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Numerical analysis of water infiltration in an unsaturated residual soil by using the water retention curve

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The water infiltration analysis in soils is indispensable in order to understand how the moisture variations in the soil occurs in real situations as well as its influence in the engineering properties. However, such analysis requires the unsaturated soil parameters for the computations. These param...

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Detalles Bibliográficos
Autores: Carnero Carnero, Erasmo G., Carnero Guzmán, Gonzalo G.
Formato: artículo
Fecha de Publicación:2018
Institución:Universidad Nacional del Altiplano
Repositorio:Revista de Investigaciones Altoandinas
Lenguaje:español
OAI Identifier:oai:ojs.pkp.sfu.ca:article/107
Nivel de acceso:acceso abierto
Materia:Unsaturated soil
soil water retention curve
suction
water infiltration in soils
finite elements
Suelo no saturado
curva de retención de agua
succión
infiltración en suelos
elementos finitos
Descripción
Sumario:The water infiltration analysis in soils is indispensable in order to understand how the moisture variations in the soil occurs in real situations as well as its influence in the engineering properties. However, such analysis requires the unsaturated soil parameters for the computations. These parameters, such as the unsaturated hydraulic conductivity can be estimated by using the soil water retention curve (SWRC). The SWRC governs the hydration and dehydration process in soils. The current research, studies the water infiltrations in a residual soil from Brazil under two unsaturated initial conditions. The analysis was performed by using a finite elements software employing the SWRC of the soil obtained experimentally. The results show that the saturation time is in function of the initial saturation of the soil and the quality of experimental data in the SWRC.
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