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Raman spectroscopy of mackinawite FeS in anodic iron sulfide corrosion products

机译:阳极硫化铁腐蚀产物中mackinawite Fes的拉曼光谱

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摘要

Raman spectroscopy in a confocal microscope was used to study electrochemically synthesized corrosion products from sour gas experiments. When exposed to oxygen-containing atmosphere, the initial mackinawite FeS corrosion product transformed under laser irradiation to hematite, Fe2O3. Measurements with a thin water layer on top of the corrosion products prevented the transformation, as drying was prevented. In situ Raman measurements of mackinawite formation avoided the problem of transformation completely. In situ and operando, the initially formed mackinawite showed two Raman peaks in the wavenumber range > 180 cm− 1 centered around 200–215 cm− 1 and 285–300 cm− 1. On an empirical basis, these modes were assigned to a B1g mode of the iron sublattice and an A1g mode of the sulfur sublattice, respectively. A comparison with a literature assignment for aged mackinawite suggests that the aging observed involves significant changes in the sulfur sublattice.
机译:共聚焦显微镜中的拉曼光谱用于研究酸性气体实验中电化学合成的腐蚀产物。当暴露于含氧气氛中时,最初的马基钠铁矿FeS腐蚀产物在激光照射下转变为赤铁矿Fe2O3。在腐蚀产物的顶部进行薄水层测量可以防止这种转变,因为可以防止干燥。原位拉曼法测定马基金刚石的形成完全避免了转变的问题。在原位和操作过程中,最初形成的马基诺石在波数范围> 180 cm− 1处以200–215 cm− 1和285–300 cm− 1为中心显示了两个拉曼峰。根据经验,这些模式被指定为B1g铁亚晶格的Al模式和硫亚晶格的Alg模式。与针对老化的马基金石的文献资料进行的比较表明,观察到的老化涉及硫亚晶格的显着变化。

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