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富含 Pb 的磷灰石的固态 NMR 光谱学。

Solid-state NMR spectroscopy of Pb-rich apatite.

机构信息

Center for Environmental Molecular Science, State University of New York, Stony Brook, NY 11794-2100, USA.

出版信息

Magn Reson Chem. 2009 Dec;47(12):1062-70. doi: 10.1002/mrc.2514.

Abstract

Pb-containing hydroxylapatite phases synthesized under aqueous conditions were investigated by X-ray diffraction and solid-state nuclear magnetic resonance (NMR) techniques to determine the Pb, Ca distribution. 31P and 1H magic-angle spinning (MAS) NMR results indicate slight shifts of the isotropic chemical shift with increased Ca content and complex lineshapes at compositions with near equal amounts of Ca and Pb. 31P{207Pb} and 1H{207Pb} rotational-echo double resonance (REDOR) results for intermediate compositions show that resolved spectral features cannot be assigned simply in terms of local Ca, Pb configurations or coexisting phases. 207Pb MAS NMR spectra are easily obtained for these materials and contain well-resolved resonances for crystallographically unique A1 and A2 Pb sites. Splitting of the A1 and A2 207Pb resonances for pure hydroxyl-pyromorphite (Pb10(PO4)6(OH)2) compared to natural pyromorphite (Pb5(PO4)3Cl) suggests symmetry reduced from hexagonal. We find that 207Pb{1H} CP/MAS NMR is impractical in Pb-rich hydroxylapatites due to fast 207Pb relaxation.

摘要

在水相条件下合成的含 Pb 的羟基磷灰石相,通过 X 射线衍射和固态核磁共振(NMR)技术进行了研究,以确定 Pb 和 Ca 的分布。31P 和 1H 魔角旋转(MAS)NMR 结果表明,随着 Ca 含量的增加,各向同性化学位移略有移动,而 Ca 和 Pb 含量相近的组成则出现复杂的谱线形状。对于中间组成的 31P{207Pb}和 1H{207Pb}旋转回波双共振(REDOR)结果表明,不能简单地根据局部 Ca、Pb 构型或共存相来分配分辨的谱特征。对于这些材料,很容易获得 207Pb MAS NMR 光谱,并且包含独特的 A1 和 A2 Pb 位的晶体学分辨共振。与天然磷氯铅矿(Pb5(PO4)3Cl)相比,纯羟基磷氯铅矿(Pb10(PO4)6(OH)2)的 A1 和 A2 207Pb 共振的分裂表明,从六方对称性降低。我们发现,由于 207Pb 的快速弛豫,富含 Pb 的羟基磷灰石中 207Pb{1H} CP/MAS NMR 是不切实际的。

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