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Mechanism and modeling of hexavalent chromium interaction with a typical black soil: the importance of the relationship between adsorption and reduction

机译:六价铬与典型黑土相互作用的机理和模型:吸附与还原之间关系的重要性

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Black soils have a significant retention effect on the migration of Cr( VI ) towards groundwater, and Cr( VI ) adsorption and reduction are both involved in this process. However, the adsorption and reduction of Cr( VI ) were always investigated separately in previous studies resulting in an unclear relationship between them. In this study, the adsorption and reduction kinetic processes of Cr( VI ) by a typical black soil were separately investigated under different initial Cr( VI ) concentrations (40–400 mg L ~(?1) ) and pH conditions (3.5–7.0) by the means of desorption treatment, and the equilibrium relationship between aqueous and adsorbed Cr( VI ) was innovatively established based on the kinetic data. It was found that under pH 5.7 the adsorbed Cr( VI ) content on soil particles was linearly correlated with the remaining Cr( VI ) concentration in solution with time ( R ~(2) = 0.98), and the reduction rate of Cr( VI ) in the reaction system was linearly correlated with the adsorbed Cr( VI ) content on soil particles with time ( R ~(2) = 0.99). With pH decreasing from 7.0 to 3.5, the partition of Cr( VI ) between solid and aqueous phases turned out to be of a non-linear nature, which can be fitted better by the Freundlich model. The retention of Cr( VI ) by black soil was determined to follow the “adsorption–reduction” mechanism, where the Cr( VI ) was first rapidly adsorbed onto the soil particles by a reversible adsorption reaction, and then the adsorbed Cr( VI ) was gradually reduced into Cr( III ). A two-step kinetic model was developed accordingly, and the experimental data were fitted much better by the two-step adsorption–reduction kinetic model ( R ~(2) = 0.89 on average) compared with the traditional first-order and second-order kinetic models ( R ~(2) = 0.66 and 0.76 on average respectively). This paper highlights the novel two step kinetic model developed based on the proposed “adsorption–reduction” mechanism of Cr( VI ) retention by a typical black soil.
机译:黑土对Cr(VI)向地下水的迁移具有显着的保留作用,并且Cr(VI)的吸附和还原都参与了此过程。然而,Cr(VI)的吸附和还原总是在以前的研究中分别进行研究,导致它们之间的关系不清楚。在这项研究中,分别研究了在不同初始Cr(VI)浓度(40-400 mg L〜(?1))和pH条件(3.5-7.0)下典型黑土对Cr(VI)的吸附和还原动力学过程。 )通过解吸处理,基于动力学数据创新性地建立了水和吸附的Cr(VI)之间的平衡关系。结果表明,在pH 5.7下,土壤颗粒上Cr(VI)的吸附量与溶液中剩余Cr(VI)的浓度随时间呈线性关系(R〜(2)= 0.98),并且Cr(VI)的还原率随时间的变化,R((2)= 0.99)与土壤中吸附的Cr(VI)含量呈线性关系。随着pH从7.0降低到3.5,固相和水相之间的Cr(VI)分配被证明是非线性的,这可以通过Freundlich模型更好地拟合。确定黑土对Cr(VI)的保留遵循“吸附-还原”机理,即首先通过可逆吸附反应将Cr(VI)快速吸附到土壤颗粒上,然后再吸附Cr(VI)逐渐还原为Cr(III)。相应地建立了两步动力学模型,与传统的一阶和二阶模型相比,两步吸附-还原动力学模型(平均R〜(2)= 0.89)拟合的实验数据更好。动力学模型(R〜(2)分别平均为0.66和0.76)。本文重点介绍了一种新的两步动力学模型,该模型基于拟议的典型黑土对Cr(VI)保留的“吸附-还原”机理而开发。

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