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Distribution of Co, Fe, Ni, and precious metals between blister copper and white metal

  • Keiran Holland
  • , Dmitry Sukhomlinov
  • , Lassi Klemettinen
  • , Petri Latostenmaa
  • , Hugh O’Brien
  • , Ari Jokilaakso
  • , Pekka Taskinen*
  • *Tämän työn vastaava kirjoittaja
  • Boliden Harjavalta Oy
  • Geological Survey of Finland

Tutkimustuotos: Lehtiartikkeli › Article › Scientific › vertaisarvioitu

3 Sitaatiot (Scopus)

Abstrakti

The distribution coefficients of Co, Ni, Ag, Au, Pd, and Fe at low concentrations between liquid copper and molten white metal (low-iron copper matte, ‘Cu2S’) were investigated experimentally as a function of temperature (1250–1350°C) and SO2 partial pressure (0.01–1 atm). The experimental technique involved samples equilibration at controlled temperature and gas atmosphere, followed by quenching and subsequent elemental analysis of equilibrium phases with electron probe X-ray microanalysis and laser ablation-inductively coupled plasma-mass spectrometry. The distribution coefficient of silver, nickel, gold and palladium between liquid copper and white metal indicated that they favour the blister copper whereas cobalt and iron distribute more to the white metal. The distribution coefficient of nickel, e.g. increased from 2.1 at 0.1–1.0 atm PSO2 and 1250°C to 3.2 at 1350°C. The distribution coefficients were only slightly dependent on temperature. The relatively strong dependence of the distribution coefficient of cobalt on PSO2 was discussed.

AlkuperäiskieliEnglanti
Sivut313-323
Sivumäärä11
JulkaisuMineral Processing and Extractive Metallurgy: Transactions of the Institute of Mining and Metallurgy
Vuosikerta130
Numero4
Varhainen verkossa julkaisun päivämäärä23 heinäk. 2019
DOI - pysyväislinkit
TilaJulkaistu - 2 lokak. 2021
OKM-julkaisutyyppiA1 Alkuperäisartikkeli tieteellisessä aikakauslehdessä

Rahoitus

This work was supported by European Institute Innovation and Technology (EIT) Raw Materials-KIC [grant number SGA2017/1]. Boliden Harjavalta (Finland), Eramet (France) and EIT-Raw Materials KIC (EU Horizon 2020) through NewEco project (grant # EIT/RAW MATERIALS/SGA2017/1) are gratefully acknowledged for the financial support received by Aalto University. The authors are indebted to GTK (Geological Survey of Finland) for the EPMA analyses.

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