Kj. Henley et al., Evaluation of a diagnostic leaching technique for gold in native gold and gold +/- silver tellurides, MINER ENG, 14(1), 2001, pp. 1-12
A detailed investigation of the stability in cyanide solutions of native go
ld and gold +/- silver tellurides in a flotation concentrate from the Golde
n Mile, Kalgoorlie, has been undertaken to assess whether leaching under di
fferent conditions can be used to quantify the distribution of Au between n
ative gold and gold +/- silver tellurides, as suggested by, for example, Ch
ryssoulis and Cabri (1990).
The leaching was carried out on +20 mum native gold and gold +/- silver tel
lurides separated from a high-grade flotation concentrate and then diluted
with barren quartz. The material leached assayed 270 ppm Au and 118 ppm Te.
About 77% of the Au was present as native gold (largely liberated) and abo
ut 23% was in gold +/- silver tellurides (predominantly calaverite with tra
ce petzite and Au-bearing hessite, also largely liberated). The grainsize o
f the gold-bearing minerals was mainly in the range 20 mum to 100 mum. The
leach conditions used were:
Stage 1: Leaching in dilute cyanide (0.1%) at pH 9.5 for 24 hours to dissol
ve native gold but not gold +/- silver tellurides.
Stage 2: Leaching the residue from Stage 1 in strong cyanide (2%) at pH 12.
5 for 96 hours to dissolve gold +/- silver tellurides.
Extractions of native gold and gold +/- silver tellurides in the two stages
of leaching were found to be as follows:
[GRAPHICS]
The results showed that the bulk of the native gold dissolved in the Stage
1 leach (weak cyanide, moderate pH), along with aborts half the hessite and
petzite but hardly any of the calaverite. The estimate of Au in native gol
d from the Stage 1 leach corresponded fairly closely to the native gold con
tent as the hessite/petzite concentrations were low. However, although the
Stage 2 leach (strong cyanide, high pH) dissolved almost all the remaining
hessite/petzite, only a small proportion of the calaverite dissolved.
The main conclusions of the investigation are that calaverite is very refra
ctory to cyanidation, much more so than hessite/petzite, and that the diagn
ostic leaching procedure studied did not provide a good estimate of Au in g
old +/- silver tellurides. For the diagnostic leach procedure to be effecti
ve, a treatment, such as chlorination, which breaks down calaverite prior t
o the Stage 2 cyanidation is required. (C) 2000 Published by Elsevier Scien
ce Ltd. All rights reserved.