Recovery of Valuable Metals from Sea Nodules in Presence of Pyrite and Sulphur

The biodissolution of copper, nickel and cobalt front the Indian Ocean manganese nodules has been investigated in presence of pyrite and elemental sulphur using Thioba-cillus ferrooxidans(Tf) and Thiobacillus thiooxidans (Tt) as the microorganisms. The leaching of manganese nodules proceeds with reduction of Mn4+ to Mn2+ by ferrous ions
generated from pyrite and H2SO3, from that of sulphur by bacterial action. Breaking the lattice structure of manganese and iron based minerals like todorokite, birne-ssite, lithiophorite and goethite by chemico-bacterial action, releases the valuable metals such as copper;
nickel and cobalt thereby dissolving them in the aqueous solution.
Recovery of the metals was highest for finer size (-75,um) fraction of the nodules. For an instance, in presence of 10% pyrite at 5% pulp density and pH 2.0, 97% Cu, 85%a Ni, and 55% Co were leached in 50 days. With the particle size of -300 +200Um, the metal recoveries at 30°C were 81% Cu, 67% Ni and 39% Co in 50 days tune in presence of pyrite. Under these conditions 61% Cu, 58% Ni and 26% Co diss- olution was observed in presence of sulphur Raising the temperature from 20-35°C increased the metal recovery.