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Porous Ore Structure and Deposited Carbon Type during Integrated Pyrolysis-Tar Decomposition

机译:多孔矿石结构和沉积碳类型在整合热解焦油分解期间

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Carbon deposited by tar decomposition within pores of iron ore exhibited a high reactivity during the reduction reaction. The structure of porous low-grade ore was investigated in detail using transmission electron microscopy (TEM); a layered structure with 3 nm diameter pores was observed after dehydration, because of the removal of the hydroxide (OH) group from FeOOH. This pore size was deemed to be appropriate for tar decomposition and resultant carbon deposition. However, it was found that not all pores were filed with carbon. The TEM image showed that some of the deposited carbon partially blocks the pores, which negatively affects the carbon deposition process. In addition to the ore structure, the type of carbon deposited was also successfully evaluated using Raman spectroscopy and found to consist of two main peaks, G and D. The position of the G peak was found to shift slightly, indicating that the sp~3 content was reduced at elevated temperatures because of a greater degree of graphitization. The carbon deposited by integrated pyroh/sis-tar decomposition over low-grade ore was categorized as amorphous carbon (a-C), with a sp~3 content of 19—21%. These results can also be explained by high reactivity of the deposited carbon, which was improved by not only nanoscale contact between iron and carbon but also specific molecule bonding and arrangement of amorphous carbon.
机译:在铁矿孔内焦油分解沉积的碳在还原反应期间表现出高反应性。使用透射电子显微镜(TEM)详细研究多孔低级矿石的结构;在脱水后观察到具有3nm直径孔的分层结构,因为除去FeOOH的氢氧化物(OH)组。这种孔径被认为是适合于焦油分解和所得碳沉积的适当。然而,发现并非所有孔都归碳。 TEM图像表明,一些沉积的碳部分阻断孔,其负面影响碳沉积过程。除了矿石结构之外,还使用拉曼光谱成功评估沉积的碳的类型,发现由两个主峰,G和D组成。发现G峰的位置稍微偏移,表明SP〜3表示由于更大程度的石墨化,含量在升高的温度下降低。通过低级矿石沉积的碳沉积的碳沉积在低级矿石中被分类为无定形碳(A-C),Sp〜3含量为19-21%。这些结果也可以通过沉积的碳的高反应性来解释,其不仅通过铁和碳之间的纳米级接触而改善,而且还通过纳米级接触而改善,而且是特定的分子键合和无定形碳的布置。

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