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碳酸钙多晶型物方解石和文石的拉曼光谱:一项实验与计算相结合的研究。

The Raman spectrum of CaCO3 polymorphs calcite and aragonite: a combined experimental and computational study.

作者信息

De La Pierre Marco, Carteret Cédric, Maschio Lorenzo, André Erwan, Orlando Roberto, Dovesi Roberto

机构信息

Dipartimento di Chimica, Università di Torino and NIS (Nanostructured Interfaces and Surfaces) Centre of Excellence, Via P. Giuria 7, 10125 Torino, Italy.

Laboratoire de Chimie Physique et Microbiologie pour l'Environnement (LCPME), UMR 7564, Université de Lorraine-CNRS, 405 rue de Vandœuvre, 54601 Villers-lès-Nancy, France.

出版信息

J Chem Phys. 2014 Apr 28;140(16):164509. doi: 10.1063/1.4871900.

Abstract

Powder and single crystal Raman spectra of the two most common phases of calcium carbonate are calculated with ab initio techniques (using a "hybrid" functional and a Gaussian-type basis set) and measured both at 80 K and room temperature. Frequencies of the Raman modes are in very good agreement between calculations and experiments: the mean absolute deviation at 80 K is 4 and 8 cm(-1) for calcite and aragonite, respectively. As regards intensities, the agreement is in general good, although the computed values overestimate the measured ones in many cases. The combined analysis permits to identify almost all the fundamental experimental Raman peaks of the two compounds, with the exception of either modes with zero computed intensity or modes overlapping with more intense peaks. Additional peaks have been identified in both calcite and aragonite, which have been assigned to (18)O satellite modes or overtones. The agreement between the computed and measured spectra is quite satisfactory; in particular, simulation permits to clearly distinguish between calcite and aragonite in the case of powder spectra, and among different polarization directions of each compound in the case of single crystal spectra.

摘要

利用从头算技术(使用“混合”泛函和高斯型基组)计算了碳酸钙两种最常见相的粉末和单晶拉曼光谱,并在80K和室温下进行了测量。拉曼模式的频率在计算和实验之间非常吻合:方解石和文石在80K时的平均绝对偏差分别为4和8cm⁻¹。至于强度,总体上吻合良好,尽管在许多情况下计算值高估了测量值。联合分析几乎可以识别出这两种化合物的所有基本实验拉曼峰,但计算强度为零的模式或与更强峰重叠的模式除外。在方解石和文石中都识别出了额外的峰,这些峰被归因于¹⁸O卫星模式或泛音。计算光谱和测量光谱之间的吻合相当令人满意;特别是,模拟能够在粉末光谱的情况下清楚地区分方解石和文石,在单晶光谱的情况下区分每种化合物的不同偏振方向。

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