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血清中的磷酸钙相变

Calcium phosphate phase transformations in serum.

作者信息

Eidelman N, Chow L C, Brown W E

出版信息

Calcif Tissue Int. 1987 Jul;41(1):18-26. doi: 10.1007/BF02555126.

DOI:10.1007/BF02555126
PMID:3040199
Abstract

A better knowledge of the pathological calcification mechanisms should provide a rational basis for their control. In the present study, dicalcium phosphate dihydrate (DCPD, CaHPO4 X 2H2O) was used as a source of calcium and phosphate ions to investigate the mechanism of formation of more basic and more insoluble calcium phosphates in ultrafiltered serum (u.f.s.). DCPD crystals were suspended in u.f.s. at 37 degrees C by constant stirring; samples were removed periodically for calcium and phosphate analysis and pH measurement. Occasionally, samples of solids were removed for X-ray diffraction. The experiments were carried out both with and without a 5.5% CO2 atmosphere. After initially becoming saturated with DCPD, the u.f.s. composition changed and became saturated with respect to octacalcium phosphate (OCP, Ca8H2(PO4)6 X 5H2O). At this point OCP crystals were detected in the solid phase by X-ray diffraction. Further stirring changed the composition so that it became undersaturated with both DCPD and OCP and shifted toward, but did not reach, a value so low as to be saturated with hydroxyapatite (OHAp, (Ca5(PO4)3OH). The presence of CO2 in the atmosphere slowed down, but did not prevent, the above sequence of events. The above results strongly suggest that calcifications, beneficial and pathological, that take place in serum may involve OCP as a precursor, which hydrolyzes in situ to a more basic apatitic product. The results also indicate that direct formation of OHAp in u.f.s. is a very slow process and may occur only rarely. The process appears to be similar in whole serum.

摘要

对病理性钙化机制有更深入的了解,应为控制钙化提供合理依据。在本研究中,磷酸二钙二水合物(DCPD,CaHPO₄·2H₂O)被用作钙和磷酸根离子的来源,以研究在超滤血清(u.f.s.)中形成碱性更强、更难溶的磷酸钙的机制。将DCPD晶体在37℃下通过持续搅拌悬浮于u.f.s.中;定期取出样品进行钙、磷分析和pH测量。偶尔取出固体样品进行X射线衍射分析。实验分别在有和没有5.5% CO₂气氛的条件下进行。最初u.f.s.被DCPD饱和后,其成分发生变化,相对于磷酸八钙(OCP,Ca₈H₂(PO₄)₆·5H₂O)达到饱和。此时通过X射线衍射在固相中检测到OCP晶体。进一步搅拌使成分发生变化,以至于对DCPD和OCP均不饱和,并向但未达到与羟基磷灰石(OHAp,(Ca₅(PO₄)₃OH))饱和时那么低的值转变。大气中CO₂的存在减缓了但并未阻止上述一系列事件的发生。上述结果强烈表明,血清中发生的有益和病理性钙化可能涉及OCP作为前体,它在原位水解为碱性更强的磷灰石产物。结果还表明,在u.f.s.中直接形成OHAp是一个非常缓慢的过程,可能很少发生。在全血清中该过程似乎类似。

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