Rates of reaction of covellite and blaubleibender covellite with ferric ion at Ph 2.0.
Can Mineral 1986 Jan; 24(1):35-44
This study evaluates the rates of oxidation of covellite and blaubleibender (blue-remaining) covellite by fe3+ at ph 2 in a batch reactor system to better understand the geochemical processes involved in second-cycle weathering of enriched zones of copper- bearing ore deposits.
The Canadian Mineralogist
Virginia Polytechnic Inst & St Univ