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Earth’s Magnetism
Magnetism
- Magnetism is the property of certain materials to create a magnetic force
- Magnetic force attracts or repels similar materials
- Ferrous metals like steel, nickel or cobalt can be magnetised
- Non-ferrous metals like aluminium cannot be magnetised
Magnetic Field
- Magnetic field is the space around magnet where magnetic influence is felt
- Magnetic lines of force is pattern in a magnetic field
- Varies with shape and strength of magnet
- Red end is the north seeking end which points to magnetic north
- Blue end is south seeking end which points to magnetic south
- Like poles repel whereas unlike poles attract each other
Magnetisation
- A metal can be magnetised by three methods
- Moving magnet repeatedly over a metal called stroking
- Hammering magnetic material with a magnet
- Applying direct current in a coil of wire wound around magnetic material
De-Magnetisation
- A magnetised metal can be de-magnetised by three methods
- Hammering magnet by placing it at right angles to earth magnetic field
- Heating the magnet above 900 deg c
- Applying alternating current and reducing current slowly
- Polarity reversal removes magnetism
Hard and Soft Iron
- Hard iron are metals such as cobalt and tungsten steel
- Hard iron is difficult to magnetise but retains magnetism longer
- Hard iron are called permanent magnets
- Soft iron are metals such as silicon and pure iron
- Soft iron are easy to magnetise but retains magnetism temporarily
- Soft iron remains magnetised only till passage of current in solenoid
Earth Magnetic Field
- Magnetic compass is the primary direction finding instrument in an aircraft
- Earth’s magnetic field is not exactly aligned to its polar axis
- Magnetic north is not co located with True north
- Magnetic north is approximately 400 NM away from True north
- Magnetic north moves at 22 NM per year
- Magnetic North and South poles are not diametrically opposite
- Magnetic compass uses only the North seeking end for direction finding
Magnetic Variation
- Variation is the difference between the True and Magnetic north in degrees
- Expressed as magnetic north being east or west of true north
- Variation dependent on the relative position of the Magnetic north and Aircraft
- Maximum value of variation can be 180 deg east or west
- Isogonal are lines joining places of equal variation
- Converge on the True and Magnetic poles
- Agonal are lines joining places zero variation
Magnetic Variation
- Plus and Minus signs are applied to magnetic heading to get true heading
- Magnetic direction can be calculated from variation
- Variation west (-) magnetic best
- Variation east (+) magnetic least
Magnetic Dip
- Magnetic field can be resolved into horizontal & vertical components
- Horizontal component is the directive force to determine magnetic north
- Magnetic dip is the angle between the earth’s magnetic field from horizontal
- Dip angle is zero at equator, magnet is horizontal to surface of earth
- Dip angle is 90 degrees at poles. magnet is vertical to earth’s surface
Effect of Magnetic Dip
- Lines of Inclination join places of equal magnetic dip
- Aclinical line joins places of zero dip angle seen at the magnetic equator
- Field strength is the measure of directive force in micro teslas
- Compass requires a minimum of 6 micro teslas to function properly
Compass Deviation
- Electric and metallic objects near aircraft compass cause error called deviation
- Compass deviation is difference between the magnetic & compass north
- Expressed in degrees east or west of magnetic north
Calculation of Compass Deviation
- Compass swing is the procedure to prepare a compass deviation card
- Plus and Minus signs are applied to compass heading to get magnetic heading
- Compass direction can be calculated from magnetic direction and deviation
- Deviation west (-) compass best
- Deviation east (+) compass least
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