2005
DOI: 10.1016/j.envpol.2005.02.016
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2,4-Dichlorophenoxyacetic acid (2,4-D) sorption and degradation dynamics in three agricultural soils

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Cited by 153 publications
(87 citation statements)
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“…Therefore, their dissipation was mainly due to biodegradation mediated by microbial processes. Biodegradation process, catalyzed by soil microbes, is governed by both abiotic and biotic factors (Boivin et al 2005). There were several possible ways through which root exudate components enhanced the biodegradation of BDE-28 and BDE-47 in the soils.…”
Section: Discussionmentioning
confidence: 99%
“…Therefore, their dissipation was mainly due to biodegradation mediated by microbial processes. Biodegradation process, catalyzed by soil microbes, is governed by both abiotic and biotic factors (Boivin et al 2005). There were several possible ways through which root exudate components enhanced the biodegradation of BDE-28 and BDE-47 in the soils.…”
Section: Discussionmentioning
confidence: 99%
“…Although 2,4-D is highly mobile, rapid mineralization rates may reduce the potential of 2,4-D to affect groundwater (Boivin et al, 2005). The compound 2,4-D has been detected in streams and shallow groundwater at low concentrations, in both rural and urban areas (McPherson et al, 2003).…”
Section: Characterization Of the Physico-chemical Properties Of The Hmentioning
confidence: 99%
“…The overall mineralization rates of [pyrimidine-4,6-14 C] ZJ0273 and [benzyl-U-14 C] ZJ0273 were correlated with soil pH (p < 0.05) and organic matter content (p < 0.05). The soil S 1 was more acidic (pH 4.20) and also had less organic matter than the other two soils (Table 1), which may have brought about limited microbial activity in this soil and hence a limited mineralization potential (Boivin et al, 2005). The slow mineralization of ZJ0273 in acidic soil and implications for risk assessment and management merit were further investigated.…”
Section: Mineralizationmentioning
confidence: 99%