








Study with the several resources on Docsity
Earn points by helping other students or get them with a premium plan
Prepare for your exams
Study with the several resources on Docsity
Earn points to download
Earn points by helping other students or get them with a premium plan
Community
Ask the community for help and clear up your study doubts
Discover the best universities in your country according to Docsity users
Free resources
Download our free guides on studying techniques, anxiety management strategies, and thesis advice from Docsity tutors
aerodynamıcs notes for ırrotatıonal flow
Typology: Study notes
1 / 14
This page cannot be seen from the preview
Don't miss anything!
1 - 1
These presentations are prepared by
Dr. Cüneyt Sert
Department of Mechanical Engineering
Middle East Technical University
Ankara, Turkey
csert@metu.edu.tr
You can get the most recent version of this document from Dr. Sert’s web site.
Please ask for permission before using them to teach. You are not allowed to modify them.
1 - 2
2 𝑉
𝜇 𝑤𝑎𝑡𝑒𝑟 = 10
− 3 Pa s
𝜇 𝑎𝑖𝑟 = 2 × 10
− 5 Pa s
2
Exercise: Starting from the Euler’s equation derive the BE.
Airfoil
Viscous flow close to the object and in the
wake of it (non negligible shear forces)
Adapted from
http://web.cecs.pdx.edu/~gerry/class/ME
Inviscid flow away from the
object (negligible shear forces)
𝜉 = 2 𝜔 = 𝛻 × 𝑉 = 0 (irrotational flow)
or
𝑧
𝜃
𝑟
𝑟
𝑧
𝜃
𝜃
𝑟
𝑧
Vorticity (ksi) Angular velocity
Exercise: Sketch the developing flow inside a pipe with uniform entrance and
show the uniform and non-uniform flow regions.
1 - 5
𝑥
𝑦
𝑧
𝑢 = 𝑈
𝑤 = 0
Airfoil
Close to the body velocity gradients
are high, shear forces are high and
flow becomes rotational.
Away from the body, flow has small velocity
gradients (uniform-like flow), small shear
forces and can remain irrotational.
Uniform
approach
velocity
(irrotational)
rotation because
Exercise: Show how a fluid element will rotate inside the developing flow region
of a pipe with uniform entrance.
1 - 6
Airfoil
Uniform
upstream
flow
(irrotational)
In an inviscid flow, a fluid element
that originates from an irrotational
flow region will remain irrotational.
over an airfoil.
yield unrealistic results.
Exercise: What will happen if we assume pipe flow with uniform entrance to be
inviscid and irrotational?
Assuming external flow over a body to
be inviscid and irrotational everywhere
will result in zero air drag, which is not
correct. This is known as d’Alambert’s
paradox.
𝐹 drag =?
Note: There are other
factors that can cause
rotation, but they are
not as common as
viscous effects.
Exercise: Repeat the exercise of Slide 1-3 (derive BE) for irrotational flow.
necessarily two points on the same streamline.
1
3
𝑝
𝑉
2
1
=
𝑝
𝑉
2
2
=
𝑝
𝑉
2
3
Inviscid, irrotational
flow over an object
1 - 13
Exercise : The two-dimensional flow of a nonviscous, incompressible fluid in the
vicinity of a corner is described by the stream function
2 sin(2𝜃)
where 𝜓 has units of m
2 /s when 𝑟 is in meters. Assume the fluid density is
1000 kg/m
3 and the 𝑥𝑦 plane is horizontal.
a) Determine, if possible, the corresponding velocity potential.
b) If the pressure at point 1 on the wall is 30 kPa, what is the pressure at point 2?
Reference: Munson’s book.
𝑥
𝑦
𝜃
1
2
1 m
0.5 m
1 - 14
Exercise : A horizontal slice through a tornado is
modeled by two distinct regions. The inner or core
region ( 0 < 𝑟 < 𝑅) is modeled by solid body rotation.
The outer region (𝑟 > 𝑅) is modeled as an irrotational
region of flow. The flow is 2D in the 𝑟𝜃-plane, and the
components of the velocity field are given by
𝑉 𝑟 = 0 , 𝑉 𝜃 =
𝜔𝑟 0 < 𝑟 < 𝑅
𝜔𝑅
2
𝑟
𝑟 > 𝑅
where 𝜔 is the magnitude of the angular
velocity in the inner region. The ambient
pressure (far away from the tornado) is
equal to 𝑝 ∞
. Obtain the shown nondimen-
sional pressure distribution.
