Mindmap
Geography - Rivers_1

Inhalt der Mindmap
Geography - Rivers_1
How easily can a drainage basin be impacted?
- Human impacts on the hydrological cycle
- CO2 emissions
- It interrupts the rainfall patterns, this leads to more evaporation
- Dams
- Stops the flow of water so it builds up and then floods
- Chemicals
- Polluting the water which can cause animals and humans to die
- Ubranisation
- Building roads and buildings means less infiltration and more surface run-off causing flooding
- Overabstraction of groundwater
- This can lead to desertifacation as there isn't any water
- Desforestation
- There is less interception which causes more surface run-off and leading to flooding
- CO2 emissions
- Stormhydrographs
- Lag time
- This is the delay between peak rainfall and peak discharge
- Rising limb
- This is the part of the graph up to peak discharge
- Peak discharge
- This is the highest point on the graph, when the river discharge is at its greatest
- Falling limb
- This is part of the graph after peak discharge
- Lag time
- The system theory
- Geographers use an aspect of the system theory as a way of explaining how natural phenomenas function
- Open system
- Inputs and outputs of both energy and matter e.g. most environmental systems e.g. the hydrological cycle
- Closed system
- Input transfer and output of energy but not of matter or mass e.g. the planet
- Isolated system
- No imput or output of energy or matter (the universe)
- Key words
- Percolation
- It is water seeping down through the soil into the water table
- Evapotranspiration
- It is the process of evaporation and transpiration
- Percolation
- Water balance
- Water balance is worked out from inputs (precipitation) and output (channel discharge and evapotranspiration)
- The water balance affects how much water is stored in the basin
- General water balance in the UK
- In wet seasons, precipitation exceeds evapotranspiration. This creates a water surplus
- The ground stores fill with water so there's more surface runoff and higher discharge, so river levels rise
- In drier seasons, precipitation is lower than evapotranspiration. Ground stores are depleted as some water is used and some flows into the river channel, but isn't replaced by precipitation
- So, at the end of the dry season, there's a deflicit (shortage) of water in the ground. The ground stores are recharged in the next wet season (i.e. autumn)
- In wet seasons, precipitation exceeds evapotranspiration. This creates a water surplus
- Water balance is worked out from inputs (precipitation) and output (channel discharge and evapotranspiration)
- Human impacts on the hydrological cycle
How do rivers and valleys change downstream?
- Erosion
- Hydraulic action
- The pressure of the water breaks the particles from the river bedand banks. Water pushes into the cracks, air becomes compressed and the bank collapses
- Corrasion
- The sediment carried by a river scours the bed and banks, this causes pebbles to spin around and turn into potholes
- Attrition
- Eroded rocks collide and break into smaller fragements, the edges become smooth and rounded
- Corrosion
- CO2 dissolves in the river to form a weak acid, this dissolves the rock
- Hydraulic action
- Transportation
- Suspension
- The materials are made up of very fine particles, that are lifted as a result of turbulance and transported by the river
- Solution
- When material is dissolved and carried by the river
- Saltation
- When material is too heavy to be carried in suspension it is bounced along the river by the force of the river
- Traction
- When large materials are rolled and pushed along the river bed by the force of the river
- Suspension
- What influences velocity
- Channel shape
- Roughness of the channel bed
- Banks of the river
- Channel slope/gradient
- Hydraulic radius
- The ratio between the cross sectional area and the length of the wetted perimter
- This measures the efficiency of the river at moving water
- Compentence
- Is the maxium size of load a river is capable of transporting
- Capacity
- Refers to the total volume of sediment a river can transport
- What factors affect capacity and competence?
- Velocity
- Long profile
- Thalweg
- Lowest line of elevation in the river valley
- Hjulstrom Curve
- This graph represents the realtionship between erosion, transportation and deposition of sediment.
- Erosion
Do all rivers look the same?
