Toluene degradation occurred in anaerobic flow-through sediment column
s filled with contaminated sediment and sludge to which either amorpho
us or highly crystalline manganese oxide was added. An enrichment cult
ure from these sediment columns was able to grow on toluene under stri
ctly anaerobic conditions in the presence of manganese oxide. The oxid
ation of toluene was coupled to the production of CO2 and to the reduc
tion of Mn(IV). Of the different manganese oxides tested, the rate was
slowest with crystalline manganese oxide. After several transfers of
the enrichment culture, its ability to degrade toluene became less and
it was ultimately lost, unless sterilized Rhine river sediment was pr
esent in the medium. Direct contact between the bacteria and the manga
nese oxide was found to be advantageous for a rapid toluene degradatio
n. The degradation rate could be further increased by adding organic l
igands such as oxalic acid or nitrilotriacetic acid.