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The Monetite Structure Probed by Advanced Solid-State NMR Experimentation at Fast Magic-Angle Spinning

机译:高速魔角旋转中高级固态NMR实验探测的磁铁矿结构

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摘要

We present a solid-state nuclear magnetic resonance (NMR) spectroscopy study of the local P and H environments in monetite [CaHPO ; dicalcium phosphate anhydrous (DCPA)], as well as their relative spatial proximities. Each of the three H NMR peaks was unambiguously assigned to its respective crystallographically unique H site of monetite, while their pairwise spatial proximities were probed by homonuclear H– H double quantum–single quantum NMR experimentation under fast magic-angle spinning (MAS) of 66 kHz. We also examined the relative H– P proximities among the inequivalent {P1, P2} and {H1, H2, H3} sites in monetite; the corresponding shortest internuclear H– P distances accorded well with those of a previous neutron diffraction study. The NMR results from the monetite phase were also contrasted with those observed from the monetite component present in a pyrophosphate-bearing calcium phosphate cement, demonstrating that while the latter represents a disordered form of monetite, it shares all essential local features of the monetite structure.
机译:我们提出了在磁铁矿[CaHPO中的局部P和H环境的固态核磁共振(NMR)光谱研究。无水磷酸氢钙(DCPA)]以及它们的相对空间邻近度。三个H NMR峰中的每一个都明确地分配给了它们在晶体学上独特的H磁铁矿位点,而它们的成对空间邻近度则通过在快速魔术角旋转(MAS)为66的同核H-H双量子-单量子NMR实验中进行探测千赫。我们还研究了在磁铁矿中不等价的{P1,P2}和{H1,H2,H3}位点之间的相对H–P邻近度。相应的最短核内H–P距离与先前的中子衍射研究相符。橄榄石相的NMR结果也与从含焦磷酸盐的磷酸钙水泥中存在的橄榄石成分观察到的结果进行了对比,表明尽管后者代表了无序形式的莫纳石,但它共享了莫纳石结构的所有基本局部特征。

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