12.4.6. Explain how air density varies with altitude within the atmosphere.
Density of air is measured by how many molecules are present in any given volume Near the earths surface the density is higher than at greater altitudes. It reduces rapidly at lower levels and more slowly at higher levels.
Density of air is measured by how many molecules are present in any given volume
Near the earth’s surface the density is higher than at greater altitudes
12.4.6. Explain how air density varies with altitude within the atmosphere.
Density of air is measured by how many molecules are present in any given volume
Near the earth’s surface the density is higher than at greater altitudes. It reduces rapidly at lower levels and more slowly at higher levels.
12.4.8. State the relationship between pressure/temperature and the density of an air mass.
Pressure and temperature affect the density of any parcel of air.
High temperature and low pressure will result in low density. Low temperature and high pressure will result in high density.
12.4.10. Describe how pressure, temperature and density normally vary within the atmosphere.
The pressure, temperature and density will normally all decrease with increasing altitude
Pressure decreases rapidly at lower levels and more slowly at higher levels. Temperature decreases at a constant rate up to the troposphere. Density
decreases rapidly at lower levels and more slowly at higher levels. (image)
12.4.12. Explain the basis for the International Standard Atmosphere (ISA)
– hypothetical set of atmospheric conditions which represents an average of the conditions experience worldwide
Sea level pressure = 1013.2hPa (hectopascals) Sea level temperature +15 degrees C Sea level density 1.225kg/m3
Lapse
rates
12.4.14. State the ISA sea level pressure and temperature conditions.
ISA Sealevel pressure = 1013.2hPa
ISA Sealevel temperature = +15deg C
12.4.16. State the approximate temperature lapse rate up to the tropopause.
The ISA temperature lapse rate up to the Troposhere is 1.98degC per 1000ft.
is the proportionally the object’s Inertia. e.g. how hard it is to get an object moving or to stop / slow downed a moving object.
Example of Inertia
Let’s start off with a scooter (motorbike) it doesn’t take much energy to get the scooter moving and you don’t have to run into much, let alone a power pole before coming to a stop. Scooter has a lot less mass than a train. Train
on the other hand requires a lot of energy to get moving and would probably knock over 2 or 3 power poles before even look like slowing down let alone stopping
Momentum
Formula
= Mass x Velocity
Formula in action
1. Body 10 units of Mass multiplied by moving at Velocity of 2 units = 20 units of Momentum. 2. Body 5 units of Mass multiplied by moving at Velocity of 4 units = 20 units of Momentum.
The first one had a greater mass and second had a greater velocity but they both had the same momentum thus both would be equally difficult to stop.
Example of Momentum
A train that has a large mass and a low velocity compared with a bullet with a small mass and a high velocity both will be difficult to stop and both can do considerable damage to anything that tries to stop them.
An object with mass always has inertia, however a body only has momentum while it is moving, if body is stationary the momentum is 0.
Force – a push or a pull – identified by what it does moving an object out of its state of rest or of uniform motion in a straight line. Force Vectors – usually drawn as an arrow, indicating a vector’s quantities of both magnitude and
direction
Couples – consists of two equal but opposite parallel forces which create a twisting moment about a point between the two force lines.
Components – these are the resolution of a force vector into two components at right angles to
each other. Used to show the amount of a total force acting in a particular direction. An Example: Weight and Lift Couple which in balanced by the Tail Plane.
Components – these are the resolution of a force vector into two components at right angles to each other. Used to show the amount of a total force acting in a particular direction.
An Examples: Reaction of the Wing, Components
of Lift and Drag Reaction of the Propeller, Components of Thrust and Torque
By understanding the centripetal force calculations you will see the big effect that speed has on your turning radius.
Let look at the centripetal force on mass EG no gravity.
( CPF = frac{Mass x Velocity 2 }{Radius} )
( CPF = frac{Mass x Velocity 2 }{Radius} )
Diagram
Mass(m)
Increase Mass then there is a an Increase of Force
Velocity(V2)
Increase Velocity then there is an Increase in Force is now Squared. E.g. Double the Speed with equal 4 time the Force. 100 units Double speed would become 400 units
Radius(r)
Increase the Radius the Force is Decreased. Double the Radius the Force is halved. 100 unit is now 50 units
Now the centripetal force using weight e.g. in the earth with gravity.
Start with
( CPF = frac{Mass x Velocity 2 }{Radius} )
Replace Mass(m)
With ( frac{weight}{g} )
CPF use on an Aircraft in Flight
( CPF = frac{Weight x Velocity 2 }{‘g’ x Radius} )