aoe 2104--aerospace and ocean engineering fall 2009
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AOE 2104--Aerospace and Ocean Engineering Fall 2009. AOE 2104 Introduction to Aerospace Engineering. Lecture 2 Basic Aerodynamics. Virginia Tech. Lecture 2. 1 September 2009. AOE 2104--Aerospace and Ocean Engineering Fall 2009. - PowerPoint PPT PresentationTRANSCRIPT
AOE 2104--Aerospace and Ocean Engineering Fall 2009
Virginia Tech 1 September 2009Lecture 2
AOE 2104
Introduction to Aerospace Engineering
Lecture 2Basic Aerodynamics
Virginia Tech
Reminder: The first homework assignment (paper copy) is due AT THE BEGINNING OF
NEXT CLASS!!
Also I would appreciate any feedback on the class that you have. You are welcome to see me after class, tell me during class, or send me an
email.
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
3 steps to determine p, r, and T at any altitude ?
2 equations used to construct the standard atmosphere model ?
Name and define the different types of altitudes.
2 types of regions found in the temperature variations with altitude and their characteristics ?
Any questions ?
Standard Atmosphere
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Basic Aerodynamics
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Basic Aero – Why? How? What do we have so far?
Why are we looking into aerodynamics?To determine the forces acting on a vehicle in flightRemember aerodynamic forces arise from two natural phenomena
How are we going to proceed ? Using Laws of Physics to quantify the interaction between the vehicle and the environment it is evolving in.
What do we have so far ?
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Our Aerodynamic Tool Box
Four aerodynamic quantities that define a flow field
Steady vs unsteady flow
Streamlines
Sources of aerodynamic forces
Equation of state for perfect gases
Hydrostatic Equation
Standard Atmosphere Model
6 different altitudes
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Aerodynamic Tools Needed: Governing Laws
We are going to need the 3 following physical principles to describe the interaction between the vehicle and its associated flow field:
Conservation of MassContinuity Equation (§§ 4.1-4.2)
Newton’s 2nd Law (and Conservation of Momentum)
Euler’s and Bernoulli’s Equations (§§ 4.3-4.4)
Conservation of EnergyEnergy Equation (§§ 4.5-4.7)
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Conservation of Mass – The Continuity Equation
Physical Principle:Mass can neither be created nor destroyed (in other words, input = output).
Eq.(4.2)
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Streamline
A streamline is a line that is tangent to the local velocity vector.
If the flow is steady, the streamline is the path that a particle follows.
v v
v
v
v
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Remarks on Continuity
The equation we just derived assumes that both velocities and densities are uniform across areas 1 and 2.
In reality, both velocities and densities will vary across the area
Continuity Equation is extensively used in the design and operation of wind tunnels and rocket nozzles (we will see how later).A stream tube is delimited by 2 streamlines and does not have to be bounded by a solid wall.
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
AOE 2104--Aerospace and Ocean Engineering Fall 2007
Virginia Tech
Compressible Versus Incompressible Flows
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Continuity for Incompressible Flows
• All fluids are compressible in reality.
• However, many flows are “incompressible enough” so that the incompressibility assumption holds.
• Incompressibility is an excellent model for Flows of liquids (e.g. water and oil)Air at low speed (V < 100 m/s or 225 mi/h)
• Equation of Continuity for Incompressible Flows reduces to
• So that if A2 < A1 then V2 > V1.
1
2
2
1
VV
AA
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Continuity – Sample Problem 1
A convergent duct was found in the basement of Randolph. The inlet and exit areas are measured to be Ai = 5m2 and Ae = 2m2. Assuming we use this duct with an inlet velocity of Vi = 9 mi/h, find the exit velocity.
First, we need to be consistent with the unit system. Let’s work in SI units.Vi = 9 mi/h = 9x1609/3600 m/s Vi = 4 m/s.Vi << 100 m/s so the flow is considered incompressible.
From Incompressible Continuity, Therefore, the exit velocity will be 10 m/s.
10m/sV425V
AAV ei
e
ie
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Continuity – Sample Problem 2
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Momentum Equation
Continuity is a great addition to our toolbox, however it says nothing about pressure.
Why is pressure important? Let’s look at Newton’s 2nd Law:Sum of the forces = Time rate of change of momentum
F = d(mv)/dtF = m dV/dt assuming m = const.F = m a
The pressure is going to translate into force, which by Newton’s 2nd Law results in change of momentum. Assuming incompressibility (m = const), this will result in change of velocity (thus impacting performance for example).
To find momentum, simply apply F = ma to an infinitesimally small fluid element moving along a streamline.
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Assume fluid element is moving in the x-direction.3 types of force act on the element:
• Pressure force (normal to the surface) p• Shear stress (friction, parallel to the surface) tw
• Gravity r dxdydz gIgnore gravity (smaller than other forces) and assume inviscid flow (non-viscous i.e. no friction), balance of the forces on x.
vO
Streamline
p F = ma
dxdz
dydx
dxdpp
Momentum Equation – Free Body Diagram
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Momentum Equation – Force Balance
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Momentum for Incompressible Flows – Bernoulli’s Equation
• For incompressible flows, r = const.
• Integrating Euler’s equation between 2 points along a streamline gives:
• This equation is known as Bernoulli’s Equation.
streamline a along
wordsother in
as rewritten be can which
02
211
222
21
2212
pconstρV21p
ρV21pρV
21p
VV21ρpp
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Description of Bernoulli’s Equation
02 pρV
21p
Static Pressure• Pressure felt by an object or person suspended in the fluid and moving with it.• Can be thought of as internal energy.
