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First published online January 3, 2006
Journal of Experimental Biology 209, 238-248 (2006)
Published by The Company of Biologists 2006
doi: 10.1242/jeb.01974
Unifying constructal theory for scale effects in running, swimming and flying
1 Duke University, Department of Mechanical Engineering and Materials
Science, Durham, NC 27708-0300, USA
2 Pennsylvania State University, Department of Biology, University Park, PA
16802, USA
* Author for correspondence (e-mail: dalford{at}duke.edu)
Accepted 8 November 2005
| Summary |
|---|
|
|
|---|
, and
shows why these relations hold for running, flying and swimming. Animal
locomotion is an optimized two-step intermittency: an optimal balance is
achieved between the vertical loss of useful energy (lifting the body weight,
which later drops), and the horizontal loss caused by friction against the
surrounding medium. The theory predicts additional features of animal design:
the Strouhal number constant, which holds for running as well as flying and
swimming, the proportionality between force output and mass in animal motors,
and the fact that undulating swimming and flapping flight occur only if the
body Reynolds number exceeds approximately 30. This theory, and the general
body of work known as constructal theory, together now show that animal
movement (running, flying, swimming) and fluid eddy movement (turbulent
structure) are both forms of optimized intermittent movement.
Key words: design in nature, animal locomotion, optimality theory, optimal speed, maximum range speed, optimal frequency, stride frequency, wing beat frequency, Strouhal number, force output, scaling, allometry, turbulence, gravitational wave, constructal theory
| Introduction |
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|
|
|---|
In the absence of a theory that unifies design features across different
forms of locomotion, biologists have concentrated on potentially common
constraints. For example, Drucker and Jensen
(1996
) hypothesized that the
scaling of muscle shortening velocity for maximal power output during
oscillatory contraction (M-0.17;
Anderson and Johnston, 1992
)
might explain the common scaling of stride frequency. Numerous authors have
hypothesized that scale effects in locomotion are caused by constraints
related to biomechanical safety factors and the need to avoid premature
structural failure (McMahon,
1973
,
1975
;
Biewener and Taylor, 1986
;
Biewener, 2005
;
Marden, 2005
), or to maintain
dynamic similarity (Alexander and Jayes,
1983
; Alexander,
2003
).
Here we take the different approach of starting not with constraints but with general and presumably universal design goals that can be used to deduce principles for optimized locomotion systems. Our approach is approximate (order of magnitude accuracy) and is not intended to account for all forms of biological variation. Rather it predicts central tendencies. Furthermore, such a theory is not mutually exclusive of other hypotheses such as common constraints, because constraints have evolved within a design framework, i.e. perhaps theory can provide explanations for the nature of constraints.
The theory presented here follows from the more general constructal theory
of the generation of flow structure in nature (Bejan,
1997
,
2000
,
2005
). According to the
constructal law, in order for a flow system to persist (to survive) it must
morph over time (evolve) in such a way that it accomplishes the most based on
the amount of power or fuel consumed. The latest reviews show that the
constructal law accounts for spatial and temporal flow self-optimization and
self-organization in animate and inanimate natural flow systems (Bejan,
1997
,
2000
;
Poirier, 2003
;
Bejan and Lorente, 2004
).
Examples include river basins, lung design, turbulent structure,
vascularization, snowflakes and mud cracks.
How can constructal theory be applied to the streams of mass flow called
running, flying and swimming? In the same way that it has been applied to
design features of inanimate flow systems such as the morphing of river basins
and atmospheric circulation (Bejan,
1997
,
2000
), by examining how
locomotion systems can minimize thermodynamic imperfections (friction, flow
resistances) together, such that at the global level the animal moves the
greatest distance while destroying minimum useful energy (or food, or `exergy'
in contemporary thermodynamics; Bejan,
1997
). We show that this theoretical approach delivers in
surprisingly simple and direct fashion the body-mass scaling relations for
running, flying and swimmingthe complete relations, the slopes and the
intercepts, not just the exponents of the body mass.
