lecture-15 - flight dynamics-i · ρ(h) = atmospheric density (a function of height) v = relative...

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Lecture Lecture Lecture Lecture – 15 15 15 15 Overview of Flight Dynamics Overview of Flight Dynamics Overview of Flight Dynamics Overview of Flight Dynamics – I Prof. Radhakant Padhi Prof. Radhakant Padhi Prof. Radhakant Padhi Prof. Radhakant Padhi Dept. of Aerospace Engineering Indian Institute of Science - Bangalore Optimal Control, Guidance and Estimation Aircraft Designs Aircraft Designs Aircraft Designs Aircraft Designs Prof. Radhakant Padhi Prof. Radhakant Padhi Prof. Radhakant Padhi Prof. Radhakant Padhi Dept. of Aerospace Engineering Indian Institute of Science - Bangalore

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Page 1: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

Lecture Lecture Lecture Lecture –––– 15151515

Overview of Flight Dynamics Overview of Flight Dynamics Overview of Flight Dynamics Overview of Flight Dynamics –––– IIII

Prof. Radhakant PadhiProf. Radhakant PadhiProf. Radhakant PadhiProf. Radhakant Padhi

Dept. of Aerospace Engineering

Indian Institute of Science - Bangalore

Optimal Control, Guidance and Estimation

Aircraft DesignsAircraft DesignsAircraft DesignsAircraft Designs

Prof. Radhakant PadhiProf. Radhakant PadhiProf. Radhakant PadhiProf. Radhakant Padhi

Dept. of Aerospace Engineering

Indian Institute of Science - Bangalore

Page 2: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore3

First to Fly

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore4

Wright Brothers

Page 3: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore5

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore6

Page 4: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore7

Commercial Aircrafts

� High Lift/Drag ratio

� High fuel efficiency

� High reliability & safety

requirements

� Good handling quality

and passenger comfort

� All weather operational

capability

� Speed and agility

(maneuverability) are

not critical

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore8

Page 5: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore9

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore10

Geometry of Conventional Aircrafts

Page 6: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore11

� On the tailless aircraft the pitch controls and roll controls must both be on the wing. There can be separate elevators and ailerons or they can be combined into one set of controls known as Elevons and still usually has a vertical Fin with a rudder

Tailless Aircraft

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore12

Canard Aircraft

� Horizontal stabilizer and elevators are in front.

� Advantage: Better control characteristics (including elimination of the non-minimum phase behavior)

� Drawback: Disturbed flow pattern over the body, good aerodynamic modeling is difficult.

Page 7: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

Force Balance in Flying VehiclesForce Balance in Flying VehiclesForce Balance in Flying VehiclesForce Balance in Flying Vehicles

Prof. Radhakant PadhiProf. Radhakant PadhiProf. Radhakant PadhiProf. Radhakant Padhi

Dept. of Aerospace Engineering

Indian Institute of Science - Bangalore

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore14

Basic Force Balance

� Weight

� Lift

� Drag

� Thrust

Page 8: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore15

Lift

� Lift is generated by differential pressure

on upper and lower side of the wing

Lift

Lift

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore16

Page 9: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore17

Lift

ρ(h) = atmospheric density (a function of height)

V = relative velocity of air

S = wetted surface area

= coefficient of lift

21

2L LL q S C V S Cρ

= =

LC

21 : Dynamic Pressure

2q Vρ

=

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore18

Dynamic pressure

Total pressure of any fluid

= static pressure + dynamic pressure

21

2gh Vρ ρ= +

Dynamic pressure of a fluid represents its kinetic energy

Page 10: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore19

Atmospheric density

0 0( )

