Yes! High temperatures disorder materials and destroy magnetic order. Permanent magnets can be demagnetized by heating them, often to surprisingly modest temperatures. Many household magnets can be spoiled by putting them in a hot oven. Even electromagnets will lose most of their strength at very high temperatures because they rely on iron and iron undergoes several phase transitions at high temperatures that destroy its magnetic order. You can show that iron loses its magnetism at high temperatures by heating a steel nail red hot with a propane torch and then trying to pick it up with a magnet. Be careful not to burn yourself. The hot nail won't stick to the magnet because it won't have any magnetic order. Once the nail cools, its magnetic order will reappear.
There are several way in which objects in our universe can push or pull on one another and one of these ways is through electric or magnetic forces. Two objects that have electric charges are observed to push or pull on one another and two objects that have magnetic poles are also observed to push or pull on one another. That's simply the way our universe works. With electric forces, things are relatively easy—when you pull a sock and shirt out of the dryer, the sock may well stick to the shirt because friction has given the two different electric charges (one is positively charged and the other negatively charged). By playing around with electrically charged objects, you can convince yourself that (1) there are two different types of electric charge—normally called "positive" and "negative"—and (2) that like charges repel while opposite charges attract.
With magnetic forces, there is an annoying complication: magnetic poles (the magnetic equivalent of "charge") always come in equal but opposite pairs. As with electric charges, there are two types of magnetic poles—normally called "north" and "south"—and like poles repel while opposite poles attract. However, you won't be able to find a pure north pole anywhere; it always comes attached to a south pole (and vice versa). So any magnet you find will have at least one north pole and at least one south pole (while they typically have only one of each, they can also have many of each). The forces that these poles exert on one another are fundamental to our universe—I can't explain them in terms of more basic phenomena because they are already basic except at a very abstract level. (In fact, electric and magnetic forces are intimately related to one another and it is actually electric charges that are creating the magnetic poles that you observe in a magnet.) If you play around with several magnets for a while, you should be able to convince yourself about the existence of two different poles and that like poles repel while opposite poles attract. You should also notice that the magnets push one another directly toward or away from them (the forces between poles are parallel to the line separating them) and that the forces become stronger as the poles become nearer (the force is inversely proportional to the square of the distance separating the poles).
As for how a permanent magnet works, it's made from a material that contains ordered electrons. Electrons are intrinsically magnetic and, in a few special materials, that magnetism as organized so that the overall materials are themselves magnetic. Each electron has its own north and south pole, but together they give the material a giant north and south pole.
A magnetic recording tape is usually a Mylar ribbon, coated with a thin layer of plastic that's impregnated with tiny permanent magnets. As long as it's store away from heat and moisture, the Mylar film itself shouldn't age. However, the layer of permanent magnets can change slightly with time. When a tape is left tightly wound on its reel for a long time, the magnetic layers can begin to affect one another—the magnetic fields from one layer of tape can alter the magnetization of the layers above and below it. The result is that sounds from one layer of tape can gradually transfer themselves weakly to the adjacent layers, creating faint echo effects. The solution to this problem is to unwind and rewind the tape, so that the layers shift slightly relative to one another. But while these echoes may be annoying in a recording of classical music, they probably aren't important in a recording of a noisy courtroom. Unless I hear otherwise from someone reading this note, I wouldn't worry about unwinding and rewinding your tapes. The slight imperfections that will result from transfers between layers shouldn't affect their utility in later trials. Properly stored, I'd expect the tapes to outlive everyone involved with the trials, even without any unwinding and rewinding.
A ferromagnetic material is one that contains intrinsic magnetic order. Iron, for example, is a ferromagnetic material—meaning that if you were to examine a microscopic region of the iron, you would find that it was highly magnetic. The magnetism in a ferromagnetic material is often hidden by a domain structure, in which microscopic magnetic regions or "domains" all point in random directions to give the material no apparent magnetism. Only when you expose the ferromagnetic material to a magnetic field does its magnetic character suddenly reveal itself. A ferromagnetic material becomes strongly magnetic when it's exposed to a magnetic field.
A diamagnetic material is one in which the electrons begin moving when it's place in a magnetic field. These moving electric charges create a second magnetic field that partially cancels the original field. A diamagnetic magnetic field partially shields itself from magnetism when it's exposed to a magnetic field.
A paramagnetic material is one in which individual magnetic electrons respond magnetically to any external magnetic field. It becomes weakly magnetic when it's exposed to a magnetic field. Unlike a ferromagnetic material, a paramagnetic material has no intrinsic magnetic order before it's exposed to an external field.
