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Ferromagnetism Some substances cause magnetic lines of flux to bunch closer together than they would in the medium of air or a vacuum This property is called ferromagnetism, and materials that exhibit it are called ferromagnetic You ve already learned something about this! Diamagnetism Another property is known as diamagnetism, and materials that exhibit it are called diamagnetic This type of substance decreases the magnetic flux density by causing the magnetic flux lines to diverge Wax, dry wood, bismuth, and silver are examples No diamagnetic material reduces the strength of a magnetic field by anywhere near the factor that ferromagnetic substances can increase it Diamagnetic materials are generally used to keep magnetic objects apart, while minimizing the interaction between them In recent years, they have also found some application in magnetic levitation devices.

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The presence of the geomagnetic field was first noticed in ancient times. Some rocks, called lodestones, when hung by strings would always orient themselves a certain way. This was correctly attributed to the presence of a force in the air. Even though it was some time before the details were fully understood, this effect was put to use by early seafarers and land explorers. Today, a magnetic compass can still be a valuable navigation aid, used by mariners, backpackers, and others who travel far from familiar landmarks. The geomagnetic field and the magnetic field around a compass needle interact, so that a force is exerted on the little magnet inside the compass. This force works not only in a horizontal plane (parallel to the earth s surface), but vertically at most latitudes. The vertical component is zero only at the geomagnetic equator, a line running around the globe equidistant from both geomagnetic poles. As the geomagnetic lattitude increases, either towards the north or the south geomagnetic pole, the magnetic force pulls up and down on the compass needle more and more. You have probably noticed this when you hold a compass. One end of the needle seems to insist on touching the compass face, while the other end tilts up toward the glass. The needle tries to align itself parallel to the magnetic lines of flux.

Permeability Permeability is a quantitative indicator of the extent to which a ferromagnetic material concentrates magnetic lines of flux It is measured on a scale relative to a vacuum, or free space Free space is assigned permeability 1 If you have a coil of wire with an air core, and a current is forced through the wire, then the flux in the coil core is at a certain density, just about the same as it would be in a vacuum Therefore, the permeability of pure air is about equal to 1 If you place an iron core in the coil, the flux density increases by a large factor The permeability of iron can range from 60 (impure) to as much as 8000 (highly refined).

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Magnets stick to some metals. Iron, nickel, and alloys containing either or both of these elements, are known as ferromagnetic materials. When a magnet is brought near a piece

If you use certain ferromagnetic alloys as the core material in electromagnets, you can increase the flux density, and therefore the local strength of the field, by as much as a million times Such substances thus have permeability as great as 1,000,000 (106) Table 8-1 gives permeability values for some common materials Retentivity When a substance, such as iron, is subjected to a magnetic field as intense as it can handle, say by enclosing it in a wire coil carrying a massive current, there will be some residual magnetism left.

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