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sources of fresh water
surface stores
aquifers, rainwater
sea water stores via desalination
artificial stores
factors affecting the siting of reservoirs
topography
geology
catchment area
water supply
existing land use
pollution risk
sedimentation
infrastructure
topography- perfect for reservoirs
a valley with a large volume and a small surface area
geology- perfect for reservoirs
the rock should be impermeable with no unstable faults, fissures or seismic activity
catchment area- perfect for reservoirs
the river that has been dammed should have a large catchment area to allow maximum water volume reaching the reservoirs
water supply- perfect for reservoirs
there should be reliable, regular rainfall and low evapotranspiration rates
existing land use- perfect for reservoirs
the land should be of low value, so therefore not used by any important land use
pollution risk- perfect for reservoirs
there should be no urban, industrial or agricultural activity within the catchment that might cause a risk of the water becoming polluted
sedimentation- perfect for reservoirs
little sediment - the water arriving in the reservoir would become clogged with sediment and the dam may become stressed
infrastructure- perfect for reservoirs
near to supplies of construction workers and materials, the reservoirs should not be too far from an area of high water demand
effects of reservoirs
sedimentation
habitats change
microclimate changes
reduced river flow
microclimate changes
local temp will change, they will be cooler in the day and warmer in the night
wind speed will be increase as friction over the water is low
wind speed will be increase as friction over the water is low
reduced river flows
rivers downstream from dams can start to dry up
water quality is often poorer in rivers downstream for example they might have reduced dissolved oxygen levels
rivers downstream will flow less which will affect nutrient levels of floodplain ecosystems
effects of over abstraction
subsidence
salinisation
reduced river flow
ecosystem changes
salinisation
in coastal areas, if the water table is lower than sea level, the sea water will enter the aquifer
The salt will make the aquifer unsuitable for irrigation, as it will kills the crops by osmotic dehydration
subsidence
Water in the interstitial spaces of the rocks helps provide structural support
Without this water, the rock particles are compacted by the weight of the material above