“…Oxidative dissolution of chalcocite by Fe 3+ , O 2 or Cu 2+ , either in a sulfate or chloride system, occurs in two distinct stages with the production of secondary covellite (Cu 1.0-1.2 S) as an intermediate (Bolorunduro, 1999;Cheng and Lawson, 1991a;Dutrizac and MacDonald, 1974;Mao and Peters, 1983;Mcdonald and Langer, 1983;Miki et al, 2011;Mulak and Niemiec, 1969;Petersen and Dixon, 2003;Ruan et al, 2013;Ruiz et al, 1998Ruiz et al, , 2007Senanayake, 2007Senanayake, , 2009Sullivan, 1930;Thomas et al, 1967):…”