This document discusses gradually varied flow in open channels. It defines gradually varied flow and rapid flow, and lists some common causes of gradually varied flow including changes in channel shape, slope, obstructions, and frictional forces. It also lists the assumptions of gradually varied flow models including prismatic channels, constant Manning's n, hydrostatic pressure, and fixed velocity distribution. The basic differential equation for gradually varied flow relates the water surface slope, energy slope, channel bed slope, discharge, conveyance, and hydraulic radius. Channel bed slopes are also classified.