涕灭威在土壤中的降解特性

    Degradation of aldicarb residues in soil

    • 摘要: 用实验室模拟培养方法研究了土壤中涕灭威及其代谢物在不同条件下的降解规律,探讨了影响降解的主要因素。结果表明,温度和土壤微生物活性是影响降解的重要因素,温度升高、有机质含量增加均大大加快涕灭威残留物降解。25℃时,涕灭威在不同类型表层土壤中T0.5为3~8d,其残留物总量的T0.5为30~65d.在温度低、徽生物活性小的深层土壤中涕灭威T0.5为34~120d,残留物总量的T0.5为159~686d,其中亚矾较难降解。

       

      Abstract: The degradation of aldicarb and its metabolites in soil at different conditions were studied and discussed.Theresults showed that aldicarb degraded rapidly in various types of surface soil with corresponding T0.5 at 3 to 8 days. TheT0.5 of total residue including aldicarb sulfoxide and sulfone ranged from 30 to 65 days. The main factors effectingaldicarb degradation were temperature and the activity of soil micrcorganism. In deep soil which temperature and organicmatter content were lower,T0.5 of aldicarb and total residues were observed to be 34 to l20 davs and 159 to 686 davs re-spectively.And aldicarb sulfoxide was much more difficult to be degraded into sulfone.

       

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