Rivers 1- The Drainage Basin Flashcards

1
Q

Drainage basin

A

Catchment area of land drained by a river and its distributaries, bordered by a ridge of high land called the watershed

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2
Q

Hydrological cycle

A

Inputs: precipitation
Transfers: surface flow, channel flow, stemflow, interception, infiltration, throughflow, percolation, groundwater flow
Outputs: evaporation, transpiration, runoff

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3
Q

Water balance

A

The balance between inputs and outputs, together with the changes in storage
P = Q + E + DS

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4
Q

Soil moisture budget

A
  1. Soil moisture surplus
  2. Soil moisture use
  3. Soil moisture deficiency
  4. Soil moisture recharge
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5
Q

Uses of water budget graphs

A

Help people to manage river basins

Plan for irrigation or floods

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6
Q

Factors that affect water flow

A

Vegetation & land use, rainfall, gradient, climate, soil type, bedrock, conditions, size & shape of basin

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7
Q

River discharge

A

The amount of water in a river passing a given point at a given time
Area x velocity (cumecs)

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8
Q

Lag time of a hydrograph

A

The time delay between peak rainfall and peak discharge

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9
Q

Causes of a ‘flashy’ flood

A

High intensity/antecedent rainfall, impermeable rock, lack of vegetation, urbanisation (drainage), high density tributaries, steep slopes, circular basin, frozen/baked ground

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10
Q

Long profile

A

Shows the changes in altitude along its course from source to mouth
Theoretically smoothly concave in shape

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11
Q

Upper course

A

Vertical erosion, steep gradient, V-shaped valley, relatively narrow channel

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12
Q

Middle course

A

More gentle gradient, lateral erosion, U-shaped valley, relatively wide channel

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13
Q

Lower course

A

Very gentle gradient, deposition, gentle slopes (if any), very wide channel

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14
Q

Types of erosion

A

Hydraulic action
Abrasion
Solution
Attrition

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15
Q

Hydraulic action

A

Evorsion: the direct force of the water
Cavitation: the process of bubbles imploding in cracks, evicting tiny jets of water (130m/sec)

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16
Q

Abrasion

A

The wearing away of the bank and bed by the load (corrasion)

17
Q

Solution

A

The removal of chemical ions in the rock (corrosion)

18
Q

Attrition

A

The wearing away of the load carried by the river

19
Q

Types of transportation

A

Traction
Saltation
Suspension
Solution

20
Q

Types of load

A

Endogenic- eroded material form the bed and bank

Exogenic- material from the valley sides that has arrived by weathering and mass movement

21
Q

Traction

A

The load rolls and bounces along the riverbed

22
Q

Saltation

A

Smaller particles or stones bounce along the riverbed

23
Q

Suspension

A

Finer particles are carried within the flow of the river

24
Q

Solution

A

Chemical ions carried in solution, dissolved in the river

25
The Hjulström curve
Shows the relationship between the velocity of a river and the size of particles that can be eroded, transported or deposited (logarithmic)
26
Capacity
The amount of material that can be transported
27
Competence
The size of the largest particle that can be transported
28
Trends in the Hjulström curve
As velocity increases, the river's ability to erode and transport particles increases Exceptions: fine clay and silt particles are cohesive and offer less resistance, so require a greater velocity to be entrained
29
Reasons for deposition
A sudden reduction in gradient, decrease in discharge, entering a lake or sea, increase in load, shallow water, entering a floodplain
30
Erosion velocity
The rate of flow at which the river is able to pick up particles
31
Fall velocity
The rate of fall at which a river drops particles
32
Wetted perimeter
Total length of the river bed and banks in cross section that are in contact with the water in the channel (linked to channel roughness)
33
Hydraulic radius
The ratio of the channel's cross sectional area compared to its wetted perimeter
34
Bradshaw's Model
A geographical model that describes how a river's characteristics vary between the upper course and lower course of a river
35
Characteristics that increase downstream
Discharge, occupied channel width, channel depth and average load quantity
36
Characteristics that decrease downstream
Load particle size, channel bed roughness and gradient