Dynamic Pressure• Pressure due to the fluid motion.• Can be thought of as kinetic energy.
Total (stagnation) Pressure• Pressure that would be felt if the fluid was brought isentropically to a stop.• Can be thought of as total energy.
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
3 New Tools – Continuity, Euler, and Bernoulli’s Equations
• Continuity Equationr A V = constAssumptions: steady flow.
• Euler’s Equationdp = - r V dVAssumptions: steady, inviscid flow.
• Bernoulli’s Equation
Assumptions: steady, inviscid, incompressible flow along a streamline.
Euler and Bernoulli’s equations are essentially applications of Newton’s 2nd Law to fluid dynamics.
02 pρV
21p
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Momentum Equations - Sample Problem 1
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Momentum Equations - Sample Problem 2
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Practical Applications
By combining Continuity, Euler, and Bernoulli’s equation, one can obtain the velocity at any point on an aircraft assuming surrounding conditions are known (either through measurements or using Standard Atmosphere).
Two major applications for this:Low-Speed Subsonic Wind Tunnel testing/designingFlight measurements of velocity
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Low-Speed Subsonic Wind Tunnels (§4.10)
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Wind Tunnel Calculations
• From Bernoulli, between points 1 and 2:
• Using Continuity:
• Combining the two, we get:
• Since the ratio of throat to reservoir area (A2/A1) is fixed for wind tunnel and r is constant for low-speed (incompressible) flows, the quantity driving the tunnel is p1-p2.
• But how can we determine p1-p2 ???
2
12
212
AA1ρ
pp2V
21
21 V
AAV
2121
22 Vpp
ρ2V
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Manometer
fluid. ofheight the toalproportiondirectly is difference pressure that themeans thisfluid, reference for theconstant is since
fluid. reference theof e)unit volumper (weight weight specific theis where,
whwpp
gρwhwAApAp
21
f21
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Wind Tunnels – Sample Problem 1
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Wind Tunnels – Sample Problem 1 Solution
2
12
212
AA1ρ
pp2V
31
5
1
11 1.29kg/mρ
300287)10(1.011.1
RTpρ
• Height of liquid: h = 10cm = 0.1m• Specific weight of liquid mercury: w = (1.36x104)x9.8 = 1.33x105 N/m2
• Actual pressure difference: p1-p2 = w h = 1.33x104 N/m2.• To find V2 from Bernoulli, use
• We computed p1-p2, A1/A2 = 15 is given, so we need to find r.• Since we are in a low-speed wind tunnel, flow is incompressible, so r = const, which
means we can compute it at any point in the tunnel. Since p1 and T1 are given, use Equation of State to find r = r 1:
• Combining all the results we get V2 = 144 m/s (slightly over the incompressible velocity limit, which means compressibility effects should be taken into account).
2
12
212
AA1ρ
pp2V
31
5
1
11 1.29kg/mρ
300287)10(1.011.1
RTpρ
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Measurement of Airspeed (§4.11)
Bernoulli’s equation provides an easy method for determining the velocity of any fluid
Therefore, we need to know p and p0
ρ
pp2V 0
RTpρ
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Total (stagnation) Pressure (p0 ) Measurement
• The total pressure is easy to measure if the flow direction is known. An opened-
end tube aligned with the flow direction is enough. This type of tube is called
"Pitot probe”(named after Henri Pitot who invented it in 1732; see §4.3 for historical
background)
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Static Pressure (P) Measurement
The static pressure is also easy to measure using a tube with a close end and
pressure taps around its circumference.
“Static probe”
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Dynamic Pressure Measurement
Finally, it is possible to measure directly the difference between stagnation and static pressure by combining the Pitot and static probes into a Pitot-static probe (!).
“Pitot-Static probe”
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Airspeed Indicator
r
)0(2 ppv
SLind
ppv
r
)0(2
If the only known density is at sea level,
“Indicated or Equivalent Airspeed”
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
True Airspeed
alttrue
ppv
r
)0(2
Therefore, the relationship between true and indicated airspeed is:
and SL
ind
ppv
r
)0(2
21
alt
SLindtrue vv
rr
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
www.aeromech.usyd.edu.au/ aero/instruments/ http://www.tech.purdue.edu/at/courses/aeml/airframeimages/pitottube.jpg
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
www.aeromech.usyd.edu.au/ aero/instruments/ http://home4.highway.ne.jp/t-park/tp/image/seventh/s-port.jpg
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
Measurement of Airspeed – Sample Problem
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
From Standard Atmosphere (App. B), at 5000ft, p = 1761 lb/ft2.Pitot tube measures stagnation pressure so p0 = 1818 lb/ft2.
Density is found from measured temperature and tabulated pressurer = p/(RT) = 1761/(1716*505) r = 2.03x10-3 slug/ft3.
sftVpp
V truealt
true /2371003.2
)17611818(2)0(23
r
sftVpp
V indsea
ind /21910377.2
)17611818(2)0(23
r
7.6% difference
Measurement of Airspeed – Sample Problem Solution
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2
Virginia Tech
For Next Class: Review Chapter 4 and let me know what questions you have
Thursday: HW 1 due. Stay Tuned for HW 2.
AOE 2104--Aerospace and Ocean Engineering Fall 2009
1 September 2009Lecture 2