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Modeling the Effect of Suction Change on a Tropical Black Clay Aquitard during Consolidation

机译:模拟固结过程中吸力变化对热带黑粘土阿基德的影响

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Consolidation of clayey contaminant barriers such as aquitards (natural aquifer barriers) and landfill liners can be a cause for early breakthrough of contaminants. The general objective of this research was to numerically model the rate of dissipation of pore pressures (soil suction) and change in the voio ratio/soil permeability characteristics for a loaded black cotton soil (BCS) aquitard layer and thus evaluate the level of ground-water protection in semi-arid regions with BCS cover. Soil suction change was simulated by varying the degree of saturation of the expansive black clay and applying consolidation pressure. A modified Terzaghi's 1-D consolidation equation was modeled using experimental data from the compressibility characteristics of Black cotton soils for various degrees of saturation. Proposed models for predicting the rate of dissipation of pore pressures and change in void ratio were established for the loaded BCS aquitard layer. The modeling results demonstrate the significance of evaluating the hydraulic properties of soils in relationship to their environments under simulated groundwater table and degree of saturation conditions.
机译:诸如阿奎德(天然含水层屏障)之类的黏土污染物屏障和垃圾填埋场衬砌的固结可能是污染物尽早突破的原因。这项研究的总体目标是对负载的黑棉土壤(BCS)阿基塔尔层的孔隙压力消散速率(吸水率)和voio比/土壤渗透性特征的变化进行数值模拟,从而评估地基水平。带有BCS盖的半干旱地区的水保护。通过改变膨胀黑土的饱和度并施加固结压力来模拟土壤吸力变化。修改后的Terzaghi 1-D固结方程是使用实验数据根据不同饱和度的黑棉土壤的可压缩性建模的。建立了用于预测加载的BCS阿基塔尔层孔隙压力消散速率和孔隙率变化的模型。模拟结果表明,在模拟地下水位和饱和度条件下,评估土壤的水力特性与其环境的关系具有重要意义。

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