tooth mineral are consistent with the model that the constituents are a mixed microcrystalline apatite (AP)-octocalcium phosphate (OCP) like phase and an amorphous or submicrocrystalline calcium phosphate (ACP) like phase whereby these phases can occur in different proportions. An appropriate model for a description of the variable composition and the solubility behavior of the apatite phase is given by the formula (formula: see text) in which the compositional parameters x, y, z, and u each account for one type of defect mechanism. Other point defects are formed as well by incorporation of minority amounts of ions such as Cl-, K+, and F-; a number of trace elements can substitute for Ca2+ ions under in vivo conditions. It is suggested that the incorporation of ions in or loss from the crystals in contact with aqueous solutions is reversible. Literature data are used to show the direction in which the solubility product of the apatite phase shifts by incorporation of the different physiologically relevant ions. A quantitative evaluation of the available literature data revealed that Na+ and CO3= incorporation is the main cause for shifts in the solubility product of biological apatites.

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