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Atrazine Degradation in Subsurface Soil by Indigenous and Introduced Microorganisms
Significant atrazine degradation (50%) but only 1% mineralization was detected in samples taken from the upper soil layer (0−25 cm), but not in samples taken from deeper horizons. Thin layer chromatography analysis of noninoculated soil indicated dealkylation to be a major degradation pathway with d...
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Published in: | Journal of agricultural and food chemistry 1997-11, Vol.45 (11), p.4481-4486 |
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Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Significant atrazine degradation (50%) but only 1% mineralization was detected in samples taken from the upper soil layer (0−25 cm), but not in samples taken from deeper horizons. Thin layer chromatography analysis of noninoculated soil indicated dealkylation to be a major degradation pathway with deethylatrazine favoring deisopropylatrazine. Inoculation with Pseudomonas sp. strain ADP (P.ADP) resulted in 90−100% mineralization of [14C]atrazine in all samples after 15 days. Atrazine was degraded in the soil via dechlorination as the first mineralization step. C-source competition was not responsible for differences in initial mineralization rates. Higher organic matter content in the upper soil level did not result in a sorption-related decrease in degradation rates. It is concluded that the limiting factor for atrazine mineralization in the tested soil profiles was the absence of atrazine-mineralizing microorganisms. Therefore, bioaugmentation may be preferable to enhancement of intrinsic atrazine-degrading activity when complete atrazine mineralization is the goal of bioremediation activity. Keywords: Atrazine; subsurface; biodegradation; microbial activity; soil organic matter |
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ISSN: | 0021-8561 1520-5118 |
DOI: | 10.1021/jf970423t |