RIVERS Flashcards
Hydrological Cycle
the movement of water within a drainage basin
Infiltration
Water moving from surface to soil
Throughflow
– downhill transfer of water through the soil layer to the river
Percolation
deep transfer of water through permeable rocks
Base/groundwater flow
very slow transfer of water through rocks
Depression Storage
when water is temporarily stored on the ground in the form of puddles
Interception
vegetation which absorbs and slows down water transfer
Confluence
Where 2 rivers meet
Water budget
Shows changes in water balance over the year
Recharge
When precipitation exceeds potential evapotranspiration, but soil is yet to reach its field capacity
Surplus
precipitation exceeds potential evapotranspiration and soils reach full field capacity, creating run-off
Utilization
when potential evapotranspiration exceeds precipitation but soil storage is yet to reach 0
Deficit
When soil storage reaches 0
4 zones of the water budget
Recharge, surplus, utilizations, deficit
How does basin size effect water transfer?
Small basin – rapid water transfer
How does Drainage density effect water transfer?
High density speeds up transfer
How does land use effect water transfer?
Urbanisation encourages rapid water transfer Interception
How does relief effect water transfer?
Steep slopes lead to water with a higher velocity
How does soil moisture effect water transfer?
Saturated soils lead to rapid overland flow
Abrasion
grinding effect on the bed as eroded rock particles scour the banks
Hydraulic action
Action force of the water
Cavitation
Tiny bubbles of air implode in cracks of the river bed
Attrition
when rock particles hit each other, smoothening edges – explaining why particles downstream are more likely to be smaller and rounder
4 types of river transportation
Solution, suspension, Bedload : (saltation) and (traction)
Solution
dissolve – e.g. calcium carbonate from limestone
Suspension
carried within the main body of the river – fine grained mud
Saltation
series of small bounces – small stones
Traction
larger stones and rocks which roll along the river bed.
3 types of weathering
Mechanical, chemical, biological
Chemical weathering
weathering- chemical changes in the rock – carbonic acid in rain, combining with limestone to create soluble calcium bicarbonate
Biological Weathering
tree roots opening up rocks and releasing acids
Hjulstrom curve
shows the relation ship between velocity of river
Flocculate
Very small particle sticking together because of electric bonding
What 6 things increase downstream? Schumm Model
- Velocity 2.Discharge 3.Amount of load 4.CSA 5.Hydraulic Radius 6.Wetted Perimeter
What 5 things decrease downstream? Schumm Model
1.Turbelence 2.Friction 3.Gradient 4.Size of Load 5.Channel Roughness
Vertical Erosion
removal of material by cutting into rock by rivers
Lateral Erosion
general erosion or removal of surface material.
Sinuous channel
meandering
Eyot
island within a river cause by deposition
Hydraulic radius
Measure of efficiency of a channel = CSA/ wetted perimeter, the higher this number the more efficient the river is
rapids
Ridges of hard and soft rock create turbulent white water
gorge
Sudden drop forms when the overhang of a waterfall collapses
potholes
Circular depressions which are formed when rock fragments are drilled into holes and cavities creating turbulent whisky corrosion and therefore potholes
waterfalls
Created when there is isostatic change so water fly’s off the cliff forming a plunge pool and an overhang
Helicoidal flow
the flow is like a corkscrew spiralling - in a meander
Wide floodplain
Area around the river that is covered during a flood - very fertile
Bankfill discharge
Discharge measured when the river is at bankfill stage
Bankfull stage
Completely full river any more will burst the bank
Physical causes of flooding
- impermeable rock - steep slopes -snowmelt -drainage density -intense and prolonged rainfall make the ground saturated
Human causes of flooding
- building construction creates impermeable surface - deforestation - agriculture- if ploughed downhill - #bad - ineffective flood management and warning
Human factors of Cumbria nov/09
Cockermouth is situated at a confluence
Physical factors of Cumbria nov/09
-record breaking rainfall - hot air from south Atlantic -steep slopes Impermeable rock
Economic impact of Cumbria nov/09
-£100 million damage - death to livestock -agricultural machinery and buildings ruined - local businesses had to shut
Social impact of Cumbria nov/09
1300 people with flooded homes Communities cut off by flooded bridges
Responses to Cumbria nov/09
Immediate response-RAF helicopters and rescue boats saved 200 people Buildings were assessed to check whether it was save to let people back in them Network rail built a new station to connect each side of Workington The army built temporary footbridges In Cockermouth, businesses were offered temporary trading accommodation in the town centre
Human factors of Philippines Sept/09
- government were unable to predict its magnitude - torrential rain in manila on impermeable rock and a drainage system which is not advanced enough - deforestation on the neighbouring hills
Physical factors of Philippines Sept/09
-intense typhoon Ketsana -height of rainy season so the soils were already saturated -340mm in 6 hours
Economic impacts of Philippines Sept/09
Homes and businesses destroyed - $100 million damage Airport was closed for a day 3% of the countries farmland was destroyed
Social impact of Philippines Sept/09
250 killed 60000 lost homes Power shut off in areas Mental distress
Environmental impacts of Philippines Sept/09
Thick mud on roads 100,000 litres of oil leaked from factory Landslides affecting farms
Response to Philippines Sept/09
Immediate – 1000 soldiers were deployed, red cross provided rubber boats – social networking sites showed where people were and what they needed Clean-up operation took many weeks – Philippines government welcomed support from the UN and other NGO’s
Hard engineering options
Dams Reservoirs River straightening Levees and embankments Bypass channels
Hard engineering options - Dams and reservoirs
regulate river flow YEP Recreation expensive
Hard engineering options - river straightening
Increases velocity More problems downstream channelization
channelization
lining the banks with concrete to improve rate of flow
Soft engineering options
afforestation Establishing wetlands Riverbank conservation Land-use management
Soft engineering options- riverbank conservation
Plantation of bushes and vegetation on banks to hold soil together for less erosion