Lecture 5 - River Bank Erosion Flashcards

1
Q

What drives bank erosion in forms of energy?

A

Potential, kinetic and thermal energy.

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2
Q

What are the 3 energy states in stream energy?

A

It highlights the 3 energy states (potential, kinetic and mechanical through thermal)

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3
Q

River bank composition is distinguished by what?

A

Cohesive and non-cohesive sdiments

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4
Q

What is in a cohesive river bank

A
  • solid rock
  • generally silt and clay-sized material
  • resistance varies on the bonds between particles
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5
Q

What is a non-cohesive river bank?

A

comprised of a more sandy/gravel-sized material

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6
Q

What are the 2 bank composition types?

A

Fine and coarse

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7
Q

Why are roots and vegetation so important to bank composition?

A

with 16-18% root volume to 5 cm depth, offered 20,000 times more protection than a bank without vegetation (Smith, 1978)

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8
Q

What are the pre-weakening bank erosion processes?

A
  • freeze-thaw
  • slaking and positive pore water pressure (air being forced into small holes by water pressure, weakening the material)
  • soil piping (natural water pipes below the surface, weakening the surrounding river bank)
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9
Q

What is shear stress in bank erosion processes?

A

When the river bank material has exceeded the critical shear stress of entrainment (entrainment is to carry sediment)

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10
Q

What is Mass Failure?

A

Erosion by the effect of gravity on bank material

Depends on bank structure, material properties and the bank geometry

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11
Q

What is Thorne and Tovey’s (1981) cantilever system? (Bank erosion)

A

A model that shows 3 cantilever failures;

  • shear - falls straight down
  • beam - falls out bank diagonally
  • Tensile falls vertically but leaves an overhang which is only supported at the surface
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12
Q

What are the 2 main ways to measure and monitor erosion?

A

Indirectly - reconstruction of historical channel patterns

Directly - Actual measurement of contemporary erosion

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13
Q

How to measure erosion indirectly?

A
  • Using data from OS maps
  • Ariel photographs and satellite imagery
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14
Q

How to measure erosion directly?

A
  • Using steel rods stuck in the river bank with measurements

-Using a self-reading erosion pin (more expensive than steel rods)

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