Biodegradation of perfluorooctanesulfonate (PFOS) as an emerging contaminant
•We have identified the aerobic microorganism for the decomposition of PFOS.•Ca. 67% of a 600mgL−1 conc. of PFOS was biodegraded by Pseudomonas aeruginosa after 12h.•Our result is considered a major advancement in sustainable PFOS treatment. Perfluorooctanesulfonate (PFOS) is a compound of global co...
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Published in | Chemosphere (Oxford) Vol. 109; pp. 221 - 225 |
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Main Authors | , , , , , |
Format | Journal Article |
Language | English |
Published |
Kidlington
Elsevier Ltd
01.08.2014
Elsevier |
Subjects | |
Online Access | Get full text |
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Summary: | •We have identified the aerobic microorganism for the decomposition of PFOS.•Ca. 67% of a 600mgL−1 conc. of PFOS was biodegraded by Pseudomonas aeruginosa after 12h.•Our result is considered a major advancement in sustainable PFOS treatment.
Perfluorooctanesulfonate (PFOS) is a compound of global concern because of its persistence and bioaccumulation in the environment. Nevertheless, little is known of the potential for PFOS biodegradation, even though the importance of characterizing the function and activity of microbial populations detected in the environment has been discussed. This study focused on the biodegradation of PFOS by a specific microorganism. Through this study, we have identified the aerobic microorganism for the specific decomposition of PFOS from wastewater treatment sludge, as a well-known sink for environmental PFOS. This species was Pseudomonas aeruginosa strain HJ4 with a 99% similarity, a mesophilic rod type bacteria (30–37°C). A pH range of 7–9 was determined to be optimal for the growth of strain HJ4. In this study approximately 67% over a range of concentrations (1400–1800μgL−1) for PFOS was biologically decomposed by P. aeruginosa after 48h incubation. This result is reported here for the first time, which strongly pertains to the efficient biodegradation of PFOS. Therefore, our study is considered a major advancement in sustainable PFOS treatment. |
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ISSN: | 0045-6535 1879-1298 |
DOI: | 10.1016/j.chemosphere.2014.01.072 |