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Application of Raman spectroscopy to the study of graphitic carbons in the Earth Sciences

机译:拉曼光谱在地球科学中的石墨碳研究中的应用

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Graphitic (sp~2-bonded) carbons are widespread on Earth and throughout the Universe. They have a complex structural organization ranging from amorphous and turbostratic phases to perfectly crystallized graphite. Raman spectroscopy is used extensively to characterize graphitic carbon in the Earth Sciences. In this chapter, we first review the theoretical knowledge of the Raman spectrum of graphitic carbons with an emphasis on the defect-activated peaks. These peaks have unique specificities that are described and explained in terms of the double-resonance theory. More practically, we discuss in detail all the peaks, their attributions and spectral properties. A methodology section is dedicated to the review of all possible analytical artifacts when characterizing graphitic carbons by Raman spectroscopy. A reference protocol is proposed for proper analysis. The last section reviews the application of Raman spectroscopy in the study of graphitic carbons in the Earth Sciences along the following theme: graphitization during meta-morphism, fluid-rock interactions, fossils and traces of life in the geological record, cosmochemistry and Earth-surface processes.
机译:石墨(SP〜2键合)碳是地球和整个宇宙的广泛普遍存在。它们具有复杂的结构组织,从无定形和涡轮静脉相比完全结晶的石墨。拉曼光谱是广泛用来在地球科学中表征石墨碳的用途。在本章中,我们首先审查了石墨碳的拉曼光谱的理论知识,重点是缺陷活化的峰。这些峰具有在双共振理论方面描述和解释的独特特异性。更实际地,我们详细讨论了所有峰值,其归属和光谱属性。一种方法部分致力于通过拉曼光谱表征石墨碳的所有可能的分析伪影。提出了参考协议以进行适当的分析。最后一节审查了拉曼光谱在地球科学研究中的应用沿着以下主题:在地质记录,宇宙化学和地面表面的荟牙,流体岩相互作用,化石和生命痕迹期间的石墨化流程。

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