Iron and steel (not stainless) are ferromagnetic metals, meaning that they are intrinsically magnetic. While this magnetism is normally hidden by the formation of millions of tiny, randomly oriented magnetic domains, it becomes apparent when you hold a magnet near the iron or steel: they are attracted! Aluminum has no intrinsic magnetism and is not attracted to a magnet. There are far more non-magnetic metals than magnetic ones. Why don't you try to see which metals will stick to a magnet. Only the ferromagnetic ones will. Even common stainless steel is non-ferromagnetic.
As long as the tape is kept cool and dry, its magnetization should remain stable for years. However, there is the problem of magnetic imprinting from one layer of tape to the adjacent layers on a spool. With time, one layer transfers some of its magnetization to those adjacent layers. In a videotape, this imprinting leads to a gradual appearance of noise in the video images. As long as you're willing to tolerate a little video "snow," this imprinting shouldn't be too much of a problem. You can reduce its severity by occasionally winding and rewinding the tapes. But I don't see any real reason why a tape won't be reasonably useable for decades.
Magnetic fields are associated with lines of magnetic flux, invisible structures that stretch between north and south magnetic poles or that curve around on themselves to form complete loops. Unless a material has its own north or south magnetic poles, it can't terminate the magnetic flux lines and can have only small effects on magnetic fields. The few materials that do affect magnetic fields substantially are ones such as iron or steel that are intrinsically magnetic and that can easily develop strong north and south magnetic poles. These magnetic materials can significantly shift the paths of the magnetic flux lines. If you put an iron or steel box in a magnetic field, the flux lines will tend to travel through the walls of the magnetic box. As a result, there will be few magnetic flux lines inside the box and almost no magnetic field. This effect is used to shield sensitive equipment such as the picture tubes in televisions from magnetic fields.
Permanent magnets are made from materials with two important magnetic characteristics. First, these materials are intrinsically magnetic, meaning that some of the electrons in these materials retain their natural magnetism. While electrons are always magnetic, that magnetism is lost in most materials because of complete cancellations—each magnetic electron is paired with another magnetic electron so that they cancel one another perfectly. However, there are some materials in which the cancellation is imperfect and these materials (including iron, cobalt, nickel, and many steels) are the basis for most permanent magnets.
Second, the materials used in permanent magnets have internal structures that make the magnetic electrons align along particular directions. Once the electrons are aligned along one of those directions, they stay aligned and the material exhibits strong magnetic characteristics. It becomes a "permanent magnet."
A permanent magnet remains its magnetization as long as nothing spoils the alignments of its magnetic electrons. These electrons can be knocked out of alignment by vibrations, heat, or other magnets. If you hit a permanent magnet with a hammer or heat it in the oven, you will change and perhaps destroy its magnetization. This magnetization can be recovered by exposing the permanent magnet to the magnetic influences of an electric current. In fact, permanent magnets are originally magnetized by placing them near electric currents that align their magnetic electrons. Moreover, even a material that doesn't have the internal structures needed to keep its electrons aligned along a particular direction will become magnetized temporarily by placing it near an electric current. That's how a wrecking yard magnet works-an electric current temporarily turns a large piece of iron into a strong magnet.
Yes, but not in the way you're thinking of. When you bring a magnet near a piece of steel, the intrinsic magnetic character of that steel causes it to become magnetic in such a way that it attracts the magnet. There is no way for the steel, or another similar metal, to become magnetic in such a way that it would repel the magnet.
However, if the metal is already magnetized it can repel an approaching magnet. A more interesting case is when a magnet approaches a normally non-magnetic metal at high speeds; in which case electric currents begin to flow through the metal and these currents do repel the approaching magnet.
A permanent magnet was magnetized when it was first made out of metal. It did have microscopic regions of magnetic order—magnetic domains—but those regions all pointed in random directions and the magnet didn't have any overall magnetic poles. To give it poles, it had to be magnetized. It was placed in a very strong magnetic field so that its domains grew or shrank until most of them were aligned with the magnetic field. The magnet acquired overall magnetic poles for the first time. When the field was removed, the domains remained as they were and the magnet permanently retained its new magnetic poles.
If this same magnet were reversed and then placed in that strong magnetic field again, it would become remagnetized in the opposite direction from before—its domains would grow or shrink until most of them were aligned with the magnetic field again. The magnet's north poles would become south poles and vice versa. Finally, if the magnet were wiggled back and forth in that strong magnetic field and gradually removed from the field, its domains would grow or shrink almost randomly. The magnet's magnetic domains would become randomized and it would end up with no overall north or south magnetic pole at all. It would be demagnetized.
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