Theodorsen theory for deformable airfoils full derivation
Transcript of Theodorsen theory for deformable airfoils full derivation
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0.1 Derivation of Theodorsen Aerodynamic Model
Theodorsen assumed the magnitude of oscillation to be small and the oncom-ing velocity to be constant. In the present work, Theodorsen model is slightlymodified to include time varying oncoming velocity and for large magnitude ofoscillation. It is assumed that the trailing wake is harmonic in this case.
Theodorsen model is developed for thin airfoils essentially a flat plate. Con-formal mapping is used to model the flow around a flat plate from the flowaround a 2D circle. The non-circulatory lift is generated with a source-sinksheet distributed along the chord. The strength of the source-sink sheet is de-termined from the boundary condition that there is no flow penetration throughthe surface of the airfoil. The circulatory lift is generated with a vortex sheeton the airfoil and in the wake that extends upto infinity. The strength of thevortex sheet is determined from the kutta condition that the flow leaves the
trailing edge smoothly.
The Joukowski conformal mapping that is used to map a circle of radius bcentered at the origin to a flat plate of semichord 2b is given by
x + iy = X+ iY +b2
X+ iY(0.1)
where(x, y)- mapped domain(flat plate)(X, Y)-unmapped domain(circle)
This transformation maps all points outside the circle to a location outside
the flat plate, points inside the circle to a location outside the flat plate but ondifferent Rieman surface, points on the circle to locations on the flat plate.For an airfoil, the deformation is given by
y =h
b+ x (0.2)
wherex and y are non-dimensionalized with respect to semi-chord(b).
y and h are positive downwards and is positive clockwose.
Non-Circulatory Flow
The Non-circulatory flow is represented by source-sink pair sheet.The net velocity potential due to source-sink sheet distributed along the chordof the flat plate is given by
=
1c
sourcesinkbdx1 (0.3)
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wherec is the location of the leading edge of flat plate.
The velocity potential at a point on the unit circle (X, Y) due to a sourceor sink placed at origin is given by
=
4log
X2 + Y2
(0.4)
where- Strength of source or sink(X, Y)- Spatial location in the unmapped domain(circle)
The velocity potential of a source or sink placed at (X1, Y1) is given by
=
4log(XX1)2 + (Y Y1)2 (0.5)
Putting the double source of strength of 2 at (X1, Y1) and a double sink ofstrength of2 at (X1,Y1) as shown in [1], we get the flow around a circle[Figure 0.1]. The combined velocity potential is obtained by the summation ofindividual potentials. The combined velocity potential in the unmapped domainis given by
=
2log
(XX1)2 + (Y Y1)2
(XX1)2 + (Y + Y1)2(0.6)
where is defined on a unit circle and it implies Y =
1X2 and Y1 =1X12.
Using Joukowski mapping, we map the points on the circle directly to locationson the flat plate.
x + iy = X+ i
1X2 + b2
X+ i
1X2(0.7)
x + iy = X+ i
1X2 + X i
1X2X2 + (1X2) (0.8)
x + iy = X+ i
1X2 + X i
1X2 (0.9)x = 2X (0.10)
By Joukowski transform of a unit circle, the flat plate domain is from 2 to 2.Applying change of variables to change the domain from
1 to 1, x becomes
2x.This implies
x = X (0.11)
Y =
1 x2 (0.12)
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Fig. 0.1: Conformal mapping of flat plate by a circle
Applying the transformation to [Eqn 0.6], we get the velocity potential due tosource-sink pair as
sourcesink =
2
log(x x1)2 + (y y1)2
(x x1)2
+ (y + y1)2 (0.13)
Put [Eqn 0.13] in [Eqn 0.3], we get
=
1c
2log
(x x1)2 +
1 x2
1 x122
(x x1)2 +
1 x2 +
1 x122 bdx1 (0.14)
The strength of source or sink as determined by the boundary condition thatthere is no flow penetrating the airfoil [Figure 0.2]. At the airfoil surface, thevelocity must be perpendicular to the surface and the velocity of the fluid flowingout of the source is the strength of the source. To satisfy this, the velocitygenerated by the source or sink must be equal and opposite to the componentof freestream minus the transverse motion of the airfoil.
v x
y = ty (0.15)
Changing to the non-dimensionalised quantities,
= v
xy + b
ty (0.16)
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wherev-free stream velocity
y-motion of the airfoil which is positive upwards non-dimensionalised with re-spect to semi-chord(b).