There is a long and productive history of optimality models in analyses of
animal locomotion (e.g. Tucker,
1973
; Alexander,
1996
,
2003
;
Ruina et al., 2005
), so much
so that the term maximum range speed is part of the common vocabulary of the
field and instantly brings to mind a U-shaped curve of cost vs speed
on which there is one speed that maximizes the ratio of distance travelled to
energy expended. Our approach is similar in that it predicts maximum range
speeds, but differs from previous efforts by simultaneously predicting
stride/stroke frequencies and net force output, while being general across
different forms of locomotion. Like other optimality models, our theory does
not maintain that animals must act or be designed in the predicted fashion,
only that over large size ranges and diverse taxa predictable central
tendencies should emerge. Ecological factors will often favour species that
move in ways other than that which optimizes distance per cost, for example
where energy is abundant and the risk of being captured by active predators is
high. Evolutionary history and the chance nature of mutation can also restrict
the range of trait variation that has been available for selection. These and
other factors should act primarily to increase the variation around predicted
central tendencies.
|
| Running |
|---|
|
|
|---|
![]() | (1) |
Throughout this paper we use the method of scale analysis
(Bejan, 2004
), which consists
of solving the appropriate conservation equations as algebraic equations, with
the additional simplification that dimensionless factors of order 1 are
neglected. A first illustration of this method is in estimating the vertical
loss term W1/L, where L=Vt, and
t is the time scale of frictionless fall from the height of the run
(H), namely
t
(Hg-1)1/2. Since the
types of animal motion that we are considering are cyclical, with motion of
body parts along a roughly circular or oblong path and re-establishment of
starting positions at the beginning of each cycle, it follows that height
deviations, in this case the height of the run H, scales with the
body length scale
Lb=(Mb/
b)1/3,
where
b is the body density. In conclusion,
H
Lb and the vertical loss term becomes
W1/L=MbgH/Vt=MbgH/V(Hg-1)1/2,
which yields:
![]() | (2) |
The horizontal loss W2/L depends on what friction effect dominates the horizontal drag. Here we consider three different drag models, and show that because they are of similar dimension, the choice of friction model does not affect the predicted optimal speed significantly.
Assume first that the drag is dominated by air friction. The air drag
FD is on the order of:
![]() | (3) |
a is the air density. The horizontal loss of useful
energy is W2
FDL, which
means that W2/L is replaced by
FD in Eqn 1.
The total loss per unit length traveled is:
![]() | (4) |
.
The result is the optimal speed:
![]() | (5) |
b/
a)1/3
10, because
b
103 kg m-3 and
a
1 kg m-3. A compilation of velocity data
(Fig. 2A) for animals running
over a variety of terrains shows that the speeds and their trend are
anticipated well by Eqn 5. Note
that the same optimal speed as in Eqn
5 is obtained if one sets equal (in an order of magnitude sense)
the two terms appearing on the right side of
Eqn 4. In this way, we see that
to run at optimal speed is to strike a balance between the vertical loss (the
first term) and the horizontal loss (the second term). Optimal running means
optimal distribution of losses (imperfections) during locomotion. In this
regard it is noteworthy that human runners recover approximately 50% of
external kinetic energy and gravitational potential energy stored in elastic
tissues (Ker et al., 1987
|
µFs, where
the coefficient of friction µ is a number of order 1, F is the
normal force during the foot contact time tc, and
s is the foot sliding distance, s=Vtc.
The contact time scale is dictated by the impact that the body experiences in
the vertical direction, such that when the body makes contact with the ground
it is decelerated from its free fall velocity (gH)1/2 to
zero. Writing Newton's second law of motion,
F
Mb(gH)1/2/t, and using
H
Lb, we find
W2
µFs
µ[Mb(gH)1/2/t]Vt
µVMb
(gLb)1/2, such that
Eqn 1 becomes:
![]() | (6) |
The horizontal loss term
W2/L
µMbg
could have been evaluated more directly by recognizing
Mbg as the vertical force exerted by the
animal body on the ground, µMbg as the
horizontal friction force, and
µMbgL as the work destroyed by
ground friction along the travel distance L.
The monotonic function of V obtained for the total loss in
Eqn 6 indicates that there is a
lower bound for the optimal running speed. Minimum work per distance is
achieved when V exceeds the scale:
![]() | (7) |
Consider finally the model of a highly deformable ground surface such as
sand, mud or snow of density
(Fig.
