Je. Teer et al., THE TREATMENT OF IRON OXALATE LEACH LIQUORS IN A UASB WITH SULFATE REDUCTION, Water science and technology, 36(6-7), 1997, pp. 383-390
Citations number
15
Categorie Soggetti
Water Resources","Environmental Sciences","Engineering, Civil
The presence of small amounts of iron (> 0.013% Fe) in sand creates pr
oblems in the manufacture of high quality glass. Removal by hot sulphu
ric acid is possible, but creates environmental problems, and is costl
y. Hence organic acids such as oxalic have been investigated since the
y are effective in removing iron, and can be degraded anaerobically. T
he aim of this work was to identify key intermediates in the anaerobic
degradation of oxalate in an upflow anaerobic sludge blanket reactor
(UASB) which was removing iron from solution in the sulphide form, and
to determine the bacterial species involved. 2-bromoethanesulfonic ac
id (BES) and molybdenum were selected as suitable inhibitors for metha
nogenic and sulphate reducing bacteria (SRB) respectively. 40mM molybd
enum was used to inhibit the SRB in a reactor with a 12hr HRT. Total S
RB inhibition took place in 20 hrs, with a complete breakthrough of in
fluent sulphate. The lack of an immediate oxalate breakthrough confirm
ed Desulfovibrio( vulgaris subspecies oxamicus was not the predominant
oxalate utilising species. Nevertheless, high concentrations of molyb
denum were found to inhibit oxalate utilising bacteria in granular rea
ctors but not in suspended population reactors; this observation was p
uzzling, and at present cannot be explained. Based on the intermediate
s identified, it was postulated that oxalate was degraded to formate b
y an oxalate utilising bacteria such as Oxalobacter formigenes, and th
e formate used by the SRBs to reduce sulphate. Acetate, as a minor int
ermediate, existed primarily as a source of cell carbon for oxalate ut
ilising bacteria. Methanogenic inhibition identified that 62% of the C
H4 in the reactor operated at 37 degrees C originated from hydrogenotr
ophic methanogenesis, whilst this figure was 80% at 20 degrees C. Poss
ible irreversible effects were recorded with hydrogenotrophic methanog
ens. (C) 1997 IAWQ. Published by Elsevier Science Ltd.