The motion of aileron is represented by
y = (x c) (0.17)
wherec-location of aileron hinge from the midpoint.
Fig. 0.2: Airfoil with no penetration boundary condition Ref.[2]
To account for the effect of flap deflection by an angle (positive clockwise), is replaced by
= v (0.18)Put [Eqn 0.18] in [Eqn 0.14], we get
=
1c
log(x x1)2 +
1 x2
1 x12
2(x x1)2 +
1 x2 +
1 x12
2 bdx1 (0.19)
From [1], we have1c
v2
log(x x1)2 +
1 x2
1 x12
2(x x1)2 +
1 x2 +
1 x12
2 dx1 =2 (x c) (log) N 2
1 x2 cos1 (c)
(0.20)
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where
N= 1 cx1 x21 c2x c (0.21)
The net velocity potential due to is
=v b
1 x2 cos1 (c) (x c)log N
(0.22)
where
N=1 cx
1 x2
1 c2
x c (0.23)
To account for the effect of flap deflecting at an angular velocity ddt is repre-
sented by = (x1 c) ddtb which gives
ddt =
1
c
(x1 c) ddtb2
log(x x1)2 +
1 x2 1 x122(x x1)2 +
1 x2 +
1 x12
2 bdx1 (0.24)From [1], we have
1c
(x1 c)log(x x1)2 +
1 x2
1 x12
2(x x1)2 +
1 x2 +
1 x12
2 dx1 =
1 x2
1 c2 cos1 (c) (x 2 c)
1 x2 + (x c)2 logN (0.25)
The net velocity potential due to ddt is
ddt =ddtb
2
2
1 x2
1 c2 + cos1 (c) (x 2 c)
1 x2 (x c)2 logN
(0.26)
To account for the effect of angle of attack of the airfoil , put c = 1 in [Eqn0.22] which gives
= v b
1 x2 (0.27)To take into account, the effect of airfoil in downward motion with a velocityddth, replace in [Eqn 0.27] by tan
1
d
dth
v
which gives
ddth(t) = tan1
ddthv
vb
1 x2 (0.28)
To account for the rotation of airfoil around a at an angular velocity ddt, weshould consider two cases.
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1. Effect of rotation of the entire airfoil around the leading edge obtained bysubstituting c =
1 in [Eqn 0.26].
2. Subtract the effect of the vertical velocity of the actual point of rotation
which is obtained by substitutingd
dt(1+a)b
v for in [Eqn 0.27] .
ddt =
1
2
d
dt
b2 (x + 2)
1 x2
d
dt
(1 + a) b2
1 x2 (0.29)
which gives
ddt =
d
dtb2
x2 a
1 x2 (0.30)
The various integrals evaluated are listed here.
1
c
dx =1
2bvT4 (0.31)
11dx =
1
2bv (0.32)
d
dt
11dx =
b
2
vd
dt +
d
dtv
(0.33)
1c
ddthdx =
12
bd
dthT4 (0.34)
11 ddthdx =
b
2 v tan1
ddth
v
(0.35)
d
dt
11 ddthdx =
b
2
d
dtv
tan1
ddth
v
+
b
2 v
d2
dt2h
v (ddth) ddtv(v)2
1 +( ddth)
2
(v)2
(0.36)1c
ddtdx =
d
dtb2T9 (0.37)
11 ddtdx =
12
d
dtb2 a (0.38)
d
dt
11 ddtdx =
12
d2
dt2b2 a (0.39)
1
c
dx =12
bv T5
(0.40)
11dx =
12
bv T4 (0.41)
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d
dt 1
1
dx = T4b
2 vd
dt+
d
dtv (0.42)1
c
ddtdx =
12
b2d
dtT2 (0.43)
11 ddtdx =
12
b2d
dtT1 (0.44)
d
dt
11 ddtdx =
12
b2d2
dt2T1 (0.45)
where T are Theodorsen constants which are given below.
