Lecture 7 - Channel Pattern Flashcards
What are the 3 river channel patterns?
Straight - straight channel
Meandering - curving channel
Braided - channel with multiple channels
Which channel pattern is mostly man-made?
Straight channels.
Most natural river channels are either meandering/wandering or braided
What is the channel sinuosity of a straight and meandering channel?
s = 1.0 - straight
s = 1.3-1.5 - threshold
s = > 1.5 - meandering
What is anabranching?
Where multiple channels have bars with vegetation on them, reducing the erosion of the bars
What is the difference between power and energy?
Energy is defined as the amount of work that can be performed.
Power is the rate at which work is performed.
Why do different planforms develop?
Thresholds can be observed where a change occurs in either:
- sediment
- velocity
- slope
Straight channel planforms
- Low slope angle
- Low power (Ω)
- Relatively narrow and deep channels
Braided channel planforms
- Wide and shallow channels
- High slope angle
- High power (Ω)
- High discharge Variability
- High sediment load
Meandering channel planforms
- Intermediate - enough energy for erosion, but bank resistance is enough to maintain a single channel
What is the natural evolution of river channels?
Straight channels will start to meander due to differences in erosion rates and velocity within the channel.
Meandering channels will continue to meander and eventually have enough power to start braiding.
Braided channels are not common in the uk due to the unstable and sensitive conditions in sediment load and discharge