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In this paper, the hydraulic conductivity of fine sands with different fines content and relative density are reported under saturation conditions, in alterated samples. Each sample was prepared by mixing preespecified amounts of sand and silt in different proportions. The compacted samples were adjusted so that their optimum water content and dry volumetric weight provided the void ratio corresponding to that of single fine sand. The hydraulic conductivity of the samples was determined by both constant head and falling head apparatus. The hydraulic conductivity values were found to be independent of the measurement technique.

VARIACIÓN DE LA CONDUCTIVIDAD HIDRAÚLICA SATURADA DE ARENAS CON EL CONTENIDO DE FINOS LIMOSOS