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碳酸高铁羟磷灰石 2H 和 2M 假晶型的晶体结构精修。

Crystal structure refinements of the 2H and 2M pseudomorphs of ferric carbonate-hydroxyapatite.

机构信息

School of Materials Science and Engineering, Nanyang Technological University, Blk N4.1, Nanyang Avenue, Singapore 639798.

出版信息

Dalton Trans. 2010 Jul 28;39(28):6488-95. doi: 10.1039/c001612h. Epub 2010 Jun 15.

DOI:10.1039/c001612h
PMID:20552124
Abstract

The crystal structures of the ferric carbonate-hydroxyapatite (Fe-CHAp) and oxyapatite (Fe-OAp) pseudomorphs were investigated by powder neutron diffraction and Fourier transform infrared spectroscopy. At low iron loadings, Fe-CHAp (x = 0.1) is A-B type carbonate apatite-2H, where atmospheric CO(2) displaces tunnel hydroxyl and framework phosphate (Ca(2+) + 2PO(4)(3-) --> square(Ca) + 2CO(3)(2-) and Ca(2+) + OH(-) --> Fe(3+) + CO(3)(2-)), while Fe-CHAp (x = 0.2) is A type carbonate apatite-2M. For high iron loadings (x = 0.5), near the solubility limit, Fe(3+) incorporation includes concomitant oxidation of hydroxyl groups (Ca(2+) + OH(-) --> Fe(3+) + O(2-)). The discontinuity in the lattice metric at x approximately 0.2 together with a progressive reduction of OH(-) and CO(3)(2-), substantiates these incorporation mechanisms. The general formula of Fe-CHAp is [Ca(4-x)(F)Fe(x)][Ca(6-y)(T) square(y)][(PO(4))(6-y)(CO(3))(y)][(OH(4))(2-x)(CO(3))(x)] (0 < or = x < or = 0.2, 0 < or = y < or = 0.2) and Fe-OAp is [Ca(3.8)(F)Fe(0.2)][Ca(6-x)(T)Fe(x)][(PO(4))][O(0.2+x)(OH)(1.8-x)] (0 < x < or = 0.3). These new data are placed in the context of earlier crystallographic studies, with the Ca(I)O(6) metaprism twist angle (phi) shown to be a reliable indicator of symmetry, such that for phi(max) > 27.(0) degrees, monoclinic and triclinic structures are preferable.

摘要

通过粉末中子衍射和傅里叶变换红外光谱研究了碳酸铁-羟磷灰石(Fe-CHAp)和氧磷灰石(Fe-OAp)的假晶结构。在低铁负载下,Fe-CHAp(x = 0.1)为 A-B 型碳酸磷灰石-2H,其中大气 CO₂取代隧道羟基和框架磷酸盐(Ca²⁺ + 2PO₄³⁻ → 方(Ca)+ 2CO₃²⁻和 Ca²⁺ + OH⁻ → Fe³⁺ + CO₃²⁻),而 Fe-CHAp(x = 0.2)为 A 型碳酸磷灰石-2M。对于高铁负载(x = 0.5),接近溶解度极限,Fe³⁺的掺入包括羟基的同时氧化(Ca²⁺ + OH⁻ → Fe³⁺ + O²⁻)。在 x 约为 0.2 时,晶格度量的不连续性以及 OH⁻和 CO₃²⁻的逐渐减少,证实了这些掺入机制。Fe-CHAp 的通式为 [Ca₄-x(F)Fe(x)][Ca₆-y(T)方(y)][(PO₄)₆-y(CO₃)y][(OH₄)2-x(CO₃)x](0 ≤ x ≤ 0.2,0 ≤ y ≤ 0.2)和 Fe-OAp 为 [Ca₃.8(F)Fe(0.2)][Ca₆-x(T)Fe(x)][(PO₄)][O(0.2 + x)(OH)(1.8 - x)](0 < x ≤ 0.3)。这些新数据被置于早期晶体学研究的背景下,表明 Ca(I)O₆ 五角棱镜扭曲角(phi)是对称性的可靠指标,因此对于 phi(max)>27.(0)度,单斜和三斜结构是优选的。

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