Catalyzed oxidation kinetics of dissolved Fe2+ ions to Fe3+ over active car
bon in concentrated H2SO4-FeSO4 solutions was studied with isothermal and i
sobaric experiments carried out in a laboratory-scale pressurized autoclave
. The experiments were performed at temperatures between 60 and 130 degrees
C, and the pressure of oxygen (O-2) was varied between 4 and 10 bar. The k
inetic results revealed that the oxidation rate was enhanced by increasing
the temperature and pressure and that the catalytic and noncatalytic oxidat
ions proceed as parallel processes. A rate equation was obtained for the ca
talytic oxidation process, based on the assumption that the oxidation of Fe
2+ with adsorbed oxygen is rate determining. The rate equation for the cata
lytic oxidation has the simplified form r = k " c(Fe)c(O) (0.5)(K-O" c(O)(0
.5) + 1) where c(Fe) and c(O) are the concentrations of Fe2+ ions and disso
lved oxygen, respectively, and k " and K-O" are experimentally determined k
inetic parameters. The total oxidation rate was simulated by including a pr
eviously determined rate equation for the noncatalytic oxidation into the g
lobal model, from which the kinetic parameters of the catalytic oxidation r
ate were determined. A comparison of the model fit with the experimental da
ta revealed that the proposed rate equation is applicable for the predictio
n of the Fe2+ oxidation kinetics in acidic ferrous sulfate solutions.