TOPIC 3: MAGNETISM | PHYSICS FORM 2
Concept of Magnetism
The Origin of Magnetism
Chinese were the first to use the metal magnetite called lodestone. A Lodestone was capable of attracting small iron pieces and it was used as a crude navigation compass by Greeks. Lodestones were the earliest magnets.
Iron, nickel and cobalt are the only naturally occurring magnetic materials. Magnet has two ends known as magnetic poles in which the greatest attraction power is concentrated.
Magnetic and Non-magnetic Materials/Substances
These are substances which have a property of being attracted by a magnet.E g; iron,steel,cobalt and nickel.
Pole strength refers to the ability of a magnet to attract objects.
Ferromagnetic substances have very high magnetic susceptibility (easily magnetized).Eg; iron, nickel and cobalt.
Electromagnet is the substance which requires electric current to attain magnetism.
Permanent magnet is a substance which is already a magnet and it doesn’t require electric current to attain magnetism.
These are substances which are not attracted by a magnet.Eg; copper, brass, aluminium,glass,plastic and wood.These substances have very weak magnetic properties.
The Properties of Magnets
Magnets have a tendency of attracting magnetic substances and have no action on non-magnetic materials.
Types of magnetic materials
There are three types of magnetic materials:
i. Diagmatic materials: Are substances which have a tendency to repel from a stronger to weaker magnetic field. Eg; bismuth, water, gold,air,hydrogen,common salt,diamond,silver and copper.
ii. Paramagnetic materials: Are substances which become weakly magnetized when placed in magnetic field. Eg; aluminium,platinum,chromium,oxygen and manganese.
iii. Ferromagnetic materials: Are substances which becomes magnetized when placed in magnetic field. Their magnetic domain become aligned in one direction when they are placed in magnetic field. Eg; iron, cobalt and nickel.
Refers to the molecular magnets lined up with each other which constitute ferromagnetic materials.
The direction of magnetic poles varies from one domain to another if the magnet is unmagnified
Types of Magnets
Magnets may also be classified according to their shapes. This includes:
Horse shoe magnet
Rod shaped magnets
Ring shaped magnet
Application of Magnets
Magnets are used in:
- women handbags closing
- picking up heavy loads
- electrical appliances like meter and receivers
- sound and video recording equipment
- computer memory and disks
- electrical trains
Magnetization and Demagnetization
The Concept of Magnetisation and Demagnetisation
Magnetisation: Is a process of making a magnet from a magnetic substance.
Demagnetisation: Is the process by which a magnet is made to lose its magnetism.
Methods of magnetisation
There are various ways, including;
- Electrical method
This is done by placing a piece of unmagnetised steel bar near or in contact with a pole of a magnet and then removing it.
In this case an iron nail placed near a bar magnet will be induced with magnetism.
This is done by stroking a bar magnet into an unmagnetised steel bar.There are two stroking methods, namely;
>> Single touch: A magnetised bar magnet is formed by a single stroke.-A steel bar is stroked repeatedly by a very strong bar magnetism the same direction with the north pole i.e from A to B. The bar magnet is lifted at B and then returned at A. After several strokes the steel bar will be magnetised with north pole at A and south pole at B.
>> Double touch: Two bar magnets are used to magnetise a single steel bar. The steel bar is magnetised by two bar magnets from its center to its ends using left and right hands simultaneously for several times. Between each stroke the two bar magnets are lifted up high and returned to the center for another stroking.
In this case the steel bar will be magnetized with south pole at A and north pole at B.
In both single and double touch methods, the magnetising magnet none of their strengths.
Between successive strokes, the pole is lifted high above bar, otherwise the magnetism already induced in it will tend to be weakened.3.Consequent poles will be formed at the center of the steel bar when the two bar magnets placed at the center are of like poles. Same poles will be obtained on both ends.
A cylindrical coil wound with many of insulated copper wire is connected in series with a battery. A steel bar is placed inside the solenoid and the current switched on and off.When the steel bar is removed and tested, it is found to be magnetised.
If the current is switched off for so long, the bar will not be magnetized.The poles of the bar magnet depends on the direction of flow of current. The end at which the direction of the current is in clockwise direction will be south pole and if anticlockwise it will be north pole.
Methods of demagnetization
The magnet is placed inside a solenoid through which an a. c is flowing.The magnet is withdrawn from the solenoid while the current is flowing pointing in the W-E direction. When the magnet is held in W-E direction, it doesn’t remain with residue magnetism due to induction from earths magnetic field.
Other methods of demagnetisation include;
- Heating a magnet.
- Hammering while pointing E-W direction.
Methods of Storing Magnets
Magnets are stored in magnetic keepers.They are stored in pairs,with unlike poles together and with pieces of iron(magnetic keepers) across both ends.The keepers are magnetised by induction.
Magnetic Fields of a Magnet
The Concept of Magnetic Fields of a Magnet
Magnetic field:Is a space surrounding a magnet in which a magnetic force is exerted or experienced. It consists of magnetic field lines which are imaginary lines of force around a magnet from North Pole to South Pole.
The Magnetic Lines of Force around a Magnet using Iron Fillings or Compass Needle
Aim:To study the properties of magnetic field lines around a bar magnet.
Materials: Iron fillings, bar magnets and a piece of paper.
- Place a sheet of plane paper over a bar magnet.
- Sprinkle iron fillings on the sheet of paper.
- Gently tap the sheet of paper.
- Iron fillings will form a pattern which depends on the magnetic lines of force of the magnet.
- The lines of equal magnetic strength are seen flowing between magnetic poles .The lines are referred to as lines of magnetic flux or field lines. The pattern magnetic force is called a magnetic field.
