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Adsorption and Movement of Carbofuran in Four Different Soils Varying in Physical and Chemical Properties

机译:四种物理化学性质不同的土壤中呋喃丹的吸附和移动

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Laboratory studies were conducted to determine the adsorption and movement of carbofuran on four divergent textured Indian soils at a fixed volume fraction (fs = 0.1) of methanol/water mixtures using batch equilibrium and soil thin layer chromatography (soil TLC) techniques. The measured equilibrium adsorption isotherms for silt loam (FSL and ASL) and loam (KL) soils were L-shaped and for sandy loam (BSL) soil S-shaped, all being well fitted by the Freundlich isotherm. A higher adsorption of carbofuran was observed on FSL followed by ASL, KL and BSL soils as anticipated by the values obtained for the Freundlich constant, KF and partition coefficient, KD. The Frontal Retardation factor (FRf) values obtained from soil TLC studies were inversely proportional to the KF and KD values. The affinity of carbofuran towards organic carbon, organic matter and clay content of the soils was evaluated by calculating the KOC, KOM and KC values. The negative magnitude of the Gibbs' free energy (ΔG0) indicated the spontaneity of the adsorption of carbofuran onto the soils studied. The leaching index (LI) of carbofuran calculated for the soils studied indicated its high potential to leach into shallow aquifers and ground water. Pearson's correlations calculated for KF and KD against the soil properties showed a highly significant correlation with the clay + silt content of the soils. Multiple regression of KF and KD against the soil properties indicated that the mineral content of the soils (clay and clay + silt) is the best predictor of carbofuran adsorption, followed by soil pH. Predicted log KOM values were also evaluated by using the aqueous solubility, the 1-octanol/water partition coefficient (KOW), the adsorbability index (AI) and the first-order molecular connectivity index (1χ) of carbofuran. Use of the aqueous solubility, and the 1-octanol/water partition coefficient (KOW) to predict the extent of adsorption gave values which displayed a considerable error in comparison to those measured experimentally, whereas the use of the adsorbability index (AI) and the first-order molecular connectivity index (1χ) of carbofuran improved the predictions considerably.
机译:使用分批平衡和土壤薄层色谱法(实验室)研究确定了呋喃呋喃在甲醇/水混合物固定体积分数(f = 0.1)的四种发散纹理印度土壤上的吸附和迁移(土壤TLC)技术。测得的粉壤土(FSL和ASL)和壤土(KL)土壤的平衡吸附等温线为L形,沙质壤土(BSL)土壤为S形,均通过Freundlich等温线拟合。弗氏常数,K F 和分配系数K D 的值预示了FSB,ASL,KL和BSL土壤上对呋喃丹的吸附较高。 。从土壤薄层色谱研究得到的前沿迟滞因子(FR f )值与K F 和K D 值成反比。通过计算K OC ,K OM 和K C 来评估呋喃丹对土壤中有机碳,有机质和粘土含量的亲和力。价值观。吉布斯自由能的负强度(ΔG 0 )表明了呋喃丹吸附在土壤上的自发性。根据研究土壤计算得出的呋喃丹的浸出指数(LI)表明其具有向浅层含水层和地下水中浸出的潜力。计算出的K F 和K D 与土壤特性的皮尔逊相关性与土壤中的粘土+粉砂含量具有极高的相关性。 K F 和K D 对土壤性质的多元回归表明,土壤中的矿物质含量(粘土和粘土+粉砂)是呋喃丹吸附的最佳预测指标,其次是由土壤pH值决定。还通过使用水溶性,1-辛醇/水分配系数(K OW ),吸附指数(AI)和第一个数值来评估预测的log K OM 值呋喃丹的有序分子连通性指数( 1 χ)。使用水溶性和1-辛醇/水分配系数(K OW )预测吸附程度所给出的值与实验测量的值相比显示出相当大的误差,而使用呋喃丹的吸附指数(AI)和一级分子连通性指数( 1 χ)大大改善了预测值。

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