T1 = 1/31 c2
2 + c2
+ c cos1 (c) (0.46)
T2 = c
1 c2
1 c2
1 + c2
cos1 (c) + c
cos1 (c)2 (0.47)
T3 =
1/8 + c2
cos1 (c)2
+ 1/4 c
1 c2 cos1 (c)
7 + 2 c2
1/8
1 c2
5 c2 + 4 (0.48)
T4 = cos1 (c) + c
1 c2 (0.49)
T5 = 1 + c2
cos1 (c)2
+ 2 c
1 c2 cos1 (c) (0.50)T6 = T2 (0.51)
T7 =
1/8 + c2
cos1 (c) + 1/8 c
1 c2
7 + 2 c2
(0.52)
T8 =
1/31 c
2 2 c2 + 1+ c cos1 (c) (0.53)T9 = 1/2p + 1/2 aT4 (0.54)
wherep = 1/3
1 c2
3/2T10 =
1 c2 + cos1 (c) (0.55)
T11 = cos1 (c) (1 2 c) +
1 c2 (2 c) (0.56)
T12 =
1 c2 (2 + c) cos1 (c) (2 c + 1) (0.57)T13 = 1/2T7 1/2 (c a)T1 (0.58)
T14 =1
16+
1
2ac (0.59)
Non-Circulatory Forces
The forces can be calculated by finding out the pressure difference and integrat-ing over the surface. Bernoulli equation for unsteady flow is given by
p0 = p + 1/2 V2 +
t (0.60)
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Applying for free stream condition, we get
p0 = p + 1/2 v2 (0.61)
where v is the free stream velocity.
Bernoulli equation is linearized for small disturbances along x and y namelyv
and w
respectively.
V =v + v
i + w
j (0.62)
V2 = v2 + 2 vv
(0.63)
The linearised Bernoulli equation is given by
pp = v
x +
t (0.64)
Non-dimensionalising x with respect to semi-chord b, we get
pp = v
b
x +
t
(0.65)
The pressure difference between the upper and lower surface is given by
p = 2v
b
x +
t
(0.66)
The lift is obtained by integrating the pressure difference over the entire airfoilas follows
LNC = b11pdx (0.67)
which gives
LNC = b2 v
d
dt +
d
dtv +
d
dtv tan1
ddth
v
b2 v
d2
dt2h
v d
dth ddtv
v2
1 +( ddth)
2
v2
ba d2
dt2
+ b2T4
vd
dt+
d
dtv
bT1
d2
dt2
(0.68)
which is positive downwards.The non-circulatory flow gives forces due to accelerations only.
Circulatory Flow
The non-circulatory lift force is derived by considering the boundary conditionthat there is no flow penetrating the airfoil. The non-circulatory flow model does
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not satisfy kutta condition which states that the flow should leave the trailingedge smoothly. The circulatory flow is developed using a vortex sheet on the
airfoil as well as in the wake that extends upto infinity as show in [Figure 0.3].These pair of vortices does not violate the no penetration boundary conditionas the normal velocities on the unit circle due to this vortex pair is zero.
Fig. 0.3: Vortex locations for the airfoil-aileron combination
The velocity potential of a point vortex is given by
=
2 tan1 Y Y1XX1 (0.69)
where is the Vortex strength(X, Y) is the spatial location in the unmapped domain(unit circle)(X1, Y1) is the location of point vortex in the unmapped domain
The combined velocity potential for a pair of point vortices, one outside cir-cle at a distance X0 and the other inside the circle at a distance
1X0
is givenby
=2
tan1
Y Y0XX0
tan1
Y Y0X 1X0
(0.70)
whereX and Y are spatial variables in the unmapped plane is the vortex strength at X0
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Using properties of tangents, the above equation gets simplified to
=2
tan1X0 1X0
Y
X2 X0 +
1X0
X+ Y2 + 1
(0.71)Applying Joukowski transformation,For X0,
x + iy = X0 +1
X0(0.72)
x0 = X0 +1
X0(0.73)
For 1X0 ,
x + iy =1
X0 +11
X0
(0.74)
x0 =1
X0+ X0 (0.75)
Both X0 and1X0
in the unmapped domain get transformed to the same locationx0 in the mapped domain.We have,
x0 =1
X0+ X0 (0.76)
2X= x (0.77)
The mapped domain is from -2 to 2 for x and from 2 to for x0. Apply changeof variables to change the domain for x from -1 to 1 and for x0 from 2 to , weget
x0 2x0 (0.78)x 2x (0.79)
This implies,
