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Physico-chemical characterization and sulphatization roasting of low-grade nickeliferous laterites

机译:低品位含镍红土的理化表征和硫酸盐焙烧

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摘要

Low-grade nickeliferous laterites from the Sukinda region, Orissa, India, were characterized by microscopic investigations, using X-ray diffraction (XRD), DTA/TG, SEM and IR techniques. The major minerals were goethite, hematite, quartz and chromite. No specific nickel mineral was present. The in situ high-temperature XRD study indicated a structural change of goethite at 300 deg C. The DTA/TG and IR data of different laterite samples are discussed in detail. The fixation of nickel in laterite was established by sequential chemical extraction methods. It was observed that more than 50 percent of nickel was present as lattice substitutions in goethite. Laboratory-scale samples were pugged with sulphuric acid and roasted. The roasted mass was cooled to room temperature and leached with water at 90-95 deg C for 30 min at a solid/liquid ratio of 1:10. A mass balance was performed for each experiment, based on total nickel and iron present in the feed, the leach solution and residue. A temperature of 700 deg C, 25 wt. percent acid and 15 mm processing time are found to be most effective for the preferential extraction of around 85 percent nickel with 2.5 percent iron.
机译:通过使用X射线衍射(XRD),DTA / TG,SEM和IR技术的显微镜研究对印度Suissada地区Sukinda地区的低品位含镍红土进行了表征。主要矿物为针铁矿,赤铁矿,石英和铬铁矿。没有特定的镍矿物质存在。原位高温XRD研究表明针铁矿在300℃时发生了结构变化。详细讨论了不同红土样品的DTA / TG和IR数据。通过顺序化学萃取方法确定了红土中镍的固定。观察到,针铁矿中有超过50%的镍以晶格取代形式存在。将实验室规模的样品加入硫酸并烘烤。将焙烧的物料冷却至室温,并在90-95℃下以固液比1:10浸出30分钟。根据进料中存在的镍和铁总量,浸出溶液和残留物,对每个实验进行质量平衡。温度为700℃,25wt。%。发现酸含量为15%的处理时间和15毫米的处理时间对于优先提取约85%的镍和2.5%的铁最为有效。

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