首页> 外文期刊>Journal of King Saud University >Combined effect of unsaturated soil condition and soil heterogeneity on methylene blue adsorption/desorption and transport in fixed bed column: Experimental and modeling analysis
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Combined effect of unsaturated soil condition and soil heterogeneity on methylene blue adsorption/desorption and transport in fixed bed column: Experimental and modeling analysis

机译:非饱和土壤条件和土壤异质性对固定床塔中亚甲基蓝吸附/解吸和迁移的综合影响:实验与模型分析

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Several series of batch and fixed bed column experiments have been carried out to study the methylene blue sorption and transport in sandy and clay soil under different experimental conditions. The non linear forms of the pseudo-second order kinetic model and the Freundlich and Langmuir isotherm models were used to quantify the maximum adsorption capacity of the used materials. The effects of several experimental factors (flow rate, initial concentration, saturation condition of soil and soil heterogeneity) on the breakthrough curves have been undertaken. Experimental data revealed that the breakthrough curves depend on flow rate, methylene blue inlet concentration, saturation condition of soil and soil heterogeneity. A two dimensional model based on Richards equation and advection–dispersion equation coupled with adsorption model was developed. A comparative analysis between this model and Thomas model showed the effectiveness of advection–dispersion model to describe the experimental breakthrough curves and particularly in an unsaturated heterogeneous medium. The advection dispersion model reproduces perfectly the transfer mechanisms in porous media and seems to be a useful tool to better understanding the physical processes and the effect of capillary barrier of methylene blue transport in unsaturated heterogeneous soil. The result shows also that the soil heterogeneity has a significant effect on methylene blue adsorption through unsaturated layered media. Furthermore, in the interface between two layers with different hydrodynamic proprieties, the adsorption capacity increases with a decrease in kinetic adsorption rate caused by the decrease in pore water velocity.
机译:为了研究亚甲基蓝在不同实验条件下在沙质和黏性土壤中的吸附和迁移,已经进行了一系列系列的间歇和固定床实验。伪二级动力学模型以及Freundlich和Langmuir等温线模型的非线性形式用于量化所用材料的最大吸附容量。研究了几种实验因素(流速,初始浓度,土壤饱和度条件和土壤非均质性)对穿透曲线的影响。实验数据表明,穿透曲线取决于流速,亚甲基蓝的入口浓度,土壤饱和度和土壤异质性。建立了基于理查兹方程,对流扩散方程和吸附模型的二维模型。该模型与Thomas模型之间的比较分析表明,对流扩散模型可用于描述实验突破曲线,尤其是在非均质非均质介质中。对流弥散模型完美地再现了多孔介质中的传递机理,并且似乎是一个有用的工具,可以用来更好地了解非饱和非均质土壤中亚甲基蓝迁移的物理过程和毛细屏障的作用。结果还表明,土壤异质性对不饱和层状介质吸附亚甲基蓝有显着影响。此外,在具有不同流体动力学特性的两层之间的界面中,由于孔隙水速度的降低而引起的动力学吸附速率的降低,吸附容量增加。

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