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原子水平上的生物磷灰石与羟基磷灰石

Biological apatite vs hydroxyapatite at the atomic level.

作者信息

Young R A

出版信息

Clin Orthop Relat Res. 1975 Nov-Dec(113):249-62. doi: 10.1097/00003086-197511000-00036.

Abstract

Known differences in chemical content of biological apatites, specifically the dense (sp.g. greater than 2.95) portion of human tooth enamel (TE), and of stoichiometric hydroxyapatite (OHAp) imply atomic-scale crystal-structural differences, via major and minor substitutions, which can impart very different characteristics to the two materials. Further, some substitutions are shown to produce important effects not predictable from study of pure materials alone. A number of crystal-detail differences between TE and OHAp, both at room temperature and in response to heating (which occurs to some degree locally in hard tissue in vivo as a result of grinding, laser action, etc.), are tabulated. They include CO3 content and incorporation, lattice parameters, water content, non OHAp phases formed on heating, structural OH deficiency, and hydrogen-bonding of F and Cl "impurities" to OH. The significance of these differences is such that it is clearly misleading to speak of tooth enamel, and by inference other biological apatites, as "hydroxyapatite" without considerable qualification of the statement. The differences between biological apatite and OHAp are, in fact, of greater current interest and probable biological significance than are the similarities.

摘要

生物磷灰石化学组成上的已知差异,特别是人类牙釉质(TE)致密部分(比重超过2.95)与化学计量比羟基磷灰石(OHAp)的差异,意味着通过主要和次要取代作用在原子尺度上存在晶体结构差异,这会赋予这两种材料截然不同的特性。此外,一些取代作用显示出仅通过对纯材料的研究无法预测的重要影响。文中列出了TE和OHAp在室温下以及加热时(由于研磨、激光作用等,在体内硬组织中会局部发生一定程度的加热)的一些晶体细节差异。这些差异包括CO3含量及掺入情况、晶格参数、含水量、加热时形成的非OHAp相、结构中OH的缺失以及F和Cl“杂质”与OH的氢键作用。这些差异的重要性在于,如果不加相当程度的限定就将牙釉质以及由此推断的其他生物磷灰石称为“羟基磷灰石”,显然会产生误导。事实上,生物磷灰石与OHAp之间的差异在当前比它们的相似性更受关注,并且可能具有更大的生物学意义。

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