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Transcript of [IEEE 2013 American Control Conference (ACC) - Washington, DC (2013.6.17-2013.6.19)] 2013 American...
Reduced-Order Modeling of Propulsive Vortex Shedding from a Free
Pitching Hydrofoil with an Internal Rotor
Phanindra Tallapragada Scott David Kelly
Abstract— The efficient development of control strategies forbiomimetic aquatic vehicles that exploit vortex shedding forpropulsion requires mathematical models that are sufficientlyrich to capture the necessary hydrodynamic phenomena whileremaining computationally tractable, and if possible while offer-ing some interface to analytical (in addition to computational)tools. In a sequence of recent papers, the authors have detailedan approach to modeling such systems that exploits certainidealizations to realize equations of motion that accommodatethe formalism of geometric mechanics on manifolds, andhave demonstrated the relevance of resulting models to actualrobotic systems. In the present paper, we describe an amendedapproach to modeling propulsive vortex shedding in the planethat retains critical features of previous models while providinga significant decrease in model dimension. We illustrate ourupdated approach by simulating the dynamics of a prototypicalfishlike swimmer comprising a free rigid hydrofoil that can beinduced to pivot about a body-fixed point through the oscillationof an internal rotor, shedding propulsive vorticity from itstrailing edge.
I. INTRODUCTION
The motion of a solid body through any fluid is influenced
by the fluid’s viscosity. The viscous boundary layer that
forms over the body’s surface reconciles the no-slip condition
at the surface with discrepancies between the velocity of the
body and that of the fluid nearby, and even a streamlined
body experiences drag as a result of shear in this boundary
layer. A body that isn’t entirely streamlined may experience
additional dynamic consequences from localized boundary
layer detachment. This phenomenon is essential to the de-
velopment of lift on a translating wing, for instance, which
requires boundary layer detachment to occur at the wing’s
trailing edge, imparting downward momentum to the air left
behind.
The forces associated with localized boundary layer de-
tachment from select contours on marine animals — for
instance, from the trailing edge of a tuna’s caudal fin or
from the lip of a medusa’s bell — are so significant that
qualitatively accurate models for marine animal locomotion
may be realized that prioritize these forces over all others
associated with fluid viscosity. Analogous models may be
used as the basis for the analysis and control of robotic
vehicles that rely on fin-like structures for propulsion and
steering.
This material is based upon work supported by the National ScienceFoundation under grant CMMI-1000652.
Phanindra Tallapragada and Scott David Kelly are with the Departmentof Mechanical Engineering and Engineering Science, University of NorthCarolina at Charlotte, Charlotte, NC 28223, USA.
Correspondence should be directed to [email protected].
At the trailing edge of a moving airfoil or hydrofoil, fluid
in the boundary layer is suddenly liberated both from the no-
slip condition and from the proscription on motion normal
to the foil. As a result, fluid rolls off the foil, potentially
(depending on the foil’s geometry) encountering fluid rolling
in the opposite sense off the foil’s opposite side. Fluid in the
wake of the foil thus acquires net vorticity, and the dynamic
influence of boundary layer detachment on the fluid as a
whole may be understood in terms of the dynamic creation
of this vorticity. The dynamic influence on the motion of
the body, meanwhile, may be understood in terms of the
forces required to reconcile the creation of vorticity with the
conservation of circulation around general material curves in
the fluid — according to Kelvin’s circulation theorem [1] —
and with the conservation of momentum overall.
The interpretation of fishlike swimming in terms of the
planar dynamics of a hydrofoil shedding vorticity from its
trailing point has a long history, dating at least to [2]. In
[3], [4], the second author and collaborators presented a
model for the fishlike swimming of a deformable foil realized
as the image of a circle under a time-varying Joukowski
transformation — a canonical conformal map generating a
foil with a cusp at its trailing point — and demonstrated
that a simple feedback law could be used to steer the foil
in the plane. The fluid surrounding the foil was assumed to
be inviscid and a Kutta condition was enforced periodically
in time to model boundary layer detachment at the trailing
point in a discretized way. This condition required that the
preimage of the trailing point correspond to a stagnation
point in the preimage of the flow under the Joukowski
map, and thus that the fluid separate smoothly from the
trailing point in the physical plane of the foil. With each
discrete application of the Kutta condition, a point vortex
was introduced to the fluid near the trailing point and an
impulsive change was made to the foil’s momentum so that
the desired fluid velocity was realized at the trailing point
without violating the conservation of momentum.
