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One-dimensional model for biogeochemical interactions and permeability reduction in soils during leachate permeation

机译:渗滤液渗透过程中土壤生物地球化学相互作用和渗透率降低的一维模型

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This paper uses the findings from a column study to develop a reactive model for exploring the interactions occurring in leachatecontaminated soils. The changes occurring in the concentrations of acetic acid, sulphate, suspended and attached biomass, Fe(II), Mn (II), calcium, carbonate ions, and pH in the column are assessed. The mathematical model considers geochemical equilibrium, kinetic biodegradation, precipitation-dissolution reactions, bacterial and substrate transport, and permeability reduction arising from bacterial growth and gas production. A two-step sequential operator splitting method is used to solve the coupled transport and biogeochemical reaction equations. The model gives satisfactory fits to experimental data and the simulations show that the transport of metals in soil is controlled by multiple competing biotic and abiotic reactions. These findings suggest that bioaccumulation and gas formation, compared to chemical precipitation, have a larger influence on hydraulic conductivity reduction.
机译:本文利用专栏研究的结果开发了反应模型,以探索在渗滤液污染土壤中发生的相互作用。评估色谱柱中乙酸,硫酸盐,悬浮和附着的生物量,Fe(II),Mn(II),钙,碳酸根离子和pH值发生的变化。该数学模型考虑了地球化学平衡,动力学生物降解,沉淀-溶解反应,细菌和底物的运输以及细菌生长和产气引起的渗透率降低。采用两步顺序算子分裂方法求解耦合的运移和生物地球化学反应方程。该模型对实验数据给出了令人满意的拟合,并且仿真表明,土壤中金属的运输受到多种竞争性生物和非生物反应的控制。这些发现表明,与化学沉淀相比,生物富集和气体形成对水力传导率的降低影响更大。

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