Magnetic Domains
About this simulation
A ferromagnetic material — iron, nickel, cobalt — is divided into microscopic regions called magnetic domains. Within each domain, all the atomic magnetic moments are aligned in the same direction, producing a strong local field. In an unmagnetized piece of iron, these domains point in random directions so their fields cancel, and the material appears non-magnetic overall.
When an external field is applied — or when the domains are physically forced into alignment — their fields add constructively, and the material becomes a permanent magnet. This simulation models that process: ten draggable bar magnets represent individual magnetic domains. A field-strength meter registers the combined effect of any magnets you place in its measurement zone, letting you observe how alignment directly controls field strength.
Learning goals
- Describe what a magnetic domain is and how it differs from an individual atomic dipole
- Explain why aligning domains increases the strength of the overall magnetic field (constructive superposition)
- Predict how the field-meter reading changes as magnets are aligned versus disordered
- Connect domain alignment to the creation of permanent magnets in real ferromagnetic materials
How to use
- Open the simulation — all ten bar magnets start on the shelf in their default (aligned) orientation
- Drag magnets one at a time into the dashed measurement box and observe the field-meter reading
- Right-click (or two-finger tap on Mac) any magnet to flip it 180°, reversing its polarity — watch the meter drop
- Arrange all magnets pointing the same direction, as close together as possible, to achieve the maximum reading