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首页> 外文期刊>Journal of Hydrology >Analytical solution for one-dimensional contaminant diffusion through unsaturated soils beneath geomembrane
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Analytical solution for one-dimensional contaminant diffusion through unsaturated soils beneath geomembrane

机译:通过土工膜下面的非饱和土的一维污染物扩散的分析解决方案

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摘要

Diffusion is the dominating process in the migration of contaminants through landfill liners, below which the soils are generally unsaturated. Analytical method is often considered as a preferred approach over numerical method to solve diffusion problems. In this study, a one-dimensional diffusion model of contaminants is firstly developed to account for unsaturated properties of the soils beneath landfill barriers. Based on an assumption of linear water pressure distribution, the nonlinear governing equation in the diffusion model is transformed into a linear equation using an exponential expression of soil water retention curve and a linear model of unsaturated diffusion coefficient. Subsequently, the corresponding analytical solution is obtained and the solution is then applied to investigate the effects of soil type, water pressure condition and groundwater depth on the diffusion of contaminants. The analytical results show that groundwater depth has the most influential effect on the steady flux rate of contaminants. Furthermore, the obtained steady flux rates in soil layers with high desaturation rate are negligible when the groundwater depth exceeds 3 m and 2 m. The results also indicate that a thicker soil layer with high desaturation rate is recommended to be an effective diffusion barrier to mitigate the pollution of the underlying soils and groundwater.
机译:扩散是通过垃圾填埋衬垫迁移污染物迁移的主导过程,下面的土壤通常是不饱和的。分析方法通常被认为是通过数值方法来解决扩散问题的优选方法。在该研究中,首先开发了污染物的一维扩散模型,以考虑垃圾填埋场屏障下的土壤的不饱和性质。基于线性水压分布的假设,扩散模型中的非线性控制方程使用土壤保水曲线的指数表达和不饱和扩散系数的线性模型转化为线性方程。随后,获得相应的分析溶液,然后施用溶液以研究土壤型,水压条件和地下水深度对污染物扩散的影响。分析结果表明,地下水深度对污染物的稳定通量速率具有最有影响力的影响。此外,当地下水深度超过3米和2米时,具有高去饱和速率的土壤层中获得的稳定通量速率可忽略不计。结果还表明,建议具有高去饱和速率的较厚的土壤层是有效的扩散屏障,以减轻底层土壤和地下水的污染。

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