Fluvial Geomorphology 2 Flashcards

1
Q

even though average velocity is relatively lower at headwaters, ___ velocity can be very high. Why?

A

instantaneous

b/c there is lots of up & down (pools and riffles on the bed)

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2
Q

If slope/ gradient were the only factor, velocity would ___ downstream, but because channel roughness, wetted perimeter ratio, and discharge all change downstream too, velocity actually ___ as you go downstream

A

decrease

actually increases

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3
Q

why does discharge increase downstream?

A

Because tributaries combine= increases the volume of water flowing through the channel = higher discharge

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4
Q

as area increases, ___ water is in contact with the bed (ie. ____ and ____)- deeper/shallower, wider/ narrower
This means ___ friction and therefore ___ velocity

A

less
deeper & narrower
less
higher

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5
Q

What is the range of manning’s roughness coefficient (n)?

A

0.01 to 0.05
(smooth to rough)

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6
Q

Reynolds number=

A

measure of flow turbulence (internal friction in the fluid column due to flow destruction)

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7
Q

more turbid= bigger or smaller range of instantaneous velocities?

A

more turbid= bigger range

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8
Q

higher bed loads typically= ___ (wider or narrower) channels

A

wider
b/c harder to move

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9
Q

which is easier to measure, bedload or suspended load?

A

suspended load

bed load hard to measure because it happens very episodically (high velocities are needed)

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10
Q

dissolved load relates to rate of ___ weathering

A

chemical

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11
Q

When might chemical weathering be high?
ie high dissolved load

A

high temp, high rainfall, high groundwater flow inputs

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12
Q

t/f
fine clays can be classified as dissolved load

A

true!
They’re sometimes small enough that they’re classified as ‘dissolved’

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13
Q

sediment yield=

A

amount of sediment transported by a river relative to its upstream basin area

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14
Q

sediment yield ___ with drainage basin size

A

decreases

b/c dilution?

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15
Q

how do you convert sediment yield to erosion/ denudation rate?

A

turn tonnes into density

depth/time x 1/rock density

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16
Q

Globally, there is a negative sediment-yield to drainage area relationship, but in Canada we see the opposite (larger drainage area= higher sediment yield). Why is that?

A

b/c of the glaciation history here!
-lots of loose sediments b/c of glaciers still sitting around, not just bedrock

17
Q

paraglacial=

A

non-glacial processes that are a direct result of glaciation

18
Q

paraglaciation=

A

“unstable” conditions caused by a “relaxation time lag” to move sediments from upland valleys to major valleys following glaciation

19
Q

t/f
both sediment load and bedload increase as discharge increases

A

true

20
Q

suspended load= -% of total sediment load
bedload= __% of sediment transport in river systems

A

90-99%

1% for bedload

21
Q

If bedload is only 1% of total sediment load, why is it so important for river morphology?

A

b/c it contributes a lot to roughness!

higher bed load= wide channels

22
Q

bed load=

A

material transported along the bed by railing, traction, saltating

23
Q

suspended load=

A

materials transported within the fluid column itself (air or water)
- fine sand and clays

24
Q

dissolved load=

A

ions being transported, products of chemical + biological weathering

25
Q

laminar sublayer=

A

zone of low turbulence + lower velocity caused by friction along the bed

26
Q

What’s the main role of turbulence?

A

changes in the instantaneous velocity are key for entraining particles

27
Q

Once a particle is in motion, it requires ___ (less or more) force to remain in motion

This is empirically described by the ___ curve

A

less
Hjulstrom

28
Q

What does the Hjulstrom curve represent?

A

sediments entrained by water and the role of grain size on critical shear stress

29
Q
A