12.6.4(c) . chord;
The length of a straight line joining the leading and trailing edges (Image)
12.6.4(c) . chord;
The length of a straight line joining the leading and trailing edges (Image)
12.6.4(b) . trailing edge;
The edge at the downstream side (image)
12.6.4. Define:
Term | Description | |
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(a) . leading edge; |
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The edge at the downstream side (image) |
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(c) . chord; |
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(d) . chord line |
; A straight line joining the leading and trailing edges. |
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The depth of the aerofoil On most aerofoils the point of maximum thickness is forward towards the leading edge |
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(f) . camber. |
Is the curvature of an aerofoil surface. The curvature of a line drawn equidistant between the upper and lower surfaces of the aerofoil is the mean camber of the aerofoil. |
12.6.2. Describe what an aerofoil is and distinguish between different aerofoil designs.
The wings and tail sections of an aircarft are aerofoils
Various designs include:
General Purpose
High lift
Pre-1916
High Speed (image)
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.
12.4.14. State the ISA sea level pressure and temperature conditions.
ISA Sealevel pressure = 1013.2hPa
ISA Sealevel temperature = +15deg C
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 |
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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. |
12.4.12. Explain the basis for the International Standard Atmosphere (ISA).Sub Topic Syllabus Item
– 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
12.4.10. 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)
12.4.8. 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.