L. Ludvigsen et al., ANAEROBIC MICROBIAL REDOX PROCESSES IN A LANDFILL LEACHATE CONTAMINATED AQUIFER (GRINDSTED, DENMARK), Journal of contaminant hydrology, 33(3-4), 1998, pp. 273-291
Citations number
27
Categorie Soggetti
Water Resources","Environmental Sciences","Geosciences, Interdisciplinary
The distribution of anaerobic microbial redox processes was investigat
ed along a 305 m long transect of a shallow landfill-leachate polluted
aquifer. By unamended bioassays containing sediment and groundwater,
37 samples were investigated with respect to methane production, sulfa
te, iron, and manganese reduction, and denitrification. Methane produc
tion was restricted to the most reduced part of the plume with rates o
f 0.003-0.055 nmol CH4/g dry weight/day. Sulfate reduction was observe
d at rates of maximum 1.8 nmol SO42-/g dry weight/day along with metha
ne production in the plume, but sulfate reduction was also observed fu
rther downgradient of the landfill. Iron reduction at rates of 5-19 nm
ol Fe(II)/g dry weight/day was observed in only a few samples, but thi
s may be related to a high detection limit for the iron reducing bioas
say. Manganese reduction at rates of maximum 2.4 nmol Mn(Il)/g dry wei
ght/day and denitrification at rates of 0.2-37 nmol N2O-N/g dry weight
/day were observed in the less reduced part of the plume. All the redo
x processes were microbial processes. In many cases, several redox pro
cesses took place simultaneously, but in all samples one process domin
ated accounting for more than 70% of the equivalent carbon conversion.
The bioassays showed that the redox zones in the plume identified fro
m the groundwater composition (e.g. as methanogenic and sulfate reduci
ng) locally hosted also other redox processes (e.g. iron reduction). T
his may have implications for the potential of the redox zone to degra
de trace amounts of organic chemicals and suggests that unamended bioa
ssays may be an important supplement to other approaches in characteri
zing the redox processes in an anaerobic plume. (C) 1998 Elsevier Scie
nce B.V. All rights reserved.