Serveur d'exploration sur le nickel au Maghreb

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Acid and oxidizing leaching of chalcopyrite concentrate by ferric sulphate and fluorosilicic-nitric media

Identifieur interne : 000B76 ( Main/Exploration ); précédent : 000B75; suivant : 000B77

Acid and oxidizing leaching of chalcopyrite concentrate by ferric sulphate and fluorosilicic-nitric media

Auteurs : K. Elamari [Maroc] ; E. A. Jdid ; P. Blazy ; A. Bouhafid ; M. El Meray ; I. Akalay

Source :

RBID : Pascal:01-0032413

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English descriptors

Abstract

A hydrometallurgical treatment was applied to the Hajar Mine Copper Concentrate (HMCC), Morocco, containing ≃ 28.1% copper (the major copper mineral phase is chalcopyrite, CuFeS2), ≃ 26.3% iron, ≃ 5.8% zinc, ≃ 1.9% lead, ≃ 33.7% sulphur, and small amounts of silver (269 g/t) and nickel (219 g/t). Three acid media were used: ferric sulphate in sulfuric acid, ferric sulphate in hexafluorosilicic acid, and a hexafluorosilicic acid-nitric acid mixture. The results show that when a ferric sulphate reagent is used, in H2SO4, as well as in H2SiF6 media, dissolution of copper and iron do not exceed 30%, because of the formation of a passivation layer on chalcopyrite particles, whereas zinc is dissolved at about 90%. The final solid leachate residue represents 75% by weight of the initial solid and remains rich in copper (≃ 28%) and iron (≃ 25%). However, under strong acid and oxidizing conditions, in the hexafluorosilicic acid-nitric acid mixture, the dissolution of copper is more efficient, although it is nonselective, (92% Cu, 89% Fe, 98% Zn). The solid leachate residue represents only 40% by weight of the original sample, and assays 5.9% Cu, 7.3% Fe, 0.2% Zn, 4.1% Pb, and 56.4% Stotal. Mineralogical characterizations of the leachate solid residues show the formation of both elemental sulphur and a Cu1-xFe1-yS2-z layer on the surface of the nondissolved chalcopyrite.


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<term>Experiments</term>
<term>Ferric sulphate</term>
<term>Fluorosilicic acid</term>
<term>Hydrometallurgy</term>
<term>Leaching</term>
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<term>Nitric acid</term>
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<term>Minéralogie</term>
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<div type="abstract" xml:lang="en">A hydrometallurgical treatment was applied to the Hajar Mine Copper Concentrate (HMCC), Morocco, containing ≃ 28.1% copper (the major copper mineral phase is chalcopyrite, CuFeS2), ≃ 26.3% iron, ≃ 5.8% zinc, ≃ 1.9% lead, ≃ 33.7% sulphur, and small amounts of silver (269 g/t) and nickel (219 g/t). Three acid media were used: ferric sulphate in sulfuric acid, ferric sulphate in hexafluorosilicic acid, and a hexafluorosilicic acid-nitric acid mixture. The results show that when a ferric sulphate reagent is used, in H2SO4, as well as in H2SiF6 media, dissolution of copper and iron do not exceed 30%, because of the formation of a passivation layer on chalcopyrite particles, whereas zinc is dissolved at about 90%. The final solid leachate residue represents 75% by weight of the initial solid and remains rich in copper (≃ 28%) and iron (≃ 25%). However, under strong acid and oxidizing conditions, in the hexafluorosilicic acid-nitric acid mixture, the dissolution of copper is more efficient, although it is nonselective, (92% Cu, 89% Fe, 98% Zn). The solid leachate residue represents only 40% by weight of the original sample, and assays 5.9% Cu, 7.3% Fe, 0.2% Zn, 4.1% Pb, and 56.4% Stotal. Mineralogical characterizations of the leachate solid residues show the formation of both elemental sulphur and a Cu1-xFe1-yS2-z layer on the surface of the nondissolved chalcopyrite.</div>
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