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Changes in an Australian laterite ore in the process of heat treatment

Journal Article


Abstract


  • This paper examines an Australian garnieritic-type ore and changes in phase composition and morphology caused by heating in argon at 400-1000 °C using XRF, XRD, DTA/TG, SEM/EDS and BET analyses. The mineral phases detected by XRD in the original ore include chlorite, talc, hematite and quartz. Traces of iron silicate, Fe-Cr spinel and monoxide phase (predominantly manganese oxide) were observed by EDS. Nickel was detected in chlorite, talc, iron silicate and monoxide phase. Heat treatment at 400-500 °C did not change XRD patterns. At 600 °C, dehydroxylation of the brucitic phase of chlorite occurred. Chlorite was converted into olivine (forsterite) and enstatite at 600-800 °C. Upon heating to 900-1000 °C, talc was also converted into olivine and enstatite. Ni-bearing phases after heat treatment at 800-850 °C were forsterite, enstatite, talc, iron silicate and monoxide.

Authors


  •   Yang, Jun (external author)
  •   Zhang, Guangqing
  •   Ostrovski, Oleg (external author)
  •   Jahanshahi, Sharif (external author)

Publication Date


  • 2013

Citation


  • Yang, J., Zhang, G., Ostrovski, O. & Jahanshahi, S. (2013). Changes in an Australian laterite ore in the process of heat treatment. Minerals Engineering, 54 110-115.

Scopus Eid


  • 2-s2.0-84889645923

Ro Metadata Url


  • http://ro.uow.edu.au/eispapers/2568

Number Of Pages


  • 5

Start Page


  • 110

End Page


  • 115

Volume


  • 54

Abstract


  • This paper examines an Australian garnieritic-type ore and changes in phase composition and morphology caused by heating in argon at 400-1000 °C using XRF, XRD, DTA/TG, SEM/EDS and BET analyses. The mineral phases detected by XRD in the original ore include chlorite, talc, hematite and quartz. Traces of iron silicate, Fe-Cr spinel and monoxide phase (predominantly manganese oxide) were observed by EDS. Nickel was detected in chlorite, talc, iron silicate and monoxide phase. Heat treatment at 400-500 °C did not change XRD patterns. At 600 °C, dehydroxylation of the brucitic phase of chlorite occurred. Chlorite was converted into olivine (forsterite) and enstatite at 600-800 °C. Upon heating to 900-1000 °C, talc was also converted into olivine and enstatite. Ni-bearing phases after heat treatment at 800-850 °C were forsterite, enstatite, talc, iron silicate and monoxide.

Authors


  •   Yang, Jun (external author)
  •   Zhang, Guangqing
  •   Ostrovski, Oleg (external author)
  •   Jahanshahi, Sharif (external author)

Publication Date


  • 2013

Citation


  • Yang, J., Zhang, G., Ostrovski, O. & Jahanshahi, S. (2013). Changes in an Australian laterite ore in the process of heat treatment. Minerals Engineering, 54 110-115.

Scopus Eid


  • 2-s2.0-84889645923

Ro Metadata Url


  • http://ro.uow.edu.au/eispapers/2568

Number Of Pages


  • 5

Start Page


  • 110

End Page


  • 115

Volume


  • 54