1.1.2 The drainage basin system Flashcards

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1
Q

What scale is the drainage basin system

A

Local

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2
Q

What type of system is the drainage basin system

A

Open

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3
Q

Inputs

A

Precipitation - rain, snow and hail

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4
Q

Types of rainfall

A

Convectional, relief and frontal warm

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5
Q

Convectional Rainfall

A

Sun heats land, warm air rises, condenses at higher altitudes and falls

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6
Q

Relief rainfall

A

Warm air is forced upward by a barrier such as mountains , causing it to condense at higher altitudes and fall as rain.

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7
Q

Frontal Warm Rainfall

A

Warm air rises over cool air when two bodies of air at different temperatures meet, because the warm air is less dense and therefore lighter. It condenses at higher
altitudes and falls as rain.

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8
Q

Outputs

A

Evapotranspiration and Streamflow

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9
Q

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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10
Q

Streamflow (as output)

A

All water that enters a drainage basin will either leave through the atmosphere, or through streams which drain the basin. These may flow as tributaries into other rivers or directly into lakes and oceans.

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11
Q

Flows (7)

A

Infiltration, Percolation, Throughflow, Surface runoff (overland flow), Groundwater flow, Streamflow, Stemflow

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12
Q

Infiltration (f)

A

This is the process of water moving from above ground into the soil. - Moderate/Fast

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13
Q

Percolation (f)

A

Water moves from the ground or soil into porous rock or rock fractures. - Slow

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14
Q

Throughflow (f)

A

Water moves through the soil and into streams or rivers. Speed of flow is dependent on the type of soil. - Moderate/Fast

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15
Q

Surface runoff (f)

A

Water flows above the ground, as sheetflow, or in rills - Fast

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16
Q

Sheetflow

A

lots of water flowing over a large area

17
Q

Rills

A

small channels similar to streams, that are unlikely to carry water during periods where there is not any rainfall

18
Q

Groundwater flow (f)

A

Water moves through the rocks. Ensures that there is water in rivers, even after long period of dry weather. - Usually slow but variable

19
Q

Streamflow (f)

A

Water that moves through established channels - Fast

20
Q

Stemflow (f)

A

Flow of water that has been intercepted by plants or trees, down a stem, leaf, branch or other part of a plant - Fast.

21
Q

Stores (4)

A

Soil water, groundwater, River channel, Surface storage

22
Q

Soil water (s)

A

Water stored in the soil which is utilised by plants - Mid-term

23
Q

Groundwater (s)

A

Water that is stored in the pore spaces of rock - Long-term

24
Q

River Channel (s)

A

Water that is stored in a river - Short-term

25
Q

Interception (s)

A

Water intercepted by plants on their branches and leaves before reaching the ground - Short-term

26
Q

Surface Storage (s)

A

Water stored in puddles, ponds, lakes etc. - Variable

27
Q

water table

A

upper level at which the pore spaces and fractures in the ground become saturated.

28
Q

Use of water table by researchers

A

to assess drought conditions, health of wetland systems, success of forest restoration programmes etc.

29
Q

how quickly infiltration occurs.

A

Infiltration capacity

30
Q

overland flow will occur

A

If precipitation falls at a greater rate than the infiltration capacity

31
Q

Percolation rate

A

is dependent on the fractures that may be present in the rock and the permeability of the rock

32
Q

Infiltration capacity can be increased by

A

Grass crops and tree roots create passages for water to flow through from the surface into the soil

33
Q

Field capacity

A

Clay soils with a high field capacity and smaller pore spaces have a slower flow rate. Sandy soils drain quickly because they have a lower field capacity, larger pore spaces and natural channels from animals such as worms. Some sports fields have sandy soils, to reduce the chance of waterlogged pitches, but this may also increase the flood risk elsewhere

34
Q

Area with faster groundwater flow

A

Jointed rocks such as limestone in Karst environments where there are many underground streams and caves , may transfer water very rapidly