1
1 1 2 2 Brooke E. Flammang , George V. Lauder , Daniel R. Troolin , Tyson Strand 1 2 Museum of Comparative Zoology, Harvard University, Cambridge, MA, 02138, USA. Fluid Mechanics Division, TSI Incorporated, St. Paul, MN, 55126, USA INSTANTANEOUS VOLUMETRIC WAKEANALYSIS OF LOCOMOTION IN TELEOST FISHES ABSTRACT: Previous studies of the wake hydrodynamics of fishes have been restricted to two-dimensional digital particle image velocimetry (DPIV) slices by available technology. By comparing multiple slices, previous researchers hypothesized the three-dimensional structure of the vortex wakes produced by swimming fishes. In teleost fishes, such as the bluegill sunfish, the homocercal tail produces a single jet with each lateral pass. Using conventional two-dimensional DPIV, vorticity shed by the homocercal tail was visualized as two counter-rotating vortices which were hypothesized to be part of a three-dimensional rotating ring through which a jet of fluid passed. Now, using a volumetric DPIV system, we have confirmed that the three- dimensional structure of the vortex ring produced by the homocercal tail fin is indeed as predicted. In addition, multiple lateral passes of the tail produced a linked chain of vortex rings. Using this volumetric DPIV system we were also able to instantaneously capture the three-dimensional wake interactions of the dorsal and anal fins with the caudal fin in both live fishes and robotic analogs. HYPOTHESIS 1: Each lateral pass of the homocercal tail produces a single jet of fluid, which passes through a vortex ring. Multiple lateral passes performed during swimming produce a series of linked vortex rings. (Figure from Lauder and Drucker, 2002) HYPOTHESIS 2: Vorticity produced by the dorsal and anal fins of a swimming fish interacts with that produced by the caudal fin. (Figure from Tytell, 2006) Fig. 1 Fig. 2 Fig. 3 Fig. 1. Experimental arrangement of the flow tank, lasers, and volumetric imaging system for capturing the instantaneous volumetric wake behind freely swimming fishes and robotic tail models. Total volume imaged was 14*14*10 cm. Fig. 2. Volumetric 3-component velocimetry (V3V) volumetric flow imaging tripod camera probe captured image pairs at 7.25 Hz with a time of 3500 us between each image pair at 12 bit resolution. Fig. 3. Schematic representation of 3D particle identification. Particle images from the left image (L) are represented by white, particle images from the right image (R) are represented by red, and particle images from the top image (T) are represented by blue. The centroid of the triplet represents the x and y location, the and the size gives the z location. (Figure from Troolin and Longmire, 2009). REFERENCES: Lauder, G.V. and E.G. Drucker. (2002) Forces, fishes, and fluids: Hydrodynamic mechanisms of aquatic locomotion. News Physiol Soc 17:235- 240 Troolin D.R. and E.K. Longmire. (2009) Volumetric velocity measurements of vortex rings from inclined exits. Exp Fluids DOI 10.1007/s00348-009-0745-z Tytell, E.D. (2006) Median fin function in bluegill sunfish Lepomis macrochirus: streamwise vortex structure during steady swimming. J Exp Biol 209:1516-1534 Fig. 4. (A) Robotic simplified homocercal tail model in laser volume and (B) volumetric reconstruction of wake produced. Note how downstream edge constricts jet (white arrows). METHODS: Fig. 8. (A, top) Volumetric reconstruction of wake of a bluegill sunfish swimming far back enough in volume to see wake produced by the dorsal fin (outlined in red). (B, bottom) Planar slice (XY) through vortex caused by dorsal fin, colored by z vorticity. Tangent vectors are displayed and indicate direction and velocity of flow, with mean stream flow velocity subtracted. A B Fig. 5. (A) Live bluegill sunfish swimming in laser volume and (B) volumetric reconstruction of wake produced (at 40% translucency). * = trailing edge vortices separating from tail fin. A B A B Fig. 6. (A) Live cichlid swimming in laser volume and (B) volumetric reconstruction of wake produced. A B Fig. 7. (A) Robotic bluegill homocercal tail model in laser volume and (B) volumetric reconstruction of wake produced by the dorsal (red), anal (blue) and caudal (green) fins. A B -5.0 5.0 0 -1 Z Vorticity (s ) * * CONCLUSIONS: The ability to capture an instantaneous snapshot of the complete wake structure produced by a swimming fish removes the potential error involved with previous technologies, where researchers had to integrate multiple data sets to produce a 3D structure. Using this new technology, we have confirmed that homocercal tails produce a series of linked ring vortices during steady swimming. We have also been able to identify dorsal and anal fin wake structures and are beginning to build a better understanding of how they interact with the wake produced by the caudal fin. Anaglyph of Fig. 6B, view with 3D glasses. DORSAL FIN JET FISH BODY

