Magnetism: What Are Magnets & How Do They Work?

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SUMMARY

This discussion provides a comprehensive overview of magnets, detailing their formation and functionality. It explains that magnets arise from the alignment of electrons within certain elements, primarily iron, nickel, and cobalt, which possess "uncompensated spin" electrons that contribute to their magnetic fields. The formation of natural magnets, such as lodestone from magnetite, is also discussed, highlighting the conditions under which these minerals acquire magnetic properties. Additionally, the conversation touches on the significance of ferro-ceramic magnets in audio speakers.

PREREQUISITES
  • Understanding of electric fields and magnetic fields
  • Knowledge of atomic structure and electron behavior
  • Familiarity with the concept of uncompensated spin in electrons
  • Basic principles of magnetism and ferromagnetism
NEXT STEPS
  • Research the properties of magnetite and its role in natural magnet formation
  • Explore the concept of uncompensated spin and its implications in magnetism
  • Learn about the manufacturing processes of Alnico magnets
  • Investigate the applications of ferro-ceramic magnets in modern technology
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Students of physics, materials scientists, and engineers interested in the principles of magnetism and its applications in technology.

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What are magnets, how do they form, how do they attract and repel?
 
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Any charged particle has associated with it an electric field. Once a charged particle begins to move then it also sets up a magnetic field around itself that is perpendicular to both the direction of motion and the electric field.
Any moving charged particle with it's own magnetic field will experience a force due to the first moving charged particle and vice versa. This is the magnetic force.

Bar magnets are a special case as they don't seem to be moving, but the electrons inside the individual atoms are moving. Usually they are moving round in random directions but the theory goes that in a bar magnet the electrons all line up and so rather than the total magnetic field adding up to 0, the magnetic forces of all of the moving charged particles builds up to form a more noticable magnetic field. (At least that's how it was explained to me.)

Does this description help at all?
 
Originally posted by lavalamp
"...in a bar magnet the electrons all line up and so rather than the total magnetic field adding up to 0, the magnetic forces of all of the moving charged particles builds up to form a more noticable magnetic field.
It is important to emphasize that only certain elements can form "permanent" magnets. Iron is the chief among these and most permanent magnets are mostly composed of iron. The very strong ferro-ceramic magnets that are at the heart of an audio speaker are an example of this.

Other elements that can be made into permanent magnets are nickle, cobalt, and the "rare earth" elements. (Strangely enough, single atoms of aluminum can become magnets, but this property is offset when two or more aluminum atoms are joined together.) Permanent magnets made from an alloy of aluminum, nickle and cobalt Alnico make very strong permanent magnets.

The reason that magnets can only be made from this small set of elements is that it is only these who have one or more electrons in their orbits with an "uncompensated spin". In all other elements the "spin" of all the electrons is "compensated". It is ony the electric field from these "uncompensated" electrons that contributes to the magnetic field.

Someone who understands the phenomenon of an uncompensated spin will have to jump in here and explain it, because I'm not sure what it means.

The point is that iron, nickle, cobalt, etc have these electrons with an "uncompensated spin" which are able to contribute their electric field to the greater phenomenon of a magnetic field when these elements are prepared in the right manner.

Magnets form in Nature from the mineral Magnetite which is one of the oxides of iron that is easily produced by heating iron red hot or hotter and letting it react with the O2 in the air. This would happen whenever iron were ejected in molten form from a volcano. As it cooled it would simply pick up a magnetic orientation from the Earth's magnetic field. The common name for rock like this when it is found in nature is lodestone.
 

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