River Exe case study
- Created by: roseb00d
- Created on: 01-05-23 19:07
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- River Exe -case study
- location
- the source is at exehead in south west somerset
- the mouth is in exmouth devon
- the towns Exmouth and Tiverton are on the river
- the river is more than 5 miles long
- two major tributaries of the river -river elyst and creedy
- prominently in devon
- the river catchment
- the exmoor national park at the source of the river has an higher elevation
- the land is mostly low permeability with areas of moderate permeability
- the areas of moderate permeability are have either a fissure or intergranular rock formations
- higher levels of precipitation recorded near the source of the river than near the mouth
- water balance
- high levels of precipitation
- large amount of the precipitation is absorbed by the peaty moorland soils of the exmoor mires
- run-off accounts for 65% of the water balance due to the impermeable nature of the bedrock and the drainage basin ditches on exmoor
- reservoir (wimbleball lake)
- completed in 1979
- on a tributary of the river Exe (river haddeo)
- contains 374 acres of water
- reduced the water down stream
- the exmoor mire project
- in 2010 research was funded to understand how the southwest peat land was structures and functioned
- peat bogs are essential water and carbon stores
- they provide essential services to the ecosystem including
- in 2011 it was identified that peat bogs were the most important terrestial carbon store
- peat bogs are essential water and carbon stores
- the project aims to restore and rejuvenate the exmoor mires
- Cost: £4.5 million (2010 to 2020) to restore 3,000ha of peatland, with 1,400ha achieved by December 2016.
- A rise in the water table level of 2.65cm on average across the areas monitored and up to 21cm in some deeper peat locations
- By blocking up drainage ditches, the aim is to enhance water storage, improve water quality and facilitate a rise in water table levels, which will allow the peat to accumulate quicker and store more carbon.
- the peat land had become degraded due to :
- peat extraction
- over-grazing
- burning
- disturbance from military use
- climate change
- nutrient decomposition
- in 2010 research was funded to understand how the southwest peat land was structures and functioned
- location
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