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铅和钒取代羟基磷灰石的固态核磁共振研究。

A solid-state NMR study of lead and vanadium substitution into hydroxyapatite.

作者信息

Pizzala Hélène, Caldarelli Stefano, Eon Jean-Guillaume, Rossi Alexandre Malta, San Gil Rosane A S, Laurencin Danielle, Smith Mark E

机构信息

Universite Aix-Marseille I-CNRS, UMR 6264 Laboratoire Chimie Provence, Spectrometries Appliquees a la Chimie Structurale, F-13397 Marseille, France.

出版信息

J Am Chem Soc. 2009 Apr 15;131(14):5145-52. doi: 10.1021/ja808270v.

Abstract

A systematic study on cationic and anionic substitution in hydroxyapatite structures was carried out, with the aim of understanding the impact of ion exchange on the crystalline structure and properties of these materials. Lead and vanadium were chosen for the exchange, due to their known effects on the redox and catalytic properties of hydroxypatites. Hydroxyapatites with variable Pb and V contents, Pb(x)Ca(10-x)(VO(4))(y)(PO(4))(6-y)(OH)(2) (x = 0, 2, 4, 6, 8 and 10 for y = 1; y = 0, 0.5, 1, 2, 3 and 6 for x = 10) were synthesized and characterized by NMR spectroscopy. Solid-state NMR allowed an analysis of the chemical environment of every ion after substitution into the hydroxyapatite network. (43)Ca and (207)Pb NMR spectra at different lead concentrations provided clear evidence of the preferential substitution of lead into the Ca(II) site, the replacement of the Ca(I) site starting at x = 4 for y = 1. Two NMR distinguishable Pb(I) sites were observed in Pb(10)(PO(4))(6)(OH)(2), which is compatible with the absence of a local mirror plane perpendicular to the c direction. In contrast with (31)P NMR, for which only small variations related to the incorporation of Pb are observed, the strong change in the (51)V NMR spectrum indicates that lead perturbs the vanadium environment more than the phosphorus one. The existence of a wide variety of environments for OH in substituted apatites is revealed by (1)H NMR, and the mobility of the water molecules appears to vary upon introduction of lead into the structure.

摘要

对羟基磷灰石结构中的阳离子和阴离子取代进行了系统研究,目的是了解离子交换对这些材料的晶体结构和性能的影响。由于铅和钒对羟基磷灰石的氧化还原和催化性能有已知影响,因此选择它们进行交换。合成了具有可变铅和钒含量的羟基磷灰石Pb(x)Ca(10-x)(VO(4))(y)(PO(4))(6-y)(OH)(2)(y = 1时,x = 0、2、4、6、8和10;x = 10时,y = 0、0.5、1、2、3和6),并通过核磁共振光谱进行了表征。固态核磁共振允许分析每个离子在取代进入羟基磷灰石网络后的化学环境。不同铅浓度下的(43)Ca和(207)Pb核磁共振光谱提供了明确的证据,表明铅优先取代Ca(II)位点,对于y = 1,从x = 4开始Ca(I)位点被取代。在Pb(10)(PO(4))(6)(OH)(2)中观察到两个核磁共振可区分的Pb(I)位点,这与不存在垂直于c方向的局部镜面是一致的。与(31)P核磁共振相反,对于(31)P核磁共振仅观察到与铅掺入相关的小变化,(51)V核磁共振光谱的强烈变化表明铅对钒环境的扰动比对磷环境的扰动更大。(1)H核磁共振揭示了取代磷灰石中OH存在多种环境,并且水分子的迁移率似乎在将铅引入结构后发生变化。

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