首页> 外文期刊>Journal of the American Chemical Society >Calcium-43 Chemical Shift Tensors as Probes of Calcium Binding Environments. Insight into the Structure of the Vaterite CaCO_3 Polymorph by ~(43)Ca Solid-State NMR Spectroscopy
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Calcium-43 Chemical Shift Tensors as Probes of Calcium Binding Environments. Insight into the Structure of the Vaterite CaCO_3 Polymorph by ~(43)Ca Solid-State NMR Spectroscopy

机译:钙43化学位移张量作为钙结合环境的探针。通过〜(43)Ca固态NMR光谱了解球ate石CaCO_3多晶型物的结构

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Natural-abundance ~(43)Ca solid-state NMR spectroscopy at 21.1 T and gauge-including projector-augmented-wave (GIPAW) DFT calculations are developed as tools to provide insight into calcium binding environments, with special emphasis on the calcium chemical shift (CS) tensor. The first complete analysis of a ~(43)Ca solid-state NMR spectrum, including the relative orientation of the CS and electric field gradient (EFG) tensors, is reported for calcite. GIPAW calculations of the ~(43)Ca CS and EFG tensors for a series of small molecules are shown to reproduce experimental trends; for example, the trend in available solid-state chemical shifts is reproduced with a correlation coefficient of 0.983. The results strongly suggest the utility of the calcium CS tensor as a novel probe of calcium binding environments in a range of calcium-containing materials. For example, for three polymorphs of CaCO_3 the CS tensor span ranges from 8 to 70 ppm and the symmetry around calcium is manifested differently in the CS tensor as compared with the EFG tensor. The advantages of characterizing the CS tensor are particularly evident in very high magnetic fields where the effect of calcium CS anisotropy is augmented in hertz while the effect of second-order quadrupolar broadening is often obscured for ~(43)Ca because of its small quadrupole moment. Finally, as an application of the combined experimental-theoretical approach, the solid-state structure of the vaterite polymorph of calcium carbonate is probed and we conclude that the hexagonal P6_3/mmc space group provides a better representation of the structure than does the orthorhombic Pbnm space group, thereby demonstrating the utility of ~(43)Ca solid-state NMR as a complementary tool to X-ray crystallographic methods.
机译:开发了21.1 T时的自然丰度〜(43)Ca固态NMR光谱和包括发射器增强波(GIPAW)的量规DFT计算工具,可提供洞察钙结合环境的工具,特别着重于钙化学位移(CS)张量。据报道,方解石对〜(43)Ca固态NMR光谱进行了首次完整分析,包括CS的相对取向和电场梯度(EFG)张量。一系列小分子的〜(43)Ca CS和EFG张量的GIPAW计算显示了实验趋势;例如,可用的固态化学位移趋势以0.983的相关系数再现。该结果强烈暗示了钙CS张量在一系列含钙材料中作为钙结合环境的新型探针的实用性。例如,对于CaCO_3的三种多晶型,CS张量跨度范围为8至70 ppm,并且与EFG张量相比,CS张量中钙的对称性表现出不同。表征CS张量的优势在非常高的磁场中尤为明显,其中钙CS各向异性的影响以赫兹为单位增加,而〜(43)Ca由于其四极矩小而常常使二阶四极展宽的效果模糊不清。最后,作为实验理论组合方法的应用,探索了碳酸钙球v石多晶型物的固态结构,并得出结论,六角形的P6_3 / mmc空间基团比正交晶形的Pbnm能更好地表示结构空间基团,从而证明〜(43)Ca固态NMR可作为X射线晶体学方法的补充工具。

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