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Carbothermal solid state reduction of manganese oxide and ores in different gas atmospheres

机译:在不同气体气氛下碳锰氧化物和矿石的碳热固态还原

摘要

The aim of the project was to establish rate and mechanisms of solid state reduction of manganese ores. The project studied carbothermal reduction of manganese oxide MnO, two Groote Eylandt (Australian) and Wessels (South African) manganese ores in hydrogen, helium and argon atmospheres at temperatures up to 1400C for MnO and 1200C for manganese ores. Experiments were conducted in the fixed bed reactor with on-line off-gas analysis. The major findings are as follows.•Rate and degree of reduction of MnO and ores increased with increasing temperature. •Reduction of MnO and manganese ores at temperatures up to 1200C was faster in helium than in argon, and much faster in hydrogen than in helium. The difference in MnO reduction in hydrogen and helium decreased with increasing temperature to 1400C.•Addition of up to 7 vol% of carbon monoxide to hydrogen had no effect on MnO reduction at 1200C.•In the process of carbothermal reduction of ores in hydrogen at 1200C, silica was reduced.•Reduction of both GE ores was slower than of Wessels ore. This was attributed to high content of iron oxide in the Wessels ore.•Carbon content in the graphite-ore mixture had a strong effect on phases formed in the process of reduction; thus, in the reduction of Wessels ore with 12-16 wt% C, a-Mn and Mn23C6 were formed; when carbon content was above 20 wt%, oxides were reduced to carbide (Mn,Fe)7C3.•Kinetic analysis showed that mass transfer of intermediate CO2 from oxide to graphite in carbothermal reduction in inert atmosphere was a contributing factor in the rate control.•High rate of reduction of manganese oxide in hydrogen was attributed to formation of methane which facilitated mass transfer of carbon from graphite to oxide. Hydrogen was also directly involved in reduction of manganese ore reducing iron oxides to metallic iron and higher manganese oxides to MnO.Reduction of Wessels and Groote Eyland Premium Fines ores in the solid state is feasible at temperatures up to 1200C; while temperature for solid state reduction of Groote Eyland Premium Sands is limited by 1100C.
机译:该项目的目的是确定锰矿石固态还原的速率和机理。该项目研究了在氢气,氦气和氩气气氛中,MnO的最高温度为1400C,MnO的最高温度为1200C时,氧化锰Mn,两种Groote Eylandt(澳大利亚)和Wessels(南非)锰矿石的碳热还原。在具有在线废气分析的固定床反应器中进行了实验。主要发现如下:•MnO和矿石的还原速率和还原度随温度升高而增加。 •在1200℃以下的温度下,氦气中的MnO和锰矿石的还原速度比氩气中的还原速度快,而氢气中的还原速度则比氦气中快得多。氢气和氦气中MnO还原的差异随温度升高至1400C而降低。•在氢气中添加至多7 vol%的一氧化碳对1200C下的MnO还原没有影响。•在碳热还原矿石中氢气中的过程中1200℃,二氧化硅被还原。•两种GE矿石的还原都比Wessels矿石的还原慢。这归因于韦塞尔斯矿石中的氧化铁含量高。•石墨矿石混合物中的碳含量对还原过程中形成的相具有强烈的影响。因此,在以12-16wt%的C还原Wessels矿石中,形成α-Mn和Mn23C6。当碳含量超过20 wt%时,氧化物被还原为碳化物(Mn,Fe)7C3。•动力学分析表明,在惰性气氛中碳热还原过程中,中间体CO2从氧化物向石墨的传质是速率控制的一个重要因素。 •氢气中锰氧化物的高还原速率归因于甲烷的形成,甲烷促进了碳从石墨到氧化物的质量转移。氢气还直接参与了锰矿石的还原,将铁氧化物还原为金属铁,将高锰氧化物还原为MnO。在高达1200°C的温度下,固态还原Wessels和Groote Eyland Premium细矿是可行的。而Groote Eyland Premium Sands固态还原的温度限制在1100℃。

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