Tt. Chen et Je. Dutrizac, MINERALOGICAL CHARACTERIZATION OF ANODE SLIMES .10. TELLURIUM IN RAW ANODE SLIMES, Canadian metallurgical quarterly, 35(4), 1996, pp. 337-351
A mineralogical study of the raw anode slimes (that is, the slimes bef
ore decopperizing) from the refining of a typical commercial copper an
ode and three Te-rich copper anodes was carried out to elucidate the b
ehaviour of tellurium in the refining circuit. Most of the Te occurred
as tiny particles of Ag-Cu selenide-telluride that retained the morph
ologies of the selenide-relluride grain boundary inclusions in the ori
ginal anodes. An important amount of Te was also present in the oxidat
e phase, which is likely an intimate mixture of various precipitated C
u-Ag-Pb sulphates, selenites, arsenates and tellurites with fine grain
ed Au and Ag and/or selenide-telluride compounds. A trace amount of Te
is also contained in the abundant secondary Cu2O phase and much rarer
Cu-Te oxide, both of which precipitated in the raw anode slimes. The
precipitated Te in the oxidate phase, Cu2O and Cu-Te oxide may have or
iginated from the small amount of Te in solid solution in the copper a
node or from the superficial dissolution of the Ag-Cu selenide-telluri
de. Other species in the raw anode slimes such as CuSO4.5H(2)O, PbSO4,
Sb-As-Bi-Sn-Pb-Cu oxide and CuCl are insignificant overall Te carrier
s. Copyright (C) 1996 Canadian Institute of Mining and Metallurgy. Pub
lished by Elsevier Science Ltd.