A thermodynamic
model of the Fe(II)–Fe(III)–Cu(II)–H2SO4–H2O system is developed and
shown to reliably simulate the species distribution in the industrial
copper electrorefining electrolyte from 25 to 70 °C. The previously
developed model of the Fe(II)–Fe(III)–H2SO4–H2O system under leaching conditions was
first evaluated, and it proved that its applicability can be extended
to a much higher acid concentration (185 g/L). Cu(II) species were
then identified, and their thermodynamic data were collected and assessed
for modeling calculations. Results reveal that after addition of a
high amount of copper (40–50 g/L), Fe(II) is still distributed
as free Fe2+, FeHSO4
+, and FeSO4°; Fe(III) is distributed as free Fe3+, FeSO4
+, FeHSO4
2+, and Fe(SO4)2
–. Cu(II) is dissolved as Cu2+, CuSO4°, and CuHSO4
+. The proposed model was validated by reliable and accurate prediction
of the measured redox potential throughout all solution conditions.
An expression developed previously to predict the redox potential
can still be applied in this work. Analysis of speciation results
strongly supports that the redox potential of acidic iron sulfate
solutions with such a high acid and copper concentration can still
be solely determined by the Fe3+/Fe2+ couple.
The pH and effective ionic strength were also obtained and discussed.
These findings contribute to further investigation on speciation of
other solutions during copper production.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.