1) Find the rate of flow in m³/sec/m (at right angles to the cross section shown in Figure 7.33) through the permeable soil layer. Given: H = 4 m, H1 = 2 m, h = 2.75 m, S = 30 m, a = 14°, and k = 0.075 cm/sec. Direction of flow Figure 7.33 H h Impervious layer Impervious layer S Cengage Learning 2014

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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.