The present authors expanded upon the control design
from [4] in [5] and demonstrated its applicability to the
fishlike swimming of a real aquatic robot in [6]. The authors
then presented adaptations of the modeling approach from
[4] to the context of a planar bluff body shedding point
vortices from an arbitrary surface point [7] and to that of
a spherical body shedding vortex rings from an oscillating
circular surface contour [8], [9], the latter system reminiscent
of a swimming jellyfish.
In each of the papers cited in the preceding paragraph,
the assumption of an ideal fluid subject to a purely localized
2013 American Control Conference (ACC)Washington, DC, USA, June 17-19, 2013
978-1-4799-0178-4/$31.00 ©2013 AACC 615
Fig. 1. Acceleration from rest of a rigid hydrofoil shedding point vorticesin accordance with the periodic application of a Kutta condition at the foil’strailing cusp, subject to the simultaneous conservation of momentum. Thefoil pitches because of sinusoidal oscillations in the relative orientation of aninternal rotor. Shed vortices may differ from one another in absolute strengthas well as sign, but the sign and strength of each remain constant overtime. Blue vortices correspond to counterclockwise vorticity, red vortices toclockwise vorticity.
mechanism for vortex shedding represented a substantial
simplification of the true viscous hydrodynamics of the
system being modeled. Between vortex shedding events, each
model benefitted further from the presence of a Hamiltonian
structure in the equations governing the interaction of the
body with the existing singular distribution of vorticity, as
detailed in [10] for the two-dimensional case and in [11],
[12] for the three-dimensional case. Nevertheless, each of the
models presented in these papers suffered from an analytical
intractability resulting from the rapid increase in dimension
associated with a large number of vortex shedding events.
Fig. 1 illustrates this issue. The vehicle depicted appears
in none of the preceding references, but comprises a rigid
Joukowski foil with zero camber coupled to an internal rotor
that’s driven to oscillate sinusoidally relative to the foil.
The figure represents a single frame from a simulation of
the foil accelerating from rest in a fluid initially devoid of
vortices. In accordance with the periodic application of a
Kutta condition at the foil’s trailing cusp, vortices are shed
at frequent regular intervals throughout the simulation, each
imparting an impulsive change in momentum to the foil at its
instant of creation and each interacting with the foil thereafter
according to the Hamiltonian equations from [10]. Hundreds
of vortices are present in Fig. 1, each requiring the addition
of two ordinary differential equations to the description of
the system’s dynamics.
The behavior of the discrete vortices in Fig. 1 reflects the
behavior observed of vorticity shed continuously from a real
oscillating foil in a viscous fluid in a critical way. Groups
of vortices of similar sign are shed over alternating intervals
of time; each group is observed to “roll up” thereafter into
a coherent structure approximating a single vortex. As more
vortices are shed with additional oscillations of the foil, the
wake of the foil will come to resemble the inverse Karman
vortex street highlighted in [2] as a hallmark of fishlike
swimming.
This observation suggests a strategy for decreasing the
dimension of the model represented by Fig. 1. If frequently
shed vortices with relatively low strength reliably roll up,
at lower frequency, into approximations of vortices with
relatively high strength, then vortices of the latter kind might
as well be shed directly at lower frequency. In particular,
instead of introducing a sequence of vortices with like
sign and individually fixed strength with each sweep of the
foil through the fluid, we might allow a single vortex of
time-varying strength to adjust the fluid velocity as needed
throughout each sweep at the foil’s trailing point. With each
reversal of the foil’s motion, a change in sign occurs in the
shed vorticity; this might provide a criterion for fixing the
strength of the most recently formed vortex, releasing this
vortex to the foil’s wake, and beginning the shedding process
anew.
