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Coupled infiltration model of unsaturated porous media for steady rainfall

机译:稳定降雨的非饱和多孔介质耦合入渗模型

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Unsaturated soil slopes introduce complex hydro-mechanical coupled processes which greatly alter matric suction distribution of an unsaturated soil during rainfall. In order to investigate matric suction and volume change of unsaturated soils, a two-dimensional hydro-mechanical coupled infiltration model (YS-Slope) is developed by incorporating the hydraulic and mechanical characteristics of unsaturated soils, such as the soil-water characteristic curve, permeability function, shear strength, and porosity. Special attention is given to the porosity-dependent permeability function of unsaturated soils. In addition, in order to highlight effectiveness of YS-Slope and coupling effects of hydro-mechanical processes on the infiltration behavior of unsaturated soils, a series of infiltration analyses for a soil column under various soil properties is conducted and their results are compared with those of commercial software, GEO-SLOPE (2012). The results of the numerical analyses show good agreement with data from the analytical solution and laboratory tests, which indicates that the proposed model is appropriate for use in the simulatfion o the infiltration of rainwater into deformable soils. The transient seepage and rainwater flow in deformable soils are influenced by the volume change of the soil. The change in matric suction on a slope due to rainfall infiltration influences change in effective stress while the effective stress alters seepage processes according to hydraulic properties. The results indicate that hydro-mechanical coupled behavior of soils has a positive effect on the stability of unsaturated soil slops during rainfall. (C) 2017 The Japanese Geotechnical Society. Production and hosting by Elsevier B.V.
机译:不饱和土壤边坡引入了复杂的水力耦合过程,极大地改变了降雨过程中非饱和土壤的基质吸力分布。为了研究非饱和土壤的基质吸力和体积变化,通过结合非饱和土壤的水力和力学特性(例如土壤-水特征曲线),建立了二维水力耦合渗流模型(YS-Slope)。渗透率函数,抗剪强度和孔隙率。特别注意非饱和土壤的孔隙度相关的渗透率函数。另外,为突出YS-坡度的有效性和水力作用过程对非饱和土壤入渗行为的耦合作用,对各种土壤性质下的土柱进行了一系列入渗分析,并将其结果与分析结果进行了比较。商业软件GEO-SLOPE(2012)。数值分析结果与分析溶液和实验室测试的数据吻合良好,这表明所提出的模型适用于模拟雨水渗入可变形土壤中的情况。可变形土壤中的瞬态渗流和雨水流量受土壤体积变化的影响。由于降雨入渗引起的斜坡上基质吸力的变化影响有效应力的变化,而有效应力则根据水力性质改变渗流过程。结果表明,在降雨过程中,土的水力耦合行为对非饱和土边坡的稳定性有积极影响。 (C)2017日本岩土学会。 Elsevier B.V.的制作和托管

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