拉曼光谱在地球与材料科学中的应用进展

1区 地球科学 Q1 Earth and Planetary Sciences Reviews in Mineralogy & Geochemistry Pub Date : 2014-01-01 DOI:10.2138/RMG.2013.78.13
D. Neuville, D. Ligny, G. Henderson
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引用次数: 136

摘要

当单色辐射νo入射到一个系统(气体、固体、液体、玻璃,无论有色或透明)时,大多数辐射都在系统中传输而不发生变化,但也会发生一些辐射散射(约为107个光子中的1个)。散射辐射对应于ν ' = νo±ν m。在分子系统中,散射光的能量(以波数为单位,ν m)主要位于与振动能级、旋转能级和电子能级之间的跃迁有关的范围内。散射辐射的偏振与入射辐射的偏振一般不同,散射强度和偏振都取决于观测方向。在20世纪20年代,世界各地不同的物理小组都在研究这个问题:1)一个由拉曼和克里希南(1928)组成的印度小组,他们在1928年首次观察到液体中的现象(拉曼因此工作获得1930年诺贝尔物理学奖);2)苏联的Landsberg和Mandelstam(1928)报道了石英中随频率变化的光散射的观测结果。3)法国的Cabannes和Rocard(1928)证实了Raman和Krishnan(1928)的观测结果,而Rocard(1928)发表了第一个理论解释。拉曼光谱的原理是用可见光谱范围内的单色光(激光)照射材料,然后入射光子与分子振动或晶体声子相互作用,引起散射光子波长的轻微位移。当分子的振动、转动或电子能量发生变化时,就会发生散射。如果散射是弹性的,并且入射光子与散射光子具有相同的能量,则该过程称为瑞利散射,这是主要的散射相互作用。如果……
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Advances in Raman Spectroscopy Applied to Earth and Material Sciences
When monochromatic radiation νo, is incident on a system (gas, solid, liquid, glass, whether colored or transparent) most of the radiation is transmitted through the system without change, but some scattering of this radiation can also occur (approximately 1 in 107 photons). The scattered radiation corresponds to ν′ = νo ± ν m . In molecular systems, the energy of the scattered light (in wavenumbers, ν m ) is found to lie principally in the range associated with transitions between vibrational, rotational and electronic energy levels. Furthermore, the scattered radiation is generally polarized differently from that of the incident radiation with both scattered intensity and polarization dependent upon the direction of observation. During the 1920’s different physics groups worked on this subject around the world: 1) an Indian group composed of Raman and Krishnan (1928), who made the first observations of the phenomenon in liquids in 1928 (Raman won the Nobel Prize in Physics in 1930 for this work); 2) Landsberg and Mandelstam (1928) in the USSR reported the observation of light scattering with change of frequency in quartz and finally 3) Cabannes and Rocard (1928) in France confirmed the Raman and Krishnan (1928) observations while Rocard (1928) published the first theoretical explanation. The principle of Raman spectroscopy is the illumination of a material with monochromatic light (laser) in the visible spectral range followed by the interaction of the incident photons with the molecular vibrations or crystal phonons which induces a slight shift in the wavelength of the scattered photons. Scattering can occur with a change in vibrational, rotational or electronic energy of a molecule. If the scattering is elastic and the incident photons have the same energy as the scattered photons, the process is called Rayleigh scattering and this is the dominant scattering interaction. If …
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来源期刊
Reviews in Mineralogy & Geochemistry
Reviews in Mineralogy & Geochemistry 地学-地球化学与地球物理
CiteScore
8.30
自引率
0.00%
发文量
39
期刊介绍: RiMG is a series of multi-authored, soft-bound volumes containing concise reviews of the literature and advances in theoretical and/or applied mineralogy, crystallography, petrology, and geochemistry. The content of each volume consists of fully developed text which can be used for self-study, research, or as a text-book for graduate-level courses. RiMG volumes are typically produced in conjunction with a short course but can also be published without a short course. The series is jointly published by the Mineralogical Society of America (MSA) and the Geochemical Society.
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