Geography -- Overall info about the river case study
- Created by: Katy Matey
- Created on: 11-06-18 18:23
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- How and why does river velocity change downstream? Case study of the river Holford -- Overall information
- The Bradshaw model
- The Bradshaw model shows that river velocity actually increases as it travels further towards sea level.
- The Bradshaw model shows how going downstream many things happen
- Some things increase
- The discharge
- The occupied channel width
- The channel depth
- The load quantity
- The average velocity
- Some things decrease
- The load particle size
- The channel bed roughness
- The gradient
- Some things increase
- Why do rivers run faster downstream?
- 1) Higher discharge downstream will force water to move along fast
- 2) Smaller stones downstream mean that there is less friction slowing the water down
- 3) More obstacles/rocks in the channel upstream slow water
- 4) more tributaries join= add in water
- 5) irregular channel shape upstream slows water
- 6) the efficiency increases downstream = the hydraulic radius
- The river Holford
- It is located in North Somerseton the coast
- It's source is south and it travels north until it meets the sea
- The length of the river is around 6-7 km
- The area of the drainage basin is around 10km squared
- The flow is from the Quantocks to the British channel
- The Bradshaw model
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