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羟基氧化铁磷灰石的晶体化学

The crystal chemistry of ferric oxyhydroxyapatite.

作者信息

Low H R, Phonthammachai N, Maignan A, Stewart G A, Bastow T J, Ma L L, White T J

机构信息

School of Materials Science and Engineering, Nanyang Technological University, 50 Nanyang Avenue, Singapore 639798.

出版信息

Inorg Chem. 2008 Dec 15;47(24):11774-82. doi: 10.1021/ic801491t.

Abstract

Ferric hydroxyapatites (Fe-HAp) and oxyapatites (Fe-OAp) of nominal composition [Ca(10-x)Fe(x)(3+)][(PO(4))(6)][(OH)(2-x)O(x)] (0 < or = x < or = 0.5) were synthesized from a coprecipitated precursor calcined under flowing nitrogen. The solid solubility of iron was temperature-dependent, varying from x = 0.5 after firing at 600 degrees C to x approximately 0.2 at 1000 degrees C, beyond which Fe-OAp was progressively replaced by tricalcium phosphate (Fe-TCP). Crystal size (13-116 nm) was controlled by iron content and calcination temperature. Ferric iron replaces calcium by two altervalent mechanisms in which carbonate and oxygen are incorporated as counterions. At low iron loadings, carbonate predominantly displaces hydroxyl in the apatite channels (Ca(2+) + OH(-) --> Fe(3+) + CO(3)(2-)), while at higher loadings, "interstitial" oxygen is tenanted in the framework (2Ca(2+) + (vac) --> 2Fe(3+) + O(2+)). Although Fe(3+) is smaller than Ca(2+), the unit cell dilates as iron enters apatite, providing evidence of oxygen injection that converts PO(4) tetrahedra to PO(5) trigonal bipyramids, leading to the crystal chemical formula [Ca(10-x)Fe(x)][(PO(4))(6-x/2)(PO(5))(x/2)][(OH)(2-y)O(2y)] (x < or = 0.5). A discontinuity in unit cell expansion at x approximately 0.2 combined with a substantial reduction of the carbonate FTIR fingerprint shows that oxygen infusion, rather than tunnel hydroxyl displacement, is dominant beyond this loading. This behavior is in contrast to ferrous-fluorapatite where Ca(2+) --> Fe(2+) aliovalent replacement does not require oxygen penetration and the cell volume contracts with iron loading. All of the materials were paramagnetic, but at low iron concentrations, a transition arising from crystallographic modification or a change in spin ordering is observed at 90 K. The excipient behavior of Fe-OAp was superior to that of HAp and may be linked to the crystalline component or mediated by a ubiquitous nondiffracting amorphous phase. Fe-HAp and Fe-OAp are not intrinsically suitable magnetic agents for drug delivery but may be useful in reactive cements that promote osteoblast proliferation.

摘要

标称组成为[Ca(10-x)Fe(x)(3+)][(PO(4))(6)][(OH)(2-x)O(x)](0≤x≤0.5)的铁羟基磷灰石(Fe-HAp)和氧磷灰石(Fe-OAp)由在流动氮气下煅烧的共沉淀前驱体合成。铁的固溶度取决于温度,从600℃煅烧后的x = 0.5变化到1000℃时的x≈0.2,超过该温度后Fe-OAp逐渐被磷酸三钙(Fe-TCP)取代。晶体尺寸(13 - 116纳米)由铁含量和煅烧温度控制。三价铁通过两种二价取代机制取代钙,其中碳酸根和氧作为抗衡离子掺入。在低铁负载量时,碳酸根主要取代磷灰石通道中的羟基(Ca(2+) + OH(-) --> Fe(3+) + CO(3)(2-)),而在较高负载量时,“间隙”氧占据晶格(2Ca(2+) + (空位) --> 2Fe(3+) + O(2+))。尽管Fe(3+)比Ca(2+)小,但随着铁进入磷灰石,晶胞膨胀,这提供了氧注入的证据,氧注入将PO(4)四面体转变为PO(5)三角双锥,从而得到晶体化学式[Ca(10-x)Fe(x)][(PO(4))(6-x/2)(PO(5))(x/2)][(OH)(2-y)O(2y)](x≤0.5)。在x≈0.2时晶胞膨胀的不连续性以及碳酸根FTIR指纹的大幅降低表明,超过该负载量后,氧注入而非通道羟基取代占主导。这种行为与亚铁氟磷灰石相反,在亚铁氟磷灰石中Ca(2+) --> Fe(2+)的异价取代不需要氧渗透,并且晶胞体积随铁负载量收缩。所有材料都是顺磁性的,但在低铁浓度下,在90K时观察到由晶体学修饰或自旋有序变化引起 的转变。Fe-OAp的赋形剂行为优于HAp,这可能与晶体成分有关,或者由普遍存在的非衍射无定形相介导。Fe-HAp和Fe-OAp本质上不是适合用于药物递送的磁性剂,但可能对促进成骨细胞增殖的活性水泥有用。

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