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鎳鐵礦選擇性還原焙燒相變研究

Mineral phase transformation study of catarinite selective reduction roasting

  • 摘要: 對鎳鐵礦原料及不同溫度還原焙砂進行礦物學研究,探究鎳鐵礦選擇性還原焙燒發生的相變.研究結果表明:鎳鐵礦主要金屬礦物為褐鐵礦,其次為赤鐵礦;Ni在不含錳的鐵礦物中分布較均勻,而在含Mn的鐵礦物中分布相對集中,并與Mn伴生.鎳鐵礦在還原焙燒過程中Fe、Ni和Co隨溫度升高逐漸發生還原、相轉化和遷移富集的過程.選擇性還原焙燒必須嚴格控制焙燒溫度,要達到Ni、Co和Fe的選擇性還原并形成Ni高、Fe低的合金相和磁鐵礦,焙燒溫度采用750℃較合適,在該溫度下形成的合金相組成為55.55% Ni、9.86% Co及33.99% Fe,Ni的金屬轉化率為88.49%,鐵氧化物主要為磁鐵礦.

     

    Abstract: Mineralogical studies on catarinite raw ore and reduced samples at different temperatures were carried out, and phase transformation was explored in the catarinite selective reduction roasting process. The results show that the main metal minerals in the catarinite are limonite and then hematite. The distribution of Ni in Mn-free iron minerals is relatively homogeneous, but it is relatively concentrated in Mn-contained iron minerals, and Ni is associated with Mn. Reduction, phase transformation, migration and enrichment of Fe, Ni and Co gradually occur in the process of catarinite reduction roasting with increasing temperature, so the selective reduction roasting temperature should be controlled strictly. To reduce Ni, Co and Fe selectively and form a more Ni and less Fe alloy phase and magnetite, 750℃ is a proper roasting temperature, at which the formed alloy phase contains Ni of 55. 55%, Co of 9. 86% and Fe of 33. 99% averagely, the metal conversion rate of Ni is 88. 49%, and the iron oxide is mainly magnetite.

     

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