A material that retains its magnetic properties after an external magnetic field is removed.A permanent magnet is a material that generates its own persistent magnetic field without any external power source. Unlike temporary magnets, which only exhibit magnetism while in the presence of an external field, permanent magnets retain their magnetization after the field is removed. This property arises from the alignment of magnetic domains—microscopic regions where atomic magnetic moments point in the same direction—which remain locked in place due to the material's internal structure.
The earliest known permanent magnets were lodestones, naturally magnetized pieces of magnetite, used in compasses by ancient civilizations. The modern understanding of ferromagnetism was developed in the early 20th century, with Pierre Weiss proposing the domain theory in 1907.
In ferromagnetic materials like iron, cobalt, and nickel, atoms have unpaired electrons that act as tiny magnetic dipoles. In an unmagnetized state, these dipoles are randomly oriented, canceling each other out. When exposed to an external magnetic field, the domains align, and in permanent magnets, the material's crystal structure and defects (such as lattice defects) pin these domains in place, preventing them from returning to randomness. This creates a stable, self-sustaining magnetic field.
Permanent magnets are ubiquitous in technology, from electric motors and generators to hard disk drives, loudspeakers, and magnetic resonance imaging (MRI) machines. They are also used in magnetic separators, sensors, and in research on magnetic traps for neutral atoms.
The strongest permanent magnets, made from neodymium-iron-boron alloys, can lift over 1,000 times their own weight.


















