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Micro Raman Spectroscopy and Electron Probe Microanalysis of Graphite Spherulites and Flakes in Cast Iron

机译:铸铁中石墨球晶和薄片的显微拉曼光谱和电子探针显微分析

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In this investigation, the evolution and formation of graphitized microstructure of cast iron has been studied by using micro Raman spectroscopy and electron probe microanalysis (EPMA). The samples were prepared by carbothermic reduction of iron ore powder by plasma smelting in an extended arc thermal plasma reactor. Magnesium was added in the ladle to spherodize the graphite. Elemental mapping of the sample across the spherulites and flakes was performed by EPMA. Raman scattering data were collected at different positions across graphite spherulites and flakes. Micro Raman analysis shows graphite peaks at 1350 cm~(-1) (D), 1580 cm~(-1) (G), and higher order graphite peaks for both spherulites and flakes. Additional peaks between 200 and 800 cm~(-1) are found to be present only in the case of spherulites. These extra peaks originate from cementite (Fe_3C) present in and around the spherulites. It is inferred from the available experimental data that graphite spherulites are formed in areas richer in cementite.
机译:在这项研究中,已经通过使用显微拉曼光谱和电子探针显微分析(EPMA)研究了铸铁的石墨化微观结构的演变和形成。通过在扩展电弧热等离子体反应器中通过等离子体熔炼铁矿石粉末的碳热还原来制备样品。将镁添加到钢包中以球化石墨。通过EPMA对样品在球晶和薄片上的元素作图。拉曼散射数据是在横跨石墨球和薄片的不同位置收集的。显微拉曼分析显示在1350 cm〜(-1)(D),1580 cm〜(-1)(G)处的石墨峰,以及球晶和片状的高阶石墨峰。仅在球晶的情况下,发现在200至800 cm〜(-1)之间存在其他峰。这些多余的峰源自球晶中及其周围存在的渗碳体(Fe_3C)。从现有的实验数据中可以推断出,石墨球晶是在渗碳体含量较高的区域形成的。

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