Reference: Çengel’s book.
𝑟
𝑥
𝑦
𝜃
Inner
region
Outer region
0 1 2 3 4 5
𝑟/𝑅
𝑝 − 𝑝 ∞
𝜌𝜔
2 𝑅
2
0
Inner
region Outer region
1
2
3
1
2
3
1
2
3
Potential flow 1 Potential flow 2 Potential flow 3
= 0 → 𝑓 = constant
Exercise : Show that streamfunction equation is 𝜓 = 𝑈𝑦
1 - 17
𝑥
𝑦
𝜙
=
𝜙
0
𝜙
=
𝜙
1
𝜓 = 𝜓 0
𝜓 = 𝜓 1
Exercise : Determine the equations of 𝜙 and 𝜓
for uniform flow in a direction making an angle
of 𝛽 with the 𝑥 axis.
𝑥
𝑦
𝛽
𝑈
outward in all directions with a total flow rate per depth of 𝑞.
𝑟 decreases with 𝑟, i.e. effect of source diminishes with 𝑟.
1 - 18
View from the top
𝑥
𝑦
Constant
𝜙 lines
Streamlines
𝑞 : Flow rate per depth
(Strength of source [m
2 /s])
𝑟
𝜃
𝑥
𝑦
𝑟
ln(𝑟) + 𝑓(𝜃)
𝜃
= 0 → 𝑓 = constant
ln(𝑟)
Exercise : Show that the streamfunction equation is 𝜓 =
𝑞
2 𝜋
use a negative 𝑞 value.
ln 𝑟 1
1
or equivalently using 𝑥 and 𝑦 coordinates
ln 𝑥 − 𝑎
2
2
arctan
Some useful relations
𝑥 = 𝑟 cos(𝜃)
𝑦 = 𝑟 sin(𝜃)
𝑟 = 𝑥
2
2
𝜃 = arctan
𝑦
𝑥
𝑥
𝑦
𝑟 1
1
𝑎
𝑟
(𝑥, 𝑦)
Exercise : Elementary components of a potential flow of water is shown below.
Find the velocity and pressure at point A if the pressure at infinity is 100 kPa.
1 - 25
Exercise : For the previous problem determine the equations of velocity potential
and streamfunction by superimposing elementary flows. Find the velocity at point
A by differentiating both 𝜙 and 𝜓 equation.
𝑈 = 3 m/s
𝑞 = 10 m
2 /s
𝑎 = 0. 8 m
𝑥 𝑏 = 0. 6 m
𝑦
Sink (−𝑞) Source (𝑞)
Exercise: Study the flow obtained by the combination of uniform flow in 𝑥
direction and a source at the origin. Obtain the location of the stagnation point(s)
and draw the stagnation streamline.
1 - 26
Uniform flow: 𝑢 = 𝑈 , 𝑣 = 0 , 𝜙 = 𝑈𝑥 , 𝜓 = 𝑈𝑦
Source: 𝑉 𝑟
𝑞
2𝜋𝑟
𝜃
𝑞
2 𝜋
ln 𝑟 , 𝜓 =
𝑞
2 𝜋
𝑥
𝑦
𝑈
𝑞
a body with a blunt nose.
stagnation streamline.
𝑥
𝑦
𝑠
Movie
Flow Over Half Body
𝑈
𝑞/2𝜋𝑟
Stagnation point
𝑠
Stagnation
streamline
Exercise : Consider the top part of a half body. Draw speed vs. 𝜃 and pressure vs. 𝜃
using the following values: 𝜌 = 1000 kg/m
3 , 𝑈 = 5 m/s , 𝑞 = 10 m
2 /s and
∞
= 100 kPa.
Exercise: A 64 km/h wind blows toward a hill that can be approximated with the
top part of a half body. The maximum height of the hill approaches 60 m.
a) What is the air speed at a point directly above the origin (at point 2)?
b) What is the elevation of point 2?
c) What is the pressure difference between point 2 and point 1 far from the hill?