1B). A `high enough' speed means that the accelerated terrain
material does not have time to interact by friction with and entrain its
neighbouring terrain material. This model is analogous to the behaviour of a
pool of fluid that is hit by a blunt body at a sufficiently high speed. In
summary, we assume that the sand behaves as an inviscid liquid when it is
suddenly impacted by a blunt body (the foot),
Fig. 1B.
The foot contact surface is A. The foot hits the ground with the
vertical Galilean velocity
Vy
(gLb)1/2. By analogy
with drag in high-Reynolds flow, the vertical force felt by the foot during
impact scales as
Fy
Vy2ACD,
where CD is a constant of order 1. The work done by the
foot to deform the sand vertically is Fy
, where
is the depth of the sand indentation. This work is the same as
W1, hence
Fy
MbgLb.
The foot also moves horizontally to the distance
through the sand. The
horizontal drag force is
Fx
V2A1/2
CD,
where CD
1 and A1/2
is the
frontal area of the foot as it slides horizontally through the sand. The work
destroyed by horizontal deformation of the sand is
W2
Fx
, where
=Vtc, and the time of contact with the ground is
tc
/Vy. Putting these
formulae together, we find
W2
V3Mb2/
A3/2
(gLb)1/2, and
Eqn 1 becomes:
![]() | (8) |
Vertical loss Horizontal loss
The optimal running speed for minimal work per unit of length traveled is:
![]() | (9) |
The simplest reading of this result makes use of the rough approximation
that animal bodies are geometrically similar (especially when compared over
large size ranges). In this case
(
A3/2/Mb)1/3 is a
factor of order 1 that does not depend on Mb.
Eqn 9 shows that the optimal
running speed or deformable ground is:
![]() | (10) |
The corresponding stride frequency scale is
topt
Vopt/Lb,
which yields:
![]() | (11) |
In sum, the effect of the horizontal friction model is felt through a
factor that is a dimensionless constant in the range 110, namely
(
b/
a)1/3 for air drag,
µ-1 for hard ground, and
(
A3/2/Mb)1/3 for
deformable ground. The optimal running speed is a remarkably robust result,
always on the order of
.
We propose that it is this robustness that accounts for the allometric law
connecting V with
and
frequency with
in animals of
so many different sizes and habitats (Fig.
2A,B).
The analysis is summarized by the observation that we have taken into account all the forces that the ground places on the leg and which dissipate through friction all the work done by the animal. We had to do this fully, without bias, without postulating that the forces are aligned with the leg or some other direction. The ground forces have one resultant, with two components, horizontal and vertical. The work dissipated by the horizontal component (W2) was estimated in three ways in the preceding analysis. The work dissipated by the vertical `friction' forces (W1) is known exactly: it is the kinetic energy stored in the body at the peak of its cycloid-shaped trajectory. We did not have to model the friction process on the vertical because we know its total effect: W1. This feature alone cuts through a lot of would be modelling, which is not relevant to the minimization of what counts, namely the total dissipation per cycle (W1+W2).
Additional support for this running theory comes from the calculation of
the vertical force F that propels Mb to the
height H during each cycle (Fig.
1C). The force F acts during a short time
t1, when the leg makes contact with the ground, and the
movement of Mb upward is governed by Newton's second law
of motion:
![]() | (12) |
![]() | (13) |
![]() | (14) |
![]() | (15) |
When t exceeds t1, the body continues to move
upward, reaching y=H at t=t2,
where dy/dt=0. Integrating
Eqn 12 with F=0, and
satisfying the continuity conditions,
![]() | (16) |
![]() | (17) |
![]() | (18) |
t3. Eliminating
t1 and t2 from the results derived
above, we obtain:
![]() | (19) |
![]() | (20) |
In conclusion, the force produced by the leg while running at optimal speed
is a multiple (of dimension 1) of the body weight. Below we show that the same
theoretical force characterizes flying and swimming.
Fig. 2C shows that these
predictions are supported by the large volume of data on the maximal force
produced by animal motors over sizes ranging from small insects to large
mammals (Marden and Allen,
2002
).
| Flying |
|---|
|
|
|---|
has been examined previously
using constructal theory, to predict speeds of animal and machine flight
(Bejan, 2000
(H/g-1)1/2.
