First published online August 9, 2007
Journal of Experimental Biology 210, 2767-2780 (2007)
Published by The Company of Biologists 2007
doi: 10.1242/jeb.000265
Fish biorobotics: kinematics and hydrodynamics of self-propulsion
George V. Lauder1,*,
Erik J. Anderson2,
James Tangorra3 and
Peter G. A. Madden1
1 Museum of Comparative Zoology, Harvard University, 26 Oxford Street,
Cambridge, MA 02138, USA
2 Department of Engineering, Grove City College, 100 Campus Drive, Grove
City, PA 16127, USA
3 Bioinstrumentation Laboratory, Massachusetts Institute of Technology, 77
Massachusetts Avenue, Cambridge, MA 02139, USA

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Fig. 1. (A,B) Bluegill sunfish Lepomis macrochirus, hovering in still
water, and (C) snowy grouper Epinephelus niveatus skeleton, showing
the positions of the major fins and their internal skeletal supports. The
pectoral and pelvic fins are paired, while the dorsal, anal and caudal fins
are median (midline) fins. The dorsal and anal fins of ray-finned fishes have
internal skeletal supports (pterygiophores), which support musculature that
moves the fin rays. Fin rays are labeled in yellow for the dorsal and anal
fins. The caudal fin also has a complex series of intrinsic musculature that
allows fishes to actively control tail conformation
(Drucker and Lauder, 2001 ;
Lauder, 1982 ;
Lauder, 1989 ). Metal
supporting elements for the grouper skeleton have been digitally removed for
clarity.
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Fig. 2. Motion of the pectoral fin in a bluegill sunfish (17 cm total length,
L) during steady locomotion at 0.5 L s–1.
Each row shows frames from simultaneous lateral, ventral and posterior digital
videos (taken at 250 Hz) at three time intervals, 97 ms (A), 142 ms (B) and
174 ms (C), during a single pectoral fin beat. Yellow arrows indicate the
major fin motions (smaller amplitude movements of the fin surface are not
labeled with yellow arrows), the small red and blue arrows show the position
of the upper (dorsal) and lower (ventral) pectoral fin edges respectively, and
the green arrow shows the location of the `dimple' on the dorsal fin margin
that forms as a wave of bending passes out along the fin from base to tip. The
large blue arrows and dot in A show the direction of water flow, which is
perpendicular to the page in the posterior view. Note the considerable
twisting and bending of the fin, and the cupped shape as the upper and lower
fin margins move away from the body at the same time (A: posterior view). The
fin beat begins at time 0 ms. Scale bars, 1.0 cm.
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Fig. 3. Hydrodynamic function of the pectoral fin in bluegill sunfish swimming at
0.5 L s–1, as seen in posterior view looking
upstream. A laser-generated sheet of light illuminates a thin slice of water
flow as well as the pectoral fin and body, which casts a shadow to the right.
Laser light penetrates the translucent fin, allowing flow between the fin and
the body to be quantified. Water flow in this figure is out of the page,
toward the reader. Images were obtained from 500 Hz digital video. (A–C)
Particle image velocimetry images showing the movement of the fin illuminated
by the laser light sheet in relation to the body and position of the other
fins. Duration of movement shown=0.48 s from panels A–C. Yellow arrows
show the key fin movements: note the cupped fin shape in A and B. (D–F)
Water flow patterns as a result of pectoral fin movement. This column is from
a different sequence than the frames in the left column. Yellow arrows
indicate water velocities (every other vector is shown), and the background
color scheme is coded so that black color indicates free stream flow velocity
(7 cm s–1), red color flow accelerated by the fin to greater
than free stream velocity, and blue color showing flow slowed below free
stream. Note that the pectoral fin accelerates flow on both the outstroke and
return stroke (red color in E and F).
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Fig. 4. Hydrodynamic analysis of the dorsal fin and caudal fin in swimming bluegill
sunfish, to show that these two fins can act as dual flapping foils in series,
and that flow leaving the dorsal fin can affect caudal fin function. The
caudal fin of ray-finned fishes does not move through undisturbed free stream
flow, but rather has its flow environment highly modified by upstream fins.
