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首页> 外文期刊>Geostandards and geoanalytical research >Crystal Chemical Characterisation of Red Beryl by 'Standardless' Laser-Induced Breakdown Spectroscopy and Single-Crystal Refinement by X-Ray Diffraction: An Example of Validation of an Innovative Method for the Chemical Analysis of Minerals
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Crystal Chemical Characterisation of Red Beryl by 'Standardless' Laser-Induced Breakdown Spectroscopy and Single-Crystal Refinement by X-Ray Diffraction: An Example of Validation of an Innovative Method for the Chemical Analysis of Minerals

机译:“标准”激光诱导的击穿光谱和X射线衍射单晶细化的红细胞晶体化学表征:矿物化学分析的创新方法验证示例

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摘要

Laser-induced breakdown spectroscopy (LIBS) is a valuable technique for performing qualitative and quantitative chemical determinations of all elements in one shot, including low atomic number elements such as Li and Be. This technique does not require any sample preparation to reveal the atomic species, even when present in trace amounts (m/m). In this study, for the first time, we provide an accurate mineral formula for a Cs-rich red beryl by combining crystallographic data obtained using the traditional single-crystal X-ray diffraction technique and quantitative chemical data obtained with an innovative 'standardless' method: Calibration-free-LIBS (CF-LIBS). In particular, a new LIBS prototype coupled with a petrographic microscope (CF-mu LIBS) was used to analyse chemically homogeneous areas of about 10 mu m spot size, causing minimal damage to the mineral. The results showed that calibration-free quantitative analysis is suitable for the quantification of major and minor low and high atomic number elements in beryl. The accuracy of quantification of low atomic number elements by CF-mu LIBS led to the empirical formula: (12])(Cs0.006Na0.019K0.017Ca0.019)(Sigma 0.061) ([4])(Be2.989Li0.011)(Sigma 3.000) ([6])(Ti0.053Mn0.051Mg0.007Al1.890)(Sigma 2.000) ([4])(Be0.116Fe0.024Si5.860)(Sigma 6.000)O-18. This formula is consistent with the crystal-structure refinement data and demonstrates the validity of CF-mu LIBS for chemical analyses of minerals containing low atomic number elements.
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