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Numerical Modeling of Consolidation of Unsaturated Soils Considering Hydraulic Hysteresis

机译:考虑水力滞后的非饱和土固结数值模拟

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The consolidation of soils is important to geotechnical engineering practice, such as when assessing the rate of settlement of shallow foundations, embankments, and landfills. In this paper, numerical analyses are performed to study the consolidation of unsaturated soils. The variations of excess pore-air and pore-water pressures and settlement with time are established by solving the governing equations. The flow and deformation of the different constituents of an unsaturated soil are fully coupled in the governing equations. The dependency of soil parameters, including the coefficients of permeability for air and water phases and the constitutive coefficients, is allowed to vary as changes to soil volume and suction occur. The effect of hydraulic hysteresis is investigated by considering different initial locations of the hydraulic states on the soil-water characteristic curve. It is shown that the different initial locations of hydraulic states result in different normalized instantaneous settlements and different initial excess pore pressures. The influence of the degree of saturation is also studied. It is shown that for the lowest degree of saturation, the most significant instantaneous settlement occurs and the total consolidation time is longest. The results of this study provide new insights into unsaturated soil consolidation. This is important because the hydraulic loading history and degree of saturation of the soil should be considered when assessing the rate and magnitude of consolidation settlement.
机译:土壤的固结对于岩土工程实践非常重要,例如在评估浅层基础,路堤和垃圾填埋场的沉降速率时。本文通过数值分析来研究非饱和土的固结。通过求解控制方程,可以确定多余的孔隙空气压力和孔隙水压力随时间的变化以及沉降。在控制方程中,非饱和土不同成分的流动和变形完全耦合。土壤参数的依赖性,包括空气和水相的渗透系数和本构系数,可以随土壤体积和吸力的变化而变化。通过考虑水力状态在土壤-水特征曲线上的不同初始位置来研究水力滞后的影响。结果表明,水力状态的不同初始位置会导致不同的归一化瞬时沉降和不同的初始超孔隙压力。还研究了饱和度的影响。结果表明,对于最低的饱和度,最大的瞬时沉降发生,并且总固结时间最长。这项研究的结果为非饱和土固结提供了新的见识。这很重要,因为在评估固结沉降的速率和幅度时,应考虑水力负荷历史和土壤的饱和度。

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