In fact, the approach just described has a long history of
its own, traceable to [13], but has traditionally been invoked
to model vortex shedding from solid boundaries executing
prescribed motions, and not from bodies moving according
to dynamic interactions with their wakes. A recent exception
appears in [14], in which vortices with time-varying strength
— so-called Brown-Michael vortices, named for the authors
of [13] — are used to model the wake of the falling flat plate
famously considered by Maxwell [15]. The presentation in
[14] encompasses more than just Maxwell’s example, but
focuses on the explicit computation of forces and moments
in determining the influence of a vortical fluid on a moving
body.
In the remainder of the present paper, we develop a
model for the self-propulsion of the vehicle from Fig. 1
shedding Brown-Michael vortices rather than the more nu-
merous fixed-strength vortices of our prior work. Unlike the
falling body considered in [14], this vehicle is driven by the
actuation of an additional degree of freedom as a control
input, and we determine its motion not by computing forces
or moments explicitly but by imposing the condition that
momentum be conserved in the system overall throughout the
vortex shedding process. We expect it to be straightforward
for us to adapt the method we describe both to the fishlike
swimming of the flexing foil from [3], [4] and to the
jellyfishlike swimming of the three-dimensional body from
[8], [9].
II. MODELING
A. Physical Model
Consider a Joukowski foil surrounded by fluid of unit
density that extends to infinity in a two-dimensional plane,
represented by the complex domain C. The geometry and
motion of the foil are described by mapping its boundary ∂Bin the physical space from a circle C of radius rc centered
at the origin in the mapped plane through the Joukowski
transformation
z = F (ζ) = ζ + ζc +a2
ζ + ζc, (1)
where ζc ∈ C and a ∈ R. We refer to the plane of the foil’s
motion as the foil plane and the plane of the circle’s motion
as the circle plane. For the shape of the foil shown in Fig.
2, ζc ∈ R. The preimage of the sharp trailing edge of the
foil is given by ζt = a−ζc. The transformation is conformal
616
Fig. 2. The Joukowski transformation maps a circle of radius rc in thecomplex ζ plane to the foil in the z plane.
everywhere in the open set |ζc| > rc. The derivative of the
transformation
F ′(ζ) = 1−a2
(ζ + ζc)2
exists everywhere except at ζt.The foil has three degrees of freedom; it can translate
with velocity U = (U1, U2) and rotate about its center with
angular velocity Ω. We suppose the foil to be coupled to
a balanced rotor with no direct coupling to the fluid, as
depicted in Fig. 1. Let the combined mass of the foil and
the rotor be m and the moment of inertia of the rotor about
its center be Ic.
B. Motion of the Point Vortices
The fluid is assumed to be ideal almost everywhere, with a
singular distribution of vorticity modeled by N point vortices
with circulations Γn located at points ζn in the circle plane.
We note that each such vortex is mapped to a vortex with
circulation Γn at zn = F (ζn) in the foil plane. Following
[16], the complex potential describing the velocity of the
fluid in a frame of reference collocated with the foil may
be decomposed in terms of its dependence on the translation
of the foil, the rotation of the foil, and each of the N point
vortices in the form
w(ζ) = W (z) = U1w1(ζ)+U2w2(ζ)+Ωw3(ζ)+N∑
k=1
wkv (ζ).
On the boundary of the circle, the real components φkv(ζ),
φ1(ζ), φ2(ζ), φ3(ζ) of the complex potentials wkv (ζ), w1(ζ),
w2(ζ), w3(ζ) satisfy the boundary conditions
∇φkv ·n = 0, ∇φ1 ·n = 0, ∇φ2 ·n = 0, ∇φ3 ·n = 0, (2)
where n is a vector normal to the boundary. The rigid-body
potential functions are given by
w1(ζ) =−r2cζ
+a2
(ζ + ζc),
w2(ζ) = −ı
(
r2cζ
+a2
(ζ + ζc)
)
,
w3(ζ) = −ı
(
r2cζ
(
ζc +a2
ζc
)
−
(
kζc +a2
ζc
)
a2
ζ + ζc
)
.
