Seepage is occurring through a porous media shown in the figure. The hydraulic conductivity values (k₁, k2, k3) are in m/day. The seepage discharge (m³/day per m) through the porous media at section PQ is 1 15 m 3 m :k₁ = 2 20 m k₂ = 3 Impervious P 10 m 20 m 4-13m 10 m 10 m

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Principles of Seepage

In hydrology, when water flows down in a pore or crack of unsaturated soil due to gravity, the deep layer of soil is called seepage. It is the slow movement of water in the soil layer. Seepage is mainly found near hydraulic structures and is responsible for the stability of earthen-type hydraulic structures.