Some students were performing a hydraulic jump experiment using a wide channel during their laboratory session. During a hydraulic jump experiment, the flow depth amplified from 0.6 m to 3 m. Estimate; a) the velocities and Froude numbers before and after the jump  b) the energy dissipation

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Laboratory Determination of Hydraulic Conductivity

Hydraulic conductivity is the measure of flowability of water inside the soil in the presence of a hydraulic gradient. The hydraulic gradient is defined as the difference in the water heads in the soil, which induces a water motion. In simple terms, a hydraulic gradient is the presence of a potential that induces a flow of water.