During the same period, the work spent on overcoming drag is
W2
FDL, where
and CD
1. Cycles in which the vertical and horizontal losses
(W1, W2) alternate in order to
maintain cruising at constant altitude are sketched in
Fig. 3A. The total work spent
per distance traveled is:
![]() | (21) |
Lb. From Eqn
21 we learn that the spent work is minimal when
(Fig. 2A):
![]() | (22) |
Vopt/Lb,
or:
![]() | (23) |
![]() | (24) |
(
a/
b)1/3
10-1.
This agrees with the large volume on St data on animal flight
(Taylor et al., 2003
|
| Swimming |
|---|
|
|
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The new aspect of the present analysis of swimming is the vertical loss,
W1
MbgLb.
This work is spent by the fish in order to lift above itself the body of water
(Mw, the same as the fish mass because the fish and the
water have nearly equal density) that it displaces during one cycle. The
theory is that the product MwLb
represents W1/g, not that during each
cycle the fish lifts the mass Mw to the height
Lb. The duration of the cycle, t
(L
g-1)1/2, is the time in which the lifted
water mass falls, to occupy the space just vacated by the fish. During this
time, the fish (Mb) and its water-body partner
(Mw) can be thought of as a `big eddy' that will dissipate
W1 in time and space, in the wake. The fish mass
Mb is as much a part of the eddy as the water mass
Mw.
During the same time interval, the fish also overcomes drag by performing
the work W2
FDL, where
L
Vt
bV2L2CD
and CD
1. The fish body density
b is
the same as the water density. In sum, the total work spent per unit travel
is:
![]() | (25) |
![]() | (26) |
![]() | (27) |
The net force output for travel at the speed that minimizes work per
distance traveled is 2gMb. The force
2gMb plotted in
Fig. 2C is the order of
magnitude of the average force exerted by the fish, which is remarkably close
to the maximum force indicated by the empirical data in
Fig. 2C. The average force
scale 2gMb also holds for flying (eqn 9.49
in Bejan, 2000
,
p. 239), and is
comparable with the maximum force estimated in this article for running
(H/y1)gMb.
This is why in Fig. 2C the line
F=2gMb is compared with the force
data for all forms of animal locomotion. [Note that this differs from the
6gMb figure for motor force output
(Marden and Allen, 2002
;
Marden, 2005
) because in the
present case Mb refers to total body mass rather than
motor mass, and animal motors average about 2075% of body mass].
To put swimming in the same theory with flying and running
(Fig. 2) may seem
counterintuitive, because fish are neutrally buoyant and birds are not. This
`intuition' has delayed the emergence of a theory that unifies swimming with
the rest of locomotion. In reality, there are gravitational effects in
swimming just as in flying and running. Water in front of a moving body can
only be displaced upward, because water is incompressible and the lake bottom
and sides are rigid. Said another way, the only conservative mechanical system
(the only spring) in which the fish can store (temporarily) its stroke work
W1 is the gravitational spring of the water surface that
requires a work input of size
W1
Mbg
Lb.
Elevation of the water surface has been demonstrated and used in the field
of naval warfare, where certain radar systems are able to detect a moving
submarine by the change in the surface water height (termed the Bernoulli
hump) as it passes (unpublished US Naval Academy lecture;
www.fas.org/man/dod-101/navy/docs/es310/asw_sys/asw_sys.htm)
and is also evident in the data from recent studies that have examined water
movement patterns around swimming fish. A two-dimensional study of water
movement around the body of swimming mullet
(Müller et al., 1997
)
shows positive pressure in front of and around the head of the fish
(Fig. 4C), and suction on
alternating sides of vortices that form along the fish's posterior and in its
wake. Regardless of depth, this pressure around the head must raise the water
surface (at a very low angle except when the body is near the surface) over a
large area centered near the anterior end of the fish, and some of this raised
water subsequently falls into the vortices of the wake. A three-dimensional
study of the wake of fish with a homocercal (symmetrically lobed) tail
(Nauen and Lauder, 2002
) found
that there is a measurable downward force in these wake vortices, amounting to
about 10% of the thrust force, and that there is a downward force on the head,
which we interpret as the reaction force to the elevated water surface
(Fig. 4B).
|
The swimming cycle sketched in Fig.
