Q1/Seepage takes place beneath a concrete dam with an upstream blanket and a sheet pile cutoff wall as shown below. If the permeability of the soil is 7.5 X 10 cm/s, calculate the discharge and draw the seepage flow net. 14.0 m 4.0 m 1.5 m 4.0 m 5.0 m 5.0 m Blanket B Sheet pile Impervious stratum 1.0 m 0.5 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.