Section 1: High Re, surface movement, fluid-sediment interactions Flashcards

1
Q

What Re world do copepods live in

A

Both high and low

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2
Q

What are the mechanoreceptory setae on copepod antennae used for

A

Detect change in water flow and streamline, detect food source or predators,

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3
Q

When do copepods enter high Re world

A

When jumping forwards with swimming legs to catch prey. In high Re (inertia) world can temporarily ignore viscosity

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4
Q

How does an airfoil create lift

A

Increases the angle of attack, the velocity of airflow is higher on the upper surface, lower pressure on the top of the foil means lift created

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5
Q

When does stall occur

A

Maximum lift without stall is 16 degrees. Separation point jumps up (separated flow expands), so no lift

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6
Q

How to prevent stall

A

Stop propagation of flow separation up surface- use eddy flaps. Flaps trap flow separation, stops it moving up the air foil, allows higher angle of attack

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7
Q

Adaptation of whales to overcome drag

A

Tubercules on the fins stops stalling, allows higher angle of attack for quick manoeuvres. Lower drag coefficient. Leading edge tubercules generate vortices that delay separation thus preventing stall. Vortices hug the surface until the end of the air foil, delaying separation, allows increased speed and higher angle of attack.

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8
Q

Adaptation of scallops

A

Propelled by jets as shell is clamped shut, riblet on shell optimised to prevent formation of hairpin vortices, keep vortices channelled streamwise, stops vortices crossing in the flow

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9
Q

Adaptations of fish tails

A

Counter-rotating vortex pair formed with central jet of high velocity flow that generates propulsion. Highspeed around vortex, thrust generated in the center

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10
Q

How does burrowing help with food collection

A

Using flow separation vortices to trap food particles that are slowed by the burrow

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11
Q

What happens when exopolymer substances (EPS) are exuded

A

EPS (mucus) exuded in phytoplankton blooms increase seawater viscosity. Can be so viscous that flow in fish gills retarded/stop, can kill the fish, suffocate
Becoming more common with eutrophication and warming

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12
Q

What is a hydraulic jump
Example

A

A sudden change in water level, from subcritical (tranquil) flow to supercritical(shooting) flow. Increase in flow depth, loss in flow power, generation of turbulence.
Often occurs at changes in slope that results in loss of flow power
eg Taum Sauk dam break

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13
Q

What is the Froude number that standing waves are found at

A

Fr = 1 (stable)
can form in Fr range 0.8-1.77
If less than 1 will start to move upstream, eventually washed away because wave speed faster than the current

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14
Q

What must boats do to go faster

A

Escape own bow wave to go faster than hull length (wave length)
Hull speed is highest efficient speed of vessel

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15
Q

How to leave hull speed

A

Leave bow wave
Lift hull out of the water to increase speed
Boat will bounce (planning)

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16
Q

How is surface swimming speed limited

A

By body/hull length (hard if small)

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17
Q

Fluid forces that act on a grain

A

Lift component (up)
Drag component (same direction as flow)
Resultant fluid force (in between the two)
Gravity force (down)

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18
Q

What happens in accordance with the increased strength of threshold stress

A

Increasing flow power of the fluid
Fine grain carried in suspension
Coarser grain are the bedload transport
Low energy bedload, high suspended

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18
Q

What happens in accordance with the increased strength of threshold stress

A

Increasing flow power of the fluid
Fine grain carried in suspension
Coarser grain are the bedload transport
Low energy bedload, high suspended

19
Q

Why are clays sticky

A

Subject to electrochemical inter-particle forces (van der Waals bonds)
Cohesive behaviour applies for muds & sand/mud mixtures with clay contents >15-20%

20
Q

Stabilising biotic factors

A

Biofilms (EPS) or filamentous networks
Compaction by burrowing macrofauna increases density
Sediment armouring: organisms cover surface, shielding sediment
Biofiltration & bio-deposition: filter feeding removes suspended sediment

21
Q

Destabilising biotic factors

A

Pelletisation enhances erodibility
Grazing reduces stabilising influence of microphytobenthos
Burrow cleaning results in ejected material
Blistering: bubble formation under biofilms results in suspension

