Lecture 5: Fluvial processes and landforms Flashcards

1
Q

What is the driving force and resisting force in open channel flow? What does the balance of these determine?

A

Driving force - gravity
Resisting force - friction between water and channel surface
Determines the ability of water to entrain and transport material

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2
Q

How do you calculate mean depth?

A

area / top width

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3
Q

How do you calculate hydraulic radius?

A

area / wetted perimeter

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4
Q

What is river discharge the product of?

A

Water-surface width X average depth of flow X average flow velocity

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5
Q

How do you calculate discharge and what does this show?

A

Cross-sectional area X velocity

Shows that cross sectional shape varies with discharge

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6
Q

How do you calculate perimeter of stream?

A

width plus 2Xdepth

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7
Q

Gradient decreases downstream, but what 3 other things increase downstream with increasing discharge?

A

Width, depth and velocity

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8
Q

Spatial temporal variations in flow velocity may be caused by what 3 factors?

A

Channel slope, roughness and cross sectional form.

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9
Q

What is the effect of friction on velocities within a channel?

A

Decreases from centre to bed, with highest rates of decrease closest to bed

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10
Q

Velocity increases with height above bed through what 5 layers?

A

Viscous sublayer to buffer layer to logarithmic layer to outer layer

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11
Q

What affects thickness of flow in the boundary layer?

A

friction between fluid and solid boundary

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12
Q

If flow is steady through time, what does not change?

A

Depth

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13
Q

If flow is uniform in space then what properties must the channel display?

A

no variation in depth/velocity along a reach of constant slope and cross sectional shape

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14
Q

Shear stress (T) imposed by a velocity can deform a water mass, but where is this felt greatest and how is it calculated?

A

Felt greatest at bottom as lowest velocity

T = Viscosity (resists shear) X (difference in downstream velocity / difference in distance above bed)

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15
Q

For laminar flow, what does not occur between layers?

A

Mass transfer

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16
Q

How do you calculate the reynolds number?

A

(4 X mean velocity X hydraulic radius) / kinematic viscosity

17
Q

What happens when Re is below 2000? Above 8000?

A

Below 2000 - laminar flow

Above 8000 - turbulent flow (eddies and mixing)

18
Q

How can the velocity of turbulent flows be estimated?

A

The chezy or manning equations

19
Q

How can the velocity of laminar, turbulent and transitional flows be measured?

A

Darcy-weisbach equation

20
Q

What is the hardest parameter to measure that affects velocity?

A

The roughness

21
Q

Why do rivers create landforms?

A

They are primary agents of erosion, transport, deposition

22
Q

Describe the movement of sediment in the hydrological system.

A

Headwaters = production
1st order streams = sediment transfer
Deltas, lowslopes = deposition

23
Q

What do sediment transport and bedform development contribute to one another?

A

Sediment transport contributes deposition whilst bedform development determines sediment availability, flow geometry and local rates.

24
Q

What does beform development contribute to turbulent flow?

A

Resistance

25
Q

What exchange occurs between sediment transport and turbulent flows?

A

Sed transport induces resistance and turbulence damping whilst turbulent flows provide unsteady forces and interactions

26
Q

What are the average annual transport distances of gravel, sand and silt?

A
  • Gravel 50 –500 m/yr
    • Sand 100-10,000 m/yr
    • Silt-clay many km, or into floodplain, where it
    stays for a long time
27
Q

What is suspended load?

A

Carried in water, during which time has no contact with bed.

28
Q

What is washload?

A

Carried in water, not present in bed

29
Q

For lanes stability constant, Sediment load X median grain size = ?

A

Discharge X slope

30
Q

What are the three main types of river channel?

A

Bedrock, alluvial, semicontrolled

31
Q

For alluvial channels, what represents the irregularity of channel course?

A

Sinuousity (ratio of channel length:valley length)

32
Q

What is the pattern and shape of channels related to?

A

Quantity and size of sediment being transported and valley floor gradient

33
Q

Meandering channels are highly sinuous (>1.5) but what acts as controls on them?

A

Correlations between meander
wavelength, mean radius of curvature
and channel width

34
Q

Where are the finest particles and lowest velocities found in a meander?

A

The inside

35
Q

What characterises the dynamic nature of braided channels?

A

High rates of fluvial activity, complex flow patterns, large % coarse material transported as bed load

36
Q

What is often the case in braided channel width?

A

Erodible banks = large width

37
Q

Where are braided channels often found, and what is typical of their discharge?

A

On steep slopes, discharge is variable