Reference: Munson’s book
64 km/h
2
𝑥
60 m
1
𝑢𝑛𝑖
𝑠𝑜𝑢
𝑠𝑖𝑛𝑘
𝑞
2 𝜋
ln 𝑟 1
𝑞
2 𝜋
ln(𝑟 2
𝑢𝑛𝑖
𝑠𝑜𝑢
𝑠𝑖𝑛𝑘
𝑞
2 𝜋
1
𝑞
2 𝜋
2
1 - 29
𝑥
𝑥
𝑦
𝑐 𝑐
𝑟 1 𝑟 2 𝜃 1
𝜃 2
1 - 30
Exercise : Determine the location of the stagnation points of the shown Rankine
oval. Determine its length and thickness of the oval. Plot the variation of speed
and pressure (with respect to 𝑝 ∞ ) on it as a function of 𝜃.
𝑞
𝑥
𝑦
−𝑞
𝑐 𝑐
origin. Skipping the details we can get
𝑑𝑜𝑢𝑏𝑙𝑒𝑡
cos 𝜃 , 𝜓 𝑑𝑜𝑢𝑏𝑙𝑒𝑡
sin 𝜃
where 𝑑 is the strength of the doublet.
𝑟
2
cos 𝜃
𝜃
2
sin 𝜃
𝑥
𝑦
Constant 𝜙 lines
Streamlines
𝑢𝑛𝑖
𝑑𝑜𝑢𝑏𝑙𝑒𝑡
𝑑
2 𝜋𝑟
cos(𝜃)
𝑢𝑛𝑖
𝑑𝑜𝑢𝑏𝑙𝑒𝑡
𝑑
2 𝜋𝑟
sin(𝜃)
𝑥
𝑦
𝑑
1 - 37
Exercise : When a small circular cylinder is placed in a uniform stream, a
stagnation point is created on the cylinder. If a small hole is located at this point,
the stagnation pressure, can be measured and used to determine the approach
velocity, 𝑈 (similar to a Pitot tube).
a) Show how 𝑝 𝑠𝑡𝑎𝑔
and 𝑈 are related. Pressure far away is 𝑝 ∞
b) If the cylinder is misaligned by an angle 𝛼, but the measured pressure is still
interpreted as the stagnation pressure, use potential flow theory to determine an
expression for the ratio of the true velocity, 𝑈, to the predicted velocity, 𝑈′. Plot
this ratio as a function of 𝛼 for the range 0 ° < 𝑎 < 20 °.
Reference: Munson’s book.
𝑈
𝑅
Stagnation point
𝑈
𝛼
1 - 38
located at the origin,
2
2
cos 𝜃 +
2
2
sin 𝜃 −
ln 𝑟
radius 𝑅.
with 𝑅 = 𝑑/𝑈
𝑥
𝑦
𝑑
Γ
Exercise : For the flow shown above, obtain the following results
𝑉 𝜃 𝑐𝑦𝑙
= −2𝑈 sin 𝜃 +
Γ
2𝜋𝑅
𝑐𝑦𝑙
∞
𝜌𝑈
2
1 − 4 sin
2 𝜃 +
2Γ
sin 𝜃 −
Γ
2
Integrate the above pressure distribution to get the following results
𝑑𝑟𝑎𝑔
𝑙𝑖𝑓𝑡 = −𝜌Γ𝑈 (per unit depth)
𝑥
𝑦
𝑈
𝑑
Γ
𝑅
Γ
4 𝜋𝑈𝑅
< 1
Γ
4 𝜋𝑈𝑅
Γ
4 𝜋𝑈𝑅
= 1
White’s book
𝑅
Exercise: Determine the direction of
the lift force.
1 - 41
Γ
𝑈
𝑈
Γ
Top
𝑉 𝜃 𝑡𝑜𝑝
= − 2 𝑈 +
Γ
2𝜋𝑅
Opposite signs
Velocity is low.
Pressure is high.
Bottom
𝑉 𝜃 𝑏𝑜𝑡𝑡𝑜𝑚
= 2 𝑈 +
Γ
2𝜋𝑅
Same signs
Velocity is high.
Pressure is low.
1 - 42
Exercise : Magnus effect acts not only on cylinders but also on other rotating bodies
such as spheres. It can be used to explain how a spinning ball moves in a curved
trajectory. A football player wants to make a penalty kick as sketched below. Will a
CW or a CCW spin do the trick?
