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Reactive transport of chemicals in unsaturated soils: numerical model development and verification

机译:化学物质在非饱和土壤中的反应性传输:数值模型的建立和验证

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This paper presents the development of a numerical model for reactive transport of multicomponent chemicals in unsaturated soils. The model has been developed based on a coupled thermal, hydraulic, chemical, and mechanical (THCM) formulation, and extended by the inclusion of geochemical processes under mixed equilibrium and kinetically controlled reactions in-between the solid, aqueous, and gas phases in soil. This has been achieved by coupling the transport model, COMPASS, with the geochemical model, PHREEQC. Key coupling between the geochemical modelling and the flow of chemicals has been established via the inclusion of porosity modification from mineral precipitation-dissolution reactions and the consequential effects on flow processes. Verification of the developed model is addressed via a series of benchmark simulations with a focus on testing the coupling between the transport model and geochemical model. Good results have been achieved for the verification of the theoretical and numerical implementation of the new developments in the model. A simulation is presented to demonstrate the effects of mineral reactions on porosity evolution and chemical diffusion in a low porosity soil. The model developed is an advanced tool for studying the hydrogeochemical processes in unsaturated soils under variable THCM conditions.
机译:本文提出了在非饱和土壤中多组分化学物质反应性迁移的数值模型的发展。该模型是基于热,水,化学和机械(THCM)耦合公式开发的,并通过在土壤中的固相,水相和气相之间混合平衡和动力学控制反应下纳入地球化学过程来扩展。这是通过将运输模型COMPASS与地球化学模型PHREEQC耦合来实现的。地球化学模型与化学物质流之间的关键耦合是通过包含矿物沉淀-溶解反应的孔隙度变化及其对流动过程的影响而建立的。通过一系列基准模拟来解决对开发模型的验证,重点是测试运输模型与地球化学模型之间的耦合。在验证模型中新进展的理论和数值实现方面取得了良好的结果。进行了模拟,以证明矿物反应对低孔隙度土壤中孔隙演化和化学扩散的影响。建立的模型是研究可变THCM条件下非饱和土壤中水文地球化学过程的先进工具。

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