- When investigating a magnetic field with iron fillings the field is strongest where the fillings are crowded.
- By investigating a magnetic field lines and a bar magnet using a small compass needle, the magnetic flux(lines) runs from north pole to south pole.
Neutral point is a point at which the resultant magnetic flux density is zero.
this area, X, the two magnetic field s cancel or neutralize each other.It happens when two like magnetic poles are brought together.
Therefore neutral point is;
- an area in a magnetic field where the resultant magnetic field strength is zero.
- a point which exists where two magnetic field neutralize each other.
The Methods of Magnetic Shielding
Magnetic shielding: Is a screen made from high permeability material used to isolate any material from unwanted magnetic fields
Example; The electron beam in the cathode ray tubes of TV sets, and very delicate measuring instruments are shielded(protected)from magnetic influence by placing them in soft iron cases with thick wells.
Here the object is shielded from the strong magnetic fields by a soft iron ring around it.
Earth’s Magnetic Field
The Phenomenon of Earth’s Magnetism
Earth is imagined as a single big magnet, with its south seeking pole near the geographic north called a north magnetic pole and the north seeking pole is near geographic south pole called south magnetic pole.
The earth behaves as if at its center there is a short piece of a bar magnet inclined at a small angle to its rotation (spinning) axis. When a bar magnet is hanged horizontally with a string, it will oscillates for a short time and then comes to rest with its poles pointing in the N-S direction due to the earth’s magnetic field.
This gives a notion that the earths north pole is in the southern hemisphere where any magnets north pole will always point.The two earth’s magnetic poles are joined by a line called magnetic meridian.The geographic meridian joins the true north and true south.
Direction of Earth’s Magnetic Field
Compass needle: Is a thin magnet balanced on a point, usually at the center of gravity used to identify N-S direction.Spinning a compass needle, it will eventually come to rest with its poles pointing to the N-S direction.This gives direction at any point on the earth’s surface.
The Earth’s Magnetic Lines of Force about a Bar Magnet
The magnetic field lines around a bar magnet can be mapped with the help of a magnetic compass. The magnetic field lines due to a bar magnet are closed loops. They leave at the north pole and enter at the south pole. When you plot the magnetic field lines around a bar magnet, the horizontal component of the earth’s magnetic field, B0, influences the magnetic field induction, B, due to the bar magnet. At points close to the bar magnet, magnetic induction B due to the bar magnet is very high as compared to the horizontal component of the earth’s magnetic field, B0. Thus, B0is negligible.
According to the inverse square law of magnetism, magnetic field induction B due to the bar magnet decreases as we move away from it. At certain points around the bar magnet, B and B0are equal in magnitude and opposite in direction. Therefore, they cancel each other out, and the resultant magnetic field is zero.
Thus, the point where magnetic field induction B due to a bar magnet is equal in magnitude and opposite in direction to the horizontal component of the earth’s magnetic field induction, B0, is called a neutral point.
The neutral points around a bar magnet can be located in two different cases
- When the north pole of the bar magnet points towards the earth’s north pole
- when the south pole of the bar magnet points towards the earth’s north pole.
When the north pole of a bar magnet points towards the north pole of the earth.
> Fix a sheet of white paper on a drawing board with brass pins.
> Take a compass needle, place it at the centre of the paper, and mark the north and south directions.
> Draw a straight line along the paper connecting the two points. This represents the magnetic meridian of the earth.
> Represent the geographical directions at the corner of the paper.
> Draw an arrow from the geographical south to the geographical north on the right side of the paper to indicate the direction of the horizontal component of the earth’s magnetic field, B0.
> Take a bar magnet and place it at the centre of the paper such that the north pole of the bar magnet points towards the north pole of the earth.
> Now place the compass needle at the north pole of the bar magnet and mark a point where the north pole of the compass needle is.
> Shift the compass such that the south pole of the compass needle is at the point you just marked.
> Mark another point at the north of the compass needle, and then shift the compass, as done earlier.Repeat the procedure till the compass needle reaches the other end of the bar magnet.
> Join all the points to get a continuous smooth curve, which represents a magnetic field line.
> Repeat the procedure from the north pole of the magnet, but from different points, and draw the magnetic field lines.
The two points on either side of the bar magnet at equal distances from its centre, where the compass needle does not show any specific direction. At these points, the magnetic field induction B due to the bar magnet and the horizontal component of the earth’s magnetic field induction, B0are equal in magnitude and opposite in direction. The resultant magnetic field is zero. These points represent the neutral points denoted by N1and N2. These two points fall on the equatorial line of the bar magnet.
Thus, when the north pole of a bar magnet points towards the geographical north pole of the earth, the two neutral points lie on the equatorial line of the bar magnet such that they are equidistant from the centre of the bar magnet.
The Angle of Inclination (dip) and Angles of Declination
Angle of dip is the angle between the direction of the earth’s magnetic flux and the horizontal.
Measurement of angle of dip
The angle of dip is not constant over the earth’s surface; it varies from place to place.
This difference is brought about by the earth’s magnetic field direction at a point on the earth’s surface. The easiest way to measure the angle of dip is using a thin iron rod.The rod is suspended by length of a thread such that it balances horizontally.
Without disturbing the position of attachment, the rod is magnetised by bringing close a bar magnet and touching. On re-suspending the rod will dip with its north pole pointing downwards as shown in the diagram above. Using a protractor, the angle between the axis of the rod and the horizontal can be measured.
Angle of declination
Is the angle between the magnetic meridian and geographic meridian. The angle of declination varies from place to place all over the world. Maps shows declination at different points of the world.
Application of Earth’s Magnetic Field
The earth’s magnetic field is used to:
- indicate poles of unknown magnets.
- enables the use of magnetic needle.
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