channel morphology Flashcards
Discharge
Volume of water flowing through a cross-section @ any point in time (in a channel)
Stream gradient
Inclination of water surface to the horizontal distance covered
- decreases downstream
- represented by a long profile graph
Long profile graph
Illustration of stream gradient β shows channel height in relation to the base level
- shows amount of potential energy potential for vertical erosion to take place
Cross-sectional area
Area of a vertical slice along any point of the channel
- channel depth x bankfull width
Hydraulic radius
Proportion of water in constant contact with the stream channel
- higher ratio = lower friction & turbulence
Wetted perimeter
Length of a channel the cross-section in contact with the water in a channel
Velocity
Rate of water flow in a channel
- controlled by driving & resisting forces
Driving forces of velocity:
- Channel gradient β steeper gradient = higher velocity
- volume of water in the channel β higher volume = higher impact of local factors
Resisting forces of velocity
- Amount of friction βfiner bed material = higher velocity
- channel shape β wider channel = lower RH = higher friction = lower velocity energy
Channel width & bankfull
Width = shortest distance from 1 edge of the channel to the other
Bankfull β immediate channel state before a flood
- bankfull width β width measurement airing the bankfull stage
W/d ratio of a channel
Ratio of bankfull width against the channel depth