Jm. Zinck et Je. Dutrizac, ENVIRONMENT - THE BEHAVIOR OF ZINC, CADMIUM, THALLIUM, TIN AND SELENIUM DURING FERRIHYDRITE PRECIPITATION FROM SULFATE MEDIA, CIM bulletin, 91(1019), 1998, pp. 94-101
Citations number
13
Categorie Soggetti
Mining & Mineral Processing","Metallurgy & Metallurigical Engineering
Ferrihydrite is often the initial precipitate resulting from the rapid
neutralization of Fe(lll) sulphate solutions, and it seems to be a ma
jor constituent of zinc plant neutral leach residues. The most importa
nt parameters affecting ferrihydrite precipitaton are temperature, sol
ution pH and the neutralization rate, low temperatures and rapid neutr
alization rates yield poorly filterable ferrihydrite, whereas higher t
emperatures and slower neutralization rates produce readily filterable
precipitates; in all instances, however, the precipitates are two-lin
e ferrihydrite. Significant amounts of Zn are incorporated in the ferr
ihydrite precipitates, and the Zn contents increase with increasing Zn
concentration, pH or temperature. Generally, the sulphate contents of
the precipitates decrease as the Zn contents increase, and this may i
ndicate that the Zn is adsorbed on the ferrihydrite. Discrete Zn phase
s were not detected. Neither Cd nor TI is precipitated with ferrihydri
te, although thallium jarosite co-precipitates with ferrihydrite at hi
gh TI concentrations and elevated temperatures. Virtually all of the S
n added to the solution precipitates with the ferrihydrite, but the ti
n is believed to be present as intimately admired amorphous SnO2.nH(2)
O. Although selenite extensively precipitates with the ferrihydrite, s
elenate remains mostly in solution, likely because of the close simila
rity of the SeO42- ion to the SO42- ion which is present in high conce
ntrations and saturates the available sites for anion adsorption.