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INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON
53

INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Dec 15, 2015

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Dakota Dandy
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Page 1: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

INVERTEBRATES AND FLUID DYNAMICS:

HOLDING ON

Page 2: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

BOUNDARY LAYER

Mainstream Velocity (U)

Boundary layer thickness (99%)

Boundary layer thickness (90%)

Dis

tanc

e fr

om s

ubst

rate

Velocity

Page 3: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

BOUNDARY LAYER

Using the boundary layer – water pennies (Psephenidae)

Page 4: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

BOUNDARY LAYER

Mainstream Velocity (U)

Dis

tanc

e fr

om s

ubst

rate

Velocity

Page 5: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

BOUNDARY LAYER

Using the boundary layer – water pennies (Psephenidae)

Page 6: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Other stream insects

Plecoptera

Trichoptera

Ephemeroptera

Page 7: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Stream animals– Strategies for holding on

Baetis

Rhithrogena

Ancylus

Page 8: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Psephenus

Neothremma

Bibliocephala

Stream animals– Strategies for holding on

Page 9: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Extreme Gradients – Swash Zone

Page 10: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Donax

Page 11: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Swash Surfing

Page 12: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Donax

Density

Shape

Weight distribution

Page 13: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Density

2.0

1.0

0

Density(103 kg/m3)

DonaxChione

Mercenaria

Spisula

Macrocallis

ta

Divaric

ella

Tellina

Tagellus

Page 14: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Weight Distribution

Pivot point

Page 15: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

AnteriorPosterior

Ventral

Dorsal

Page 16: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.
Page 17: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.
Page 18: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Behaviour in a Swash Zone

Page 19: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.
Page 20: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.
Page 21: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

WAVE STRESS

a. Limitation of size

Water flow100%

90%

Boundary layer

Page 22: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

WAVE STRESS

a. Limitation of size

Water flow

Page 23: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

WAVE STRESS

b. Holding on – flow tolerance

Flow rate(m/s)

3

0

Time to dislodge

Page 24: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

WAVE STRESS

c. Holding on - orientation

Keyhole limpet

Page 25: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

WAVE STRESS

c. Holding on - orientation

Water flow

Page 26: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

WAVE STRESS

c. Holding on - orientation

<.5 m/s

-90 0 90 -90 0 90

>.5 m/s

Freq

Orientation (º to flow)

Page 27: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

WAVE STRESS

d. Holding on - tenacity

What is “tenacity”?

1. Testing holding power

Page 28: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

WAVE STRESS

d. Holding on - tenacity

What is “tenacity”?

1. Testing holding power

Kg required to dislodge

100

0

Foot area (cm2)15

Page 29: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

WAVE STRESS

d. Holding on - tenacity

What is “tenacity”?

1. Suction?

Atmospheric pressure ≈ 1 kg/cm2

Patella ≈ 3 - 7 kg/cm2

-can’t generate a force > atmospheric pressure

- No negative pressure under foot

Page 30: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

WAVE STRESS

d. Holding on - tenacity

What is “tenacity”?

Patella

Mucous layer

Page 31: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

WAVE STRESS

d. Holding on - tenacity

What is “tenacity”?

2. Adhesion area

surface tension

Thickness of fluid

Theoretical adhesion = 600 kg/cm2

Page 32: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

3. WAVE STRESS

d. Holding on - tenacity

What is “tenacity”?

2. Adhesion

Tenacity(kg/cm2 to detach)

Weight of mucous

Page 33: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

3. WAVE STRESS

d. Holding on - tenacity

What is “tenacity”?

Foot rigidity

Page 34: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

3. WAVE STRESS

d. Holding on - tenacity

What is “tenacity”? Foot rigidity

l

d

Page 35: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

3. WAVE STRESS

d. Holding on - tenacity

What is “tenacity”? Foot rigidity

Tenacity

Flexibility

High

HighLow

Low

In field -

Page 36: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

3. WAVE STRESS

d. Holding on - tenacity

What is “tenacity”? Drag

FLOW

Resistance to water movement depends on:

1) Size

2) Shape

3) Texture

Page 37: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

3. WAVE STRESS

d. Holding on - tenacity

What is “tenacity”? Drag

Drag

Side Front Rear

Drag – not well correlated with density

Page 38: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Types of Limpets

Non-Migratory Migratory

-don’t move far

-often fixed and territorial

-low r

-low growth

-move up shore

-high r

-high growth

(need high food intake)

-react to predators by clamping -flee from predators

LESS FLEXIBLE MORE FLEXIBLE

Page 39: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

A COMPROMISE OF SEVERAL FACTORS

Sea Urchins - Echinoidea

lunules

Page 40: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

WHAT IS THE FUNCTION OF LUNULES?

1) Aid in burrowing

2) Removal of feces

3) Maintain a “communication” with the surface if buried

4) Maintain inclined posture

5) Feeding

Page 41: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Log lunule length

Log test diameter

p < .05

If lunules have a hydrodynamic function-they should grow with the animal

isometric

observed

Page 42: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Time to burrow

Burrowing speed

Plugged Not plugged

230 sec231 sec

Page 43: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Flow through a sand dollar

Page 44: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Lift

Weight

Weight

Page 45: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Lift

Weight

Burrowing to add weight

Page 46: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Sand Dollar reorientation - Dendraster

Page 47: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Adding weight – incorporate magnetite

Page 48: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Reducing lift and drag

Skin drag – important?

Pressure drag – depends on shape

Page 49: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Reducing lift and drag

Skin drag – important?

Pressure drag – depends on shape

Very flat

Page 50: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Reducing lift and drag

Skin drag – important?

Pressure drag – depends on shape

Rounded

Area of lower pressure

Page 51: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

How do you reduce lift

Reduce pressure differential between

upper and lower surfaces

Page 52: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Can sand dollars tell the direction of orientation?

Anterior

Posterior

Page 53: INVERTEBRATES AND FLUID DYNAMICS: HOLDING ON. BOUNDARY LAYER Mainstream Velocity (U) Boundary layer thickness (99%) Boundary layer thickness (90%) Distance.

Can sand dollars tell the direction of orientation?

-inverted sand dollars – can flip over more easily with posterior edge facing upstream(i.e critical velocity to re-orient is lower)

Hardy & Merz. 2013. Invert. Bio 132:52

Initial orientation

Final orientation(1 hr)