1.1 The drainage basin system Flashcards

1
Q

What are the different outputs?

A

evaporation
evapotranspiration
channel flow

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2
Q

What affects evaporation?

A

Meteorological factors:
temperature, humidity and windspeed
- other factors e.g amount of water available, vegetation cover and colour of the surface (albedo or reflectivity of surface)

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3
Q

What is evapotranspiration?

A
  • combined effects of evaporation and transpiration
  • evaporation = when water heated by the sun, so becomes a gas and rise into atmosphere
  • transpiration : occurs in plants when they respire through their leaves. releasing water they absorb through their roots, which then evaporates
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4
Q

What is P.EVT?

A

Potential evapotranspiration
- main difference between actual evapotranspiration is moisture availability
- P.EVT is water loss which would occur with unlimited supply of water in the soil for use by the vegetation

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5
Q

What is river discharge?

A
  • volume of water passing through a cross sectional point of the river at any one point in time
  • unit = cubic metres per second (Cumecs)
  • water leaves the basin through streams which drain basin
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5
Q

What are the 5 stores?

A

Interception
Soil Water : upper levels of soil
Surface water
Groundwater : in pore spaces of rock
Channel storage

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6
Q

What is interception?

A
  • water caught/stored by vegetation
    3 main components:
    canopy interception - water caught by leaves/branches of trees
    stemflow - water that runs down the stems/trunks of plants
    litter interception - water trapped by the leaf litter and other organic debris on the forest floor
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7
Q

What causes interception loss to vary?

A
  • surface area: less from grasses than deciduous woodland due to smaller surface area of grass shoots
  • density: agricultaral crops interception increases with crop density
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8
Q

What is soil water?

A
  • water stored in upper levels of soil and utilised by plants
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9
Q

What factors affect soil water store?

A
  • soil depth
  • land use management (heavy machinery destroy soil structure)
  • soil texture (sand, silt or clay)
  • soil structure (large or small pores)
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10
Q

What is it and what factors affect surface storage?

A

water stored in puddles, ponds, lakes etc
- precipitation type
- aquilude - rock cannot hold water
- precipitation duration
- rock permeability
- flat land
- soil texture
- precipitation intensity

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11
Q

What is groundwater and what affects it?

A

water stored in pore spaces of rock or lower soil
- aquifers (water bearing rocks)
- rock permeability (permeable rocks = more underground storage)
- soil depth
- land use management
- soil structure (large or small pores)
- time of year

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12
Q

What is channel storage and what factors affect it?

A

water stored in a river’s channel
- flat land (relief)
- impermeable rocks
- some channels are underground
- abstraction by humans
- rock type

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13
Q

What are the different types of above ground flows?

A

throughfall
stemflow
overland flow
channel flow

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14
Q

What are the 5 different types of below ground flows?

A

infiltration
percolation
throughflow
groundwater
baseflow

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15
Q

What is throughfall flow?

A
  • water flows from leaves/foliage onto ground
  • prominent in areas with large canopy that receives lots of rainfall e.g rainforest
  • but will occur whenever precipitation falls onto plants/trees
16
Q

What is stem flow?

A

intercepted water stored on plants and trees flows down a stem onto the ground

17
Q

What is overland flow?

A

water flows above ground as sheetflow (lots of water flowing over large area) or on rills (small channels unlikely to carry water when no rainfall)
- will occur when water cannot infiltrate the soil

18
Q

What is channel flow?

A
  • water that moves through established channels (e.g streams/rivers)
  • led by 2 sources: overland flow and groundwater flow
19
Q

What is infiltration and what affects it?

A
  • movement of water from above ground into soil
  • permeability of soil
  • rate of precipitation
  • relief
  • saturation levels of soil
20
Q

What is percolation?

A

slow vertical movement of water into permeable rocks

21
Q

What is through flow?

A
  • through soil that is not saturated and vertically
22
Q

What is groundwater flow?

A

slow horizontal movement of water under the surface through saturated ground

23
Q

What is baseflow?

A
  • portion of streamflow that comes from groundwater seeping into a river or stream
  • no contribution from precipitation
24
Q

What are aquifers?

A
  • underground water stores
  • permeable rocks such as sandstone and limestones
  • full body of groundwater
25
Q

What is the water table?

A
  • level at which the pore spaces and fractures in the ground become saturated
  • above water table is unsaturated soil and below water table is saturated soil
26
Q

What happens if the surface dips below the water table?

A
  • groundwater will fill the surface space to become surface water
  • if surface water dries up, groundwater will continue to replenish area underneath water table
  • water table can rise/fall and surface water will rise/fall accordingly
27
Q

What causes groundwater recharge?

A
  • infiltration of precipitation until it reaches groundwater
  • seepage through banks and bed of surface water such as rivers
  • groundwater leakage and inflow from adjacent rocks and aquifers
  • artificial recharge from irrigation, reservoirs etc
28
Q

What causes losses of groundwater?

A
  • Evapotranspiration:
  • natural discharge by seepage into surface water bodies
  • groundwater leakage and outflow into adjacent aquifers
  • artificial abstraction
29
Q

What is a spring and how do they form?

A
  • they form when groundwater that is stored underground finds a way to reach the surface
  • it can happen when there’s a crack or opening in the Earth’s surface, allowing the water to flow out and form a spring