ll Seepage takes place around a retaining wall shown in Figure P2.9. The hydraulic conductivity of the sand is 1.5 x 10-³ cm/s. The retaining wall is 50 m long. Determine the quantity of seepage across the entire wall per day. FIGURE P2.9 5m Retaining wall Impervious stratum Sand

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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.