Rivers Flashcards
What is the difference between the hydrological cycle and the drainage basin
- Hydrological cycle is a closed system, where water is constantly recycled
- Drainage basin is an open system
define drainage density
the number of tributaries in a drainage basin
what influences drainage density
permeability of the rocks/soil under the surface
* impermeable = water can’t infiltrate = high drainage density
* permeable = throughflow or groundwater flow = low drainage density
how does temperature affect surface run-off
high temp = increased evaporation, less surface runoff
how does precipitation affect surface runoff
- more precipitation
- more runoff
- water doesn’t have time to inflitrate
how does rock type affect surface runoff
- impermeable rocks, rapid runoff
- permeable, reduced runoff, infiltration
define channel network density
the system of surface and underground channels that collect and traansport the percipitation that falls on the drainage basin
state the 3 stores in the hydrological cycle
- atmosphere: water vapour/droplets in clouds
- land: ice sheets, glaciers, lakes, groundwater, resovoirs
- the sea
what does a river regime demonstrate
the variations in a river’s discharge throughout the year
what does a storm hydrograph represent
changes in river discharge after a storm event
what can affect a river regime
- levels of precipitation
- temperature changes throughout the year
- evapotranspiration
what is base flow
normal discharge
define peak rainfall
highest rainfall during a storm
define peak dischage
highest discharge during the storm event
define lag time
time between peak rainfall and peak discharge
what is the receeding limb
river discharge returning to normal
what is river discharge measured in
cumecs (m^3/s)
it is the river volume
what are the three main processes in shaping landforms
- erosion
- transporation
- deposition
define weathering
the breakdown of rocks in situ
how does physical weathering occur
changes in temperature
freeze-thaw and exfoliation
how does chemical weathering occur
rocks disintegrate in slightly acidic rainwater
how does biological weathering occur
rocks broken by the roots of plants
define mass movement
weathered material moves downhill because of gravity
define slumping
slope eroded by river, undercutting slope causing large-scare movement of material down
define soil creep
gravity causes weathered material to slowly move down the river
define erosion
the wearing away of material by force of water or other materials
hydraulic action
EROSION
force of water removes material from bed/banks of river
corrosion (solution)
EROSION
rocks dissolved in slightly acidic water
abrasion
EROSION
materials scrape away at banks and bed
attrition
EROSION
- like ATTRACTION
- materials hit eachother, pieces become rounder and smaller
solution
TRANSPORTATION
material dissolved
suspension
TRANSPORTATION
light material carried in the river
saltation
TRANSPORATION
material too heavy to be suspended, bounces up and down
traction
TRANSPORTATION
larger rocks roll across river bed
where is vertical erosion found, and what does it do
- upper course
- inc. river depth + valley
- river erodes DOWNWARDS
where is lateral erosion found, and what does it do
- middle and lower course
- inc. width of river + valley
define deposition
when a river no longer has enough energy to carry material
why/where does deposition occur
what causes a river to deposit material
- reduced discharge: lack of percipitatio, abstraction upstream
- decreased gradient
- slower flow on inside of river bed (meander)
- at the mouth
how is river material deposited
in order of size
- bedload: heaviest, deposited first
- alluvium: finer load, deposits last
- dissolved materials: carried out to sea
what factors affect river proccesses
- wet climate: more weathering, more mass movement, more discharge, more powerful erosion and transportation –> more load deposited downstream
- less resistant rocks weathered and eroded more rapidly
- gentler slopes means reduced river energy, deposits load
what is a long profile
changes in the river gradient from source–>mouth
characteristics of upper course
- low velocity
- large bedload
- vertical erosion
- steep valley sides, shallow channel
- rough channel bed
- most erosion
characteristics of middle course
- deeper than upper course
- gentle valley sides
- bedload size decreases
- lower friction
* lateral erosion
characteristics of the lower course
- deepest
- flat floodplains
- widest
- greatest velocity
- dominantly deposition
how are v-shaped valleys formed
UPLAND LANDFORMS
- VERTICAL EROSION dominant in upper course
- CUTS down into the river bed
- WEATHERING+MASS MOVEMENT = valley sides collapse into the river
- mass movement adds LOAD, aiding ABRASION
how are waterfalls and gorges formed
UPLAND LANDFORMS
- drop in river bed from one level to another
- hard rock overlies soft rock
- soft rock erodes quicker, undercutting hard rock, creates plunge pool
- development of an overhang of resistant rock, collapses overtime due to gravity
- waterfall retreats upstream, leaving** steep-sided gorge**
how are interlocking spurs formed
UPLAND LANDFORMS
- upper course: river starts to meander
- erosion happens on outside bend
- vertical erosion between spurs, rather than lateral erosion on them
how are meanders formed
LOWLAND LANDFORMS
- lateral erosion dominant in lower courses
- meander increases in size
- thalweg on outside of river bed = erosion
- erosion undercuts banks = river cliff
- river bank collapses, meander moves further out
- slowest flow is on the inside of bends = deposition
- deposition creates slip-off slope
- deposition on one side, erosion on other = meander migrates accross valley
how are ox-bow lakes formed
- distance downstream, meander size increases
- erosion on outer bends = meander neck
- flooding = river cuts through neck forming straighter course for water
- flow of water at entry/exit of meander is slower, meaning deposition
- meander cut off from main river channel = ox bow lake
how are flood plains and levees formed
- migration of meanders = floodplains
- high discharge can cause the river to break its banks (flooding)
- increased friction –> reduced velocity –> material deposited along floodplain –> floodplain increases in height
- heaviest material deposited nearest to the channel, forms embankments called levees
what are the percentages for global water use
70% agriculutre: irrigation/livestock
20% industry
10% domestic
what is the threshold for water stress
below 1700m^3 a year per person
what is the threshold for water scarcity
below 1000m^3 a year per person
how does agriculture affect water quality
- waste water from manure, fertilisers, herbicides, pesticides, soil erosion
- death of fish + other wildlife due to bioaccumilation
- eutrophication, poisonous
- inc. sediment, decreased oxygen levels
how does industry affect water quality
- oil spillages
- water used as coolant, returned to river at high temperatures
- toxic substances from industrial processes
- wildlife coated in oil, unable to move/eat/fly
- organisms cannot survive high temperatures
- toxins enter food chain
how does domestic use of water impact water quality
- untreated sewage
- leisure - treated with chlorine
- water used for bathing or washing clothes
- more nitrogen, more bacteria
- chemicals are harmful for wildlife
- chlorine causes chemical burn to wildlife
describe the process for cleaning water
- AERATION: removes dissolved iron and maganese
- CHLORINATION: removes biological growth
- DISINFECTION: removes bacteria
- SEDIMENTATION: removes suspended soils
- FILTRATION: removes very fine sediment
define flooding
when the capacity of the river channel is exceeded
what is hard engineering
- building of structures
- expensive to construct and maintain
what do dams and resovoirs do
HARD ENGINEERING
control amount of discharge
what do levees do
HARD ENGINEERING
increase capacity of river channel
what do straightened channels do
HARD ENGINEERING
river flows more quickly past vulnerable areas
what do flood relief channels do
HARD ENGINEERING
allow water to flow out of the main channel
what does river restoration do
SOFT ENGINEERING
restoring rivers (like straightened channels) back to their original regime
what does wetland conservation do
SOFT ENGINEERING
provide excess water area to go and slow down flow of floodwater
conserves an area of land that can get wet
what does floodplain zoning do
SOFT ENGINEERING
only certain land uses allowed on flood plains
what do flood resistant buildings typically consist of
- homes raised on stilts
- carpets replaced with tiles
- power sockets built above level of likely flood