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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 (f(s) = 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, K-F and partition coefficient, K-D. The Frontal Retardation factor (FRf) values obtained from soil TLC studies were inversely proportional to the K-F and K-D values. The affinity of carbofuran towards organic carbon, organic matter and clay content of the soils was evaluated by calculating the K-OC, K-OM, and K-C values. The negative magnitude of the Gibbs' free energy (Delta G(0)) 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 K-F and K-D against the soil properties showed a highly significant correlation with the clay + silt content of the soils. Multiple regression of K-F and K-D 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 K-OM values were also evaluated by using the aqueous solubility, the 1-octanol/water partition coefficient (K-OW), the adsorbability index (AI) and the first-order molecular connectivity index ((1)chi) of carbofuran. Use of the aqueous solubility, and the 1-octanol/water partition coefficient (K-OW) 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 ((1)chi) of carbofuran improved the predictions considerably.
机译:使用批次平衡和土壤薄层色谱法(土壤薄层色谱),进行了实验室研究,以确定甲醇和水混合物在固定体积分数(f(s = 0.1)下,在四种发散纹理的印度土壤上的呋喃丹的吸附和迁移。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。如弗氏lik常数,K-F和分配系数K-D所获得的值所预期,在FSL上接着是ASL,KL和BSL土壤上观察到了呋喃呋喃的更高吸附。从土壤薄层色谱研究获得的前沿迟滞因子(FRf)值与K-F和K-D值成反比。通过计算K-OC,K-OM和K-C值,评估了呋喃丹对土壤中有机碳,有机质和粘土含量的亲和力。吉布斯自由能的负幅值(Delta G(0))表明了呋喃丹吸附在研究的土壤上的自发性。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。根据K-F和K-D计算的Pearson相关性与土壤特性之间的相关性显示出与土壤中的粘土+粉砂含量高度相关。 K-F和K-D对土壤性质的多重回归表明,土壤中的矿物质含量(粘土和粘土+淤泥)是呋喃丹吸附的最佳预测指标,其次是土壤pH值。还通过使用水溶性,1-辛醇/水分配系数(K-OW),吸附性指数(AI)和一阶分子连通性指数((1)chi)评估了预测的log K-OM值。呋喃丹。使用水溶性和1-辛醇/水分配系数(K-OW)来预测吸附程度,得出的值与实验测量的值相比显示出相当大的误差,而使用吸附指数(AI)呋喃丹的一级分子连通性指数((1)chi)大大改善了预测。

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