Je. Dutrizac et al., THE MINERALOGICAL DEPORTMENT OF GERMANIUM IN THE CLARKSVILLE ELECTROLYTIC ZINC PLANT OF SAVAGE-ZINC-INC, Metallurgical and materials transactions. B, Process metallurgy and materials processing science, 27(4), 1996, pp. 567-576
Citations number
15
Categorie Soggetti
Material Science","Metallurgy & Metallurigical Engineering
A mineralogical study was carried out on the neutral leach residue and
weak acid leach residue generated from Gordonsville zinc concentrate
at the Clarksville Electrolytic Zinc Plant of Savage Zinc Inc. The int
ent was to characterize the mineral forms and associations of germaniu
m. The Gordonsville zinc concentrate consists mostly of sphalerite whi
ch has a solid solution Ge content of similar to 400 ppm; the sphaleri
te is the dominant, if not only, Ge carrier in the concentrate. The ne
utral leach residue consists principally of iron gel-silica gel, ZnO,
and basic zinc sulfate (Zn,Cu)(4)(SO4)(OH)(6) . 4H(2)O, together with
minor amounts of ZnFe2O4, sphalerite, Zn2SiO4, Zn-Fe-Pb silicate, and
PbSO4, as well as traces of quartz, silicates, Pb-K jarosite solid sol
ution, Fe2O3, and FeO . OH. The major Ge carrier is the iron gel-silic
a gel phase, but modest amounts of Ge are present in the ZnO, ZnFe2O4,
sphalerite, and Zn-Fe-Pb silicate phases. The weak acid leach residue
consists mostly of iron gel-silica gel, ZnFe2O4, PbSO4, Pb-K jarosite
, Zn-Fe-Pb silicate, and quartz. The major Ge carrier is the iron gel-
silica gel phase which contains up to 1.7 pct Ge and accounts for simi
lar to 70 pct of the total Ge content of this residue. The remaining G
e is carried by the Zn-Fe-Pb silicate, ZnFe2O4, and some of the rare M
n-Pb-Fe oxide phases.