Be. Morgan et al., Fundamental study of a one-step ambient temperature ferrite process for treatment of acid mine drainage waters, WATER SA, 27(2), 2001, pp. 277-282
A novel approach towards the removal of iron and heavy metals from South Af
rican acid mine drainage (AMD) waters is presented. The approach involves t
he controlled oxidation of ferrous-containing AMD water at ambient temperat
ures in the presence of magnetite seed. The resulting oxidation product is
the ferrite (Ml(2)(3+)M2(2+)O(4)) magnetite (Fe3O4), which has the capacity
for non-ferrous metal removal, and which forms a stable sludge that is eas
ily separated from the effluent. Sludge characterisation studies (XRD, SEM
and dissolution tests) show that oxidation of ferrous solutions under contr
olled pH and oxidation conditions (pH 10.5, air flow rate = 0.05 l/min) in
the presence of magnetite seed (initial seed : ferrous ratio = 7:1) yields
almost pure magnetite at ambient temperature. It was found that magnetite s
eed channels the end products of the AMD oxidation reaction towards magneti
te. Under identical conditions, but in the absence of magnetite seed, a poo
rly characterised mixture of largely amorphous iron oxides are formed with
magnetite comprising not more than 17% of the total iron. The kinetics of t
he reaction under the investigated conditions were found to be very favoura
ble, with magnetite forming at a rate of 12.8 mg Fe/l/min. The total iron c
oncentration in the affluent was always less than 1 mg/l representing an ir
on removal efficiency of 99.9%. The precipitant settled well (SVI 8 ml/g) a
nd showed substantial stability at pH 3 (dissolution of 1.1% after 120 h).
An outline for a one-step ambient temperature ferrite process is presented.