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School Physics Notes: Magnetism - magnetic fields, making and uses of magnets

Electricity and magnetism 9: Magnetism - magnetic materials - temporary (induced) magnets and permanent magnets - uses

 Doc Brown's school physics revision notes: GCSE physics, IGCSE physics, O level physics,  ~US grades 8, 9 and 10 school science courses or equivalent for ~14-16 year old students of physics

 This page will help you answer questions such as ...   What are the rules concerning magnetic poles?    How can you make a magnet without electricity?   What is magnetic induction?   What is the difference between permanent and temporary magnets?   What do we use magnets for? (excluding electromagnets, on a separate page)

Sub-index for this page

1. Introduction to magnetism and magnetic fields

2. Magnetic fields - plotting and diagrams

3. Magnetisation and making magnets - induced and permanent magnets

4. Uses of permanent magnets (See other page for uses of electromagnets)

5. The Earth's magnetic field and the compass



1. Introduction to magnetism and magnetic fields

You might ask the question 'what is magnetism', the answer is the same for gravity, nobody is really quite sure and the answer will lie somewhere in some deep quantum theory, well above school physics level and my little grey cells!

However, the causes and effects of magnetic fields are well understood and can be described by 'working models' e.g. little atomic magnets to do with electrons in atoms like iron, magnetic fields from compass plotting and accurate mathematical models from very simple equations to the extremely complex!

Only relatively few materials display magnetic properties - that is, they are naturally magnetic, or more usually, capable of being magnetised.

Typical magnetic materials are iron and its alloys like steel, nickel and its alloys and cobalt and its alloys - the alloys, in particular, are used to produce very strong permanent magnets.

Other common structural metals like aluminium, copper and lead are not magnetic.

Jewellery metals like gold, platinum and silver are also not magnetic.

Actually most materials are NOT magnetic!

A bar or rod of magnetic material can be shown to have two poles, one at each end - a north seeking pole (north) and a south seeking pole (south).

e.g. a bar magnet is suspended by a fine thread, one end will point to the Earth's magnetic north and the other end to the Earth's magnetic south.

This is evidence that the metallic core of the Earth (lots of iron) is permanently magnetic.

As with electric charges, when you bring poles together, one of two things can happen.

Either the poles attract or they repel each other.

In other words any two magnetic objects exert a force on each other - attraction or repulsion.

The rule of magnetic poles

The rule is quite simply like poles repel (<= N N => or <= S S =>) and unlike poles attract (N => <= S).

You can easily demonstrate these rules with two bar magnets (of known polarity) suspend on string and bringing the various ends together (as in diagram above).

=> <=   or   <= =>   or   <= =>

Previously magnetised materials will attract other magnetic materials whether they were or were not, already magnetised.

e.g. a magnet will always and readily attract an item of iron or steel.

In other words when a magnet is placed near a magnetic material the two objects always experience an attractive force - it doesn't matter which pole of the magnet is placed nearest the object - see induction later.

A magnetic force is a non-contact force, even if the objects eventually touch.

Electrical and gravitational forces are also non-contact forces.

All, already magnetised materials are surrounded by a magnetic field, which we will look at in detail next.

 


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2. Magnetic fields- plotting them, drawing them

You can map out the magnet field around a bar magnet by using a small plotting compass.

A magnetic field is the region around a magnetic (magnetised) object where a force acts on another magnet or another magnetisable object/material.

represent compass plotting positions on the diagram below (N=>S).

The magnetic field lines should indicate that the 'magnetic flux' runs from the north pole to the south pole.

Inside the plotting compass a tiny bar magnet (compass needle) aligns itself so that its north pole is attracted to the south pole of the magnet it is near.

The same thing happens with a navigation compass, which aligns itself with the Earth's magnetic field.

Your plotting compass does same thing when well away from the magnet - which shows the Earth creates a magnetic field - because the Earth has an iron core and this swirling mass of mainly molten iron generates a magnetic field.

Plotting! On a sheet of white paper, place a bar magnet in the middle and draw a rectangle around it, so you can always make sure it is in the same place when plotting the magnetic field.

You carefully select a starting point close to a pole and mark on the paper a dot by the end of the compass needle arrow closest to the compass (* →).

Then mark another dot at the other end of the compass needle arrow (→ *).

Then, move the plotting compass around, making a dot adjacent to each end of the compass needle as you move from one position to another.

Gradually a line a force can be drawn by joining up the points all the way round from one end to the other end of the magnet.

You just repeat the procedure from a different starting point from the north pole.

How to plot the magnetic field of a bar magnet

The results of plotting a magnetic field around a permanent bar magnet.

By convention, the lines of force run around from the north pole to the south pole.

The lines of force show which way a force would act on a north pole if it was placed at that point in the field - see how the compass needle aligns itself along the line of force.

The closer the lines of force are together, the stronger the magnetic field.

The lines of force are closer together nearest the poles - this means the strength of the magnetic field is strongest close to the poles.

The further you get away from a magnet, the weaker the magnetic field.

The strength of the magnetic field is called the magnetic flux density and is measured in teslas (T).

For on magnetic field density see Electromagnetism, solenoid coils, uses of electromagnets

 

attraction of unlike poles

Diagrams A and B show the magnetic field around a permanent bar magnet.

How to plot this was described above with the lines of force running from north to south.

You can clearly show this pattern using iron filings.

You place a permanent bar magnet under a sheet of paper or plastic.

You then sprinkle iron filings randomly on top of the sheet.

Then, tap the sheet gently and repeatedly until the pattern of the magnetic field emerges.

The permanent magnet induces magnetism in the iron filings and converts them into temporary magnets which all line up - N - S - N - S - etc. along the lines of force of the magnetic flux.

Its quicker than doing the compass plot method, but you don't end up with a plot unless you photograph it!

