abrasion (sandpaper action)
material carried in the river scrapes and wears away at the river bed, causing the river to widen and deepen
attrition
rocks in the flow of the water knock against each other, causing rounder and smaller loads
biological weathering
roots of plants grow in the cracks of a rock and splits it
characteristics of middle course river land forms
less vertical erosion; more lateral erosion
deeper wider
deposition at inside band
characteristics of upper course river land forms
narrow and shallow
vertical erosion
chemical weathering
weathering by acid rain, causing decay
cons of channelisation
alters ecosystem
flood downstream
cons of dams
expensive
destructions
traps sediment > dam failure
cons of levees
expensive
breaching
creeping
soil moves slowly
deposition
deposition occurs when the river doesn't have enough energy to carry the material any further
drainage basin
an area of land drained by a river and its tributaries
environmental effects of flooding
loss of wildlife
land slides
destroy vegtation
spread pollutants
erosion
wearing away and removal of rocks by the action of water wind or ice
factors affecting the amount of discharge
size of basin
vegetation
rainfall
land saturation
steepness
human land use (urbanisation)
factors affecting the speed of river discharge
rock type
human land use
relief
external climate
factors effecting deposition
reduction of gradient reduction in volume of water increasing friction from bed and banks
features of a drainage basin
main channel
confluence
tributaries
watershed
estuary
source
features of a waterfall
> cap rock > overhang > less resistant rock > scree > plunge pool > gorge
flooding effects on humans
outbreak of waterborne diseases
injuries, deaths
loss of properties
destroy infrastructures
contamination
expensive rebuilding
groundwater flow
flow of water at the aquifer until it reaches the river
hard managements for flooding
dams
levees
channelisation
floor barriers
HIC water usage
70% agricultural 20% industrial 10% domestic
human causes of flooding
urbanisation
deforestation
agriculture
soil erosion
climate change
hydraulic action
water is forced into cracks in the bed and pressure expands the cracks further
hydrological cycle
the global circulation of water between the atmosphere, lidosphere, biosphere and hydrosphere
hydrological cycle order
> precipitation > interception > stem flow/drip tip > surfacae runoff > infiltration > through flow > percolation > groundwater flow > evapotranspiration > condensation
Infiltration/Percolation
Downward movement of water through soil rock due to gravity.
mass movement
the bulk movement of substance due to gravitational pull
middle course river land forms
meander
levees
oxbow lakes
natural causes of flooding
prolonged period of intense rainfall
rapid snowmelt
impermeable rock
steep relief > lower course flooding
vegetation
physical weathering
caused by temperature or climate changes
precipitation
Any form of water that falls from clouds and reaches Earth's surface.
pros of channelisation
increase velocity and reduce friction
pros of dams
prevent flooding downstream
multi purpose
pros of levees
can still use flood plain
River Processes
erosion, transportation, deposition
rockfall
big material falling fast
saltation
small material bounces in small hops along the river bed
slamping
material slides along bedding planes
soft engineering for flooding
land use planning
afforestation
Solution
river water reacts with alkaline in the bed and banks dissolving them
solution
soluble material dissolved in river water and transported downstream
suspension
fine loads being carried along by the river flow
Three Gorges Dams cons
flooded 13 cities, 140 towns, 1350 villages
1.4 million people relocated
temples and monuments destroyed
polluted by industrial wastes
3000 earthquakes since building of dam
loss of wildlife; Yangtze Dolphins
expensive $131.3 million
Three Gorges Dams facts
2009
Yangtze River
185 km high
2 km wide
600 km far; ShangHai to ChongQing
reduced flooding risk
Three Gorges Dams pros
6% of China's energy
flood control for WuHan
irrigation
navigation
tourism
through flow
the flow of water between ground surface and the top of ground water store, moves slowly under the influence of gravity until it reaches a body of water
traction
heavy material is rolled along the river bed
transportation
the movement of material downstream. The bigger the material the more energy the river needs to carry it
Types of mass movement
rockfall, slamping, creeping
types of transport
traction, solution, suspension, saltation
types of weathering
physical, chemical, biological
upper course river land forms
> V-shaped valleys > interlocking spurs > waterfalls and gorges
virtual water
Water that is not directly consumed but is used to produce food and other products.
Water management
collection
purification
delivery
Water pollution from farms
fertiliser leaching eutrophication increased bacteria growth and deoxygenation
Water pollution from industries
chemical run-off
oil spillage
factory wastes
offshore dumping of sewage sludge
Water pollution from other sources±§§§§
domestic untreated sewage
chlorinated swimming pools
Water purification methods
filtration and sedimentation
bacterial disinfection
microorganisms: chlorination
minerals: aeration
weathering
the breaking down or dissolving of rocks in situ