22
Q

What is saltation trajectory

A

If fluid force is sufficient, the grain will take off in an impulse
Turbulence can cause grain0grain collisions

23
Q

Major components of hydraulic sorting in relation to particle size distribution

A

(least frequent) Traction: always in contact with the bed, big
(most frequent) Intermittent suspension, mid size
(least frequent) Continuous suspension, silk fine particles

24
Sequence of bedform development in shallow flows with increasing flow power
1: flat plane bed 2: typical ripple patter, laminations/foresets - dip down current 3 (weak boil): dunes with ripples superposed 4 (boil, flow surface not in phase with bed): dunes, laminations/foresets - dip down current Upper stage plane bed: washed-out dunes or transition
25
The result of deposition during Upper stage plane bed regime
Parallel laminated sands Often enhanced by micas giving flag stones
26
What is a graded bed
Coarsest material deposited first Loss of flow power, heaviest first
27
What are antidunes
Flow surface in phase with the bed Air-water interface - standing waves Can steepen and break due to turbulence
28
Antidunes in deeper tidal creeks
Zones of increasing erosion Decreasing sheer stress, deposition Laminations dip up current
29
Ripple and dune nomenclature - morphology
Half height: trough or crest Stoss side: sediment moved up Lee side: sediment grain rolls down, protected from water or wind (air) Summit: particles reach top then fall down slip face Brink point: start of slip face In large dunes the summit and brink point don't align
30
Flow over ripple bedforms
Flow past a blunt object or boundary of flow, diverts from direction of flow - flow separation Occursat break point Detaches and reverse flow Separation bubble, weak eddying flow, promotes erosion in the trough, enhances the amplitude of the bedform
31
Define the buffer layer
A zone of intense interaction between turbulent and viscous forces Also known as turbulence generation layer
32
Structure of boundary layer from surface up
Laminar/viscous sublayer (may not exist) Buffer layer (turbulence generation layer) Fully turbulent outer layer
33
What is a burst process
Low velocity fluid eject to higher up the flow Outward leap of low velocity fluid
34
What is a sweep process
Turbulence eddy comes down towards the bed Inward motion of high velocity fluid
35
Where is more turbulent in a boundary layer
Close to the bed Spanwise velocity component (motion): right angle to the flow
36
What is shark skin made of
Dermal denticles Riblet structures formed of crests and troughs
37
How do riblet work
Riblets are within viscous sublayer of the flow In viscous flow, ribbed surface appears as a smooth surface located at a virtual origin But location of virtual origin, depending on flow direction - higher for cross flow Cross flow width reduced by ribs: results in 10% decrease in drag Vortices always displaced further away from boundary- riblets move vortices away from skin
38
Origin of ripples
Dependent on a viscous sublayer, need a burst or sweep process to generate ripples Sweep of high velocity turbulent fluid suspends grain Grain settles to form piles Flow separation occurs causing further erosion Ripples form along bed
39
Existence of laminar sublayer
Pre-requisite for ripple formation When D 0.7mm- laminar sublayer destroyed Medium sand, grain size gets bigger than the maximum thickness of the sublayer Disrupts viscous sublayer, ceases to exist
40
Range of ripple formation
limited to grain sizes <600μm - 700μm Coincides with upper limit of stability of laminar/viscous sublayer Increase strength of flow, strength of sheer stress increase Wavelength of ripple depends on grain size Migration rate: 1-2mm per minute
41
Range of dune formation
(mega-ripples) Development time 10 minutes to 10 days Migration rate: River sand bar 1m/hour, Tidal estuary 0.3m/day Bigger bedform so take longer to form
42
What are starved ripples
Insufficient sand/silt to form full ripple bedform
43
Wave celerity
Wave orbits become compressed with depth Often consists of forwards and reverse stroke - sometimes one is more prominent
44
Vortex development
Sediment is entrained in the lee of the rippled during strong onshore flow Entrained sediment in coherent vortices in lee of the ripple as flow strength increases Flow reverses
45
Symmetrical or asymmetrical ripples
Oscillation of wave motion in shallow water can generate symmetrical ripples But asymmetrical if forwards or reverse stroke is stronger
46
Interference ripple bedforms
Wave interference generates these May also occur with wave and unidirectional (eg tidal) currents