Permanent magnets are objects manufactured from materials that have been magnetized and have the ability to generate their own persistent magnetic field. A common example is a refrigerator magnet, which is used to hold notes on the inside of a refrigerator door. Ferromagnetic materials are those that can be magnetized and are also those that are highly attracted to a magnet; these are the materials that can be magnetized (or ferrimagnetic). These include the elements iron, nickel, and cobalt, as well as their alloys, some rare-earth metal alloys, and some naturally occurring minerals, such as lodestone, among other elements and compounds. Despite the fact that ferromagnetic (and ferrimagnetic) materials are the only ones that are significantly attracted to a magnet and are therefore considered magnetic, all other substances respond weakly to a magnetic field, responding through one of several different types of magnetism.
Ferromagnetic materials can be divided into two categories: magnetically “soft” materials such as annealed iron, which can be magnetized but do not tend to remain magnetized, and magnetically “hard” materials, which do tend to remain magnetized. During the manufacturing process, permanent magnets are made from “hard” ferromagnetic materials such as alnico and ferrite, which are subjected to special processing in a strong magnetic field to align their internal microcrystalline structure, resulting in a magnet that is extremely difficult to demagnetize. To demagnetize a saturated magnet, a specific magnetic field must be provided, and the threshold at which this occurs is determined by the coercivity of the material under consideration. Coercivity is a property of “hard” materials, whereas coercivity is a property of “soft” materials. When it comes to magnets, their overall strength is assessed by their magnetic moment, or alternately, by the entire magnetic flux they produce. The magnetization of a material is used to determine the local strength of magnetism in that material.
An electromagnet is a coil of wire that behaves as a magnet when an electric current travels through it, but that ceases to function as a magnet when the current is interrupted or terminated. Most of the time, the coil is wrapped around a core made of “soft” ferromagnetic material, such as mild steel, which considerably increases the magnetic field created by the coil as a result of the wrapping.
Demagnetization (or degaussing) of magnetized ferromagnetic materials can be accomplished in a variety of methods.
Because each individual piece of iron is a small dipole, iron filings form a pattern that traces field lines when arranged in a grid (the separation between magnetic fields). In a dipole, the force experienced by the dipole is proportional to its strength and proportional to the rate at which the magnetic field changes. The dipole tries to align itself with a magnetic field, but the field lines at the ends of a bar magnet are quite close together, making this difficult. What this demonstrates is that the magnetic field changes strongly over a short distance, as opposed to the variation closer to the magnet’s center of gravity. Because of the drastic variations in the magnetic field, a dipole experiences greater force than a point magnet.
The strength of the magnetic field changes according to where it is located in relation to the magnet. Any pole of a bar magnet has the greatest magnetic field strength, and this is true for either pole of the magnet. When comparing the strength of the magnetic field at the north pole and the south pole, it is equal. The magnetic force is weakest in the center of the magnet and halfway between the pole and the center of the magnet, as shown in the diagram.
Permanent magnets are items made of magnetized materials that can generate their own magnetic field. A refrigerator magnet, for example, is used to keep notes on the inside of a refrigerator door. Ferromagnetic materials are those that can be magnetized and are greatly attracted to a magnet (or ferrimagnetic). These include iron, nickel, and cobalt, as well as their alloys, rare-earth metal alloys, and naturally occurring minerals like lodestone. All other substances respond weakly to a magnetic field, responding through one of several forms of magnetism.