Reductive Dechlorination of Polychlorinated Biphenyls:  Threshold Concentration and Dechlorination Kinetics of Individual Congeners in Aroclor 1248

Reductive dechlorination of individual PCB congeners in Aroclor 1248 was investigated using sediment microorganisms from the St. Lawrence River (NY). No dechlorination was observed at Aroclor concentrations below 40 ppm [137 nmol (g of sediment)-1]. Above this threshold, congeners could be divided i...

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Veröffentlicht in:Environmental science & technology 2003-12, Vol.37 (24), p.5651-5656
Hauptverfasser: Cho, Young-Cheol, Sokol, Roger C, Frohnhoefer, Robert C, Rhee, G-Yull
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Sprache:eng
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Zusammenfassung:Reductive dechlorination of individual PCB congeners in Aroclor 1248 was investigated using sediment microorganisms from the St. Lawrence River (NY). No dechlorination was observed at Aroclor concentrations below 40 ppm [137 nmol (g of sediment)-1]. Above this threshold, congeners could be divided into three categories:  group A, congeners that dechlorinated above 40 ppm; group B, congeners that dechlorinated only at high concentrations above 60 ppm [206 nmol (g of sediment)-1]; and group C, lower chlorinated congeners that increased in concentration. The dechlorination rate of congeners in groups A and B was a linear function of their initial sediment concentration. For group A congeners, the concentration intercepts of this linear function were the same as their concentrations in the Aroclor at the threshold concentration, and these therefore represented the threshold values. However, the intercepts of group B congeners were significantly higher than their levels at the threshold Aroclor concentration and were equivalent to their concentrations in Aroclor 1248 at about 75 ppm [258 nmol (g of sediment)-1]. The final concentrations of group A and group B congeners at the end of dechlorination were the same, regardless of their initial concentrations. These final concentrations were significantly lower than their threshold values. The accumulation rate of group C congeners was a linear function of their initial concentrations, and the total accumulation was greater at higher Aroclor concentrations in sediments.
ISSN:0013-936X
1520-5851
DOI:10.1021/es034600k