- Deltas
- Birds foot
- Spread over a wide area with many 'distributaries' extending out to sea
- E.G Mississippi
- Spread over a wide area with many 'distributaries' extending out to sea
- Accurate
- Rounded convex edges
- E.G. the Nile
- Rounded convex edges
- Cuspate
- Material evenly spread across the river
- Factors that affect the formation of deltas
- How rough the sea is
- Volume of water
- Changes in the coast level
- How much sand has been eroded away
- Positives of humans living near deltas
- Fertile land
- Good fishing grounds
- Negatives of humans living near deltas
- Unconsolidated sediments
- Unstable grounds
- Birds foot
- Estuary
- It is where fresh water and salt water meet/interact
- Rejuvenation
- Over long periods of time large changes in sea level can drastically alter the rivers potential energy and can increase the chances of vertical erosion
- Isostatic sea level changes
- Isostatic changes are local changes where the height of the land changes relative to the global sea level
- When ice goes in warmer periods the land rebounds upwards (Scotland) - rising relative to the level of the sea
- This process is also seen in deltas where sediment loading depresses the Earths surface
- Eustatic sea level changes
- Eustatic sea level change is a global change in sea level, linked directly to the temperature of the Earth
- In warmer periods there is less ice and the water is warmer, so expands and sea level rises
- In colder periods the ocean water is colder so contracts and sea level falls
- Keywords
- Incised meanders
- If a rejuvenated river occupies a valley with well-developed meanders, renewed energy results in them becoming incised or deepend
- Knickpoints
- A location of a river, where there is a sharp change in channel slope, such as a waterfall or lake
- River terraces
- A rejuvenating river can erode vertically into the former flood plain to produce river terraces
- Incised meanders
- Deltas
Erosional fluvial features
- Floodplains
- An area of low-lying ground adjacent to a river, formed mainly of river sediments and subject to flooding
- They are meant to flood but so many people build their houses on them because there isn't any room
- Levees
- It is an embankment built to prevent overflow of a river
- Levees help communities to reduce the risk of flooding
- Braiding
- A braided river is a river that had multiple channels and islands of sediment in between those channels
- Deltas
- Deltas are depositional landforms, they are created by loading of sediment onto the land as the river can't carry it anymore
- Waterfalls
- Waterfalls often form in the upper stages of a river where it flows over different bands of rock. It erodes soft rock more quickly than hard rock and this may lead to the creation of a waterfall. Formation of a waterfall: The soft rock erodes more quickly, undercutting the hard rock
- Floodplains
Flood management strategies
- Naturalisation
- Pros
- It helps old rivers, that have many meanders to reach their destination quicker, this speeds it up
- It makes more area for farmland, this is because the river isn't bending on their land
- Is an attempt to restore the river to a state closer to their original course by removing structures such as hard engineering.
- This works because it allows it to flood but the ground works like a sponge and soaks up the water, so when it reaches the main course it has reduced the risk of flooding
- Cons
- It creates less deposition so silt and other materials won't be dropped. This means that the ground/soil isn't fertile
- It isn't natural at all. This could be pointless as it destroys animals habitats and even kills off species of vegetation
- Pros
- Channelisation
- An attempt to modify a channel so that it is more efficient when transporting the water to minimise flooding. It uses concrete lining in effort to control stream erosion
- Pros
- It will create a more wild friendly environment, also by putting the wooden fencing up to make it more sustainable
- It means less flooding as the ground would act as a sponge so no excess water cause flooding
- Cons
- Most areas around the river are used for commercial, residential and/or transport. This means it would be very costly to move and knock down
- Re-locating can cause so much stress and may end up with rebelling the authorities
- Naturalisation
Case studies
- Carlisle Floods, January 2005
- Short term impacts
- Flood related injuries
- Communications were affected
- Roads unstable
- Businesses had stock damage
- Schools, hospitals and police stations were cut off
- Long term impacts
- Houses destroyed by flood water - needs rebuilding
- Businesses lost trade
- Families homeless
- Firms shut down or relocated
- Intangible impacts
- Sense of loss
- Anxiety - it may happen again
- Carlisle flood defences
- Afforestation
- Increases incerecption
- Dams
- Reduces overflow of the river banks
- No more flood plain building
- Adapt housing
- On stilts
- Straighten meanders
- Deepen the river
- More volume of water can be held
- Afforestation
- Carlisle chose to do nothing about the floods that they had. They didn't get any money from the Government which made it hard to put flood defences in.
- However they gave money to those who live near to the river's banks, so they could place things like embankments
- Short term impacts
- Bangladesh 2007
- Short term impacts
- Polluted water
- Cattle and agriculture lost
- Fertile silt deposited on the flood plains
- Long term impacts
- Country in debt
- Education would be stopped
- Lack of clean water
- Diseases
- Businesses shutdown - more unemployment
- Causes - Humans
- Deforestation
- Nepal
- Growth of urban areas to migration
- Collapse of old earth dams
- Pradesh, India
- Deforestation
- Causes - Natural
- Monsoon came after a very dry summer
- Heavy rainfall - 24 hours
- The ground was saturated
- Peak discharges of river Ganges and Brahmaputa
- Flood defences
- They don't have any
- However they wanted to have embankments near to the river
- They don't have any
- Short term impacts
- Carlisle Floods, January 2005
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- Mindmap am Geography - Rivers_1, erstellt von amzbraun am 16/04/2015.
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- amzbraun
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- Erstellt von Charlotte Mayo · 16 Apr 2015
- Kopiert von amzbraun · 16 Apr 2015
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