Citation: Bare, G.T.; Mbayo, J.J.K.;
Ndlovu, S.; Shemi, A.; Chipise, L.
Mineralogical Characterization and
Acid Pretreatment of a Gold Calcine
Leach Residue. Minerals 2022, 12, 10.
https://doi.org/10.3390/
min12010010
Academic Editor: Przemyslaw
B. Kowalczuk
Received: 1 November 2021
Accepted: 16 December 2021
Published: 23 December 2021
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minerals
Article
Mineralogical Characterization and Acid Pretreatment of a Gold
Calcine Leach Residue
Godfrey Tinashe Bare
1,2
, Jean Jacques Kalombo Mbayo
1,2
, Sehliselo Ndlovu
1,2,
* , Alan Shemi
1,2
and Liberty Chipise
1,2,3
1
School of Chemical and Metallurgical Engineering, University of the Witwatersrand,
Johannesburg 2000, South Africa; godie.t.bare@gmail.com (G.T.B.); jeanjacquesmils@gmail.com (J.J.K.M.);
alanshemi@yahoo.co.uk (A.S.); liberty.chipise@wits.ac.za (L.C.)
2
DSI/NRF SARChI, Hydrometallurgy and Sustainable Development, University of the Witwatersrand,
Johannesburg 2000, South Africa
3
Department of Metallurgical Engineering, Manicaland State University of Applied Sciences,
Mutare, Zimbabwe
* Correspondence: Sehliselo.Ndlovu@wits.ac.za
Abstract: Miners around Zimbabwe used to supply gold concentrates from sulphide flotation to the
Kwekwe Roasting Plant (Zimbabwe) for toll treatment. The concentrates were roasted in Edward’s
roasters and the calcine product was leached by cyanidation. Due to inefficient roasting, overall
gold recoveries of 75–80% left behind a rich calcine leach residue at the Kwekwe Roasting Plant.
The characterization performed to establish a potential process route involved several techniques,
such as X-ray diffraction (XRD), scanning electron microscopy (SEM), fire assaying and inductively
coupled plasma (ICP). Assays conducted on samples from the 350,000 tons tailings dam residue,
created over the operational years, gave an average Au grade of 8.58 g/t and 12.54 g/t for Ag. The
base metals assayed—0.11% Cu, 0.10% Pb, 0.17% Zn and 26.05% Fe. SiO
2
(36.1%), Fe
2
O
3
(36.9%),
Mg
3
Si
4
O
10
(OH)
2
(8.9%), NaAlSi
3
O
8
(6.9%), and Fe
3
O
4
(6.4%)—were the major mineral phases in
the cyanide leach residue. SEM gold scans on 24 polished sections showed only 2 discrete gold
particles of less than 5 μm, with one partially liberated and associated with quartz, while the other
was fully liberated. Therefore, the particulate gold in the calcine leach residue was negligible. It was
deduced from the analysis after ultrafine milling (P
80
<5 μm) followed by cyanidation that 68.53%
of the gold was sub-microscopic. Direct cyanidation using bottle roll resulted in only 2.33% of the
total gold being leachable, indicating that the calcine leach residue was highly refractory. Diagnostic
leaching by sequential use of acids in order of their strength resulted in HCl leachable phases (CaCO
3
,
CaMg(CO
3
)
2
, PbS, Fe1-XS, and Fe
2
O
3
) freeing 4.2% of the total Au during subsequent cyanidation
leach. H
2
SO
4
leachable phases (Cu–Zn sulphides, labile FeS
2
) released an additional 26.57% during
cyanidation, whereas HNO
3
leachable phases (FeS
2
, FeAsS) released a further 20.98% of Au. After
acid treatment and subsequent cyanidation, hot caustic leach of the residue followed by carbon in
pulp resulted 4.43% of the total gold being eluted. Therefore, 4.43% of the total gold was surface
bound. From the analysis after diagnostic acid leaching, it was deduced that a total of 54.08% of
the gold was in the acid-leachable phase. Due to cost and environmental considerations, H
2
SO
4
was selected for the evaluation of acid digestion as a pretreatment stage followed by cyanidation.
Increasing the H
2
SO
4
strength for the pretreatment of the calcine leach residue increased gold
recoveries during cyanidation.
Keywords: calcine leach residue; cyanidation; acid leaching; caustic leaching; gold extraction
1. Introduction
The mineralogical investigation of ores is an important tool and a critical aspect
in the prefeasibility studies of metallurgical work and quality control of metallurgical
processes. The mineralogical characterization of process tailings is performed to investigate
Minerals 2022, 12, 10. https://doi.org/10.3390/min12010010 https://www.mdpi.com/journal/minerals