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镁在37.4摄氏度下对磷酸氢钙和Ca4(PO4)2O体外形成羟基磷灰石的影响。

The effects of magnesium on hydroxyapatite formation in vitro from CaHPO4 and Ca4(PO4)2O at 37.4 degrees C.

作者信息

Martin R I, Brown P W

机构信息

Materials Research Laboratory, Penn State University, University Park, Pennsylvania 16802, USA.

出版信息

Calcif Tissue Int. 1997 Jun;60(6):538-46.

PMID:9164829
Abstract

The effects of magnesium ion on the formation of calcium-deficient hydroxyapatite [Ca9HPO4(PO4)5OH, CDHAp] from CaHPO4 and Ca4(PO4)2O dissolution were investigated using two magnesium sources: Mg3(PO4)2 (chemical system 1) or MgCl2 . H2O (chemical system 2) solutions. Because chloroapatite does not form from aqueous solutions, the use of two magnesium sources facilitated the determination of magnesium's role during synthetic hydroxyapatite formation in vitro and possible related effects during biomineralization. Isothermal calorimetry determined the progress of reactions. Two peaks are observed as heat is evolved during the formation of CDHAp in water at 37.4 degrees C. The nucleation and growth of CDHAp are the corresponding mechanisms. Although the time for complete reaction and total heat-of-reaction DeltaHr remain constant, the height of the first peak is reduced as the concentration of magnesium ion approaches 4 mM in either chemical system. Magnesium does not substitute into CDHAp even though there are calcium vacancies available. Subsequent increases cause the remaining heat peak to broaden and the time required for complete reaction to approach 24 hours as the initial MgCl2 concentration reaches 100 mM. Supersaturation limits chemical system 1 to Mg3(PO4)2 concentrations below 10 mM. A MgCl2 concentration of 3.16 M precludes CDHAp from forming for over 3 months; rather newberyite, MgHPO4 . 3H2O, precipitates. The morphology and surface area of the CDHAp formed in 100 mM MgCl2 solution are comparable to those of CDHAp formed in water. The surface areas are approximately 80 m2/g. Magnesium concentrations below 4 mM only inhibit nucleation whereas those above 4 mM inhibit growth as well. Magnesium phosphate complexes are more inhibitory than magnesium chloride complexes. Increasing the liquid-to-solids ratio or agitation significantly increases the induction period before reaction initiates. Increasing the liquid-to-solids ratio increases the time span for growth whereas increasing agitation decreases the time span for growth. The large inhibitory effect of agitation suggests quiescent systems are more suitable for determining the kinetics of HAp formation. A magnesium inorganic chemical activity (alphaMg = gammaMg[Mg2+]) many times greater than that in biological fluids is required before inhibition of hydroxyapatite formation is realized.

摘要

使用两种镁源

Mg3(PO4)2(化学体系1)或MgCl2·H2O(化学体系2)溶液,研究了镁离子对由CaHPO4和Ca4(PO4)2O溶解形成缺钙羟基磷灰石[Ca9HPO4(PO4)5OH,CDHAp]的影响。由于氯磷灰石不会从水溶液中形成,使用两种镁源有助于确定镁在体外合成羟基磷灰石形成过程中的作用以及生物矿化过程中可能的相关影响。等温量热法测定了反应进程。在37.4℃的水中形成CDHAp过程中放热时观察到两个峰。CDHAp的成核和生长是相应的机制。尽管完全反应的时间和反应总热ΔHr保持恒定,但在任何一个化学体系中,当镁离子浓度接近4 mM时,第一个峰的高度都会降低。即使存在钙空位,镁也不会替代进入CDHAp。随后浓度增加会导致剩余热峰变宽,并且随着初始MgCl2浓度达到100 mM,完全反应所需的时间接近24小时。过饱和度将化学体系1中的Mg3(PO4)2浓度限制在10 mM以下。3.16 M的MgCl2浓度可在3个多月内阻止CDHAp形成;相反,磷酸镁铵MgHPO4·3H2O会沉淀。在100 mM MgCl2溶液中形成的CDHAp的形态和表面积与在水中形成的CDHAp相当。表面积约为80 m2/g。低于4 mM的镁浓度仅抑制成核,而高于4 mM的镁浓度则同时抑制生长。磷酸镁络合物比氯化镁络合物的抑制作用更强。增加液固比或搅拌会显著增加反应开始前的诱导期。增加液固比会增加生长的时间跨度,而增加搅拌会减少生长的时间跨度。搅拌的巨大抑制作用表明静态体系更适合确定HAp形成的动力学。在实现对羟基磷灰石形成的抑制之前,需要镁的无机化学活性(αMg = γMg[Mg2+])比生物流体中的活性大许多倍。

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