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ID: 3658

Customer: Oleg Ostapenko E-mail: ostapenko2002@yahoo.com

Customer: Oleg Ostapenko E-mail: ostapenko2002@yahoo.com

CHAPTER 4: MORE ABOUT AIRFLOW AND AEROFOILS

Thin aerofoils (thickness/chord ratio about 7%) are best for high speeds. The Concorde had a thickness/chord ratio of only about 3%.

The wing section on the Piper PA28 Warrior, a popular training aircraft, is a laminar fow aerofoil (see Figure 4.9). (NB-the Warrior Pilot’s Operating Handbook describes the wing section as laminar fow, and it is certainly slimmer than the original PA28 Cherokee wing, but in cross-section is not as fne as the lower right diagram). This type of aerofoil, typically, has a thickness/chord ratio of about 12% and is so designed that the point of minimum static pressure (point of maximum camber) on the wing is at 50% chord so that the airfow is speeded up gradually to the half way point of the wing chord, giving the aircraft good performance in the cruise at small angles of attack, but poor characteristics at the stall. Laminar fow wing sections generate good lift for low drag, and are often used on high performance sailplanes. The principal disadvantage of laminar fow wings is that they are sensitive to slight changes in wing contour. Therefore, laminar fow wings, especially the leading-edge area of the wing, must be kept free of contamination from insects, raindrops, and the like at all times,. Contamination on the surface of laminar fow wings can easily break up the laminar airfow and cause aircraft handling problems for the pilot.

The different types of aerofoil mentioned above, with their different values for thickness/chord ratio, maximum thickness, maximum camber, and the position of these latter two along the chord, turn or defect the airfow to different extents.

That, in turn, will affect the air velocity and pressure distribution around the wing.

Figure 4.10 The lift characteristics of three different types of aerofoil.

Consequently, each different type of aerofoil will have a different Coeffcient of Lift and Coeffcient of Drag for any given angle of attack. This situation is illustrated for Coeffcient of Lift in Figure 4.10.

AIRFLOW THROUGH A VENTURI TUBE.

In our examination of airfow, we must take a look at what is known as the venturi effect. In the chapter on Lift, you learnt about the Bernoulli Principle and the Bernoulli Equation. One of the most common examples of the practical application of the Bernoulli Principle is the venturi tube. The most common type of venturi tube, used in practice, is a tube which narrows to what is called the throat, and then gradually widens out again, as shown in Figure 4.11, overleaf. As you have already learnt, if we assume – as we do throughout this book – that air is incompressible at speeds well below the speed of sound, the rate of mass fow through the venturi tube must

Laminar flow

wings are sensitive to

slight changes

in contour, and must be kept free of contamination, especially the leading edge.

In a venturi

tube, where the velocity of air

is highest, its

static pressure will be lowest.

77

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Customer: Oleg Ostapenko E-mail: ostapenko2002@yahoo.com

CHAPTER 4: MORE ABOUT AIRFLOW AND AEROFOILS

Figure 4.11 Airflow through a Venturi Tube.

The venturi tube creates low static pressure at its throat.

be constant. Therefore, as the cross-section of the tube decreases, the velocity of the airfow will increase, reaching its maximum velocity at the throat. Bernoulli’s

Equation tells us that where velocity is greatest, static pressure will be lowest. So, as the airfow approaches the throat, static pressure will fall, and increase again as the tube cross section increases in diameter and the airfow velocity decreases.

A venturi tube, then, is used to create a decrease in pressure, lower than that of the atmosphere. Carburettors employ the venturi effect for their basic function. On older aircraft, venturi tubes are also used in the operating systems of some fight instruments (such as the direction indicator or artifcial horizon) which operate on the so-called “partial vacuum” system. You can read about both these uses of venturi tubes in the Aeroplanes (General) volume, in this series of manuals.

The venturi tube principle may also be

Figure 4.12 Venturi Tube fitted to Auster J6. used to create areas of high airfow velocity; for example, in a wind tunnel.

The speed of the free-

stream airflow, around an

aircraft in flight, is the same as the aircraft’s true airspeed.

MEASURING AIRSPEED.

It is convenient for you to note at this point that when an aircraft is in motion, either on the ground, during the take-off and landing roll, or in the air, the relative airfow is used to measure the speed of the aircraft through the air.

