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Trace element distributions between matte and slag in direct nickel matte smelting
Authors:Dmitry Sukhomlinov  Lassi Klemettinen  Olli Virtanen  Yann Lahaye  Petri Latostenmaa  Ari Jokilaakso
Affiliation:1. School of Chemical Engineering, Aalto University, Aalto, Finland"ORCIDhttps://orcid.org/0000-0002-8752-4776;2. School of Chemical Engineering, Aalto University, Aalto, Finland"ORCIDhttps://orcid.org/0000-0001-9633-7131;3. School of Chemical Engineering, Aalto University, Aalto, Finland;4. Geological Survey of Finland, Espoo, Finland;5. Boliden Harjavalta, Harjavalta, Finland;6. School of Chemical Engineering, Aalto University, Aalto, Finland"ORCIDhttps://orcid.org/0000-0003-0582-7181
Abstract:ABSTRACT

Behaviour of trace elements in the nickel matte smelting was studied at 1673 K (1400°C) by equilibration-quenching techniques followed by direct phase analyses using electron probe X-ray microanalysis and laser ablation-inductively coupled plasma-mass spectrometry. The matte-slag samples at silica saturation were equilibrated with SO2-CO-CO2-Ar mixtures of fixed pSO2, pS2 and pO2 in order to obtain a pre-determined oxidation degree for the sulphide matte, and thus to generate a targeted iron concentration of the nickel-copper–iron sulphide matte (Ni:Cu = 5, w/w), depending on the slag chemistry. The slag composition was varied from 0 to 2 wt-% K2O and 0–10 wt-% MgO in silica saturation. The studied trace elements were Co, Ge, Pb, Se and Sn, but also the matte-to-slag distributions of the slag forming fluxing components Mg (MgO) and Si (SiO2) were determined experimentally. Selenium was the only trace element studied which strongly enriched in the low-iron nickel mattes, and the deportment became larger when the sulphide matte depleted with iron. All the other trace elements behaved in the opposite way.
Keywords:Nickel  iron silicate slag  phase diagram  MgO  K2O
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