River Exe Case Study Flashcards

Example of a river catchment

1
Q

Describe location of the River Exe

A

Flows for 82.7km from its source in the hills of Exmoor to the sea at Exmouth on the south coast of Devon

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2
Q

Physical characteristics of the River Exe

A
  • 601km^2 area
  • maximum elevation of 514m in the north
  • lowest elevation of 26m in the south
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3
Q

Human characteristics of the River Exe (land use)

A
  • majority of land is agricultural grassland (67%)
  • some woodland (15%)
  • high ground of Exmoor = moors and peatbogs (3%)
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4
Q

Characteristics of geology at the River Exe

A
  • 84.4% of catchment underlain by impermeable rocks (predominantly Devonian sandstones)
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5
Q

Factors affecting the water balance

A

High rainfall = runoff being 65% of the water balance
soil water storage is 35%

Two reasons for this;
- impermeable nature of most of the bedrock reduces percolation and base flow
- drainage ditches on Exmoor reduce the amount of soil water storage

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6
Q

What does the storm hydrograph for the River Exe show?

A
  • the Exe responds relatively slow to rainfall events
  • after flooding discharge recedes slowly reflecting the rural nature of the lower catchment
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6
Q

Describe the Wimbleball reservoir and how it reduces the risk of flooding

A
  • 1979
  • River Haddeo was dammed
  • SA = 150 hectares
  • supplies water to Exmoor and East Devon
  • regulates water flow, ensures a constantly steady regime
  • prevents peaks and troughs of water discharge; reducing flood risk
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6
Q

History of the River Exe/Exmoor Mires

A

1960s - government subsidies paid to peatland owners to drain the land

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7
Q

How did the drainage ditches affect the river?

A

Increased the speed of water flow to the river, reducing water quality as more silt was carried downstream

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7
Q

What was the Exmoor Mires Project?

A

Aims to restore 2000ha of land back to peat bogs by blockage of drainage ditches

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8
Q

How does the Exmoor Mires Project benefit the area?

A
  • improved water quality; slower throughflow means that less sediment is carried into the rivers; water is cleaner, less expensive to treat and good for wildlife, e.g. salmon (= increased biodiversity)
  • more carbon storage; dry peat releases carbon dioxide through oxidation. by encouraging the re-wetting of peat and active peat growth, carbon dioxide is naturally absorbed from the atmosphere and stored
  • more water storage in the upper catchments; water transfer is slowed, increasing storage capacity and ensuring a steady supply of water throughout the year
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9
Q

How were the effects of the Exmoor Mires Project measured?

A

Dipwells were installed to measure the depth of the water table

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10
Q

What were the results of the Exmoor Mires Project?

A

By 2015, over 1000ha of peat moorland had been restored

Nearly 100km of ditches had been blocked
water table raised by 2.65cm

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