Now, the speed of the free-stream airfow around an aircraft in fight is, naturally, equal to the forward speed of the aircraft relative to the air, referred to by pilots as the aircraft’s true airspeed.

You learnt in the chapter on Lift that the dynamic pressure exerted by a moving, ideal fuid on a body is the pressure exerted by virtue of the velocity and density

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Customer: Oleg Ostapenko E-mail: ostapenko2002@yahoo.com

Customer: Oleg Ostapenko E-mail: ostapenko2002@yahoo.com

CHAPTER 4: MORE ABOUT AIRFLOW AND AEROFOILS

Figure 4.13 The speed of the free-stream airflow is the same as the aircraft’s true airspeed.

of the fuid. Therefore, we may reasonably deduce that an aircraft’s airspeed is a function of the dynamic pressure exerted by the airfow it encounters in fight. You may remember the following equation for dynamic pressure, which can be extracted from Bernoulli’s Equation:

Dynamic pressure (Q) = ½ ρ v2

You may also recall that the total pressure in a fuid in motion, horizontally, is given by the relationship:

Total Pressure = Static Pressure (p) + Dynamic pressure (Q)

or

Total Pressure = p + ½ ρ v2

 

 

So, if we measure the total pressure

 

and the static pressure of an airfow,

 

and if we know the density of the air (ρ),

 

we can obtain quite an accurate value

 

for the dynamic pressure of the air, and,

 

therefore, deduce the aircraft’s true

 

airspeed. Knowing the true airspeed

 

(TAS) and the wind velocity

(W/V),

 

a pilot can then calculate his speed

 

over the ground (which, in navigation,

 

is called groundspeed (GS)), as well

 

as the heading (HDG) he should fy to

 

achieve a desired track (TR) over the

 

ground (See Figure 4.14). You will

 

learn how to do all these calculations in

 

the ‘Navigation & Radio Aids’ volume of

 

this series.

Figure 4.14 A pilot needs to know his True

 

Airspeed in order to navigate his aircraft.

The instrument which displays to the pilot an aircraft’s indicated airspeed is known, simply, as the airspeed indicator.

An aircraft’s

true airspeed is a function of

the dynamic

pressure acting on the aircraft in flight.

Total Pressure =

Static Pressure

+ Dynamic

Pressure.

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Customer: Oleg Ostapenko E-mail: ostapenko2002@yahoo.com

CHAPTER 4: MORE ABOUT AIRFLOW AND AEROFOILS

Dynamic Pressure, Q, = ½ ρ v2

The detailed function of the airspeed indicator is covered in our ‘Aeroplanes

(General)’ book. Here we will examine only those theoretical aspects of measuring airspeed which are relevant to the Principles of Flight.

Basically, the airspeed indicator (ASI) is an instrument whose operating system “subtracts” static pressure from total pressure, in the air fowing around the aircraft in order to give the pilot an indication of the dynamic pressure, Q, of the airfow.

Q = ½ ρ v2 = Total Pressure - p

Figure 4.15 An Airspeed Indicator (ASI) indicating 95 knots.

The ASI is calibrated in such a way that the pilot reads from the instrument the indicated airspeed of his aircraft. When the pilot corrects indicated airspeed by taking into consideration the actual density of the air (ρ), he will obtain the aircraft’s true airspeed. The indicated airspeed in Figure 4.15 is 95 knots.

The total pressure of the airfow is measured by an open tube, called a pitot tube, whose open end faces the oncoming free-stream airfow. A hole or holes (known as static vents) facing

“side-on” to the airfow, so that no air fows into the static vents, sense the static pressure within the airfow. The static vents may be ftted in the fuselage of an aircraft, as shown in Figure 4.16, or they may be incorporated into the circumference of a pitot tube to form a pitot-static tube, as depicted in Figure 4.17. The device is named after 18th century French engineer and inventor

Henri Pitot (pronounced ‘pee-tow’).

Figure 4.16 A Static Vent.

The total pressure sensed by the pitot tube (sometimes known as pitot

pressure) is fed to one side of a pressure-measuring device, (usually a sensitive diaphragm) within the airspeed indicator (ASI) system while the static pressure sensed by the static vents is fed to the other end of the ASI’s pressure-measuring device. This arrangement is illustrated in Figure 4.18.

