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关于碳酸钙球霰石多晶型体的晶体结构:钙-43固态核磁共振及计算评估

On the crystal structure of the vaterite polymorph of CaCO3: a calcium-43 solid-state NMR and computational assessment.

作者信息

Burgess Kevin M N, Bryce David L

机构信息

Department of Chemistry and Centre for Catalysis Research and Innovation, University of Ottawa, 10 Marie Curie Private, Ottawa, Ontario, Canada K1N 6N5.

Department of Chemistry and Centre for Catalysis Research and Innovation, University of Ottawa, 10 Marie Curie Private, Ottawa, Ontario, Canada K1N 6N5.

出版信息

Solid State Nucl Magn Reson. 2015 Feb;65:75-83. doi: 10.1016/j.ssnmr.2014.08.003. Epub 2014 Sep 8.

Abstract

The vaterite polymorph of CaCO3 has puzzled crystallographers for decades in part due to difficulties in obtaining single crystals. The multiple proposed structures for the vaterite polymorph of CaCO3 are assessed using a combined (43)Ca solid-state nuclear magnetic resonance (SSNMR) spectroscopic and computational approach. A combination of improved experimental and computational methods, along with a calibrated chemical shift scale and (43)Ca nuclear quadrupole moment, allow for improved insights relative to our earlier work (Bryce et al., J. Am. Chem. Soc. 2008, 130, 9282). Here, we synthesize a (43)Ca isotopically-enriched sample of vaterite and perform high-resolution quadrupolar SSNMR experiments including magic-angle spinning (MAS), double-rotation (DOR), and multiple-quantum (MQ) MAS experiments at magnetic field strengths of 9.4 and 21.1T. We identify one crystallographically unique Ca(2+) site in vaterite with a slight distribution in both chemical shifts and quadrupolar parameters. Both the experimental (43)Ca electric field gradient tensor and the isotropic chemical shift for vaterite are compared to those calculated with the gauge-including projector-augmented-wave (GIPAW) DFT method in an attempt to identify the model that best represents the crystal structure of vaterite. Simulations of (43)Ca DOR and MAS NMR spectra based on the NMR parameters computed for a total of 18 structural models for vaterite allow us to distinguish between these models. Among these 18, the P3221 and C2 structures provide simulated spectra and diffractograms in best agreement with all experimental data.

摘要

几十年来,碳酸钙的球霰石多晶型一直困扰着晶体学家,部分原因是难以获得单晶。使用(43)Ca 固态核磁共振(SSNMR)光谱和计算方法相结合的方式,对碳酸钙球霰石多晶型的多种 proposed 结构进行了评估。改进的实验和计算方法,加上校准的化学位移标度和(43)Ca 核四极矩,相对于我们早期的工作(Bryce 等人,《美国化学会志》2008 年,130 卷,9282 页),能提供更深入的见解。在这里,我们合成了球霰石的(43)Ca 同位素富集样品,并在 9.4 和 21.1T 的磁场强度下进行了高分辨率四极 SSNMR 实验,包括魔角旋转(MAS)、双旋转(DOR)和多量子(MQ)MAS 实验。我们在球霰石中确定了一个晶体学上独特的 Ca(2+)位点,其化学位移和四极参数都有轻微分布。将球霰石的实验(43)Ca 电场梯度张量和各向同性化学位移与用含规范投影增强波(GIPAW)密度泛函理论(DFT)方法计算得到的结果进行比较,试图确定最能代表球霰石晶体结构的模型。基于为总共 18 种球霰石结构模型计算的 NMR 参数,对(43)Ca DOR 和 MAS NMR 光谱进行模拟,使我们能够区分这些模型。在这 18 种模型中,P3221 和 C2 结构提供的模拟光谱和衍射图与所有实验数据最为吻合。

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