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Ethylene Dibromide Mineralization in Soils under Aerobic Conditions

机译:有氧条件下土壤中二溴乙烷的矿化

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摘要

1,2-Dibromoethane (EDB), which is a groundwater contaminant in areas where it was once used as a soil fumigant, was shown to be degraded aerobically by microorganisms in two types of surface soils from an EDB-contaminated groundwater discharge area. At initial concentrations of 6 to 8 μg/liter, EDB was degraded in a few days to near or below the detection limit of 0.02 μg/liter. At 15 to 18 mg/liter, degradation was slower. Bromide ion release at the higher concentrations was 1.4 ± 0.3 and 2.1 ± 0.2 molar equivalents for the two soils. Experiments with [14C]EDB showed that EDB was converted to approximately equal amounts of CO2 and apparent cellular carbon; only small amounts of added 14C were not attributable to these products or unreacted EDB. These results are encouraging, because they indicate that groundwater bacteria may hasten the removal of EDB from contaminated aerobic groundwater supplies. This report also provides evidence for soil-mediated chemical transformations of EDB.
机译:1,2-二溴乙烷(EDB)是曾经被用作土壤熏蒸剂的区域中的地下水污染物,已被微生物污染从来自EDB污染的地下水排放区的两种表层土壤中进行有氧降解。在初始浓度为6至8微克/升时,EDB在几天内降解到接近或低于0.02微克/升的检测极限。在15至18 mg / L时,降解速度较慢。两种土壤在较高浓度下的溴离子释放量分别为1.4±0.3和2.1±0.2摩尔当量。用[ 14 C] EDB进行的实验表明,EDB转化为大约等量的CO2和表观细胞碳;只有少量添加的 14 C不能归因于这些产品或未反应的EDB。这些结果令人鼓舞,因为它们表明地下水细菌可能会加速从受污染的需氧地下水供应中去除EDB。该报告还提供了土壤介导的EDB化学转化的证据。

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