River Exe Flashcards
Location?
Starts on Exmoor in Somerset and flows south for 60 miles, reaching the sea on the south coast of Devon.
Area?
600 km^2
Max elevation?
515m in the north
Min elevation?
26m in the south
Geology?
84.4% impermeable rocks such as Devonian sandstone
Composition of land use?
67% agricultural grasslands, 15% woodland, 3% peat bogs and 15% other (mainly arable farmland)
Water balance equation?
Precipitation(1295mm) = Evaporation +/- Soil water storage(451mm) + Runoff(844mm)
Why is runoff unusually high?
High rainfall is normally absorbed by the peaty moorlands, however, the drainage ditches and impermeable geology has resulted in high runoff.
What is the Wimbleball Reservoir?
Its a reservoir with an area of 150 hectares that was created when the river Haddeo was dammed in 1979.
What does the Wimbleball Reservoir do?
It supplies water to Exeter and parts of East Devon, whilst regulating water flow all year.
How does the Wimbleball Reservoir prevent flooding and droughts?
It regulates water flow and levels within the reservoir which helps minimise peaks and troughs in hydrographs, reducing the risk of floods and droughts.
What are drainage ditches and why have they been built?
They are deep trenches carved into the hillside to drain the water that has been absorbed by the peat bogs, allowing the land to be used for farming.
It has also been dug to be used as a biofuel and to heat homes.
What are the negative impacts of drainage ditches on the water cycle?
Increased speed of water flow into the river Exe, increasing likelihood of flooding and soil erosion, resulting in more silt in the river which lowers water quality.
What are the negative impacts of drainage ditches on the carbon cycle?
As peat bogs dry out due to lack of moisture, decomposition occurs releasing carbon in the form of CO2 and Methane.
How does the Exmoor Mires project work?
By blocking drainage ditches with peat blocks or moorland bales, water is retained in the peat and the ground returns to its natural moorland environment.
This helps to reduce the flow of water into river channels and allows the peat to store more carbon.