1.1 The drainage basin system Flashcards

1
Q

Explain what a drainage basin is:

A
  • It is the area that is drained by a river and any tributaries
  • It can be classified as a natural system
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2
Q

Explain what the outputs of a drainage basin system are:

A
  • Outputs are where matter or energy leaves the system
  • Examples include: evaporation, evapotranspiration and river discharge
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3
Q

Explain what the stores of a drainage basin system are

A
  • Stores are where matter or energy builds up and is stored in the system
  • Examples include: interception, soil water, surface water, ground water and channel storage
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4
Q

Explain what the flows above ground of a drainage basin system are

A
  • Flows are where matter or energy moves in the system
  • Examples include: throughfall, stemflow, overland flow, and channel flow
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5
Q

Explain what the flows below ground of a drainage basin system are

A
  • Flows are where matter or energy moves in the system
  • Examples include: infiltration, percolation, throughflow, groundwater and baseflow
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6
Q

Explain the output: evaporation

A
  • The change in state of water from liquid to gas
  • Evaporation occurs in the drainage basin system when water is heated by solar energy, causing it to evaporate into a gas and rise into the atmosphere
  • Water is leaving the system here, which is why evaporation is an output.
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7
Q

Explain the output: evapotranspiration

A
  • Compromised of evaporation and transpiration
  • Evaporation occurs when water is heated by the sun, causing it to become a gas and rise into the atmosphere
  • Transpiration occurs in plants when they respire through their leaves, releasing water they absorb through their roots, which then evaporates due to heating by the sun.
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8
Q

Explain the output: river discharge

A
  • The volume of water passing through a cross-sectional point of the river at any one point in time, measured in Cubic Metres Per Second (Cumecs)
  • Water leaves the basin through streams which drain the basin. These may flow as tributaries into other rivers or directly into lakes and oceans.
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9
Q

Explain the stores: interception

A
  • Water (e.g. precipitation) that is intercepted by plants’ branches and leaves before reaching the ground
  • This water is stored short-term.
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10
Q

Explain the stores: soil water

A
  • Water that is stored in the upper levels of the soil, which is utilised by plants.
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11
Q

Explain the stores: surface water

A
  • Water stored in puddles, ponds, lakes etc.
  • Dependent on the size of these stores, they can last from hours to millions of years.
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12
Q

Explain the stores: groundwater

A
  • Water that is stored in the pore spaces of rock or lower soil.
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13
Q

Explain the stores: channel storage

A
  • Water that is stored in a river’s channel.
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14
Q

Explain the above ground flows: throughfall

A
  • Water flows from leaves and foliage onto the ground
  • This is especially prominent in areas with a large canopy that receives a lot of rainfall, like a rainforest, but will occur whenever precipitation falls onto plants and trees.
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15
Q

Explain the above ground flows: stemflow

A
  • Intercepted water stored on plants and trees flows down a stem onto the ground.
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15
Q

Explain the above ground flows: overland flow

A

Water flows above the ground as:
* Sheetflow (lots of water flowing over a large area)
* Rills (small channels similar to streams, that are unlikely to carry water during periods where there is no rainfall)
* Overland flow will occur when water cannot infiltrate the soil.

16
Q

Explain the above ground flows: channel flow

A
  • Water that moves through established channels, like streams or rivers
  • Naturally, channel flow is fed by two sources: overland flow (i.e. precipitation that flows over the ground, rather than infiltrates the soil), and groundwater flow (groundwater flow contributes to channel flow where a channel intersects the water table).
17
Q

Explain the below ground flows: infiltration

A

The movement of water from above ground into the soil. Infiltration is affected by multiple factors, including:
* Permeability of soil
* Relief
* Rate of precipitation
* Saturation levels in soil

17
Q

Explain the below ground flows: percolation

A
  • Water flows from the ground or soil into porous rock or rock fractures
  • The percolation rate is dependent on the fractures that may be present in the rock and the permeability of the rock.
18
Q

Explain the below ground flows: throughflow

A
  • Water flows through the soil and into streams or rivers
  • Speed of flow is dependent on the type of soil, e.g. clay soils will have a slower flow rate than sandy soils.
19
Q

Explain the below ground flows: groundwater flow

A
  • Water flows through permeable rocks, below the water table, and may also flow as springs
  • Groundwater maintains water levels elsewhere
20
Q

Explain the below ground flows: baseflow

A
  • The baseflow is the level of channel flow when there is no overland flow, (i.e. when no precipitation has fallen)
  • This means baseflow is made up of any groundwater that contributes to channel flow (refer back to the two sources of channel flow: overland flow and groundwater flow - baseflow is the level where there is no precipitation contribution, hence only groundwater flow is contributing to the channel flow).
    In short, baseflow is the ‘normal’ or base level of water in a river, when there is no contribution from precipitation.
21
Q

Explain what groundwater is and what percentage of earths water it takes up:

A
  • Groundwater is classified as any water underground, meaning it can be held in soils or in between rock spaces
  • Underground water makes up a large amount of the Earth’s water stores, in fact it accounts for around 30% of all the Earth’s freshwater.
22
Q

Explain what a water table is:

A
  • The water table is the level at which the pore spaces and fractures in the ground become saturated, meaning above the water table is unsaturated soil, and below the water table is saturated soil.
23
Q

Explain what will happen if the surface dips below the water table:

A
  • Groundwater will fill the surface space to become surface water.
24
Q

Explain what recharge is:

A
  • When groundwater levels deplete (by human extraction, or by groundwater replenishing surface water levels) groundwater can be recharged.
25
Q

Explain why groundwater levels fall:

A
  • Groundwater levels fall when groundwater is being used more
  • For example, in hotter temperatures, there is less rainfall (summer), so more surface water bodies are drying up and therefore groundwater will somewhat replenish these stores
  • When groundwater is utilised, this can cause the water table to fall, as there is no water replenishing the used groundwater.
26
Q

What is ground water recharged by:

A
  • Precipitation infiltrating the ground until it reaches groundwater. When precipitation is
    higher, and evaporation is lower, such as in winter, groundwater levels will be recharged
  • Surface water bodies (such as lakes and rivers) seeping into groundwater stores.
27
Q

Explain how the type of precipitation effects groundwater recharge

A

In storm events, large amounts of rainfall quickly saturates the ground to its field capacity (no more water can infiltrate the soil) increasing overland flow. Storm events are therefore less effective at recharging water stores than prolonged rainfall.
* If 20mm of rain fell evenly over the course of 24 hours, this would infiltrate the soil and percolate into the groundwater stores as well, with low overland flow
* In 1 hour, if 20mm of rain fell, there would be less water infiltrating the soil and percolating into the rocks, reducing the replenishment of groundwater stores, but increasing overland flow.

28
Q

What is a spring

A
  • A natural outlet of groundwater, i.e. it is any place where groundwater flows out onto the surface.
29
Q

Explain why springs form

A
  1. Permeable rock meeting impermeable rock, causing the infiltrated water to build up and eventually escape as a spring
  2. Where the water table meets the surface (especially on a hill), causing the discharge of groundwater.