Revision notes · Magnetism and electromagnetism

Permanent and induced magnetism, magnetic forces and fields

Poles of a magnet4.7.1.1

Every magnet has two poles, north and south, where the magnetic forces are strongest. Like poles repel each other (north–north or south–south); unlike poles attract each other (north–south). The force between two magnetic poles is a non-contact force — it acts even when the magnets aren't touching.

Permanent magnetInduced magnet
MagnetismProduces its own magnetic field all the timeOnly becomes magnetic when placed in another magnetic field
Behaviour when the external field is removedKeeps its magnetismQuickly loses most/all of its magnetism
ExamplesA bar magnet, a fridge magnetIron, nickel, cobalt — e.g. a steel paperclip near a bar magnet

The force between a permanent magnet and an induced magnet (e.g. a piece of iron) is always one of attraction, never repulsion — this is how you can tell a permanent magnet apart from an induced one experimentally: bring two suspected magnets close together from both orientations; if they only ever attract (never repel), at least one of them is an induced magnet, not a permanent one.

Magnetic fields4.7.1.2

Definition: The magnetic field of a magnet is the region around it where another magnetic material, or another magnet, experiences a force.

Magnetic field lines are drawn from the north pole to the south pole of a magnet, on the outside of it. At any point, the direction of the field line shows the direction of the force that would act on a north pole placed there. The field is strongest close to the poles, and gets weaker further from the magnet — shown on a field diagram by field lines that are closer together (stronger) or further apart (weaker).

Magnetic field around a bar magnet

A plotting compass is a small compass that can be placed at different points around a magnet; the needle lines up with the field at that point, so moving the compass around and tracing its direction at each point builds up a picture of the field's shape.

The Earth itself behaves as if it has a giant bar magnet at its core, producing a magnetic field that extends into space — this is why a freely suspended compass needle lines up with the Earth's field and points towards geographic north (in reality, close to, but not exactly at, the Earth's geographic North Pole).

⚠️ Common mistake: The end of a compass needle that points north is defined as the needle's own north pole. Since unlike poles attract, the region of the Earth's magnetic field near the geographic North Pole must actually behave as a magnetic south pole (and vice versa near the geographic South Pole) — it's a common mix-up to assume the Earth's 'north magnetic pole' behaves like a north pole.

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