0

g h h

RTeρ ρ

− − =

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore20

Angle of attack

AOA

Page 11: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore21

Coeff. of Lift vs Angle of attack

2

L

1L = V S C

Lift coefficient

Stall

Region

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore22

Drag

= Coefficient of drag

= profile drag + induced drag

0

2 D LC K C= +

21

2DD V S Cρ

=

DC

Page 12: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore23

Mach Number

V = velocity of object relative to medium

C = velocity of sound in the medium

= velocity of sound in air = 340 m/s at 250 C

M < 1 Subsonic

M = 1 Sonic

0.8 < M < 1.2 Transonic

1.2 < M < 5 Supersonic

M > 5 Hypersonic

PC RT

γγ

ρ= =

/M V C=

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore24

Drag vs Mach number

Page 13: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore25

Drag

� Skin friction drag

� Pressure drag

� Induced drag

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore26

Skin friction drag

� It is caused by the interaction of the air particles against the surface of the aircraft. For the airplane, skin fiction drag can be reduced, by keeping an aircraft's surface highly polished and clean.

Page 14: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore27

Form or Pressure drag

� Pressure drag is caused by the separation of air that is flowing over the aircraft or airfoil.

� Note: New generation cars are designed to reduces pressure drag, which leads to better mileage

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore28

Induced drag

� Induced drag is the

drag created by the vortices at the tip of

an aircraft's wing.

� Induced drag is more

while maneuvering due to more flow

separation over the

entire body.

Page 15: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore29

Thrust

� Thrust is produced by engines, which counteracts the drag and hence the airplane moves in forward direction.

� Types of engines• Propeller

• Turboprop

• Turbofan

• Turbojet

• Ramjet

• Scramjet

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore30

Page 16: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore31

Propeller engine

Spitfire: Used by England in second world war.

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore32

Turboprop engine

Used by ATR flights

Page 17: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore33

Turbofan engine

Airbus A380 – Largest Passenger Aircraft

Engine Used: Either Rolls Royas or GE

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore34

Turbofan engine with afterburner

LCA - Light Combat Aircraft

Kaveri: An indigenous engine under development at GTRE (Gas Turbine Research Est.) under DRDO

Page 18: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore35

Ramjet Engines

Brahmos: A supersonic cruise missile developed jointly by

India and Russia.

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore36

Scramjet

X-43 is an experimental vehicle of NASA which

used scramjet propulsion to reach up to MACH 9

Page 19: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

Moment Balance in Flying VehiclesMoment Balance in Flying VehiclesMoment Balance in Flying VehiclesMoment Balance in Flying Vehicles

Prof. Radhakant PadhiProf. Radhakant PadhiProf. Radhakant PadhiProf. Radhakant Padhi

Dept. of Aerospace Engineering

Indian Institute of Science - Bangalore

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore38

Basic Force Balance

� Weight

� Lift

� Drag

� Thrust

� Side forceSide force

Page 20: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore39

Basic Moment Balance

X

Y

Z

� Rolling

� Pitching

� Yawing

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore40

Ailerons Roll

Page 21: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore41

Aileron Roll

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore42

Elevator Pitch

Page 22: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore43

Elevator Pitch

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore44

Rudder Yaw

Page 23: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore45

Rudder Yaw

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore46

Sensors

� Altimeter: Height above sea level

� Air Data System: Airspeed, Angle of Attack, Mach No., Air Temperature etc.

� Magnetometer: Heading

� Accelerometers: Translational motion of the aircraft in the three axes

� Gyroscopes: Rotational motion of the aircraft in the three axes

� GPS: Accurate position, ground speed

Page 24: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore47

Actuators

OPTIMAL CONTROL, GUIDANCE AND ESTIMATION

Prof. Radhakant Padhi, AE Dept., IISc-Bangalore48

Page 25: Lecture-15 - Flight Dynamics-I · ρ(h) = atmospheric density (a function of height) V = relative velocity of air S = wetted surface area = coefficient of lift 1 2 L L2 L q S C V

OPTIMAL CONTROL, GUIDANCE AND

ESTIMATION Prof. Radhakant Padhi, AE 49