Anaerobic Transformation of DDT Related to Iron(III)
Reduction and Microbial Community Structure in Paddy Soils
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Abstract
We
studied the mechanisms of microbial transformation in functional
bacteria on 1,1,1-trichloro-2,2-bis(<i>p</i>-chlorophenyl)ethane
(DDT) in two different field soils, Haiyan (HY) and Chenghai (CH).
The results showed that microbial activities had a steady dechlorination
effect on DDT and its metabolites (DDx). Adding lactate or glucose
as carbon sources increased the amount of <i>Desulfuromonas</i>, <i>Sedimentibacter</i>, and <i>Clostridium</i> bacteria, which led to an increase in adsorbed Fe(II) and resulted
in increased DDT transformation rates. The electron shuttle of anthraquinone-2,6-disulfonic
disodium salt resulted in an increase in the negative potential of
soil by mediating the electron transfer from the bacteria to the DDT.
Moreover, the DDT-degrading bacteria in the CH soil were more abundant
than those in the HY soil, which led to higher DDT transformation
rates in the CH soil. The most stable compound of DDx was 1,1-dichloro-2,2-bis(<i>p</i>-chloro-phenyl)ethane, which also was the major dechlorination
metabolite of DDT, and 1-chloro-2,2-bis-(<i>p</i>-chlorophenyl)ethane
and 4,4′-dichlorobenzo-phenone were found to be the terminal
metabolites in the anaerobic soils