INSTANTANEOUS VOLUMETRIC WAKE ANALYSIS OF LOCOMOTION … · Total volume imaged was 14*14*10 cm. Fig. 2. Volumetric 3-component velocimetry (V3V) volumetric flow imaging tripod camera

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Page 1: INSTANTANEOUS VOLUMETRIC WAKE ANALYSIS OF LOCOMOTION … · Total volume imaged was 14*14*10 cm. Fig. 2. Volumetric 3-component velocimetry (V3V) volumetric flow imaging tripod camera

11

22

Bro

oke

E.

Fla

mm

an

g,

Ge

org

e V

. L

au

de

r,

Da

nie

l R

. T

roo

lin,Tyso

n S

tra

nd

12

Museum

of C

om

para

tive Z

oolo

gy,

Harv

ard

Univ

ers

ity,

Cam

bridge, M

A, 02138, U

SA

. F

luid

Mechanic

s D

ivis

ion, T

SI In

corp

ora

ted, S

t. P

aul, M

N, 55126, U

SA

INS

TA

NTA

NE

OU

S V

OL

UM

ET

RIC

WA

KE

AN

ALY

SIS

OF

LO

CO

MO

TIO

N IN

TE

LE

OS

T F

ISH

ES

AB

ST

RA

CT:

Pre

vio

us s

tudie

s o

f th

e w

ake h

ydro

dynam

ics o

f fishes h

ave

been r

estr

icte

d to tw

o-d

imensio

nal dig

ital part

icle

im

age v

elo

cim

etr

y (

DP

IV)

slic

es b

y a

vaila

ble

technolo

gy.

B

y c

om

paring m

ultip

le s

lices, pre

vio

us

researc

hers

hypoth

esiz

ed the thre

e-d

imensio

nal str

uctu

re o

f th

e v

ort

ex w

akes

pro

duced b

y s

wim

min

g fis

hes. In tele

ost fishes, such a

s the b

lueg

ill s

unfish,

the h

om

ocerc

al ta

il pro

duces a

sin

gle

jet w

ith e

ach late

ral pass. U

sin

g

conventional tw

o-d

imensio

nal D

PIV

, vort

icity s

hed b

y the h

om

ocerc

al ta

il w

as

vis

ualiz

ed a

s tw

o c

ounte

r-ro

tating v

ort

ice

s w

hic

h w

ere

hypoth

esiz

ed to b

e

part

of a thre

e-d

imensio

nal ro

tating r

ing

thro

ugh w

hic

h a

jet of fluid

passed.

Now

, usin

g a

volu

metr

ic D

PIV

syste

m, w

e h

ave c

onfirm

ed that th

e thre

e-

dim

ensio

nal str

uctu

re o

f th

e v

ort

ex r

ing p

roduce

d b

y the h

om

ocerc

al ta

il fin is

indeed a

s p

redic

ted. In a

dditio

n, m

ultip

le late

ral passes o

f th

e tail

pro

duced a

lin

ked c

hain

of vort

ex r

ings. U

sin

g this

volu

metr

ic D

PIV

syste

m w

e w

ere

als

o

able

to insta

nta

neously

captu

re the thre

e-d

imensio

nal w

ake inte

ractio

ns o

f th

e d

ors

al and a

nal fins w

ith the c

audal fin in b

oth

liv

e fis

hes a

nd r

obotic

analo

gs.

