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首页> 外文期刊>Soil Science >The Effect of the Soil Properties on Adsorption, Single-Point Desorption, and Degradation of Chlorpyrifos in Two Agricultural Soil Profiles From Colombia
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The Effect of the Soil Properties on Adsorption, Single-Point Desorption, and Degradation of Chlorpyrifos in Two Agricultural Soil Profiles From Colombia

机译:土壤性质对哥伦比亚两种农业土壤剖面中毒死rif的吸附,单点解吸和降解的影响

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Structural composition of soil organic matter and the adsorption/desorption characteristics of the insecticide chlorpyrifos were investigated in two soil profiles (Andisol and Entisol) under agriculture production using Fourier transform infrared spectroscopy, nuclear magnetic resonance, and batch analysis methods. Throughout the soil profile, the Andisol had larger values of pH, organic carbon content, cation exchange capacity (CEC), and effective CEC than the Entisol. The Entisol showed larger amounts of kaolinite and ferric and/or aluminum oxides in deeper soil layers. Soil organic matter carbonyl-C, aryl-C, O-alkyl C, and alkyl-C were transported vertically in the vadose zone, with aryl-C being the predominant species in both soils. These results suggest that aryl-C is a reasonable predictor of chlorpyrifos adsorption properties under tropical conditions. Chlorpyrifos adsorption was found to be spontaneous and exothermic, with decreasing adsorption values of the distribution coefficient K-d (37.2-10.1 L kg(-1)) in the deeper layers of both soil types (although more significant in the Entisol). One-step desorption hysteresis showed a monotonic decrease with increasing soil depth and correlated positively with both organic carbon and CEC. The degradation of chlorpyrifos in Andisol (0-100 cm) was investigated using a laboratory incubation method. Degradation rate k was found to be approximately constant (0.011-0.015 d(-1)) throughout the soil profile where biotic and abiotic processes are active. Based on the Groundwater Ubiquity Score, chlorpyrifos presented a "transitional" leaching potential with soil depth.
机译:利用傅里叶变换红外光谱法,核磁共振法和分批分析法,研究了农业生产的两种土壤剖面(Andisol和Entisol)中土壤有机物的结构组成和毒死的吸附/解吸特性。在整个土壤剖面中,Andisol的pH,有机碳含量,阳离子交换容量(CEC)和有效CEC值均比Entisol大。 Entisol在较深的土壤层中显示出大量的高岭石以及三氧化二铁和/或氧化铝。土壤有机质羰基-C,芳基-C,O-烷基C和烷基-C在渗流带中垂直运输,其中芳基-C是两种土壤中的主要物种。这些结果表明,芳基-C是热带条件下毒死rif吸附性能的合理预测指标。发现毒死rif的吸附是自发的且放热的,在两种土壤类型的较深层(尽管在Entisol中更显着),其分配系数K-d(37.2-10.1 L kg(-1))的吸附值降低。一步解吸滞后随土壤深度的增加而单调降低,并且与有机碳和CEC均呈正相关。使用实验室培养方法研究了毒死rif在Andisol(0-100 cm)中的降解情况。发现在生物和非生物过程均活跃的整个土壤剖面中,降解速率k大致恒定(0.011-0.015 d(-1))。根据地下水的普遍性得分,毒死rif具有随着土壤深度的“过渡”浸出潜力。

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