熔渣(焊接)
辉绿岩
铜渣
冶金
粘度
铜
材料科学
合金
相(物质)
粒子(生态学)
金属
磁铁矿
冶炼
粒径
降水
化学工程
化学
矿物学
橄榄石
复合材料
物理化学
海洋学
有机化学
地质学
工程类
物理
气象学
作者
Wenbing Xiao,Yao Shi-wen,Shiwei Zhou,Yonggang Wei,Bo Li,Hua Wang
标识
DOI:10.1016/j.jallcom.2022.163751
摘要
Oxygen-enriched smelting is accompanied by the precipitation of magnetite due to fayalite-based slag systems, which deteriorates the properties of slag and increases copper content in Cu slag. In this study, the evolution of the structure and viscosity of slag during metallization-reduction were investigated. The reduction process of the Fe-containing phase in Cu slag can be divided into two steps (Fe3O4→FeO, FeO→Fe) as coal dosage increases. In Fe3O4→FeO, the solid-phase particle content in Cu slag decreases, which simplifies the macromolecular structures, thus decreasing the viscosity of Cu slag. In FeO→Fe, the solid-phase particle content in Cu slag increases because of the formation of metallic Fe and Cu-Fe alloy particles. The macromolecular structures dominated by SiO4 and AlO4 tetrahedra become complex, increasing the viscosity of the Cu slag.
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