Exercise : Watch the following movies
https://www.youtube.com/watch?v=2OSrvzNW9FE (Suprising applications of Magnus effect)
http://www.youtube.com/watch?v=23f1jvGUWJs (Magnus force on Veritasium channel)
http://www.youtube.com/watch?v=2pQga7jxAyc (Enercon's rotor ship. Audio in German)
http://www.youtube.com/watch?v=wb5tc_nnMUw (Roberto Carlos knows the Magnus force)
due to Magnus effect correctly, it may give quite inaccurate values for its
magnitude. We’ll come back to this in the next chapter.
Exercise: In 1920s Anton Flettner built a series of rotor ships that are propelled
by rotating cylinders driven by electric motors. Read about Flettner’s ship at
rexresearch.com/flettner/flettner.htm and understand how it works.
One of Flettner’s original rotating cylinder ships https://en.wikipedia.org/wiki/E-Ship_
above, known as the Kutta condition.
𝑠 1
𝑠 2
1 - 49
solution.
2 𝜓
2
2 𝜓
2
= 0 , with proper boundary conditions
10 m/s
5 m/s
(0,1)
(0,2)
(1,1)
(2,0)
(3,0)
(3,2)
𝑥
𝑦
1 - 50
Bottom wall is a streamline. 𝜓
should be constant there. Let’s set
it to zero.
bottom
At the inlet 𝑢 = 10.
Therefore
𝜕𝜓
𝜕𝑦
𝜓 varies linearly from 0 to 10.
left
Top wall is a streamline. 𝜓 should be constant
there. In order to have 10 m
2 /s flow rate per
depth between the top and bottom walls
top
At the exit 𝑢 = 5.
Therefore
𝜕𝜓
𝜕𝑦
𝜓 varies linearly from 0 to 10.
𝜓 right = 5𝑦
1
2
4
Δ𝑥
Δ𝑦
𝑖, 𝑗
𝑖 + 1 , 𝑗 𝑖 − 1 , 𝑗
𝑖, 𝑗 + 1
𝑖, 𝑗 − 1
5 point computational stencil
𝑖+ 1 ,𝑗
𝑖,𝑗
𝑖− 1 ,𝑗
2
𝑖,𝑗+ 1
𝑖,𝑗
𝑖,𝑗− 1
2
𝑖+ 1 ,𝑗
𝑖− 1 ,𝑗
𝑖,𝑗+ 1
𝑖,𝑗− 1
𝑖,𝑗
transferred to the right-hand-side of the equation.
2 𝜓
2
𝑖,𝑗
2 𝜓
2
𝑖,𝑗
𝑖,𝑗
𝑖,𝑗+ 1
𝑖,𝑗− 1
𝑖,𝑗
𝑖+ 1 ,𝑗
𝑖− 1 ,𝑗
White’s book
𝝍 = 10.00 10.00 10.00 10.00 10.00 10.00 10.00 10.00 10.00 10.00 10.00 10.00 1 0.0 0 10.00 10.00 10.
8.00 8.02 8.04 8.07 8.12 8.20 8.30 8.41 8.52 8.62 8.71 8.79 8.85 8.91 8.95 9.
6.00 6.03 6.06 6.12 6.22 6.37 6.58 6.82 7.05 7.26 7.44 7.59 7.71 7.82 7.91 8.
4.00 4.03 4.07 4.13 4.26 4.48 4.84 5.24 5.61 5.93 6.19 6.41 6.59 6.74 6.88 7.
2.00 2.02 2.05 2.09 2.20 2.44 3.08 3.69 4.22 4.65 5.00 5.28 5.50 5.69 5.85 6.
𝝍 = 0 .00 0.00 0.00 0.00 0.00 0.00 1.33 2.22 2.92 3.45 3.87 4.19 4.45 4.66 4.84 5.
0.00 1.00 1.77 2.37 2.83 3.18 3.45 3.66 3.84 4.
0.00 0.80 1.42 1.90 2.24 2.50 2.70 2.86 3.
0.00 0.63 1.09 1.40 1.61 1.77 1.89 2.
0.00 0.44 0.66 0.79 0.87 0.94 1.
0.00 0.00 0.00 0.00 0.00 0.
Red ones are
boundary values Black ones are
calculated
can be calculated using the Bernoulli
equation.
modifications need to be done.
the central node. What can be done?
White’s book
𝜓 = 10
4
6
8
Lower wall
Upper
wall
𝐶 𝑝 =
𝑝 − 𝑝 𝑖𝑛
𝜌𝑉 𝑖𝑛
2 / 2
𝑉 𝑖𝑛
𝑖𝑛