4.7 Article

A novel utilization of ferronickel slag as a source of magnesium metal and ferroalloy production

Journal

JOURNAL OF CLEANER PRODUCTION
Volume 292, Issue -, Pages -

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.jclepro.2020.125307

Keywords

Magnesium; Ferroalloy; Ferronickel slag; Carbothermic; Vacuum; Inert

Funding

  1. PT Antam
  2. ITB

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Processing of laterite nickel ore produces ferronickel slag, with main constituents including silicon oxide, magnesium oxide, and iron oxide. The amount of ferronickel slag has increased due to rising demand for ferronickel and stainless steel. Experimental results show that at temperatures of 1500-1550 degrees Celsius under argon or vacuum environments, magnesium evaporates and forms ferro-silicon-chromium.
Processing laterite nickel ore by the pyrometallurgical route produces ferronickel slag as a byproduct. The main constituents of ferronickel slag are silicon oxide, magnesium oxide, and iron oxide. The amount of ferronickel slag has sharply increased in recent years as a result of the increasing demand for ferronickel and stainless steel. Some regions recognize ferronickel slag as hazardous waste, meaning that the handling of the slag requires special attention and treatment. A zero-waste ferronickel processing plant could be realized if most of the metallic components can be extracted from the slag. Based on FactSage calculations, it is thermodynamically possible to reduce ferronickel slag into magnesium and ferroalloy, leaving only a small amount of unreduced oxides. According to experiments conducted at 1500 degrees C and 1550 degrees C under an argon atmosphere and a vacuum environment, magnesium was evaporated and ferro-silicon-chromium was formed. Some magnesium cannot be evaporated and remains in the final slag together with silicon in the form of forsterite (Mg2SiO4). Further research is still needed to increase the degree of magnesium metal evaporation and to prevent reoxidation of magnesium metal by carbon monoxide and silicon oxide gases. (C) 2020 Elsevier Ltd. All rights reserved.

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