Land and Water, River Processes Flashcards

1
Q

What two key aspects of rivers are essential to their existence and management?

A

Diveristy and adaptability. Different rivers adapt differently to different conditions

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2
Q

Impelling and resisting forces

A

Impelling forces: Drive change. Measured by river energy

Resisting forces: Resist change. Measured by flow resistance factors

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3
Q

What are the two types of flow?

A
  1. Laminar
  2. Turbulent
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4
Q

Laminar flow

A

Water layers slide over each other as thin, coherent layers, thus conserving energy

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5
Q

Turbulent flow

A

Chaotic movement of water with rough bed eddies, thus causing significant energy loss

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6
Q

What element is the main driver of gross stream power and unit stream power?

A

The amount of water because it determines the amount of energy that is distributed throughout the river

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7
Q

Describe the three measurements of river energy

A
  1. Gross stream power
  2. Unit stream power
  3. Mean boundary shear stress
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8
Q

Gross stream power

A

The avalaible energy in a river

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9
Q

Unit stream power

A

The avalaible energy in a river per unit of channel width

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10
Q

Mean boundary shear stress

A

The energy acting on the bed/banks of a river

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11
Q

What percentage of a river’s energy is dissipated by friction?

A

97%. This leaves only 3% for sediment transport

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12
Q

Describe the three types of resistance within a river

A
  1. Internal flow resistance
  2. Boundary resistance
  3. Channel resistance
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13
Q

Internal flow resistance

A

The resistance of a fluid to change shape

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14
Q

Boundary resistance

A

Grain and form roughness

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15
Q

Channel resistance

A

Bank and planform (shape) roughness

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16
Q

Thalweg

A

The highest velocity filament in a river, located away from boundary resistance in the middle of the channel near the surface

17
Q

What are the three types of channel shapes and their roughness?

A
  1. Narrow and deep
  2. Wide and shallow
  3. Rough streambed
18
Q

What are the two characteristics of narrow and deep channels?

A
  1. Less resistance
  2. Faster flow
19
Q

What are the two characteristics of wide and shallow channels?

A
  1. More resistance
  2. Slower flow
20
Q

What are the two characteristics of rough streambed channels?

A
  1. Also more resisance
  2. Also slower flow
21
Q

Lane balance

A

A balance between sediment size and stream flow, each aggrading and degrading respectively

22
Q

Why is bed stability important?

A

The bed erodes before the banks; it is the cradle of the river. River management strategies that do not address its stability are likely to fail

23
Q

What does the Hjulström curve indicate about the three types of sediment?

A
  1. Fine: Difficult to transport because sticky
  2. Sand: Easy to transport because light and not sticky
  3. Coarse: Difficult because heavy

In conclusion, rivers love sand

24
Q

What are the three ways that sediment is transported throughout a river?

A
  1. Saltation/punctuated movement
  2. Suspension
  3. Solution
25
Q

What are the two causes of sediment deposition?

A
  1. Velocity decreases
  2. Excessive load

Coarsest particles tend to be deposited first

26
Q

What causes bank erosion

A

A combination of hydraulic action and abrasion which leads to mass failure of the channel banks

27
Q

What two types of accretion cause floodplain formation?

A
  1. Lateral accretion
  2. Vertical accretion
28
Q

Lateral accretion

A

Sediment is deposited within the channel on the inside of bends to form point bars

29
Q

Vertical accretion

A

Sediment is deposited over the bank (typically occurs during floods)