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The influence of cathodic reduction, Fe2+ and Cu2+ ions on the electrochemical dissolution of chalcopyrite in acidic solution

Author
ELSHERIEF, A. E1
[1] Electrometallurgy Laboratory, Central Metallurgical R&D Institute, CMRDI, PO Box 87, Helwan, Cairo, Egypt
Source

Minerals engineering. 2002, Vol 15, Num 4, pp 215-223 ; ref : 20 ref

CODEN
MENGEB
ISSN
0892-6875
Scientific domain
Geology; Metallurgy, welding
Publisher
Elsevier Science, Oxford
Publication country
United Kingdom
Document type
Article
Language
English
Keyword (fr)
Chalcopyrite Cuivre II Electrométallurgie Etude expérimentale Fer II Hydrométallurgie Lessivage Lixiviation Minerai sulfuré Métallurgie extractive Propriété électrochimique Réduction chimique Solution acide Traitement minerai
Keyword (en)
Chalcopyrite Copper II Electrometallurgy Experimental study Iron II Hydrometallurgy Leaching Lixiviation Sulfide ore Extractive metallurgy Electrochemical properties Chemical reduction Acidic solution Ore treatment
Keyword (es)
Calcopirita Cobre II Electrometalurgia Estudio experimental Hierro II Hidrometalurgía Lavado Lixiviación Mineral sulfurado Propiedad electroquímica Reducción química Solución ácida Tratamiento minerales
Keyword (de)
Chalkopyrit Elektrometallurgie Experimentelle Untersuchung Hydrometallurgie Auslaugen Sulfiderz Elektrochemische Eigenschaft Reduktion Erzaufbereitung
Classification
Pascal
001 Exact sciences and technology / 001D Applied sciences / 001D11 Metals. Metallurgy / 001D11B Production of metals / 001D11B05 Production of non ferrous metals. Process materials / 001D11B05C Electrometallurgy

Discipline
Metals. Metallurgy
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
13612513

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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