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Adsorption and Movement of Endosulfan in Soils: A Verification of the Co-solvent Theory and a Comparison of Batch Equilibrium and Soil Thin Layer Chromatography Results

机译:硫丹在土壤中的吸附和移动:共溶剂理论的验证以及批次平衡和土壤薄层色谱结果的比较

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Batch equilibrium and soil thin-layer chromatography (soil TLC) techniques were used to investigate the influence of different volume fractions (f(s) = 0.25, 0.50, 0.75 and 1.0) of organic co-solvents (acetone and methanol) oil the adsorption and movement of endosulfan in three different types of Indian soils (silt loam, loam and sandy loam). The measured equilibrium adsorption isotherms for all three soils studied were L-shaped for both co-solvent/water mixtures at all f(s) values. All isotherms were in close agreement with the Freundlich equation. Higher adsorption of endosulfan was observed on silt loam soil followed by loam and sandy loam soils at all f(s) values for both co-solvent systems, as was anticipated from the values of the Freundlich constants, K, and the partition coefficients, K-D The order of the K and K-D values also confirmed that endosulfan adsorption was higher in methanol/water mixtures than in acetone/water Mixtures and decreased with increasing f(s) values. The R-f values obtained from soil TLC studies were inversely proportional to the K and K-D values for both co-solvent systems. The higher K and K-D values and lower R-f values in methanol/water mixtures relative to acetone/water mixtures for all the three soils studied indicated that acetone had a greater potential for ground water contamination through leaching from potential sites than methanol. The affinity of endosulfan towards the organic carbon and clay content of the soils was evaluated by calculating the K-OC and K-C values. The data obtained indicated that, although the affinity of endosulfan was better correlated with the organic carbon content, the contribution of the clay content of soils towards endosulfan adsorption cannot be ignored. The adsorption data were used to evaluate the co-solvent theory for describing the adsorption of endosulfan in acetone/water and methanol/water mixtures. The aqueous-phase partition coefficients, K-DW(mol/a), normalized with respect to f(oc) for endosulfan were evaluated via the extrapolation f(s) -> 0.
机译:分批平衡和土壤薄层色谱(土壤薄层色谱)技术用于研究有机助溶剂(丙酮和甲醇)的不同体积分数(f(s)= 0.25、0.50、0.75和1.0)对吸附油的影响硫丹在三种不同类型的印度土壤(粉壤土,壤土和沙质壤土)中的迁移和迁移。对于所有f(s)值的助溶剂/水混合物,所研究的全部三种土壤的平衡吸附等温线均为L形。所有等温线都与Freundlich方程非常吻合。对于两种共溶剂体系,在粉质壤土上的硫均较高吸附,然后在所有f(s)值的壤土和沙质壤土上均观察到硫丹的吸附,这是根据Freundlich常数K和分配系数KD所预期的K和KD值的顺序还证实,硫丹在甲醇/水混合物中的吸附量比在丙酮/水混合物中的吸附量高,并且随着f(s)值的增加而降低。从土壤TLC研究获得的R-f值与两种助溶剂系统的K和K-D值成反比。相对于丙酮/水混合物,在所有研究的三种土壤中,甲醇/水混合物的K和K-D值较高,而R-f值较低,这表明丙酮通过从潜在位点浸出比地下水具有更大的潜在地下水污染潜力。通过计算K-OC和K-C值评估硫丹对土壤有机碳和粘土含量的亲和力。获得的数据表明,尽管硫丹的亲和力与有机碳含量具有更好的相关性,但土壤中粘土含量对硫丹吸附的贡献却不能忽略。吸附数据用于评估共溶剂理论,该理论描述了硫丹在丙酮/水和甲醇/水混合物中的吸附。相对于硫丹的f(oc)归一化的水相分配系数K-DW(mol / a)通过外推f(s)-> 0进行评估。

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