Mineralogical Variations in Flash Furnace Particles produced under Varying Furnace Conditions

Reflected light microscopic examination of particles from laboratory experimental copper flash furnaces operated under varied furnace conditions shows that the particles exhibit a wide range in mineral compositions and mineral abundances that correlate with partial pressure of oxygen and concentrate/oxygen ratio. Chalcopyrite, bornite, and digenite are more abundant under low oxygen conditions. With increasing oxygen, metallic copper, delafossite and cuprite become increasingly abundant. The extent of particle agglomeration during flight varies with the furnace. Those products from the larger furnaces exhibit the greater degree of agglomeration. Significant particle fragmentation also is evidenced by cracking and brecciation of some particles.