The pressure difference sensed by the ASI is the difference between the total pressure in the relative airfow and the static pressure within the relative airfow. This difference is, of course, a measure of the dynamic pressure, Q, of the airfow, ½ ρ v2. The dial of the ASI can, therefore, be calibrated to read, the speed of the airfow, v, directly, for a given value of ρ.

80

ID: 3658

Customer: Oleg Ostapenko E-mail: ostapenko2002@yahoo.com

Customer: Oleg Ostapenko E-mail: ostapenko2002@yahoo.com

CHAPTER 4: MORE ABOUT AIRFLOW AND AEROFOILS

Figure 4.17 A pitot-static tube which senses both total and static pressure in the relative airflow.

Figure 4.18 Schematic of an Airspeed

Indicator (ASI) System.

As we have seen, an aircraft’s airspeed

– in other words, its speed relative to the air through which it is fying - is necessarily equal to the speed of the airfow over the aircraft. So, the

ASI, in measuring the v of ½ ρ v2, is measuring the airspeed of the aircraft. The airspeed measured by the ASI is called the indicated airspeed. The ASI will measure the aircraft’s true airspeed only if the local density of the air in which the aircraft is fying is equal to the value of ρ assumed by the manufacture of the ASI when the ASI was calibrated. At all other values, the pilot must apply corrections to the reading on the ASI in order to obtain his aircraft’s true airspeed. As you have already learnt, it is the true airspeed that a pilot needs for navigation calculations.

So, what is the relationship between true airspeed and the airspeed that a pilot reads from the ASI?

In the calibration of ASIs, the assumed atmospheric conditions, including, most importantly, the air density, ρ, are the conditions which prevail at sea-level in the ICAO Standard Atmosphere (ISA). The ASI, then, will be calibrated assuming an air density of 1.225 kg per cubic metre, and a temperature of 15° C. It follows, therefore, that the indicated airspeed that a pilot reads from his ASI will be different from his aircraft’s true airspeed at all times, unless the air in which the aircraft is fying corresponds exactly to ISA sea-level conditions.

As you might imagine, in reality, even at sea level, ISA conditions hardly ever prevail. Therefore, a pilot invariably has to apply corrections to the indicated airspeed (IAS) to obtain his aircraft’s true airspeed (TAS). In correcting IAS to obtain TAS there are

The ASI

“subtracts” static pressure from

total pressure to

allow dynamic pressure to be indicated on the ASI instrument face.

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Customer: Oleg Ostapenko E-mail: ostapenko2002@yahoo.com

CHAPTER 4: MORE ABOUT AIRFLOW AND AEROFOILS

several errors to take into account. The most signifcant errors are density error, temperature error, instrument error and pressure error (also known as position error.)

Instrument error and pressure error are dealt with briefy below, but, except for the density error and temperature error, the other errors are either compensated for within the ASI itself, or may be disregarded by the light-aircraft pilot fying at altitudes below 10 000 ft above sea-level.

Indicated airspeed corrected for instrument error and pressure error is known as calibrated airspeed or rectifed airspeed. We will use the expression calibrated airspeed. In practice, ASIs are tested extensively, on the bench and in fight, by the manufacturer. In light aircraft, instrument error, including temperature errors, is largely compensated for within the ASI before it is released for service; pressure error is due to the position of the static vents and changes of airfow around them with variations of speed, angle of attack, attitude and confguration, but is usually relatively small.

Consequently, a light aircraft pilot fying at typical light aircraft cruising levels can assume that the airspeed he reads from his ASI, the indicated airspeed, approximates very closely to the calibrated airspeed.

However, because density and temperature, both decrease at a signifcant rate with increasing altitude, these two factors cannot be ignored, and a pilot must apply density and temperature corrections to his aircraft’s indicated airspeed (which we assume to be equal to the calibrated airspeed) in order to obtain true airspeed. You will learn how to calculate true airspeed, using a navigation computer (see Figure

4.19), in the ‘Navigation & Radio Aids’ volume of this series. Some ASIs incorporate a feature akin to the navigation computer by which a pilot can dial in temperature against altitude to obtain a TAS reading in fight.

Figure 4.19 A Navigation Computer.

