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,Shiwen Yao,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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