Embed presentation
Downloaded 15 times


































Open channel flow is the flow of fluid with a free surface, where the free surface is exposed to atmospheric pressure. It occurs due to the force of gravity down a sloped channel bed. Open channel flow can be steady or unsteady, uniform or non-uniform, laminar or turbulent, and subcritical, critical, or supercritical. Non-uniform flow is classified as either rapidly varied flow where depth changes abruptly, or gradually varied flow where changes occur gradually over a long length. Discharge in open channels can be calculated using Chezy's formula, which relates discharge, velocity, hydraulic radius, and channel roughness.
































