赤铁矿
磁铁矿
拉曼光谱
鳞片岩
针铁矿
磁铁矿
氧化铁
矿物学
材料科学
化学
分析化学(期刊)
环境化学
光学
冶金
物理化学
物理
吸附
作者
Dalva Lúcia Araújo de Faria,S. Venâncio Silva,M. T. de Oliveira
标识
DOI:10.1002/(sici)1097-4555(199711)28:11<873::aid-jrs177>3.0.co;2-b
摘要
Hematite (α-Fe2O3), magnetite (Fe3O4), wüstite (FeO), maghemite (γ-Fe2O3), goethite (α-FeOOH), lepidocrocite (γ-FeOOH) and δ-FeOOH were studied by Raman microscopy. Such compounds have already been studied by Raman spectroscopy, but there are some disagreements in the reported data. Here, Raman microscopy was employed to investigate the laser power dependence of the spectra of these oxides and oxyhydroxides. Low laser power was used for the reference spectra in order to minimize the risks of spectral changes due to sample degradation. The results obtained show that increasing laser power causes the characteristic bands of hematite to show up in the spectra of most of the compounds studied whereas the hematite spectrum undergoes band broadening and band shifts. © 1997 John Wiley & Sons, Ltd.
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