Water flows through the pipe contraction shown in the figure below. For the given d=0.11 m difference in the manometer level, determine the flowrate. D₁ = 0.12 m and D2 = 0.04 m D1 d D₂

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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.