glaciated landscapes- SWITZERLAND DAM CASE STUDY (glaciated landscape)

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The human activity taking place and the reasons for it taking place such as dam construction

Grande Dixence Scheme-Val des Dix Switzerland

  • highest gravity dam in the world, constructed between 1950-61. Recent update 2010

  • Lengthy construction process due to inaccessibility of site and severe working conditions (glaciated landscape)- construction only took place in summer.

  • Cost 1600mil Swiss Francs (£1300mil)

  • Fed by 35 glaciers, fed by meltwater—> more in summer when there is greater ablation

  • Gravity holds dam to ground- stops sheer weight of water from pushing dam over

  • Stores over 400million m3 water a year

  • 285m high

  • Construction materials for the dam obtained locally from moraine deposits in adjacent valleys

  • 95% of Swiss energy comes from renewable energy

  • Water behind Grande Dixence dam drives turbines in 4 power stations

  • Enough energy to power 400,000 Swiss households

  • Stores glacial meltwater during summer- optimise water level, generates electricity during high demand winter

  • KE and GPE are energy involved

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Impacts on processes and flows of material, processes and/or energy through glacial system such as trapping of sediment

Energy

  • water drives turbines in 4 power stations

  • GPE and KE

  • 1/3 of Swiss energy comes from storage power stations

  • 85% of water used for electricity generation

  • Trapping of sediment in dam- lake above dam is stagnant. Lots of sediment that doesn’t flow through. This is because there isn’t much energy behind the dam. Therefore we use the other 15% of the water to flush the sediment through so there isn’t a backlog of sediment.

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Effect of impacts in changing glacial landforms such as increased channel scour below dams

  • environmental impact minimise- keep aesthetics of area for tourists.

  • Pumping stations + power plants built underground, well concealed to retain aesthetics

  • However reduced flow in Borgne River- tributary of the Rhone, below the dam has resulted in higher concentrations of pollutants at Les Haydee from agricultural and domestic sources

  • When sediment gets trapped upstream, leading to "hungry water" with more erosive power downstream, causing bed degradation and habitat loss

Impact on glacial system:

  • 85% of water in the dam used for electricity generation.

  • 15% used to deal with problems of sedimentation. When water is stored behind the dam the lack of flow means a loss in energy and the deposition of the sediment load behind the dam at rates of 20-40cm/yr. sediment concentrations are >300mg/l above the dam, <20mg/l downstream of the dam.

  • To solve problem, some water in reservoir used to purge sediment- flushing it out and moving it downstream. Water at these times has high levels of turbidity and sediment concentrations of up to 20,000mg/l

Channel scour (erosion)

  • no sediment downstream, water has lots of kinetic energy and lots of erosive potential, however not a lot of water supply in the long term and despite the fact that the river has a lot of energy, it can’t erode because there is so little water left below the dam. Channels dry up and constrict

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Consequences of these changes on landscape such as changes to valley floor

Impact on river channels

  • trapping of sediment behind dam—> clear water returned into natural river channels below power stations

  • Excess energy, none used to transport sediments—> more channel erosion

  • But lack of discharge in below-dam rivers means some almost dry up in the summer. River channels also contract, scale of contraction increases with distance away from the dam

  • Amount of sediment eventually flowing into Lake Geneva halved since dam construction

  • Val d’Herens, risk of flooding when excess water stored must be released- hindered tourist use and development along valley floor

The future:

  • climate change producing more glacial melting in Swiss Alps- meltwater available to create hydropower increasing. Eventually glaciers will have shrunk to much that meltwater supply may diminish- altering sediment supply and transportation even more