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FACTORS AFFECTING THE HYDROLYTIC DEGRADATION OF CHLORPYRIFOS IN SOIL

机译:影响土壤中氯霉素水解降解的因素

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The abiotic hydrolysis of the organophosphorus insecticide chlorpyrifos was examined in 37 different soils, which were chosen to represent a wide variety of physicochemical characteristics (e.g., pH 3.8-8.5). Samples of soil were sterilized via gamma-irradiation, treated with [C-14]chlorpyrifos at 10 mu g/g, and incubated under standardized conditions (25 degrees C, field moisture capacity, darkness) for up to 4 months. Chlorpyrifos hydrolysis proceeded at a slow rate (<0.008 day(-1)) in acidic soils (pH less than or equal to 7). In alkaline soils, however, hydrolytic rate constants varied greatly (0.004-0.063 day-l). Corresponding hydrolytic half-lives for acidic and alkaline soils ranged from 92 to 341 and 11 to 200 days, respectively. Correlation analyses indicated that soil pH was the independent variable displaying the strongest association with hydrolytic rate constant (r = 0.55), but multiple regression models based on combinations of this parameter with other soil properties, including phosphatase enzyme activities, did not offer strongly predictive models for explaining the variability in kinetics observed (best fit r(2) = 0.59). Incubation of chlorpyrifos with both sterile and nonsterile soils revealed that although both microbial and hydrolytic mechanisms contributed to chlorpyrifos degradation in all soils, there were clearly soils in which hydrolysis constituted the major route of degradation. Chlorpyrifos hydrolysis was greatly accelerated under low moisture conditions, both in acidic and alkaline soils. Additional experiments in several soils that displayed rapid chlorpyrifos hydrolysis at 10 mu g/g provided evidence that the hydrolytic reaction was inhibited at higher concentration (1000 mu g/g). Results highlight the importance but also the complex nature of the hydrolytic breakdown of chlorpyrifos in soil. Under certain conditions (e.g., some alkaline soils, air-dry soils) hydrolysis may be the driving factor modulating chlorpyrifos persistence.
机译:在37种不同的土壤中检测了有机磷杀虫剂毒死rif的非生物水解,这些土壤经选择具有多种理化特性(例如pH 3.8-8.5)。通过伽马射线辐照对土壤样品进行灭菌,以10μg / g的[C-14]毒死rif进行处理,并在标准条件(25摄氏度,田间吸湿能力,黑暗)下孵育长达4个月。毒死rif在酸性土壤(pH小于或等于7)中的水解速度缓慢(<0.008天(-1))。然而,在碱性土壤中,水解速率常数变化很大(0.004-0.063天-1)。酸性和碱性土壤的相应水解半衰期分别为92天至341天和11天至200天。相关分析表明,土壤pH是与水解速率常数之间最强关联的独立变量(r = 0.55),但是基于该参数与其他土壤特性(包括磷酸酶活性)的组合的多个回归模型并未提供强预测性模型用于解释观察到的动力学变化(最佳拟合r(2)= 0.59)。毒死rif在无菌和非无菌土壤中的孵育表明,尽管微生物和水解机制都导致毒死rif在所有土壤中降解,但显然有一些土壤中水解是主要的降解途径。在酸性和碱性土壤中低毒条件下,毒死rif的水解都得到了极大的促进。在几种显示毒死rif能以10μg/ g快速水解的土壤中进行的其他实验提供了证据,表明在较高浓度(1000μg/ g)下水解反应受到抑制。结果突出了毒死rif在土壤中水解分解的重要性和复杂性。在某些条件下(例如某些碱性土壤,风干土壤),水解可能是调节毒死rif持久性的驱动因素。

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