HY

PO

TH

ES

IS 1

: E

ach

la

tera

l p

ass o

f th

e h

om

oce

rca

l ta

il p

rod

uce

s a

sin

gle

je

t o

f flu

id,

wh

ich

pa

sse

s t

hro

ug

h a

vo

rte

x

rin

g.

Mu

ltip

le la

tera

l p

asse

s

pe

rfo

rme

d d

urin

g s

wim

min

gp

rod

uce

a s

erie

s o

f lin

ke

d v

ort

ex

rin

gs.

(Fig

ure

fro

m L

au

de

r a

nd

D

rucke

r, 2

00

2)

HY

PO

TH

ES

IS 2

: V

ort

icity

pro

du

ce

d b

y t

he

do

rsa

l a

nd

a

na

l fin

s o

f a

sw

imm

ing

fis

h

inte

racts

with

th

at

pro

du

ce

d b

y

the

ca

ud

alf

in.

(Fig

ure

fro

m

Tyte

ll, 2

00

6)

Fig

. 1

Fig

. 2

Fig

. 3

Fig

. 1

. E

xp

erim

en

tal

arr

an

ge

me

nt

of

the

flo

w t

an

k,

lase

rs,

an

d v

olu

me

tric

im

ag

ing

syste

m f

or

ca

ptu

rin

g t

he

in

sta

nta

ne

ou

s v

olu

me

tric

wa

ke

b

eh

ind

fre

ely

sw

imm

ing

fis

he

s

an

d r

ob

otic t

ail

mo

de

ls. To

tal

vo

lum

e im

ag

ed

wa

s 1

4*1

4*1

0

cm

.

Fig

. 2

. V

olu

me

tric

3-c

om

po

ne

nt

ve

locim

etr

y (

V3

V)

vo

lum

etr

ic

flo

w im

ag

ing

trip

od

ca

me

ra

pro

be

ca

ptu

red

im

ag

e p

airs a

t 7

.25

Hz w

ith

a t

ime

of

35

00

us

be

twe

en

ea

ch

im

ag

e p

air a

t 1

2

bit r

eso

lutio

n.

Fig

. 3

. S

ch

em

atic

rep

rese

nta

tio

n o

f 3

D

pa

rtic

le id

en

tifica

tio

n.

Pa

rtic

le im

ag

es f

rom

th

e

left

ima

ge

(L

) a

re

rep

rese

nte

d b

y w

hite

,p

art

icle

im

ag

es f

rom

th

e

rig

ht

ima

ge

(R

) a

re

rep

rese

nte

d b

y r

ed

, a

nd

p

art

icle

im

ag

es f

rom

th

e

top

im

ag

e (

T)

are

re

pre

se

nte

d b

y b

lue

.T

he

ce

ntr

oid

of

the

trip

let

rep

rese

nts

th

e x

an

d y

loca

tio

n,

the

an

d t

he

siz

e

giv

es t

he

z lo

ca

tio

n.

(Fig

ure

fro

m T

roo

lin a

nd

L

on

gm

ire

, 2

00

9).

RE

FE

RE

NC

ES

:

La

ud

er,

G.V

. a

nd

E.G

. D

rucke

r. (

20

02

) F

orc

es,

fish

es,

an

d f

luid

s:

Hyd

rod

yn

am

ic m

ech

an

ism

s o

f a

qu

atic lo

co

mo

tio

n.

Ne

ws P

hysio

l S

oc 1

7:2

35

-2

40

Tro

olin

D.R

. a

nd

E.K

. L

on

gm

ire

. (2

00

9)

Vo

lum

etr

ic v

elo

city m

ea

su

rem

en

ts o

f vo

rte

x r

ing

s

fro

m in

clin

ed

exits.

Exp

Flu

ids

DO

I 1

0.1

00

7/s

00

34

8-0

09

-07

45

-z

Tyte

ll, E

.D.