X0 +1
X0= 2x0 (0.80)
X= x (0.81)
Y =
1 x2
(0.82)
X0 = x0 +x02 1 (0.83)
1
X0= x0
x02 1 (0.84)
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Substitute [Eqns 0.81-0.84] in [Eqn 0.71], we get
=2
tan1
1 x2
x02 1
1 xx0
(0.85)
The Pressure difference between the upper surface and lower surface is given by
p = 2 v
x +
t
(0.86)
Since the disturbance is assumed to move with free stream velocity, we have
t = v
x0 (0.87)
The pressure difference is given by
p = 2 v
x +
x0
(0.88)
Non-dimensionalising x and x0 with respect to semi-chord b, we get the pressuredifference as
p = 2 vb
x +
x0
(0.89)
Using [Eqn 0.85], we get from [1],
2 x
=
x02 1
1 x2 (x0 x)(0.90)
2 x0
=
1 x2
x02 1 (x0 x)(0.91)
The pressure difference is given by
p = vb
1 x2
x02 1 (x0 x)+
x02 1
1 x2 (x0 x)
(0.92)
which gets simplified to
p = vb
(x0 + x)1 x2
x02 1
(0.93)
Now the lift force on the airfoil is obtained by integrating over the domain
LC = v
11
x0 + x1 x2
x02 1
dx (0.94)
LC = vx0
x02 1(0.95)
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Replacing with Ubdx0 where U is the strength of the vortex per unit lengthand integrating [Eqn 0.95] from trailing edge to infinity gives the circulatory
lift.LC = vb
1
x0Ux02 1
dx0 (0.96)
Similarly, the velocity potential of the vortex sheet is given by
0 = b
2
1
tan1
1 x2
x02 1
1 xx0
Udx0 (0.97)
Circulatory Forces
The Magnitude of vortex strength is determined by kutta condition which statesthat the flow should leave the trailing edge smoothly. In other words, velocitiesat the trailing edge should not be infinite.
For finite trailing edge angle(t.e > 0) as in [Figure 0.4], the velocities on theupper and lower surfaces must be tangential to their respective surfaces. Thisimplies the existence of two different velocities at the trailing edge. So, the onlyrealistic option is,
Vupper = Vlower = 0 (0.98)
Fig. 0.4: Flow around trailing edge- Kutta condition
Thus at x = 1,
x +
x ddth +
x +
x ddt +
x +
x ddt = finite = 0 (0.99)
At x = 1, 1 x2b
x =
1
2
1
Ux0 + 1x0 1
dx0 (0.100)
1 x2b
x = v (0.101)
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1 x2b
x ddth = v tan1
ddth
v(0.102)
1 x2b
x ddt = b (1/2 a)
d
dt (0.103)
1 x2b
x =
vT10
(0.104)
1 x2b
x ddt =
1
2
bddt
T11
(0.105)
Substituting the terms, the [Eqn 0.99] gives an important expression.
1
2
1
x0 + 1Ux0 1
dx0 =
v + v tan1ddth
v + b1
2 a
d
dt + v
T10
+
1
2
bT11ddt
= Q
(0.106)
Multiply [Eqn 0.96] by Q and divide it by 121
x0+1x01
Udx0 we get
LC = 2vbQ1
x0x021
Udx01
x0+1x01Udx0
(0.107)
which is positive downwards.
LC = 2vbQC(k) (0.108)where C(k) is the Theodorsen Lift deficiency function given by
C(k) =
1
x0x021
Udx0
1x0+1
x01Udx0
(0.109)
and its solutions are bessels function.
The complete expression for Lift is given by
L = b2 v
d
dt +
d
dtv +
d
dtv tan1
ddth
v
b2 v
d2
dt2h
v d
dth ddtv
v2
1 +( ddth)
2
v2
ba d2
dt2
+ b2T4 vd
dt+
d
dtv bT1
d2
dt2
2vbC(k) v + tan1
ddth
v
+b12 a
ddt
v
2vbC(k) vT10
+
1
2
bT11ddt
v
(0.110)
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which is positive downwards.
The above equation is the Theodorsen equation modified for varying oncom-ing air stream and for large magnitude of oscillations.
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BIBLIOGRAPHY
[1] Theodorsen, Theodore General theory of aerodynamic instability and themechanism of flutter, Technical report, National Advisory Committee forAeronautics, Technical report No. 496, 1934.
[2] Walker, William.Paul. Unsteady aerodynamics of deformable thin air-foils, Masters thesis, Virginia Polytechnic Institute, 2009.