The potential function wkv (ζ) due to a point vortex located
at ζk outside a circular cylinder can be constructed according
to the Milne-Thomson circle theorem [17] in terms of an
image vortex of circulation −Γk located inside the cylinder
at r2c/ζk. Thus
wkv (ζ) =
Γ
2πı
(
log (ζ − ζk)− log
(
ζ −r2cζk
))
.
The image vortex inside the cylinder introduces a net circula-
tion around the cylinder, consistent with Kelvin’s circulation
theorem. This development of net circulation is essential to
the propulsion of the foil.
The kth vortex in the foil plane is simply advected under
the influence of the remaining N−1 vortices, of the N image
vortices, and of the motion of the foil itself, governed by the
potential function
Wk(z) = W (z)−Γ
2πılog (z − zk).
The corresponding motion of the vortex in the circle plane
is given by
ζk =
(
dWk
dz− (U1 + ıU2 + ıΩzk)
)
1
F ′(ζ). (3)
C. Motion of the Foil
If the fluid is initially at rest, the linear and angular
impulse in the system, which can be interpreted loosely as
the combined linear and angular momenta of the foil and the
fluid, are conserved [16]. The equations of motion for the
foil and vortices together assume the form of Lie-Poisson
equations, a class of noncanonical Hamiltonian equations. It
was shown in [10] that these take the form(
d
dt+Ω×
)
L = 0,
dA
dt+V × L = 0,
where L and A are the linear and angular impulse in foil-
fixed coordinates. The linear impulse is the sum
L = MV + Lv
of the impulse due to rigid-body motion of the foil and the
impulse due to the vortices. Here M is the total effective
mass of the foil, including added mass due to the fluid, and
Lv =
∮
∂B
r× (nb ×∇φv)ds+N∑
n=1
Γnrn × e3.
The angular impulse in the foil-fixed frame is given by
A = −1
2
N∑
n=1
Γn||rn||2
−1
2
∮
∂B
||r||2(nb ×∇φb + nb ×∇φv)ds. (4)
In the preceding equations, r = (Re(z), Im(z)) and nb is
the normal vector on ∂B pointing into the fluid. Equation (4)
can be simplified considerably — for details see [10], [18]
— to obtain a conservation law of the form
I
Vx
Vy
Ω
+
(
Lv
Av
)
=
(
RTL0
A− Icφ
)
, (5)
617
where L0 is the linear impulse of the system in spatially
fixed coordinates, R is the rotation matrix that transforms
body-fixed coordinates to spatially fixed coordinates, U =RV, and I is the total effective inertia tensor for the body,
including the added inertia due to the fluid’s motion. The
linear impulse Lv and angular impulse Av are functions of
the positions of the vortices alone and do not depend on their
velocity. They are given by
Lv = −
N∑
n=1
Γn
2πı
(
ζn −r2cζn
)
(6)
and
Av =1
2π
(
2r2c (ζc +a2
ζc)
ζn−
2a2(r2c − ζcζc)
ζc(ζn + ζc)−
2a4ζc(r2c − ζcζc)
(r2c − ζcζc)(ζn + ζc)
)
−1
2
N∑
n=1
ΓnZZn . (7)
The term Icφ has been added to right-hand side of (5)
to account for the spinning of the rotor. The exchange of
momentum between the foil and the vortices governs the
evolution of the system overall.
The velocity at any point in the fluid away from a vortex
in the circle plane is given by
ζ =
(
dW
dz− (U1 + ıU2 + ıΩz)
)
1
F ′(ζ).
The boundary conditions (2) allow fluid to slip along the
surface of the foil, but at the trailing edge of the foil, which is
a singularity of the Joukowski transformation, the derivative
F ′(ζ) vanishes, causing the velocity of the fluid in the circle
plane to become undefined. The only physically allowable
value for the fluid velocity at the trailing edge in the foil
plane is zero; this is the Kutta condition. The Kutta condition
requires that at the pre-image ζt of the trailing edge,
dw(ζ)
dζ
∣
∣
∣
∣
ζ=ζt
= 0.
