Gold in arsenopyrite or high-arsenic pyrites commonly exists as submic
roscopic or ''invisible'' inclusions, making it refractory to cyanide
leaching. Current practice favour an oxidising roast to liberate the g
old for cyanidation because it is fast and energetically self supporti
ng, However the SO2 gas it produces can create a handling problem. One
alternative we are investigating is pyrolysis under N-2, CO2 and SO2
atmospheres. Instead of gaseous SO2, the process produces elemental su
lfur and, if present in the ore, arsenic metal or solid arsenic oxide.
Pyrolysis experiments were conducted on a gold-containing refractory
arsenopyrite ore to determine the effect of temperature, time and atmo
sphere on the cyanidation characteristics of the pyrolysis product. In
N-2 and CO2, the ore behaved similarly, reaching maximum mass loss at
700 degrees C and yielding maximum gold recoveries of 35 and 48 %, re
spectively. Pyrolysis under SO2 was faster reaching maximum mass loss
at 600 degrees C and resulting in gold recoveries of up to 61%. The lo
w gold recovery for N-2 and CO2 pyrolysed products was due to the enca
psulation of the exsolved gold particles by pyrrhotite as it recrystal
lised during the process. All the pyrolysis products, although compose
d mainly of pyrrhotite, did not seem to be highly active in cyanide so
lutions.