(20

06

) M

ed

ian

fin

fu

nctio

n in

blu

eg

ill

su

nfish

Le

po

mis

ma

cro

ch

iru

s:

str

ea

mw

ise

vo

rte

x

str

uctu

re d

urin

g s

tea

dy s

wim

min

g.

J E

xp

Bio

l 2

09

:15

16

-15

34

Fig

. 4

. (A

) R

ob

otic s

imp

lifie

d h

om

oce

rca

l ta

il m

od

el in

la

se

r vo

lum

e a

nd

(B

) vo

lum

etr

ic

reco

nstr

uctio

n o

f w

ake

pro

du

ce

d.

No

te h

ow

do

wn

str

ea

m e

dg

e c

on

str

icts

je

t (w

hite

arr

ow

s).

ME

TH

OD

S:

Fig

. 8

. (A

, to

p)

Vo

lum

etr

icre

co

nstr

uctio

n o

f w

ake

of

a

blu

eg

ill s

un

fish

sw

imm

ing

fa

r b

ack e

no

ug

h in

vo

lum

e t

o s

ee

w

ake

pro

du

ce

d b

y t

he

do

rsa

l fin

(o

utlin

ed

in

re

d).

(B

, b

ott

om

) P

lan

ar

slic

e (

XY

) th

rou

gh

vo

rte

x c

au

se

d b

y d

ors

al fin

, co

lore

d b

y z

vo

rtic

ity.

Ta

ng

en

tve

cto

rs a

re d

isp

laye

d a

nd

in

dic

ate

dire

ctio

n a

nd

ve

locity

of

flo

w,

with

me

an

str

ea

m f

low

ve

locity s

ub

tra

cte

d.

AB

Fig

. 5

. (A

) L

ive

blu

eg

ill s

un

fish

sw

imm

ing

in

la

se

r vo

lum

e a

nd

(B

) vo

lum

etr

ic

reco

nstr

uctio

n o

f w

ake

pro

du

ce

d (

at

40

% t

ran

slu

ce

ncy).

* =

tra

ilin

g e

dg

e v

ort

ice

s

se

pa

ratin

g f

rom

ta

il fin

.

AB

AB

Fig

. 6

. (A

) L

ive

cic

hlid

sw

imm

ing

in

la

se

r vo

lum

e a

nd

(B

) vo

lum

etr

ic r

eco

nstr

uctio

n o

f w

ake

pro

du

ce

d.

AB

Fig

. 7

. (A

) R

ob

otic b

lue

gill

ho

mo

ce

rca

l ta

il m

od

el in

la

se

r vo

lum

e a

nd

(B

) vo

lum

etr

ic

reco

nstr

uctio

n o

f w

ake

pro

du

ce

d b

y t

he

do

rsa

l (r

ed

), a

na

l (b

lue

) a

nd

ca

ud

al (g

ree

n)

fin

s.

A B

-5.0

5.0

0-1

Z V

ort

icity (

s)

* *

CO

NC

LU

SIO

NS

:

The a

bili

ty to c

aptu

re a

n

insta

nta

neous s

napshot of th

e

com

ple

te w

ake s

tructu

re

pro

duced b

y a

sw

imm

ing fis

h

rem

oves the p

ote

ntial err

or

involv

ed w

ith p

revio

us

technolo

gie

s, w

here

re

searc

hers

had to inte

gra

te

multip

le d

ata

sets

to p

roduce

a 3

D s

tructu

re. U

sin

g this

new

technolo

gy,

we h

ave

confirm

ed that hom

ocerc

al

tails

pro

duce a

series o

f lin

ked

ring v

ort

ices d

uring s

teady

sw

imm

ing. W

e h

ave a

lso

been a

ble

to identify

dors

al

and a

nal fin w

ake s

tructu

res

and a

re b

egin

nin

g to b

uild

a

better

unders

tandin

g o

f how

th

ey inte

ract w

ith the w

ake

pro

duced b

y the c

audal fin.

An

ag

lyp

h o

f F

ig.

6B

, vie

w w

ith

3D

gla

sse

s.

DO

RS

AL

FIN

JE

T

FIS

H B

OD

Y