CAA Part 66 Cat B1 Module 8 – Basic Aerodynamics Study Notes
CAA Part 66 Cat B1 Module 8 – Basic Aerodynamics
## Issue 3 14th January 2025
CONTENTS
- Physics of the Atmosphere
- Basic Aerodynamics
Physics of the Atmosphere
Composition of the Atmosphere
- The Earth's atmosphere is primarily composed of nitrogen (N2) at 78% and oxygen (O2) at 21%
- The remaining 1% consists of other gases. The ratios remain fairly constant regardless of altitude, though moisture content decreases.
- Figure 1-2: Composition of the Earth’s Atmosphere
Pressure
- Definition of Atmospheric Pressure: The force exerted against the earth's surface by the weight of the air above it.
- The formula relating force, area, and pressure is:
- To find atmospheric pressure, the formula rearranges to:
- Atmospheric pressure at sea level is approximately 14.7 psi (rounded), or equivalently 1013.25 hPa.
- Instruments for Measurement: Barometer measured in inches of mercury (inHg) or millibars (mb).
Density
- Defined as weight per unit volume.
- Air density varies directly with pressure and inversely with temperature:
- Density increases with pressure.
- Density decreases with temperature.
- Changes in density affect aircraft’s aerodynamic performance.
- Factors Influencing Density:
- Hot days decrease density.
- Humid conditions reduce density compared to dry days.
- Increased altitude results in decreased density.
Humidity
- The amount of water vapor in the air; varies with temperature.
- Types of Humidity:
- Absolute Humidity: Weight of water vapor in a unit volume of air.
- Relative Humidity: Ratio of current water vapor to the maximum it can hold at the same temperature, expressed as a percentage.
- High humidity decreases air density, requiring longer takeoff runs due to decreased lift.
Temperature and Altitude
- Temperature affects density and subsequently lift and engine performance.
- Within the troposphere (0 to 33,000 feet), temperature decreases at a rate of approximately -2°C per 1000 feet until reaching the tropopause at -57°C.
- Higher altitudes experience lower temperatures, affecting aircraft performance negatively.
- Figure 1-8: Atmospheric layers are depicted with their temperature changes.
International Standard Atmosphere
- Established values for performance comparisons and theoretical calculations.
- Air is assumed dry with:
- Pressure: 1013.25 hPa at sea level, decreasing by approximately 1 hPa every 30 feet.
- Temperature: Initially at 15°C with a lapse rate of 1.98°C per 1000 feet up to 36,090 feet; constant at -56.5°C up to 65,800 feet.
- Density: At sea level density equals 1.225 kg/m³.
AERODYNAMICS
General Definitions for Fluid Flow / Airflow
- Fluid: A substance that can flow, including liquids and gases.
- Relative Airflow (RAF): The movement of air relative to the aircraft.
- Incompressible Flow: Flow treated as incompressible when velocity is less than 0.3 Ma (100 m/s at ISA standard sea level).
- Freestream Flow: Velocity, pressure, and temperature of air unaffected by the aircraft structure.
- Streamline: Path of fluid particle moving from one point to another.
- Boundary Layer: The layer of fluid in the immediate vicinity of a bounding surface; affected by viscosity.
- Laminar Flow: Fluid flow characterized by smooth, parallel streamlines.
- Turbulent Flow: Random, chaotic motion of fluid with eddies and vortices.
- Flow Separation: Detachment of flow around an aerofoil, typically at high incidence angles.
Velocity and Acceleration
- Speed vs. Velocity: Speed denotes magnitude only; velocity includes direction.
- Acceleration: Change in velocity over time.
Newton's Laws of Motion
- First Law (Inertia): An object at rest stays at rest. The same applies to objects in motion unless acted upon by a force.
- Second Law (F=ma): A body in motion under force will change speed proportional to the force applied.
- Third Law (Action-Reaction): For every action, there is an equal and opposite reaction.
AIRFLOW AROUND A BODY
Bernoulli's Principle and Subsonic Flow
- Bernoulli's Principle: As a fluid moves through a constriction, velocity increases and pressure decreases (akin to airflow over an aerofoil).
- Visual illustration of air flowing through a constriction or across a cambered surface shows velocity increasing at the top and pressure decreasing, resulting in lift.
Upwash and Downwash
- Upwash: Air moving upward in front of the wing.
- Downwash: Air moving downward behind the wing. Upwash increases lift by lowering pressure above the wing.
AERODYNAMIC TERMS
Chord and Mean Aerodynamic Chord
- Chord: Width of the wing from leading edge to trailing edge.
- Mean Aerodynamic Chord (MAC): Average chord length of a wing, crucial for stability calculations.
DRAG
Types of Drag
- Parasitic Drag: Not associated with lift (e.g., form drag, friction drag, interference drag).
- Induced Drag: Generated by the creation of lift, associated with upwash and downwash.
- Wave Drag: Occurs at transonic and supersonic speeds due to shock waves.
Drag Coefficients
- Drag Equation: , where every term relates to the conditions affecting drag.
FORCES IN FLIGHT
Key Forces
- Thrust: Forward force from engines.
- Weight: Downward force due to gravity.
- Lift: Upward force opposing weight.
- Drag: Force opposing thrust.
CONTAMINATION
- Effects of Aerodynamic Contamination: Icing, water, or frost can severely disrupt airflow and reduce lift.
FORCES IN THE GLIDE DESCENT
- Glide Ratio: Distance traveled versus altitude lost (e.g., 10:1 = 10,000 ft forward for 1,000 ft lost). Determined by lift to drag ratio.
- Best Glide Speed: Ensures maximum distance, adjusted for weight and other factors.
TURN THEORY AND LOAD FACTORS
- Load Factor: , varies with bank angle and affects stall speeds.
FLIGHT STABILITY AND DYNAMICS
The Axes of an Aircraft
- Longitudinal, Lateral, and Vertical Axes: Each defines the motion dynamics of the aircraft through roll, pitch, and yaw.