3B is identical to that of a shallow-water gravitational wave of
depth Lb, wavelength 2Lb and
horizontal speed
V
(gLb)1/2, which
is also the speed of a hydraulic jump. This is not a coincidence. The fact
that this wave speed is the same as the optimized swimming speed
(
)
and the observed swimming speeds of fish
(Drucker and Jensen, 1996
) and
marine mammals (Rohr and Fish,
2004
) (Fig. 2A) provides additional support for the theory that, fundamentally, swimming is an
optimized intermittent movement in the gravitational field, like flying and
running.
To summarize, in order to advance horizontally by one body length, the fish lifts the equivalent of a body of water of the same size as its body, to a height equivalent to the body length. What the fish does (tail flapping) is felt by the hard bottom of the lake. The hard crust of the earth supports all the flappers and hoppers, regardless of the medium in which the particular animal moves.
| Comparison of model predictions against empirical data |
|---|
|
|
|---|
b]1/3), but small and
statistically significant deviations from this assumption tend to be the rule
rather than the exception throughout the literature on animal scaling.
Wingspan of birds shows a particularly large divergence from geometrical
similarity, scaling as
(Rayner 1987
|
| Concluding remarks |
|---|
|
|
|---|
All animals, regardless of their habitat (land, sea, air) mix air and water
much more efficiently than in the absence of flow structure. Constructal
theory has already predicted the emergence of turbulence, by showing that an
eddy of length scale Lb, peripheral speed V and
kinematic viscosity
transports momentum across its body faster than
laminar shear flow when the Reynolds number
LbV/
exceeds approximately 30 (cf. chapter 7
in Bejan, 2000
). This agrees
very well with the zoology literature, which shows that undulating swimming
and flapping flight (i.e. locomotion with eddies of size
Lb) is possible only if
LbV/
is greater than approximately 30
(Childress and Dudley,
2004
).
And so we conclude with a promising link that this simple physics theory reveals: the generation of optimal distribution of imperfection (optimal intermittency) in running, swimming and flying is governed by the same principle as the generation of turbulent flow structure. The eddy and the animal that produces it are the optimized `construct' that travels through the medium the easiest, i.e. with least expenditure of useful energy per distance traveled.
| Appendix |
|---|
|
|
|---|
(Mb/
b)1/3.
We covered a large territory with this simple first step, and we can do more
if we adopt a slightly more complex model. One reason for trying this next
step is that some of the scatter (discrepancies) between the present formulae
and speed and frequency data can be attributed to changes in body shape as
body mass increases. Another reason is to show how the present theoretical
approach can be used in future studies of more complicated living systems and
processes.
Consider the analysis shown for flying in Eqn
21,
22,
23, but instead of the
one-length body description (Lb), recognize that the
geometry of a large bird with its wings spread out (flapping or gliding) is
better captured by two length scales: the wing span Lb,
which is horizontal, and the body or wing thickness, Yb,
which is vertical. By making this change, we are saying that the flying bird
looks more like a flying saucer (volume
) than a sphere
(volume
). The body mass scale is:
![]() | (A1) |
is the geometric shape ratio of the two-scale body:
![]() | (A2) |
Next, we redo the analysis leading to Eqn
21. As before, for the W1/L term we
use H
Lb. To estimate FD, we use
LbYb in place of
Lb2, so that the second term on the right side
of Eqn 21 reads
aV2LbYb.
In place of Eqn 22 and
23 we find:
![]() | (A3) |
![]() | (A4) |
Flying bodies have smaller shape ratios (
) when they are larger.
This is true of insects, birds and airplanes alike. The fluid mechanics
reasons for why this trend must exist deserve a study of their own. Here, we
accept empirically the notion that
decreases as M increases,
and write that in a narrow enough range of large M values,
behaves as:
![]() | (A5) |
), which appears
in Eqns A3 and
A4, behaves as
Mm, where m>1 because m=1+a. In conclusion, the
M effect in Eqn A3 and
A4 is:
![]() | (A.6) |
![]() | (A.7) |
rather than
(Table 1; Rayner, 1987In conclusion, the accuracy of the theoretical approach presented in this paper can be improved by basing it on more realistic (multi-scale) body geometries.
List of symbols and abbreviations:
scales with body mass





a
b
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