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温度对克罗地亚沿海地区土壤中吡虫啉吸附-解吸过程的影响。

Effects of temperature on sorption-desorption processes of imidacloprid in soils of Croatian coastal regions.

机构信息

Department of Chemistry and Biochemistry, School of Medicine, University of Rijeka, Rijeka, Croatia.

出版信息

J Environ Sci Health B. 2012 Sep;47(8):779-94. doi: 10.1080/03601234.2012.676413.

Abstract

Sorption-desorption behavior of imidacloprid in six soils collected from five coastal regions in Croatia at 20, 30 and 40°C was investigated using batch equilibrium technique. Isothermal data were applied to Freundlich, Langmuir and Temkin equations, and the thermodynamic parameters ΔH°, ΔG°, ΔS° were calculated. The sorption isotherm curves were non-linear and may be classified as L-type, suggesting a relatively high sorption capacity for imidacloprid. Our results showed that the K( sor ) ( F ) values decreased for all the tested soils as the temperature increased, indicating that the temperature strongly influences the sorption. Values of ΔG° were negative (-4.65 to -2.00 kJ/mol) indicating that at all experimental temperatures the interactions of imidacloprid with soils were spontaneous processes. The negative and small ΔH° values (-19.79 to -8.89 kJ/mol) were in the range of weak forces, such as H-bonds, consistent with interactions and partitioning of the imidacloprid molecules into soil organic matter. The ΔS° values followed the range of -57.12 to -14.51 J/molK, suggesting that imidacloprid molecules lose entropy during transition from the solution phase to soil surface. It was found that imidacloprid desorption from soil was concentration and temperature-dependent, i.e. at lower imidacloprid concentrations and temperature, lower desorption percentage occurred. Desorption studies revealed that hysteretic behavior under different temperature treatments existed, and it was more pronounced at 20°C in the soils with higher OC content. The study results emphasize the importance of thermodynamic parameters in controlling soil pesticide mobility in different geographical locations, seasons and greenhouse conditions.

摘要

采用批量平衡技术研究了 20、30 和 40°C 时从克罗地亚五个沿海地区采集的六种土壤中吡虫啉的吸附-解吸行为。等温数据应用于 Freundlich、Langmuir 和 Temkin 方程,并计算了热力学参数ΔH°、ΔG°、ΔS°。吸附等温线曲线呈非线性,可归类为 L 型,表明吡虫啉具有较高的吸附能力。我们的结果表明,随着温度的升高,所有测试土壤的 K( sor )(F) 值均降低,表明温度强烈影响吸附。ΔG°值为负值(-4.65 至-2.00 kJ/mol),表明在所有实验温度下,吡虫啉与土壤的相互作用均为自发过程。负且较小的ΔH°值(-19.79 至-8.89 kJ/mol)处于较弱力的范围内,如氢键,与吡虫啉分子进入土壤有机质的相互作用和分配一致。ΔS°值遵循-57.12 至-14.51 J/molK 的范围,表明吡虫啉分子在从溶液相到土壤表面的转变过程中失去熵。研究发现,吡虫啉从土壤中的解吸与浓度和温度有关,即在较低的吡虫啉浓度和温度下,解吸百分比较低。解吸研究表明,在不同温度处理下存在滞后行为,在 OC 含量较高的土壤中,20°C 时更为明显。研究结果强调了热力学参数在控制不同地理位置、季节和温室条件下土壤中农药迁移性方面的重要性。

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