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Statistical Study for Leaching of Covellite in a Chloride Media

Covellite is a secondary copper sulfide, and it is not abundant. There are few investigations on this mineral in spite of it being formed during the leaching of chalcocite or digenite; the other investigations on covellite are with the use of mineraloids, copper concentrates, and synthetic covellite...

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Autors principals: Kevin Pérez, Norman Toro, Manuel Saldaña, Eleazar Salinas-Rodríguez, Pedro Robles, David Torres, Ricardo I. Jeldres
Format: Artigo
Idioma:Inglês
Publicat: MDPI AG 2020-04-01
Col·lecció:Metals
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Accés en línia:https://www.mdpi.com/2075-4701/10/4/477
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