Aerobic mineralization of 2,6-dichlorophenol by Ralstonia sp. strain RK1

A new aerobic bacterium was isolated from the sediment of a freshwater pond close to a contaminated site at Amponville (France). It was enriched in a fixed-bed reactor fed with 2,6-dichlorophenol (2,6-DCP) as the sole carbon and energy source at pH 7.5 and room temperature. The degradation of 2,6-DC...

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Veröffentlicht in:Applied and Environmental Microbiology 1998-07, Vol.64 (7), p.2566-2571
Hauptverfasser: Steinle, P. (Ciba Speciality Chemicals Inc., Switzerland.), Stucki, G, Stettler, R, Hanselmann, K.W
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Sprache:eng
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Zusammenfassung:A new aerobic bacterium was isolated from the sediment of a freshwater pond close to a contaminated site at Amponville (France). It was enriched in a fixed-bed reactor fed with 2,6-dichlorophenol (2,6-DCP) as the sole carbon and energy source at pH 7.5 and room temperature. The degradation of 2,6-DCP followed Monod kinetics at low initial concentrations. At concentrations above 300 micromolar (50 mg . liter-1), sequence of the 16S ribosomal DNA allowed us to assign the bacterium to the genus Ralstonia (formerly Alcaligenes). The substrate spectrum of the bacterium includes toluene, benzene, chlorobenzene, phenol, and all f 2,6-DCP increasingly inhibited its own degradation. The base our ortho- and para-substituted mono- and dichlorophenol isomers. Substituents other than chlorine prevented degradation. The capacity to degrade 2,6-DCP was examined in two fixed-bed reactors. The microbial population grew on and completely mineralized 2,6-DCP at 2,6-DCP concentrations up to 740 micromolar in continuous reactor culture supplied with H2O2 as an oxygen source. Lack of peroxide completely stopped further degradation of 2,6-DCP. Lowering the acid-neutralizing capacity of the medium to 1/10th the original capacity led to a decrease in the pH of the effluent from 7 to 6 and to a significant reduction in the degradation activity. A second fixed-bed reactor successfully removed low chlorophenol concentrations (20 to 26 micromolar) with hydraulic residence times of 8 to 30 min
ISSN:0099-2240
1098-5336
DOI:10.1128/aem.64.7.2566-2571.1998