A few aspects of the connections between ore mineralogy and flotation results at Hitura nickel mine in Finland

H. Miettunen*, K. Heiskanen, R. L. Keiski

*Corresponding author for this work

Research output: Contribution to journalArticleScientificpeer-review

1 Citation (Scopus)

Abstract

The serpentinite massifs of Hitura are located in the municipality of Nivala in Central Finland. The most important sulfide minerals in the ore are pentlandite, pyrrhotite and chalcopyrite. The ore body consists of amphibolite rocks in contact with serpentinite against mica gneiss. The mean Ni grade of the ore is about 0.7%, and the highest Ni grades have been encountered in close contact. In general, the inner parts of the ore are strongly serpentinized ultramafite and some sulfides have been converted to mackinawite and valleriite. The degree of alteration varies considerably within the ore body and, correspondingly, the grain size of the sulfides varies as well. In this study, flotation tests were done with samples from different zones of the ore body. The flotation test results on the bench scale and plant scale are discussed in terms of the mineralogical features of the ore. Ores in the North Hitura zone differ from those in the South Hitura zone.

Original languageEnglish
Pages (from-to)38-44
Number of pages7
JournalMinerals and Metallurgical Processing
Volume32
Issue number1
Publication statusPublished - 1 Feb 2015
MoE publication typeA1 Journal article-refereed

Keywords

  • Flotation
  • Mineralogy
  • Nickel
  • Sulfide minerals

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