Lecture 6 Flashcards

(69 cards)

1
Q

What does sediment not just move as

A

Just individual grains

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2
Q

What is a bed form

A

A morphological feature generates by sediment movement

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3
Q

What are the two main theories for how flat beds move into bed forms

A

Bed defects and wave instability

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4
Q

What does the bed defect theory link to

A

What we know about turbulence and flow structure

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5
Q

What creates the initial defect in the stream bed

A

High shear stress on an area of bedform

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6
Q

What happens when the sweep stops moving with sediment

A

creates a small pile of sediment

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7
Q

What happens once the defect is created

A

high pressure upstream, low pressure down stream

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8
Q

What zone is created downstream of the newly created high pressure

A

A low pressure recirculation zone

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9
Q

What does the change in velcocity between the high pressure and low pressure give us

A

a shear layer

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10
Q

When the shear layer attaches to the bed what does this create

A

a reattachment points, area of new erosion

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11
Q

What is the concept of wave instability

A

substances of two different densities and speeds move over each other like kelvin helmholtz instabilities

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12
Q

What is the diagram used to show bed forms, shear stress and thier diameter

A

bed form phase diagram

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13
Q

What are the proposed 4 zones to look at in terms of the bed forms phase diagram

A

sand sub, sand super, gravel sub, gravel super

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14
Q

What is the other name for bed forms which are in the super critical flow

A

Upper flow regime

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15
Q

what are the main bed form types in sub critical flow on sand beds

A

Ripples and dunes

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16
Q

What are ripples restricted by

A

grain size

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17
Q

What are dunes restricted by

A

flow depth

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18
Q

What is the average height of ripples

A

3cm

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19
Q

What are ripples controlled by

A

flow right near the bed of the channel.

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20
Q

What size do dunes start at

A

4cm

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21
Q

How long can dunes grow to be

A

100’s meters

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22
Q

The dunewave length is how much times of the depth

A

5-7 times

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23
Q

How tall is the dune in relation to the depth

A

6-10th of the depth

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24
Q

What can part of the variability be down to in terms of dunes

A

hard to measure, different rivers show different values

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25
What has been found out in terms of dune size in river systems
dunes have been seen to be larger that expected in small streams, and smaller than expected in larger streams.
26
Why might deeper channles have smaller dunes
higher shear stress=more erosion of the bed
27
Are dunes thought to be symetrical or asymetrical in river systems
asymentrial
28
What is the steeper side known as
Lee 20-35 degrees
29
What is the shallower dunes face known as
Stoss 5-10 degrees
30
What is the bottom part of the dune called
trough
31
What is the top of the dune called
crest
32
how do we work out the amplitude
trough height to crest height
33
How can the crest line be described from a planform viewpoint
Sinous crestline
34
What else is common with dunes in terms of sediment size
can see sediment sorting
35
what are the 3 forms of movement in dune form
fine sediment ricurculation, coarse avalanches, sediment overshoot of shear layer
36
What happens in high sediment transport rates
strong sorting, coase sediment avalanches with lots of fine sediment in ricurculation, may create regressive ripples
37
What happens in low sediment transport rates
all the sediment moves together, poor sorting
38
how can we see lee face deposition
can be preserved in the dunes as lines
39
What happens when each dune scours out the next one down stream
Nothing preserved, brand new dune
40
How do we get lee faces that are preserved
need a certain degree of aggredation
41
When you get a high amount of agredation what can happen to dune bed forms
can stack on each other and be draped on one another
42
How much of the lee face is generally preserved
1/3
43
How can we work out the original dune height from whats left
multiply by 3, from this we can work out the depth
44
What are the most common bed form features
dunes
45
What information can we get from a dune form
flow direction flow depth, rate of agredation and sediment transport rate
46
What sand forms are found in super critical flow
anti dunes
47
What are anti dunes best defined by
standing waves
48
Are there any flow circulation zones in anti dunes
no, super critical flow
49
Which side of the anti dunes is erosional
the lee side
50
Which way does an anto dune migrate
up stream
51
What is a pebble cluster
when grains of sediment get trapped behind a larger pebble or rock
52
What is the larger particle known as in a pebble cluster
key stone
53
What zone is created after the pebble cluster
recirculation zone that traps finer particles
54
How much of the river bed has pebble clusters
10%
55
how are bed load sheets formed
much broader areas of the sub critical flow
56
how large is the leading edge of a bed load sheet
just 2-3 grains thick
57
what is formed in super critical gravel zones
transverse ribs
58
What is a tranvserse rip
an alternating pattern of stripes, perpendicular to the flow
59
What is a bed configuration
as assemblage of bed forms in a particular area
60
When do ripples form
at the threshold of bed load motion
61
What size must grains be under to form ripples
0.7mm
62
where do ripples not occur
in mud, as it is soon entrained from the bed
63
what causes the initiation and growth of ripples
turbulent variation in near bed flow velocity
64
What is the maximum length of a ripple
60cm
65
What is a lower plane bed
just above the threshold for motion, transitional flows
66
What size do grains need to exceed to form dunes
0.1mm
67
Why can ripples not form in coarse sediments
the bed instability related to local disruption of a viscous sub layer does not exist
68
What does differential transport of bed load grains result in
size segregation of grain sizes
69
Where are pebble clusters common
poorly sorted cobble clusters