Because, in this chapter, we are considering airspeed as the measurement of v in the expression for dynamic pressure, ½ ρ v2, which is true airspeed, let us examine a little more closely how indicated airspeed and true airspeed are related by different values of air density, ρ. You may skip the maths in the blue box, if you wish.

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Customer: Oleg Ostapenko E-mail: ostapenko2002@yahoo.com

CHAPTER 4: MORE ABOUT AIRFLOW AND AEROFOILS

In calibrating the ASI, the value for ρ is assumed to be the air density in ISA sea-level conditions. We will indicate this value of air density by the symbol ρSL.

We have also said that the indicated airspeed, as read directly from the ASI, and corrected for instrument and position error is called calibrated airspeed. We will represent indicated airspeed (which we assume to be equal to calibrated airspeed) by the symbol vi.

Now, in the expression for dynamic pressure ½ρv2, v is the true airspeed.

But vi will be the true airspeed only where ρ = ρSL

Therefore, ½ρv2 = ½ ρSL vi2

Therefore, =

 

ρSL vi2

 

 

 

 

 

 

ρ

 

 

= vi2

 

v = vi

 

ρ

 

 

 

 

 

 

 

 

 

 

ρSL

 

 

 

 

 

 

 

 

 

 

Now, ρ

= relative density r

 

ρSL

 

 

 

 

 

 

 

 

Therefore,

v =

 

vi

 

And so, when ρ = ρSL , r = 1, and true airspeed, v, is the same as indicated airspeed, vi. But ρ is rarely, if ever, exactly equal to ρSL. When the aircraft is operating at altitude, it may be assumed that ρ is almost always less than ρSL. Consequently,

r and will be less that 1. Therefore, at altitude, true airspeed, v, is invariably greater than indicated airspeed.

At sea-level, then, where local air density will be very close to ISA air density, the indicated airspeed read directly from the ASI may be taken to be close to the true airspeed. But, because local air density decreases with increasing altitude, largely because of the decrease in pressure, invariably, air density at altitude, especially above 2 000 ft, will be less than the ISA sea-level air density. Therefore, at altitude, true airspeed will be greater than indicated airspeed.

Consequently, when a pilot calculates his true airspeed during his navigation preparations for a cross-country fight, at a planned indicated airspeed of, say, 110 knots and a planned cruising altitude of 3 000 ft, he will know that he can expect the true airspeed to be higher than his planned indicated airspeed. It is true airspeed that he must use for his navigation calculations.

As we have said you will learn how to carry out these calculations in the volume

Navigation & Radio Aids. However, it is important that you understand the airfow and Principles of Flight considerations behind your navigation calculations.

Where air

density is less than the ISA

sea level value,

indicated airspeed will be lower than true airspeed.

83

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Customer: Oleg Ostapenko E-mail: ostapenko2002@yahoo.com

CHAPTER 4: MORE ABOUT AIRFLOW AND AEROFOILS

In your

navigation flight planning, the difference

between indicated airspeed and true airspeed must be taken into account.

Just to give you a feel for the difference you may expect, in a temperate climate like that of much of Europe, between indicated airspeed (assumed to be equal to calibrated airspeed) and true airspeed, an indicated airspeed of 110 knots at a pressure altitude (altimeter subscale setting of 1013 millibars) of 2 500 feet, with an outside air temperature (OAT) at that altitude of 5° C, would give a true airspeed of just over 112 knots. You would be right to think that this is not a signifcant difference. But, it will make a discernible difference in your navigation fgures and must be taken into account.

If you were to fy at a pressure altitude of 6 000 feet on a hot summer’s day, with an

(Outside Air Temperature (OAT) of 12° C, an indicated (calibrated) airspeed of 110 knots would give a true airspeed of 122 knots: a signifcant difference.

More About ASI Errors.

Before we bring this chapter to a close, we will examine the main errors in the reading of the airspeed indicator (ASI) a little more closely, so that you have an appreciation of the potential that the ASI has to deceive the pilot. As we have mentioned, the two principal ASI errors are instrument error and pressure or position error. And although these may largely be compensated for during ASI manufacture and installation in an aircraft, you must be aware of their existence. As you have learnt, for typical light aircraft navigation fights, especially over short distances, the indicated airspeed shown on the ASI can be assumed to be very close to calibrated airspeed (indicated airspeed corrected for instrument and position error), however, you must consult the aircraft’s Flight Manual, or Pilot’s

Operating Handbook, to confrm this assumption.

