(Ferro) magnetism

Back in ancient times, people discovered that magnetite crystals attract or repel each other depending on their orientation. This physical phenomenon is referred to as magnetism. The words magnetite and magnesium are both derived from Magnesia, the name of an area in the Thessaly region of Greece where magnetic stone can be found in abundance.Magnetic separation

It is the iron in the rock that is responsible for the magnetic properties of magnetite. Many iron alloys possess magnetic properties. In addition to iron, we find magnetic properties in nickel, cobalt and gadolinium as well.

Although ferromagnetic (and ferrimagnetic) materials are the only kinds with strong enough magnetic properties to be drawn to a magnet (which is why they are called ‘magnetic’), all other substances also respond weakly to a magnetic field, via one or more other types of magnetism.

Ferromagnetic materials can be divided into magnetically 'soft' materials, such as annealed iron, which can be magnetized but usually do not retain the magnetization indefinitely, and magnetically 'hard' materials that do remain magnetized. Permanent magnets are made of 'hard' ferromagnetic materials such as Alnico and ferrite, which undergo special processing in a powerful magnetic field during production to 'align' their internal microcrystalline structure, making them very resistant to demagnetization.

Objects which strongly exhibit this behaviour are called magnets. There are natural and man-made magnets (e.g. Alnico, Fernico, ferrites). All magnets have two poles, which are referred to as the north pole and the south pole. The north pole of a magnet repels the north pole of other magnets and attracts the south pole of other magnets. Two south poles also repel.

Magnetism Gripper

Because the earth has a magnetic field as well, with its magnetic south pole close to the geographic north pole and its magnetic north pole close to the geographic south pole, a free-spinning magnet will always take on a north-south orientation. The names of the poles of a magnet are derived from this phenomenon. For the sake of convenience, but nevertheless slightly confusing, the south pole of “the 'earth magnet' is called the magnetic north pole and the north pole of the 'earth magnet' is called the magnetic south pole.

Magnetic field - North and South pole

A related phenomenon is electromagnetism, which is magnetism generated by an electric current. In essence, all magnetism is caused by either rotating or revolving electrical charges in eddy currents.


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Als Weiss-Bezirke werden beim Ferromagnetismus mikroskopisch kleine magnetisierte Bezirke in den Kristallen magnetischer Materialien bezeichnet. Sie wurden vom französischen Physiker Pierre-Ernest Weiss (1865–1940) entdeckt.

Wenn man ein externes Magnetfeld anlegt, verschieben sich die Grenzen der Bezirke, wobei die Bezirke, die in der Richtung des externen Felds magnetisiert sind, größer werden im Gegensatz zu den anders magnetisierten Bereichen. Dieser Prozess setzt sich bei der weiteren Steigerung des externen Felds fort bis alle Bezirke in der Richtung des externen Felds magnetisiert sind. Das Material ist dann magnetisch gesättigt.

Weiss-Bezirk Darstellung der Veränderung der Weiss-Bezirke unter Einwirkung eines externen Magnetfeld

Magnet materials


Ferrite magnets Read more

Neodymium (Neoflux®) magnets

Neodymium Neoflux Magneten Read more

Samarium-cobalt magnets

Samarium Kobalt magneten Read more

Aluminum-nickel-cobalt magnets

Aluminum-nickel-cobalt magnets Read more

Plastic bonded magnets

Plastic bonded magnets Read more