Dispersion is also a function of channel geometry.
2.
For a given flow rate and channel geometry, there is a relationship between flow depth and total energy.
3.
Normal depth is a function of channel geometry, roughness " n ", slope, and discharge.
4.
This can only occur in a smooth channel that does not experience any changes in flow, channel geometry, roughness or channel slope.
5.
The bed material load transport in alluvial rivers is the principal link between river hydraulics and river form and is responsible for building and maintaining the channel geometry.
6.
It is determined by making repeated discrete measurements of streamflow discharge using a velocimeter and some means to measure the channel geometry to determine the cross-sectional area of the channel.
7.
Locations where flow may make such a transition include : significant changes in slope, channel geometry ( e . g . bridge sections ), grade control structures, and the confluence of water bodies.
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