Instrument Error in the ASI.

Figure 4.20 Correction figures to convert indicated airspeed into calibrated airspeed may be found in the aircraft’s Flight Handbook or the Pilot’s Operating Handbook

Instrument Errors in the ASI are caused by imperfections in the design and manufacturing processes of the instrument. Instrument errors will, therefore, be different in different types and models of ASI. In general, instrument errors are negligible.

Pressure (or Position) Error in the ASI.

Pressure (or Position) Error in ASI readings can be caused either by inaccurate static pressure sensing, inaccurate total pressure sensing, or by a combination of both. Pressure error in the sensing of static pressure is most common when the static vents are incorporated into a pitot-static head. The accuracy of total pressure sensing may be affected by misalignment of the pitot or pitot-static head; for example, if the pitot tube is inclined at an angle to the free-stream airfow instead of facing directly into the fow. Pressure error will, therefore, also arise in extremes of aircraft attitude, such

84

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Customer: Oleg Ostapenko E-mail: ostapenko2002@yahoo.com

CHAPTER 4: MORE ABOUT AIRFLOW AND AEROFOILS

as fight at high angles of attack near the stall, especially when marked turbulence is present.

ASI errors can be minimised during fight testing by taking a series of ASI readings over a range of airspeeds and attitudes. Instrument calibration corrections can be made based on the results of such tests with a correction being applied to each indicated airspeed.

As we have mentioned, the indicated airspeed, when corrected for instrument and position errors, gives calibrated airspeed. The pilot applies his own temperature and density corrections to calibrated airspeed in order to obtain true airspeed.

At high speeds, in excess of half the local speed of sound (Mach 0.5) compressibility error in the ASI reading must also be taken into account. In this book, we ignore compressibility error as typical light aircraft speeds are far below Mach 0.5.

The Value of Indicated Airspeed Readings.

Although it must be corrected for navigation purposes, indicated airspeed is very a useful value in itself.

Indicated airspeed is a measure of the real dynamic pressure, ½ρv2, being exerted on an aircraft as result of its motion through the air, and is, therefore, also an indication of the aerodynamic forces (such as lift and drag) acting on the airframe. As far as the safety of the aircraft is concerned, then, it is often of greater importance to the pilot to have a direct reading of these aerodynamic forces than to be able to read directly his aircraft’s true airspeed. For this reason, all aircraft speed limitations are given as indicated airspeed.

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Customer: Oleg Ostapenko E-mail: ostapenko2002@yahoo.com

CHAPTER 4: MORE ABOUT AIRFLOW AND AEROFOILS QUESTIONS

Representative PPL - type questions to test your theoretical knowledge of Lift.

1.Total pressure sensed by a Pitot Tube comprises:

a.pitot pressure plus dynamic pressure

b.pitot pressure minus dynamic pressure

c.static pressure plus dynamic pressure

d.dynamic pressure minus static pressure

2.Two identical aircraft of the same weight fy at two different altitudes (in straight and level fight and the same angle of attack). Assuming that other factors remain constant, that the air is incompressible, and that ISA conditions prevail, how do the true air speeds of the two aircraft compare?

a.They are the same

b.The True Air Speed (TAS) of the higher aircraft will be the greater

c.The TAS of the lower aircraft will be the greater

d.Altitude has no effect on the True Air Speed required to support a given aircraft weight at constant angle of attack

3.In accordance with Bernoulli’s Theorem, where PT = Total Pressure, PS = Static pressure and q = Dynamic pressure:

a.PT + PS = Q

b.PT = PS - Q

c.PT - PS = Q

d.PS + PT = Q

4.When (normally at high angles of attack) the Boundary Layer separates from the surface of an aerofoil (at the Separation Point), airfow characteristics aft of the Separation Point can best be described as:

a.unpredictable and haphazard, leading to an abrupt decrease in lift force

b.smooth and laminar, leading to an increase in lift

c.a turbulent Boundary Layer, leading to a slight reduction in lift

d.smooth and laminar, creating a favourable Pressure Gradient

5.The symbol for dynamic pressure is:

a.Q

b.P

c.R

d.D

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