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Behavior of fenhexamid in soil and water

机译:苯六胺在土壤和水中的行为

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A study was conducted to investigate fenhexamid (FEX) behavior in soil and in water. FEX proved to be rather stable at acid pH but showed slight degradation at neutral and alkaline pH. After 101 days of FEX spiking of a soil sample, 94% at pH 4, 12% at pH 7 and 23% at pH 9 of the active ingredient was still present. In natural water the rate of FEX disappearance appeared to be slow which may be due to abiotic rather than biotic processes. The soil degradation tests showed low persistence of the active ingredient if a good microflora activity is guaranteed (DT50 about 1 day). Moreover, in absence of microorganisms, FEX proved to be stable. Humidities of 25 and 50% of Water Holding Capacity (WHC) influenced in equal measure the rate of degradation. From the same soil, a bacterium was isolated and identified as Bacillus megaterium, which was able to metabolize FEX with the hydroxylation of the cyclohexane ring. Moreover, FEX showed an elevated affinity for humic acid (73%), smectite (31%), and ferrihydrite(20%) and low affinity for vermiculite (11%) and kaolinite (7%).
机译:进行了一项研究,以研究在土壤和水中的苯六胺(FEX)行为。事实证明,FEX在酸性pH下相当稳定,但在中性和碱性pH下显示轻微降解。在FEX加标101天后,仍然存在94%的pH活性成分,12%的pH 7活性成分和23%的pH 9活性成分。在天然水中,FEX消失的速度似乎很慢,这可能是由于非生物过程而非生物过程造成的。土壤降解测试表明,如果可以保证良好的菌群活性(DT50约1天),则活性成分的持久性较低。此外,在没有微生物的情况下,FEX被证明是稳定的。持水量(WHC)的25%和50%的湿度对降解速率的影响相等。从同一土壤中分离出一种细菌,并将其鉴定为巨大芽孢杆菌,该细菌能够通过环己烷环的羟基化作用来代谢FEX。此外,FEX对腐殖酸(73%),蒙脱石(31%)和水铁矿(20%)的亲和力提高,对ver石(11%)和高岭石(7%)的亲和力低。

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