This condition can be enforced at (frequent) regular intervals
through the shedding of new vortices, fixing the strengths of
these vortices in such a way that the total linear and angular
impulse are simultaneously conserved, as
I
∆Vx
∆Vy
∆Ω
+ ΓN+1
(
∆Lv
∆Av
)
= 0,
where (∆Vx,∆Vy,∆Ω) are impulsive changes in the veloc-
ity of the foil and (∆Lv,∆Av) are changes in the fluid
impulse corresponding to the addition of a vortex of unit
circulation. It follows that whenever a new vortex is added
to the fluid, the foil receives an impulsive kick. The addition
of each new vortex increases the dimension of the system
by two.
D. Reduced-Order Model
In simulations like the one that produced Fig. 1, the
dimension of the system increases into the thousands, pre-
senting computational challenges and obscuring qualitative
aspects of the system’s dynamics that could be exploited
for controlled propulsion. It’s possible, however, to model
the shedding of a point vortex with unsteady circulation
that adjusts continuously to enforce the Kutta condition and
the conservation of impulse. It’s intuitively clear that ΓN ,
the strength of the last shed vortex, might be adjusted in
a continuous fashion to satisfy the Kutta condition in a
persistent way, but it can be shown that merely changing ΓN
violates the conservation of momentum for the fluid enclosed
in a control volume around the points zt and zN [14]. To
compensate for the change in the momentum of the fluid
within this control volume, the position of the vortex must
evolve as well.
It was shown in [14] that the dynamics of an unsteady
vortex that satisfies the conservation of momentum of the
fluid can be described by the equation
zN +ΓN
ΓN
(zN − zt) =dWN (z)
dz, (8)
where zN is the location of the unsteady vortex. The addition
of the term Γ
Γ(zN −zt) conserves the momentum of the fluid
enclosed by any branch cut around zt and zN .
Because the rollup of a vortex sheet is permanent and
cannot be undone, the circulation of the unsteady vortex
described above should not decrease in magnitude. This
places an additional constraint on the evolution of ΓN .
When the absolute value of ΓN reaches a maximum, the
unsteady vortex is released and its circulation is held constant
thereafter. Vortex shedding occurs in the instant at which
ΓN ΓN < 0,
after which the shed vortex is treated as a steady vortex with
dynamics governed by (3).
As noted, the evolution of the circulation of the unsteady
vortex has to continuously satisfy the conservation of impulse
and the Kutta condition simultaneously, i.e.,
d
dt
dw(ζ)
dζ
∣
∣
∣
∣
ζ=ζt
= 0,
Id
dt
Vx
Vy
Ω
+d
dt
(
Lv
Av
)
=
(
0
−Icφ
)
.
(9)
Thus the evolution of the unsteady vortex and the motion
of the foil are governed by (1), (8), and (9) simultaneously
while the motion of the other (N − 1) steady vortices is
governed by (3).
III. SIMULATION
We consider two simulations of a rigid Joukowski foil
propelling itself through vortex shedding. In the first case
the foil sheds steady point vortices from its trailing edge at
regularly spaced instants in time, in the second the foil sheds
618
0 0.002 0.004 0.006 0.008 0.01 0.012−5
0
5
10
15x 10
−4
y
x
(a)
0 0.005 0.01 0.015 0.02 0.025 0.03 0.035 0.04−0.12
−0.1
−0.08
−0.06
−0.04
−0.02
0
θ(t
)
t
(b)
0 5 10 15 20 25 30 35 400
0.05
0.1
0.15
0.2
0.25
0.3
0.35
0.4
Γ(N
)
N
(c)
0 0.005 0.01 0.015 0.02 0.025 0.03 0.035 0.040
1
2
3
4
5
6
7
8
9
10
ΣΓ
(t)
t
(d)
Fig. 3. (a) Trajectory of the foil in the (x, y) plane, (b) heading angle ofthe foil versus time, (c) circulation of the most recently shed vortex versustime, and (d) total shed vorticity versus time for the model in which vorticityis shed discretely.
one Brown-Michael vortex. In each case the foil is driven by
a rotor that rotates such that
φ =π
6(1− cos (ωt)),
where ω ∈ 10, 20, 30, 40, 50.