Diagram C shows the magnetic field when unlike poles of two bar permanent bar magnets are brought close together and attracted.

When a N-S or S-N attraction happens the lines of force join up from one magnet to another in a uniform pattern and the lines of force still run from a north pole to a south pole.

 

repulsion of like poles

Diagrams D and E show when like poles of two permanent magnets are brought close together and repulsion takes place.

In this case the lines of force do NOT join together from one magnet to the other, but they still run from a north pole to a south pole.

 


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3. Magnetisation and making magnets - induced and permanent magnets

There are two types of magnet we need to consider.

Permanent magnets retain their magnetism and create their own magnetic field.

These are made from 'hard' magnetic materials like steel do not readily lose their magnetism and produce their magnetic fields all the time.

You can test whether a material/object is magnetic by seeing if it is attracted to a permanent magnet.

Induced or temporary magnets are materials that only become magnetic when placed in a magnetic field and will only then produce their own magnetic field.

Temporary magnets are made from 'soft' magnetic materials like iron and some iron-nickel (steel) alloys.

For example when a permanent magnet is placed in contact with another magnetic material like iron, they will always be attracted to each other AND a north and south pole are induced in the other magnetic material.

An example of an induced magnet

e.g. If you place a permanent steel magnet in contact with a piece of iron, the piece of iron becomes magnetised and the two induced poles match the S-N attraction.

In fact, the nearest pole on the iron to the magnet will always be the opposite of the pole on the permanent magnet, hence the attraction.

In other words a permanent north pole induces a temporary south pole in the magnetised material or  permanent north pole induces a temporary south pole.

This explains why a permanent magnet can pick up any other magnetisable material - it induces the opposite poles and attraction immediately follows.

In the case of iron, when you remove the permanent magnet you remove the source of induced magnetism and the iron bar gradually loses its magnetism.

The iron bar would be described as a temporary magnet and the iron as a soft magnetic material.

 

  a magnetic chain induction!

This magnetic pole induction produces some quite interesting effects!

e.g. a bar magnet will pick up a whole chain of iron nails or paper clips as each iron/steel item becomes an induced magnet and can so attract another one.

The magnetic field effect becomes weaker down the chain and eventually the weight of the chain becomes greater than the force of the magnetic field and either no more 'stick on' or the whole lot fall off.

 

You can use the principle of induction to make a permanent magnet from another permanent magnet.

All you have to do is stroke the un-magnetised steel bar with a permanent bar magnet.

You repeatedly stroke the steel bar with the magnet repeatedly in the same direction.

All the 'atomic iron magnets' all line up to produce a permanent magnet with its own independent magnetic field - its still magnetic induction, but the effect is permanent.

 

The Earth's magnetic field can induce magnetism in materials

Even the weak Earth's magnetic field magnetises steel structures like bridges, especially if the magnetisable object is subjected to vibration - its as if you are shaking the atomic iron magnets into alignment turning the object into a weak magnet.

 


4. Uses of permanent magnets (See other page for uses of electromagnets)

Sticking things on the refrigerator!

 

Loudspeakers use permanent magnets.

Magnetic screwdrivers help hold the screw in position in hard to reach places.

Jewellery clasps can be made of permanent magnetic materials.

A compass is essentially a small bar magnet in which the steel needle of the compass measures the direction with respect to the Earth's magnetic poles.

 


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5. The Earth's magnetic field and the compass

Swirling currents of heated and cooling molten (mainly) iron metal in the Earth's outer core create an electric current, which, due to the rotation of the Earth, create a magnetic field.

The Earth's magnetic field.

A compass works by the alignment of its needle with the Earth's magnetic field.

The north pole is actually the south pole of the Earth's magnetic field - this is due to the convention established from electromagnetic science - it was an arbitrary choice, rather like the convention for the direction of flow of electricity - which is opposite to the flow of electrons!

Therefore the Earth's magnetic north pole is at the geographical south pole.

Therefore the magnetic south pole of the compass needle is attracted to, therefore points to, the geographically north pole of the Earth.

The magnetic north is a few degrees away from the true geographic north pole based on the Earth's spin axis.

The fact that a magnetised-magnetic compass needle always aligns itself in a particular direction on the Earth's surface, is proof that the Earth has a magnetic field.

However, it has been deduced from geological studies of ancient rocks that the Earth's magnetic poles flip every so often, perhaps as often as every 200 00 years now.

The trusty compass to help you navigate the countryside with your OS map.

However, these days, many walkers are using GPS systems for navigation, but I still like a 'real map' and a 'real compass'!


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What next?

Electricity and magnetism revision notes index

1. Usefulness of electricity, safety, energy transfer, cost & power calculations, P = IV = I2R, E = Pt, E=IVt

2. Electrical circuits and how to draw them, circuit symbols, parallel circuits, series circuits explained

3. Ohm's Law, experimental investigations of resistance, I-V graphs, calculations V = IR, Q = It, E = QV

4. Circuit devices and how are they used? (e.g. thermistor and LDR), relevant graphs gcse physics revision

5. More on series and parallel circuits, circuit diagrams, measurements and calculations gcse physics

6. The 'National Grid' power supply, environmental issues, use of transformers gcse physics revision notes

7. Comparison of methods of generating electricity gcse physics revision notes (energy 6)

8. Static electricity and electric fields, uses and dangers of static electricity gcse physics revision notes

6. The 'National Grid' power supply, environmental issues, use of transformers gcse physics revision notes

10. Electromagnetism, solenoid coils, uses of electromagnets  gcse physics revision notes

11. Motor effect of an electric current, electric motor, loudspeaker, Fleming's left-hand rule, F = BIL

12. Generator effect, applications e.g. generators generating electricity and microphone gcse physics

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