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
What are the two causes of sediment deposition?
1. Velocity decreases 2. Excessive load Coarsest particles tend to be deposited first
26
What causes bank erosion
A combination of hydraulic action and abrasion which leads to mass failure of the channel banks
27
What two types of accretion cause floodplain formation?
1. Lateral accretion 2. Vertical accretion
28
Lateral accretion
Sediment is deposited within the channel on the inside of bends to form point bars
29
Vertical accretion
Sediment is deposited over the bank (typically occurs during floods)