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Bradshaw Model
An explanation of changes in channel characteristics with distance downstream.
10
Geography
Not Applicable
05/06/2013

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Cards

Term
Discharge
Definition
INCREASES

Discharge is always increasing since tributaries feed more water into the stream. Throughflow, Groundwater Flow and Surface Runoff also increase contributing to discharge.
Term
Channel Width
Definition
INCREASES

Tributaries and flows directly increase 'volume' of water and river width increases due to lateral erosion.
Term
Channel Depth
Definition
INCREASES

Tributaries and flows directly increase 'volume' of water and river depth increases due to vertical erosion.
Term
Velocity
Definition
Velocity increases since water accelerates downstream due to the forces of gravity. The river is also more efficient since proportionally less water is in contact with the bed and banks thus reducing energy lost to friction.
Term
Load Quantity
Definition
INCREASES

As river velocity rises, the river has more energy and is thus capable of carrying more load.
Term
Load Particle Size
Definition
DECREASES

As a river travels downstream, the eroded material becomes more rounded and smaller due to attrition.
Term
Channel Bed Roughness
Definition
DECREASES

As a river travels downstream attrition smooths the bed since the bedload is much smoother.
Term
Gradient (Slope Angle)
Definition
DECREASES

A river conducts vigorous vertical erosion in the upper course and lateral erosion in the lower course. Water can also only travel downhill due to forces of gravity.
Term
NOT INCLUDED
Wetted Perimeter
Definition
INCREASES

Wetted Perimeter is the part of the bed and banks which is in direct contact with water. As CSA increases, wetted perimeter must rise
Term
NOT INCLUDED
Hydraulic Radius
Definition
INCREASES

Proportionally, the increase in CSA > the increase in Wetted Perimeter. It is a measure of efficiency.
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