温度和锍品位对Cu-Fe-O-S-Si系磷(SO2)下气渣-锍-鳞石英平衡的影响 = 0.25大气压

IF 0.9 Q3 MINING & MINERAL PROCESSING
A. Fallah-Mehrjardi, T. Hidayat, P. Hayes, E. Jak
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引用次数: 0

摘要

摘要对Cu-Fe-O-S-Si体系在1300°C,p(SO2)下处于化学平衡状态的炉渣、锍和鳞石英相的组成进行了实验测量 = 0.25大气压和选定的氧分压。高温平衡实验是在受控的CO-CO2-SO2-Ar气体气氛下使用二氧化硅衬底进行的。通过样品的快速淬火,将平衡得到的相保留在室温下。通过电子探针X射线微分析(EPMA)测量来自平衡实验的凝聚相组成。本研究中获得的数据与先前研究的数据相结合,使液相线炉渣温度能够准确地描述为p(SO2)下Fe/SiO2比率的函数 = 0.25大气压,适用于温度在1200和1300摄氏度之间,且含有~44至~78重量百分比铜的床垫。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The influence of temperature and matte grade on gas-slag-matte-tridymite equilibria in the Cu-Fe-O-S-Si system at p (SO2) = 0.25 atm
ABSTRACT Experimental measurements have been made of the compositions of slag, matte and tridymite phases in chemical equilibrium in the Cu-Fe-O-S-Si system at 1300°C, p(SO2) = 0.25 atm and selected oxygen partial pressures. The high temperature equilibration experiments were conducted using silica substrates under controlled CO-CO2-SO2-Ar gas atmospheres. The resulting phases obtained from the equilibrations were retained at room temperature through rapid quenching of the samples. The condensed phase compositions from the equilibrium experiments were measured by Electron Probe X-ray Microanalysis (EPMA). The data obtained in the present study, combined with those from previous studies, have enabled the liquidus slag temperature to be accurately described as a function of Fe/SiO2 ratio at p(SO2) = 0.25 atm for temperatures between 1200 and 1300oC and mattes containing from ∼44 to ∼ 78 wt pct Cu.
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CiteScore
3.50
自引率
0.00%
发文量
6
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