River Exe Case Study Flashcards
Example of a river catchment
Describe location of the River Exe
Flows for 82.7km from its source in the hills of Exmoor to the sea at Exmouth on the south coast of Devon
Physical characteristics of the River Exe
- 601km^2 area
- maximum elevation of 514m in the north
- lowest elevation of 26m in the south
Human characteristics of the River Exe (land use)
- majority of land is agricultural grassland (67%)
- some woodland (15%)
- high ground of Exmoor = moors and peatbogs (3%)
Characteristics of geology at the River Exe
- 84.4% of catchment underlain by impermeable rocks (predominantly Devonian sandstones)
Factors affecting the water balance
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
What does the storm hydrograph for the River Exe show?
- the Exe responds relatively slow to rainfall events
- after flooding discharge recedes slowly reflecting the rural nature of the lower catchment
Describe the Wimbleball reservoir and how it reduces the risk of flooding
- 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
History of the River Exe/Exmoor Mires
1960s - government subsidies paid to peatland owners to drain the land
How did the drainage ditches affect the river?
Increased the speed of water flow to the river, reducing water quality as more silt was carried downstream
What was the Exmoor Mires Project?
Aims to restore 2000ha of land back to peat bogs by blockage of drainage ditches
How does the Exmoor Mires Project benefit the area?
- 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
How were the effects of the Exmoor Mires Project measured?
Dipwells were installed to measure the depth of the water table
What were the results of the Exmoor Mires Project?
By 2015, over 1000ha of peat moorland had been restored
Nearly 100km of ditches had been blocked
water table raised by 2.65cm