Magnets and magnetic poles Knowledge-Based Study
Physics topic explanations on Magnets and magnetic poles.
Study notes
What is a Magnet?
A magnet is any object or material that produces a magnetic field and exerts a magnetic force on other magnets and certain metals. Historically discovered in naturally occurring minerals such as lodestone (magnetite), modern magnets are typically manufactured from alloys designed to retain strong magnetic properties.
Magnetic vs. Non-Magnetic Materials
Materials respond differently when placed in the presence of a magnet:
- Ferromagnetic materials: Substances such as iron, nickel, cobalt, and steel are strongly attracted to magnets and can themselves be magnetized to form temporary or permanent magnets.
- Non-magnetic materials: Most other common substances, including wood, glass, plastic, copper, and aluminum, experience no noticeable attraction to everyday permanent magnets.
Properties of Magnetic Poles
Every magnet possesses two distinct regions where its magnetic effects are concentrated the strongest. These regions are called magnetic poles:
- North-seeking pole (N pole): The pole that naturally orients toward the geographic north of Earth when freely suspended.
- South-seeking pole (S pole): The pole that points toward geographic south.
The Indivisibility of Poles (Magnetic Dipoles)
In nature, isolated magnetic poles (known theoretically as magnetic monopoles) have never been observed. A magnet is inherently a dipole.
If a bar magnet is broken or cut in half, the result is not an isolated North pole and an isolated South pole. Instead, two complete, smaller magnets are formed, each possessing its own North and South pole.
Attraction and Repulsion
Magnets exert non-contact forces on one another. The interaction between two magnetic poles follows the fundamental rule of magnetism:
- Like poles repel: Placing two North poles or two South poles near each other results in a repulsive force pushing them apart.
- Unlike poles attract: Placing a North pole near a South pole results in an attractive force pulling them together.
Important Distinction: An unmagnetized piece of iron is attracted to both the North and South poles of a magnet via induced magnetism. Therefore, repulsion is the only definitive test to confirm that an unknown object is itself a permanent magnet.
The Geomagnetic Field and Compasses
A magnetic compass works because Earth behaves as though it has a massive bar magnet buried deep within its core.
- A compass needle is a small, freely pivoted permanent magnet.
- The North pole of the compass needle points toward Earth's geographic North Pole.
- Because opposite poles attract, Earth's geographic North corresponds magnetically to a magnetic south pole.
Over time and across different locations, geographic north and magnetic north do not perfectly align; the angle between them is known as magnetic declination.
Key Takeaways
- Two Poles: Every magnet has both a North pole and a South pole.
- Interaction Rule: Like poles repel (N-N or S-S), and opposite poles attract (N-S).
- Dipole Nature: Breaking a magnet produces two complete dipoles, never isolated monopoles.
- Magnetic Identification: Repulsion between two objects proves both are magnetized; attraction can occur between a magnet and an unmagnetized ferromagnetic material.
- Compass Operation: A compass needle aligns along Earth's magnetic field lines, directing its North pole toward Earth's northern magnetic region.

