Rivers key terms Flashcards

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1
Q

Evaporation

A

The process which liquid water is transformed into water vapour

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2
Q

Transpiration

A

The process by which water is lost from a plant through stomata in its leaves

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3
Q

Evapotranspiration

A

The total amount of moisture removed by evaporation and transpiration from a vegetated land surface

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4
Q

Groundwater flow

A

The slowest transfer of water within the drainage basin. Provides the main input of water during drought or dry seasons. Flows through bands of sedimentary rock.

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5
Q

Infiltration

A

The passage of water into the soil. Takes place quickly at the beginning of a storm, but as the soil becomes more saturated, infiltration rates drop. sandy soils infiltrate more than clay.

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6
Q

Interception

A

The process by which raindrops are prevented from directly reaching the soil surface. Leaves and stems intercept water.

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7
Q

Percolation

A

The downward movement of water within the rock under the soil surface. The rate of percolation depends on the nature of the rock.

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8
Q

Precipitation

A

Water in any form that falls from the atmosphere to the surface of the earth. Includes rain, snow, sleet and hail.

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9
Q

Runoff

A

All the water that enters a river and eventually flows out of the drainage basin.

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10
Q

Stemflow

A

The water that runs down the stems and branches of plants and trees during and after rain to reach the ground

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11
Q

Throughfall

A

The water that drips off leaves during a rainstorm. It occurs when more water falls onto the interception layer of the tree canopy than can remain on the leaves.

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12
Q

Throughflow

A

The water that moves down-slope through subsoil, pulled by gravity

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13
Q

Soil moisture surplus

A

Soil water store is full which gives a surplus of soil moisture for plant use and runoff into streams

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14
Q

Soil moisture use

A

Plants must rely on stored water which is gradually used up

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15
Q

Soil moisture deficiency

A

Plants must have adaptations to survive for long periods or land must be irrigated

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16
Q

Soil moisture recharge

A

The soil water store starts to be recharged

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17
Q

Return period

A

An estimate of the likelihood of an event

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18
Q

Abrasion

A

Rocks hitting the river bed and bank

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19
Q

Hydraulic action

A

The power of moving water erodes the river

20
Q

Solution (erosion)

A

Rocks dissolved by acids and erode the river

21
Q

Attrition

A

Rocks hitting each other which make them smaller and rounder

22
Q

Suspension

A

Fine, light material carried along in the river

23
Q

Solution (transportation)

A

Dissolved rock carried along in the river

24
Q

Saltation

A

Small pebbles and stones bouncing along river bed

25
Q

Traction

A

Large rocks rolling along river bed

26
Q

Example of a waterfall and gorge

A

High force on River Tees, Northern England

27
Q

Example of a meander and oxbow lake

A

River cuckmere

28
Q

MEDC flood case study

A

Cumbria Floods - Cockermouth, Cumbria

29
Q

LEDC flood case study

A

Pakistan - Indus River

30
Q

Hard engineering case studies

A
  • Mississippi River, USA

- Three Gorges Dam, China - Yangtze River

31
Q

Soft engineering case studies

A
  • Yellow River, China - Afforestation
  • Rhine River, Germany - floodplain zoning
  • Met Office/ The EA - forecasting floods and warning
32
Q

Causes of high velocity?

A
  • High discharge
  • High hydraulic radius
  • Increase of gradient
  • Low wetted perimeter
33
Q

What is velocity determined by?

A
  • Channel shape in cross section
  • Roughness of channel beds and banks
  • Channel gradient
34
Q

What is hydraulic radius?

A

Shows channel efficiency

35
Q

Hydraulic Radius calculation

A

Cross sectional area - channel width X depth
____________________________________
Wetted perimeter

36
Q

What is the Hjultsrom curve?

A

Shows the relationship between river velocity and size of particles that can be eroded, transported and deposited.

37
Q

What are the key points on the Hjultsrom curve?

A

1) silt/sand are picked up at lowest velocities
2) clays are difficult to erode as pebbles, although small, they are cohesive and clay bed is smooth.
3) large boulders are dropped easily
4) clay particles can be transported in suspension at low velocities

38
Q

What is the Bradshaw model?

A

Illustrates the main changes expected down the long profile of a river
Can make hypotheses on expected changes in the channel characteristics down the long profile

39
Q

Formation of deltas

A

Deltas form only when the rate of deposition exceeds the rate of sediment removal.

40
Q

Formation of braided streams

A

Braiding occurs when the river is forced to split into several channels separated by islands.

41
Q

Formation of potholes

A

Potholes are formed where there are depressions, fine particles and large boulders may become trapped and swirled around by the current

42
Q

Why does river rejuvenation occur?

A

Occurs when there is a rise of fall in sea level. The river adjusts to this change and creates landforms

43
Q

What are river rejuvenation land forms?

A
  • Knick points
  • River Terraces
  • Incised Meanders
44
Q

Formation of a Knick Point

A

Formed due to sudden increase in gradient. Rejuvenation always starts closest to the sea and migrates upstream. A knick point marks each period of rejuvenation which resulted in an incised valley floor.

45
Q

Formation of a River Terrace

A

They are the remains of a former floodplain which has been left at a higher level after rejuvenation. The down cutting of a renewed river leaves old flood plain above the level of the present river at a suspended level.

46
Q

Formation of a Incised Meander

A

Renewed energy from rejuvenation results in an increase of vertical erosion and incised meanders. Ingrown meanders are also found in this process which incision is less rapid and lateral erosion is dominant.