The left panels show the laser-imaged dorsal fin and tail of a bluegill
sunfish (16.5 cm L) swimming at 17 cm s–1; laser
light illuminates from top to bottom in these images, and the dorsal fin and
tail cast shadows toward the bottom. Yellow arrows in B show the
left–right oscillatory motion of the dorsal fin and tail as seen from
above. In the right panels these images are analyzed to show water flow
velocities around the fins (vectors were not calculated in the fin shadows)
and vorticity. The views shown in this figure are from above, looking down on
the upper surface of the fish with the dorsal fin and tail (also see
Fig. 1). In A, the dorsal fin
has shed a clockwise vortex that is moving toward the tail. This vortex passes
above the tail (B) while the dorsal fin sheds a new vortex of opposite sign on
the return stroke. This pattern repeats as a clockwise vortex is just leaving
the dorsal fin again (C). Note that flow in the gap between the dorsal fin and
tail is nearly orthogonal to free-stream flow. Free-stream flow has been
subtracted from the right panel images to reveal flow structure; images on the
left have been contrast-enhanced.
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Fig. 5. Schematic figure to illustrate two different categories of fish-like
aquatic robot design and the measurements that might be made from each design.
(A) Robot is attached to a sting (a rod holding the robotic model vertically
from the carriage above) and either fixed in place while forces are measured
on the sting, or towed at a fixed velocity on a moving carriage. In either
case, the robot is not self-propelled, but rather moves at externally imposed
speed. In this case, there need be no equality between thrust and drag forces,
as it is not known if the robot is generating sufficient thrust to overcome
drag. (B) Robot swims at a self-propelled time-averaged constant speed as a
result of thrust generated by heave and pitch motions, and mean thrust force
per cycle must equal the mean drag force. The flow speed in the tank is
adjusted to a value, Ueq, where the robot propels itself
at a constant equilibrium X position, termed Xeq.
The robot is free to move itself upstream and downstream on a low friction air
bearing system. Once Xeq is determined for a particular
heave and pitch motion pattern during self-propulsion, the robot can be fixed
in position at Xeq to measure forces and torques while the
same motion pattern and flow speed used for self-propulsion are imposed. This
allows force measurement under conditions identical to self-propulsion, when
thrust and drag forces must be equal.
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Fig. 7. Force in the X-direction (see
Fig. 5) reflecting thrust and
drag, measured from the robotic pectoral fin during a single fin beat under
three different imposed movement patterns (shown in different colors). Robotic
models of the pectoral fin allow analysis of the effects of different movement
patterns in a way not possible with studies of live animals alone. When the
fin executes a cupping motion only (black trace), a force curve with two
distinct peaks is produced with no drag force at the transition from outstroke
(abduction) to instroke (adduction). A cupping and sweeping motion (blue
trace) generates considerably higher thrust forces as well as a small drag
force during the transition. Moving the fin in sweep only (red trace),
produces large drag forces on the outstroke and roughly equivalent thrust on
the return stroke.
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Fig. 8. Design of the self-propelled dual flapping foil robot to study fish fin
function. (A) Carriage that holds the dual foils, with the heave and pitch
motors for each foil mounted above the flow tank on air bearings that allow
horizontal translation in the X-direction with little friction. This
design feature is critical to allowing self-propulsion. In this image, the two
foils are suspended above the flow tank. (B) Close view of the two foils (NACA
0012 in cross-sectional shape); the foils are 6.85 cm in chord length (width)
and 19 cm high. (C) Close view of the pitch and heave motors for one foil
mounted on the carriage and air bearing system.
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Fig. 10. Hydrodynamics of a single, flexible, flapping foil self-propelling at a
speed of 24 cm s–1. The white arrow shows the heave motion
(3.5 cm heave amplitude) of the rod that actuates the flexible foil, composed
of a plastic sheet of the same dimensions as the foils in
Fig. 9. Foil thickness is 0.32
mm, foil length=19 cm, foil height=6.8 cm, and the video sample rate is 250
Hz. The left panels show the flexible foil and water illuminated by a laser
light sheet from top to bottom; the flexible foil casts a shadow toward the
bottom of each image; these images have been contrast-enhanced. Large yellow
arrows in the left-hand panels show the direction of foil surface motion from
one panel to the next. The actuating rod to which the foil is attached and the
thin black foil itself have been enhanced by a white dot and line,
respectively, for clarity. In the right panels these images are analyzed to
quantify water flow velocities and vorticity around the flexible foil (vectors
could not be calculated in the fin shadows), as in the previous analysis of
two foil self-propulsion (Fig.
9). Note that an attached leading edge vortex (LEV) is visible at
0 ms as the foil leading edge nears the end of its downward motion and begins
to move up. This attached LEV persists throughout the duration of the
downstroke, until almost 930 ms (not shown). A distinct thrust wake is evident
behind the flexible foil, with a strong side component.
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© The Company of Biologists Ltd 2007