Figs. 3 and 4 compare the two cases when ω = 50. The
first observation we make is that the total shed vorticity —
given byN∑
n=1
Γn in the first case and by the strength of the
first Brown-Michael vortex in the second — evolves similarly
in both cases. The time at which the first Brown-Michael
vortex reaches maximum circulation and is frozen is t1 =0.034. For the foil shedding steady vortices the time at which
the foil stops shedding positive vortices and begins shedding
negative vortices is t2 = 0.037.
The foil’s heading evolves almost identically in both cases,
but differences are apparent in the trajectories of the foil in
the (x, y) plane. The net displacement and the translational
velocity of the foil have a direct proportional dependence on
the positions of the shed vortices. Since the time intervals
we consider are small, the net displacement is small and
small variations in the positions of the vortices relative to
the foil can lead to large relative errors in the displacement
of the foil. Here we remark that the unsteady Brown-Michael
vortex preserves the constraint of the Kutta condition con-
tinuously in time with a small error. The discrete steady
vortex shedding mechanism preserves the constraint of the
Kutta condition only on a measure zero set of specific (but
frequent) time instants.
The angular motion of the rotor acts as a control input to
generate vorticity. The total circulation of the vortices and
their positions in turn completely determine the position,
0 0.001 0.002 0.003 0.004 0.005 0.006 0.007 0.008 0.009 0.010
0.2
0.4
0.6
0.8
1
1.2x 10
−3
y
x
(a)
0 0.005 0.01 0.015 0.02 0.025 0.03 0.035−0.12
−0.1
−0.08
−0.06
−0.04
−0.02
0
θ(t
)
t
(b)
0 0.005 0.01 0.015 0.02 0.025 0.03 0.0350
1
2
3
4
5
6
7
8
ΣΓ
(t)
t
(c)
Fig. 4. (a) Trajectory of the foil in the (x, y) plane, (b) heading angle ofthe foil versus time, and (c) total shed vorticity versus time for the modelin which vorticity is shed continuously.
orientation, and velocity of the foil. The position of the
Brown-Michael vortex in the second case and the center of
the corresponding cluster of steady vortices in the first are
almost the same; discrepancies in the total vorticity shed are
the key to discrepancies in the other simulated quantities.
This is clear from (6) and (7), which show that the total
vorticity has a significant influence on the values of Lv
and Av. We therefore proceed to compare the total vorticity
shed in the two cases when the rotor oscillates at different
frequencies ω.
This comparison is shown in Fig. 5. We observe that
in every case, the total circulation of the steady vortices
eventually exceeds the circulation of the unsteady vortex.
This discrepancy results in part from the fact that the Kutta
condition is satisfied continuously in one case but only
discretely in the other, and in part from a difference in the
way the location at which vorticity is added to the fluid
is determined in each case. For the steady-vortex model,
each new vortex is introduced midway along a circular arc
between the last shed vortex and the foil’s trailing edge, while
in the Brown-Michael model, new vorticity is added to the
fluid collocated with previously shed vorticity.
The computational advantage of the Brown-Michael model
is apparent in a comparison of the total number of vortices
shed in each case. When ω = 10, for instance, 185 vortices
are shed in the steady-vortex model, increasing the dimension
of the system’s state space over time to 373, while only the
first unsteady vortex develops in the Brown-Michael model,
for which the dimension of the state space remains 5.
ACKNOWLEDGMENT
The authors thank Jeff Eldredge for fruitful suggestions.
619
0 0.01 0.02 0.03 0.04 0.050
1
2
3
4
5
6
7
8Σ
Γ(t
)
t
(a) ω = 40
0 0.01 0.02 0.03 0.04 0.05 0.06 0.070
1
2
3
4
5
6
ΣΓ
(t)
t
(b) ω = 30
0 0.02 0.04 0.06 0.08 0.10
0.5
1
1.5
2
2.5
3
3.5
4
ΣΓ
(t)
t
(c) ω = 20
0 0.05 0.1 0.15 0.20
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
2
ΣΓ
(t)
t
(d) ω = 10
Fig. 5. Total shed vorticity versus time for different rotor frequencies ω.The red curve in each case is the circulation of the unsteady Brown-Michaelvortex and the blue curve is the running sum of the circulations of the shedsteady vortices. The running sum is shown only until the instant at whichvortices with negative circulation begin to be shed.
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